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THREE ISSUES OF SUSTAINABLE MANAGEMENT IN THE OJOS NEGROS VALLEY,
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TABLE OF CONTENTS
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1. INTRODUCTION
The Ojos Negros valley in Baja California is an important border economic resource. The valley is located 80 km South of the U.S.-Mexico border, about 40 km East of Ensenada. Agriculture and animal husbandry are the primary economic activities in the valley, with its products being commercialized in both the United States and Mexico. The valley plays an important role among the economic units of Baja California. Its future, however, remains uncertain, due to several environmental issues that remain unresolved. Three issues of importance in the Ojos Negros valley are:
2. RESEARCH OBJECTIVES
The project documents the economic and social impact of coquillo,
in terms of its capability to adversely affect the livelihood of the local
population; identifies its origins and sources, extent of infestation,
impact on the economic activities, means for its control, and strategies
for a concerted action to effectively deal with the menace.
The project documents the impact of sand and gravel
mining of the arroyos on the water resources
of the region; identifies the local stakeholders, location, mode and volume of mining;
evaluates the relationship between surface and ground water and the
effects of sand mining; and studies ways of optimizing the
effects of sand mining to minimize adverse impacts.
The project documents the economic and social effects of the climatic variability
which has plagued the valley in recent times, and seeks to work with local stakeholders
to develop strategies for coping on a long-term basis
with the variabilities of the climate.
3. RESEARCH METHODOLOGY / APPROACHES
To accomplish the stated objectives, the Ojos Negros Research Group, composed on
seven researchers, one from SDSU and six from UABC,
have implemented interdisciplinary synthesis to document, diagnose, evaluate,
consult with local stakeholders,
and develop meaningful and practical strategies capable of
solving the problems confronting the valley and the region.
The study addresses three major environmental problems currently
affecting the Ojos Negros valley and outlines corrective stategies
to redirect it along the path of sustainable development.
4. PROBLEMS / ISSUES ENCOUNTERED
The research team worked in the field and laboratory from June 1, 2001 to August 31, 2002.
There were no unforeseen problems encountered, other than those normally associated with the execution
of a research project in a binational context. The coquillo infestation was documented through literature
research, field visits
and interviews with local stakeholders.
The sand mining activities and evolving regulation was documented with literature research,
field visits and interviews with stakeholders on both sides of the border,
in Mexico and in the United States.
Samples of bed material in Arroyo El Barbon were extracted and analyzed in the
Geotechnical Laboratory at San Diego
State University. Sediment-routing analysis provided estimates of the amount
of sand that is likely to be produced in
Arroyo El Barbon within a 50-yr planning horizon.
The drought menace was documented through an extensive literature review, data collection and analysis,
and interviews with local stakeholders.
The statistical properties of drought, including intensity, duration, and frequency,
in the Ojos Negros valley and vicinity were calculated. Specific recommendations
for application to the drought-affected regions
were developed.
5. RESEARCH FINDINGS: SAND MINING
5.1 Impacts of Sand Mining
For thousands of years, sand and
gravel have been used in the construction of roads and buildings.
Today, demand for sand and gravel continues to increase.
Mining operators, in
conjunction with cognizant resource agencies,
must work to ensure that sand mining is conducted in a responsible manner.
Excessive instream sand-and-gravel mining causes the degradation of rivers.
Instream mining lowers the stream bottom, which may lead to bank erosion.
Depletion of sand in the streambed and along coastal areas causes the deepening
of rivers and estuaries and the enlargement of river mouths and coastal inlets.
It may also lead to saline-water intrusion from the nearby sea.
The effect of mining is compounded by the effect of sea level rise.
Any volume of sand exported from streambeds and coastal areas is a loss to the system.
Excessive instream sand mining may represent a threat to bridges, river banks and nearby structures.
Sand mining also affects
the adjoining groundwater system and the uses that local people make of the river.
Instream sand mining results in the destruction of aquatic and riparian habitat through
large changes in channel morphology.
Impacts include bed degradation, bed coarsening, lowered water tables near the streambed,
and channel instability.
These physical impacts cause degradation of riparian and aquatic biota, and may lead to the
undermining of bridges and other structures.
Continued extraction may also cause the entire streambed to degrade to the depth of excavation.
Sand mining generates extra vehicle traffic, which negatively impairs the environment.
Where access roads cross riparian areas, the local environment may be impacted.
5.1.1. Sand budget
Determining the sand budget for a particular stream reach requires site-specific topographic,
hydrologic, and hydraulic information.
This information is used to determine the amount of sand that can be removed from
the area without causing
undue erosion or degradation, either at the site or at a nearby location, upstream
or downstream.
In-channel or near-channel sand-and-gravel mining changes the sediment budget and may result
in substantial changes in the channel hydraulics.
These interventions can have variable effects on aquatic habitat, depending on the magnitude and
frequency of the disturbance, mining methods, particle-size characteristics of the sediment,
the characteristics of riparian vegetation,
and the magnitude and frequency of hydrologic events following the disturbance.
Temporal and spatial responses of alluvial river systems are a function of geomorphic thresholds,
feedbacks, lags, upstream or downstream transmission of disturbances, and geologic/physiographic controls.
Minimization of the negative effects of sand-and-gravel mining requires a detailed
understanding of the response of the channel to mining disturbances.
Decisions on where, how much and how often to mine require the definition of a reference state,
i.e., a minimally acceptable, or agreed-upon, physical and biological condition of the channel.
Present understanding of alluvial systems is generally not sufficient
to enable the prediction of channel responses quantitatively
and with confidence; therefore, reference states are difficult to determine.
Still, a general knowledge of fluvial processes can provide guidelines to minimize
the detrimental effects of mining.
Well-documented cases and related field data are required
to properly assess physical, biological, and economic tradeoffs.
5.1.2. Riparian habitat, flora and fauna
Instream mining can have other costly effects beyond the immediate mine sites. Many hectares of fertile
streamside land are lost annually, as well as
valuable timber resources and wildlife habitats in the riparian areas. Degraded stream habitats
result in lost of fisheries productivity,
biodiversity, and recreational potential.
Severely degraded channels may lower land and aesthetic values.
All species require specific habitat conditions to ensure long-term survival.
Native species in streams are uniquely adapted to
the habitat conditions that existed before humans began large-scale alterations.
These have caused major habitat disruptions that favored some species over others,
and caused overall declines in biological
diversity and productivity.
In most streams and rivers, habitat quality is strongly linked
to the stability of channel
bed and banks. Unstable stream channels are inhospitable to most aquatic species.
Factors that increase or decrease sediment supply
often destabilize bed and banks and result in dramatic channel readjustments.
For example, human activities that accelerate stream
bank erosion, such as riparian forest clearing or instream mining, can cause stream banks to become
net sources of sediment that often
have severe consequences for aquatic species.
Anthropogenic activities that artificially lower stream bed elevation cause bed instabilities that
result in a net release of sediment in the local vicinity.
Unstable sediments simplify and, therefore, degrade stream habitats for many
aquatic species. Few species benefit from these effects.
The most important effects of instream sand mining on aquatic habitats are
bed degradation and sedimentation, which can
have substantial negative effects on aquatic life. The stability of sand-bed and gravel-bed
streams depends on a delicate
balance between streamflow, sediment supplied from the watershed, and channel form.
Mining-induced changes in sediment supply
and channel form disrupt channel and habitat development processes. Furthermore,
movement of unstable substrates results in downstream
sedimentation of habitats. The affected distance depends on the intensity of mining,
particles sizes, stream flows, and channel morphology.
The complete removal of vegetation and destruction of the soil profile destroys
habitat both above and below the ground as well
as within the aquatic ecosystem, resulting in the reduction in faunal populations.
Channel widening causes shallowing of the streambed,
producing braided flow or subsurface intergravel flow in riffle areas, hindering
movement of fishes between pools. Channel reaches
become more uniformly shallow as deep pools fill with gravel and other sediments, reducing habitat
complexity, riffle-pool structure, and numbers of large predatory fishes.
5.1.3. Stability of structures
Sand-and-gravel mining in stream channels can
damage public and private property. Channel incision caused by gravel mining can undermine bridge piers
and expose buried pipelines and other infrastructure.
Several studies have documented the bed degradation caused by the two general
forms of instream mining: (1) pit excavation and (2) bar skimming.
Bed degradation, also known as channel incision, occurs through two primary processes:
(1) headcutting, and (2)"hungry" water. In headcutting,
excavation of a mining pit in the active channel lowers the stream bed, creating a nick point
that locally steepens channel
slope and increases flow energy. During high flows, a nick point becomes a
location of bed erosion that gradually moves upstream (Fig. 1).
Headcutting mobilizes substantial quantities of streambed sediments which are then transported
downstream to deposit in the excavated area and locations further downstream.
In gravel-rich streams, effects downstream of mining
sites may be short-lived when mining ends, because the balance between
sediment input and transport at a site can
reestablish itself relatively quickly.
Effects in gravel-poor streams may develop rapidly and persist for many years after mining has finished.
Regardless of downstream effects, headcutting in both gravel-rich and gravel-poor
streams remains a major concern.
Headcuts often move long distances upstream and into tributaries, in some watersheds
moving as far as the headwaters or until it is halted by geologic controls or
man-made structures.
A second form of bed degradation occurs when mineral extraction increases
the flow capacity of the channel. A pit excavation locally
increases flow depth (Fig. 1) and a barskimming operation increases flow width (Fig. 2).
Both conditions produce slower streamflow velocities
and lower flow energies, causing sediments arriving from upstream to deposit at the mining site.
As streamflow moves
beyond the site and flow energies increase in response to the "normal" channel form downstream,
the amount of transported sediment
leaving the site is lesser than the sediment carrying capacity of the flow.
This sediment-deficient flow or "hungry" water picks
up more sediment from the stream reach below the mining site, furthering the
bed degradation process (Fig. 1). This condition
continues until the equilibrium between input and output of sediments at the
site is reestablished.
A similar effect occurs below dams,
which trap sediment and release "hungry" water downstream, where channel incision usually ensues.
Instream mineral excavation downstream of
dams compounds this problem. Although other factors such as levees, bank protection,
and altered flow regimes also promote channel
incision, mineral extraction rates in many streams are often orders-of-magnitude in
excess of sediment supply from the watershed,
suggesting that extraction is largely responsible for observed channel changes.
Susceptibility to hungry-water effects would depend
on the rate of extraction relative to the rate of replenishment. Gravel-poor streams
would be most susceptible to disturbance.
Channel incision not only causes vertical instability in the channel bed,
but also causes lateral instability in the form of accelerated
stream bank erosion and channel widening. Incision increases stream bank heights,
resulting in bank failure when the mechanical
properties of the bank material cannot sustain the material weight.
Channel widening causes shallowing of the streambed (Fig. 2) as deep
pools fill with gravel and other sediments. Shallowing and widening of the
channel also increases stream temperature extremes, and channel
instability increases transport of sediments downstream. Mining-induced bed
degradation and other channel changes may not develop
for several years until major channel-adjustment flows occur, and adjustments
may continue long after extraction
has ended.
5.1.4. Groundwater
Apart from threatening bridges, sand mining transforms the riverbeds
into large and deep pits; as a result, the groundwater table
drops, leaving the drinking water wells on the embankments of these rivers dry.
Bed degradation from instream mining lowers the elevation of streamflow and
the floodplain water table which in turn can eliminate water
table-dependent woody vegetation in riparian areas, and decrease wetted periods in riparian wetlands.
For locations close to the sea, saline water may intrude into the fresh waterbody.
5.1.5. Water quality
Instream sand mining activities will have an impact upon the river's water quality.
Impacts include increased short-term turbidity at the mining
site due to resuspension of sediment, sedimentation due to stockpiling and dumping of excess
mining materials and organic
particulate matter, and oil spills or leakage from excavation machinery
and transportation vehicles.
Increased riverbed and bank erosion increases suspended solids in the water
at the excavation site and downstream.
Suspended solids may adversely affect water users and aquatic ecosystems.
The impact is particularly significant if water users downstream
of the site are abstracting water for domestic use.
Suspended solids can significantly increase water treatment costs.
5.1.6. Summary
Impacts of sand mining can be broadly clasified into three categories:
The large-scale extraction
of streambed materials, mining and dredging below the existing
streambed, and the alteration of channel-bed form and shape leads
to several impacts such as erosion of channel bed and banks, increase in channel slope,
and change in channel morphology.
These impacts may cause:
Mining and dredging activities,
poorly planned stockpiling and uncontrolled dumping of
overburden, and chemical/fuel spills
will cause reduced water quality for downstream users, increased cost for downstream water
treatment plants and poisoning of aquatic life.
Mining which leads to the removal of channel substrate,
resuspension of streambed sediment, clearance of vegetation, and stockpiling on
the streambed, will have ecological impacts.
These impacts may have an effect on the direct loss of stream reserve habitat,
disturbances of species attached to
streambed deposits, reduced light penetration, reduced primary production, and
reduced feeding opportunities.
5.2. Management of Sand Mining
Figure 3 shows the mining of a sand-gravel bar in which the excavated area is
limited to depths above the water table and buffer zones protect the
deep single channel and channel banks.
Two minimum-width buffers should separate the excavation area (extraction site)
from the low-flow channel and the adjacent channel bank (Fig. 4).
These buffers lessen the risk of mining-induced headcuts; however, "hungry" water
can still lead to channel incision downstream.
Bar skimming can also cause other problems such as elimination of side channels,
abrupt relocation of the low-flow channel, and higher
mobility of loosened sediments. Gravel-rich streams are less susceptible
than gravel-poor streams to disturbance from bar skimming.
This is because replenishment by excess gravel from upstream sources would
partially mitigate channel disruption.
Mining of bars in gravel-rich streams should be preferred over mining in gravel-poor streams.
Reaches that receive high rates of deposits may be better locations for
mining than reaches that do not.
The following criteria are recommended:
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5.3. Regulation of Sand Mining in the United States
Sandmining from streambeds in the U.S. is regulated by the U.S. Army Corps of Engineers under Section 404 of the Clean Water Act (U.S. Code of Federal Regulations, Title 33, Chapter 26, Subchapter IV, Section 1344: Permits for dredged or fill material). Under this legislation, the government is authorized to deny or restrict the specification of any defined area as a disposal site, whenever it is determined, after notice and opportunity for public hearings, that the discharge of dredged or fill materials into such area will have an unacceptable adverse effect on municipal water supplies, shellfish beds and fishery areas (including spawning and breeding areas), wildlife, or recreational areas. The government is authorized to issue permits for any category of activities involving discharges of dredged or fill material if the activities will cause only minimal adverse environmental effects when performed separately, and will have only minimal cumulative adverse effect of the environment. The government may also issue permits for any discharge or fill material into the navigable waters incidental to any activity having as its purpose bringing an area of the navigable waters into a use to which it was not previously subject, where the flow or circulation of navigable waters may be impared or the reach of such waters be reduced. Section 404 is strictly applicable to discharge of dredged or fill materials into navigable waters. However, the Code is actively being used to regulate sandmining activities in arroyos and washes of the Western United States. Thus, the government issues permits to sandmining operators in order to comply with the requirements of the Code, specifically, the avoidance of adverse effects on municipal water supplies, fisheries, wildlife, or recreation. The U.S. Fish and Wildlife Service regulates sandmining operations under the Endangered Species Act of 1973 (Section 9: Prohibited Acts). Under item 2(B) of Section 9, it is unlawful for any person subjected to the jurisdiction of the United States to remove and reduce to possession any endangered species of plants listed in Section 4, from areas under Federal jurisdiction; to maliciously damage or destroy any such species on any such area; or to remove, cut, dig up, or damage or destroy any species on any other area in knowing violation of any law or regulation of any state. This regulation is used by the federal government to restrict sandmining operations in the Western United States.
5.4. Strategies for the Ojos Negros Valley
Sand mining in Southern California has undergone substantial changes in the past few years.
Environmental regulations have discouraged operators from continuing to mine U.S. streambeds.
Increasingly, sand-mining operators are finding it more cost effective to import
the sand from south of the border.
For example, out of eleven operators in the San Luis Rey river, in San Diego County, about 10 years ago,
only two remain in business at the present time.
In Los Angeles County, the annual consumption of aggregate sand is about 9 million
tons; in San Diego County it is about 3.5 million tons.
In the past few years, the cost of construction-grade sand in Southern California has increased
from $6.50 to $12.00 per ton ($4.64 to $8.57 per m3).
This increase is directly linked to the prevailing regulatory environment,
which effectively discourages the mining of sand from local streambeds.
The high cost of sand and the relative proximity of the Mexican
streambeds makes it economically feasible to import sand from south of the border.
In the past 6 years, the percentage of sand used in San Diego County and originating
in Baja California has increased steadily,
from close to zero to nearly 40% at present.
The U.S. Army Corps of Engineers requires a 404 permit
(Clean Water Act: Discharge of dredged or fill material into navigable waters)
in order to operate a riverine sand-borrow pit. The U.S. Fish and Wildlife
Service and the California Department of Fish and Game require operators to
obtain "take" permits to remove habitat or endangered species.
This requirement limits the ability of operators to continue mining streambeds in Southern California.
Thus, this sets the pattern for sand mining elsewhere, particularly Baja California,
which is close enough,
and where current regulations are not as stringent as in California.
El Barbon Wash (Ponce et al., 1999)
is the main streambed in the vicinity of the Ojos Negros valley (Fig. 6).
Sand is currently being mined in El Barbon Wash (Fig. 7)
by authorized operators. The current pit has aproximate
dimensions of 1800 m length by 200 m width and 2.3 m depth,
which amounts to 828,000 cubic meters, or 1.2 million tons, in the past two years.
The extracted material is construction-grade sand. It is transported
by trucks to Ensenada, where it is shipped in barges to destinations in
Southern California. The sand is being used mostly as an aggregate for cement and asphaltic concrete.
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5.4.1. Environmental impacts
The environmental impacts of sand mining in the Ojos Negros valley and environs can be summarized as follows:
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5.4.2. Socio-economic impacts
The socio-economic impacts of sand mining in the Ojos Negros valley and environs can be summarized as follows:
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5.4.3. Current sand mining
El Barbon Wash is currently being sand mined, and the sand is exported outside of the valley to destinations in Southern California. A hydrologic and hydraulic study was undertaken to assess the extent, impact and sustainability of the sand-mining operations. The bed profile of El Barbon Wash, shown in Fig. 9, was obtained from existing topographic maps. El Barbon Wash has a steep slope, averaging 0.03 from point A to B, i.e., as it comes down from the Sierra Juarez (point A) to reach the entrance to the valley (at point B). Within the valley, the bed profile of El Barbon Wash has a slope averaging 0.00535, measured from point B to H, the latter located at the downstream point within the Ensenada sheet, close to the valley exit. Figure 10 features an image of El Barbon Wash and the Ojos Negros valley, showing the locations of points B to F (A is east of B; G and H are west of F). A field inspection undertaken on February 2002 showed that point C is the most upstream location of current sand-mining operations, and D is the most downstream location, for a total length of 1800 m of mined pit, measured along the streambed. The width of excavation was estimated to be about 250 m. The average depth of excavation was estimated at 2.3 m (Fig. 11). The total amount extracted to date is estimated to be about 1.04 million cubic meters. Current sand mining operations have a permit to mine an area of 2,530,217 m2in the streambed, amounting to a length of 10 km and a width of 253 m. With an estimated final depth of 3 m, the total volume of extraction is 7,590,651 m3. Between points C and D, six samples for grain-size analysis were collected at four representative locations, shown in Fig. 10. Summary results of the grain-size analysis are shown in Table 1. Sample grain-size distributions are shown in Fig. 12.
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Table 1. Summary of grain-size analysis, El Barbon Wash streambed samples. | |||
| Sample number/location | D50 (mm) | D60 (mm) | D90 (mm) |
| 1 | 1.070 | 1.311 | 3.384 |
| 2 | 1.033 | 1.321 | 3.728 |
| 3A (top) | 0.800 | 1.000 | 2.322 |
| 3B (middle) | 1.205 | 1.475 | 3.526 |
| 3C (bottom) | 0.870 | 1.110 | 2.656 |
| 3 Average | 0.958 | 1.195 | 2.835 |
| 4 | 0.938 | 1.136 | 2.610 |
| Average | 0.986 | 1.226 | 3.038 |
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5.4.4. Sand-transport modeling
Sand originating in upland catchments of the Sierra Juarez is delivered to El Barbon Wash at point B (Fig. 10). Downstream of this location, the stream slope decreases abruptly, to 0.00535. This change in slope makes possible the deposition of a fraction of the sediments that are brought from the upland catchments. The quantity that is deposited depends on the hydrologic, hydraulic, and sedimentological properties of the catchment-stream-flood plain system. Estimates of sand deposition in El Barbon Wash, downstream of point B (Fig. 10), were accomplished using the hydraulic model MODELRIVER. This model was developed at San Diego State University following the U.S. Army Corps of Engineers' HEC-6 standard. To determine the flood discharges at point B (Fig. 11), 4-hr storm depths for frequencies of 2 to 50 yr were obtained from the "Isohyetas de Intensidad-Duración-Frecuencia, Republica Mexicana" (1990) (see Table 2, Column 2). The conversion to 24-hr storm depths was accomplished by assuming the 4-hr storm to be encompassed within the SCS 24-hr Type I storm. Other required hydrologic data (catchment area, hydraulic length, channel slope, and curve numbers) was obtained from Ponce et al. (1999). The flood hydrographs were calculated using the U.S. Army Corps of Engineers HEC-HMS. The peak discharges are shown in Table 2 and the corresponding flood hydrographs are shown in Fig. 13. |
| Table 2. Flood hydrology characteristics of El Barbon Wash. | |||
| Return Period (yr) | 4-hr Storm depth (cm) |
24-hr Storm depth (cm) |
Peak discharge (m3/s) |
| 2 | 2.8 | 5.7 | 328 |
| 5 | 3.6 | 7.3 | 614 |
| 10 | 4.0 | 8.2 | 801 |
| 25 | 4.3 | 8.8 | 935 |
| 50 | 4.6 | 9.4 | 1068 |
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From point B to point F (Fig. 10), a study reach of 13,500 m was chosen for modeling purposes. This reach encompasses the current sand-mining operations, from point C to D, a length of 1800 m. The modeling was performed with cross sections every 100 m, for a total of 136 cross sections. Based on digital terrain modeling (DTM), the average channel width in the study reach was determined to be 240 m. Trapezoidal cross sections of 240-m bottom width and 2:1 side slopes were specified. At the upstream end of the study reach, a sediment-rating curve was developed using the Colby method (Colby, 1964) (see Fig. 14). MODELRIVER was run for a hypothetical 50-yr flood series, assuming a suitable sequence of 2-, 5-, 10-, 25- and 50-yr floods. The results of the sediment routing computations are shown in Table 3. |
| Table 3. Estimated sand deposition in
El Barbon Wash, from point B to point F (Fig. 9). | |
| Time horizon (yr) | Sand volume (m3) |
| 2 | 34,000 |
| 5 | 180,000 |
| 10 | 363,000 |
| 25 | 913,000 |
| 50 | 1,830,000 |
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The results shown in Table 3 are an approximation,
because the actual flood series cannot be determined a priori.
Furthermore, the model does not account for the hysteresis in the sediment rating curve,
the effect of which would be
to increase the amount of sand deposition
if the receding limb were to be longer than expected. This is certainly a possibility in
El Barbon Wash, where recession times of flood
hydrographs have been
documented by eyewitness accounts to last days and even weeks. In view of the uncertainties
inherent to sediment routing computations,
it is judged appropriate to multiply the amount shown in Table 3 by a safety factor equal to 3.
This would place the sand deposition in the study reach
at 5.5 million m3 for the 50-yr planning horizon.
This value can be compared with the 7.6 million m3
which is currently permitted for mining in El Barbon Wash.
The stratigraphy of wells in El Barbon Wash shows alluvial materials. For reference, Fig. 15 shows the stratigraphy of three wells in corresponding parcels of the Ojos Negros valley. |
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5.4.5. Regulation of sand mining in Mexico
The Government of Mexico, through its various agencies that have jurisdiction on water resources and the environment, is currently developing an emergency norm (Norma Oficial Mexicana de Emergencia) to regulate the extraction of sand and rock from streambeds of rivers and washes. The norm stipulates the conditions that govern sand-mining operations in the entire country, with specific reference to the emergent situation in the state of Baja California (Fig. 17). In the past few years, sand mining for import to the United States has increased steadily, and the need has arisen to enact regulation to safeguard natural resources which could possibly be impacted by the mining operations. Specific provisions of the (tentative) norm are the following:
In the case of Arroyo El Barbon, the requirement of the maintenance of an undisturbed unsaturated zone of 4-m minimum thickness appears excessive. Based on the grain-size analysis performed, the capillarity rise is estimated to be 0.5 m. In other sites, the capillarity rise will depend on the grain size; however, in sand-bed streams the capillarity rise should remain within 2 m. Noise pollution is regulated by the Municipality of Ensenada, which has jurisdiction over the Ojos Negros valley. The applicable legislation is the "Reglamento para el control de la calidad ambiental del municipio de Ensenada" (Law for the control of environmental quality in the municipality of Ensenada). Noise is defined as every sound that causes annoyance, interferes with sleep, work or rest, or that produces physical or psychological harm to the individual, flora, fauna, and public or private goods. The law specifies the permissible levels of noise pollution shown in Table 4. Sandmining operations are required to comply with this local regulation. |
| Table 4. Permissible noise levels in the Municipality of Ensenada. | |
| Source | Noise Level, Db(A) |
| Fixed | 68 (from 06:00 to 22:00) 65 (from 22:00 to 06:00) |
| Loading and unloading of goods and materials | 90
(from 07:00 to 22:00) 85 (from 22 to 07:00) |
| Automotive vehicles (Weight < 3 ton) (Weight 3-10 ton) (Weight > 10 ton) | 79 81 84 |
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5.5. Summary
The following conclusions are derived from this study:
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6. RESEARCH FINDINGS: COQUILLO
6.1. General
The "coquillo" or nutsedge is found as a weed in cultivated fields in the Ojos Negros valley,
in Baja California.
It belongs to the genus Cyperus, of which about 900 species have been documented
throughout the world. Some are grown for food, fibers, and perfume; others are considered among
the world's worst weeds.
Two species are found in Baja California:
C. esculentus L. and C. rotundus L.
Based on the color of their flowers, C. esculentus L. is commonly known as
yellow nutsedge, and C. rotundus is known as purple nutsedge.
6.1.1. Taxonomy
The nutsedge belongs to the sedge family (Cyperaceae), and to the genus flatsedge
(Cyperus L.). Its growth habit is graminoid, it is a perennial, apparently native to Eurasia,
and it is introduced in the United States. The two most important species are:
C. esculentus L. and C. rotundus L.
Other common names are: nutsedge, nutgrass, cocosedge, cocograss,
rednut sedge, coquito, and souchet rond.
There are five botanical varieties of Cyperus esculentus: four wild
varieties (esculentus, leptostachyus,
macrostachyus, and hermanii) and one cultivated variety (sativus).
This explains the
existence of two groups of plants which have similar morphology and name,
but differ in application: one is a weed and the other a crop.
The nuts (tubers) of the yellow nutsedge are widely
referred to as "chufa" nuts.
Yellow nutsedge is known as chufa, yellow nutgrass, Northern nutgrass, nutsedge,
earth almond, groundnut, tiger nut, zulu nut, rush nut, duck potato, or edible rush.
Purple nutsedge is known by one of more common names in different places,
including nutgrass, cocograss, "pakopako," "kili'o'opu,"
"chaguan humatag," "mustaka" or "musta" in Sanskrit, and "motha" in Hindustani.
The plant is listed as a noxious weed by the U.S. federal government,
and is considered a great menace to farmland in India. In Baja California, it is considered
a nuisance in La Trinidad valley and in the Ojos Negros and Maneadero valleys.
6.1.2. History
The use of yellow nutsedge has its origins in ancient Egypt. Chufa was one the first
crops to be domesticated, having been found in vases in the tombs of the ancient Egyptian
pharaohs. Chufa was widely used in Egypt and Sudan.
Its dry tubers have been found in tombs from pre-dynastic times (4000 B.C.).
The Arabs introduced the plant
to Spain during the time of the Moorish kings (up to 1200 A.D.).
The Eastern Spanish province of Valencia was the best for growing chufa.
There are written records from the 13th
century which mention the consumption of a drink made
from chufa (a predecessor to the horchata drink)
in the region of Valencia.
Yellow nutsedge occurs in most of the contiguous United States, where it now occurs
in both natural and weedy habitats. In Canada, it was found primarily in native
habitats prior to 1950.
Over the last 40 years, yellow nutsedge has become
weedy in cultivated fields. The spread of yellow nutsedge
may correspond to the increased use of selective herbicides.
6.1.3. Overall characteristics
Nutsedges develop an extensive system of rhizomes, tubers, and roots.
Rhizomes produce tubers and basal bulbs that bear aerial roots.
Tubers store starch and have several buds that produce rhizomes,
which develop more basal bulbs and new plants. Roots often grow
to greater depths than tubers or rhizomes.
Rhizomes are slender, fleshy when young, and covered with scales.
Nutsedges reproduce vegetatively from tubers and by seed.
Tubers and seeds disperse with agricultural and nursery activities, soil movement,
and in water, especially flooding. Seeds also disperse with wind. Seeds and tubers germinate
in spring. Tubers develop to soil depths of approximately 32 cm, but most are in the top 20 cm.
One plant can produce hundreds to thousands of tubers in one season. Seed production can be high,
but viability is variable; in California, seed viability is typically low. One plant
can develop into a dense colony 3 m or more in diameter. Patch boundaries can increase by more
than 1 m per year.
A single tuber can produce nearly 2000 plants and 7000 tubers in one growing season.
Very little nutsedge is produced from seed (less than 1 percent). Almost all of the nutsedge plants
come from tubers that have been laying dormant in the soil or from tubers that have been brought in by
contaminated sod, nursery stock, or machinery. Both nutsedges are able to survive in very diverse
growing conditions.
6.1.4. Habitat
Nutsedges occur in disturbed areas, cultivated fields, especially those irrigated in the summer;
in irrigation ditches, orchards, vineyards, gardens, turf, and landscaped areas.
They grow typically where moisture is plentiful.
They tolerate many soil conditions, including periods of drought and flooding.
6.1.5. Chemical control
At present, yellow and purple nutsedge require different herbicides to control them; therefore, proper
identification of the plants is vital.
If the yellow nutsedge herbicide is used to control purple nutsedge,
and vice versa, poor control of the targeted plants will result.
There has been very little success controlling nutsedges using biocontrol methods
such as fungi, insects, and nematodes. In turfgrass and ornamentals, mechanical
control of the nutshedge is not feasible. At present there are four
herbicides available for selective control of nutsedges in turfgrass:
Basagran T/O, Daconate 6, Image and Pennant.
In ornamentals,
there are three herbicides available for the control of nutsedges:
Basagran T/O, Pennant and Roundup.
In turfgrass, Basagran T/O, Daconate 6, and Image are postemergence herbicides,
while Pennant is used preemergence. Image and Daconate 6 are used for the
selective control of purple nutsedge in most warm-season grasses. Image causes
injury to cool-season grasses; at present there are no herbicides
available for control of purple nutsedge
in cool-season grasses. Basagran and Daconate6 are used for the
selective control of yellow nutsedge in most cool-season grasses.
In ornamentals both Basagran T/O and Roundup are applied postemergence, while Pennant
is applied preemergence. Roundup, a broad spectrum herbicide, is used to control weeds
such as nutsedges. Basagran T/O and Pennant are both used for the selective control of yellow netsedge
in ornamentals.
At present, there is no one herbicide available to control both nutsedges in all major turfgrasses.
Since the nutsedges are not grasses, Fusilade/Venture, Past, Excel, or Assure will not be effective.
6.1.6. Other control strategies
This refers to the control of nutsedges by a
hydrothermal process that utilizes the sun's energy to heat moist
soil that is mulched under polyethylene.
The basic concept of soil solarization is to use transparent,
thermoplastic infrared-retentive films to allow transmission
of light energy to the soil, where it is absorbed and used to heat the soil.
Increased temperatures are achieved
in this way. If the temperature under the plastic film and in
the soil reaches sufficiently high temperatures,
weeds, insects, and pathogens are damaged or killed. In arid
cloud-free regions, the soil solarization technique
has found wide application for the control of some soil-borne diseases and weeds.
An experiment was performed in Western Australia to
measure the effectiveness of soil solarization against fungi.
Four weeks with soil temperatures at
about 45oC where necessary to give good results against
a certain fungi (Fusarium). If the
temperature dropped below 45oC for 6-7 consecutive days,
the treatment time had to be extended.
Cloud cover had a marked effect on soil temperature under the plastic. With complete cloud cover and
an air temperature of 34oC,
soil temperatures of about 40oC
were reached. However, in a cloudless day with air
temperature at only 24oC, soil temperatures approaching
50oC would be achieved.
The fungus Dactylaria higginsii (Lutrell) M. B. Ellis
has been identified by University of Florida
researchers to control nutsedges. The method involves the use of the spores of
the fungus applied to weeds
to inhibit their growth or to induce mortality of the weed without adversely
affecting the growth and yield
of desired field crops. The fungus is very pathogenic to purple nutsedge.
In certain parts of Tamil Nadu, in Southern India, where rice is grown traditionally,
farmers are effectively managing
the nutsedge problem by using pigs. The pigs are of a local breed, dark black in color; they are
allowed to collect the tubers in the wastelands. Since the tubers are succulent and sweet in taste,
pigs are very fond of them. Nutsedge tubers are very nutritious food for pigs,
increasing body weight and milk production.
Pigs can easily remove the tubers even when the soil is hard.
If the soil is wet and ploughed, it will be even easier for them to remove the tubers.
Usually the field is soaked with water and puddled well when the animals are allowed to collect the tubers.
Puddling will bring out the tubers buried in deeped layers (around 30 cm) and makes collection easier.
Each animal can collect 2-4 kg of tubers in one day; 25-30 animals per acre (50-60 animals per hectare)
can remove the available tubers within a day. Farmers around Virudhasalam village (Tamil Nadu)
report that they practice this method every year before planting rice, and are able to control the
nutsedge. In this way, purple nutsedge can be managed effectively without any harm to nature and without
any additional weeding cost.
Limit tuber production and drain tuber energy reserves by repeatedly
removing small plants before the 6-leaf stage (every 2-3 weeks in summer).
Mature tubers can resprout up to about 12 times. Shading or solarization can reduce
infestations by weakening shoots and decreasing new tuber formation, but mature tubers may not be
eliminated. Cultivation (of nutsedge) can worsen an infestation if not repeated often enough
to exhaust tubers
and prevent new tuber formation.
For purple nutsedge, deep cultivate thoroughly (to about 30 cm deep) to fragment tuber
chains and cover green parts, followed by persistent repeated cultivation (to about 15 cm deep)
to kill new shoots and limit new tuber formation, especially when the soil is dry.
6.2. Yellow Nutsedge
Yellow nutsedge is found worldwide in warm and temperate zones, occurring in Europe and Africa.
It was introduced into the New World from the Old World.
In the Western Hemisphere, it grows from southern Canada to northern Argentina.
The plant is known in most of the United States, except Wyoming and Montana (see map).
It occurs elsewhere in the world in regions with temperate to tropical climates.
Yellow nutsedge is a noxious weed of wet soil.
The nutsedge is most difficult to control in cultivated soils,
often forming a solid cover over large areas in cotton fields,
sorghum and alfalfa pastures, flood plains, dams, ditches, and along streams and roadsides.
In Arizona, it is common throughout most of the state, from 100 to 8200 ft elevation,
flowering from May to November.
In California it occurs throughout the state, up to elevations of 1000 m.
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6.2.1. Habitat
Yellow nutsedge generally occurs in disturbed habitats, but can tolerate a wide range of soils types. In natural habitats, the species grows along margins of lakes, rivers, streams, and marshes. These habitats are usually flooded in the spring, giving the nutsedge little competition from other plants early in the growing season. Yellow nutsedge also occurs as a weed in cultivated fields, where it is associated with a variety of other weeds. Although yellow nutsedge appears to compete poorly with other weeds, it is resistant to many herbicides. Therefore, it often increases rapidly when other weeds are controlled by herbicides. |
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6.2.2. Characteristics
Yellow nutsedge is a tough erect fibrous-rooted perennial, 1 to 3 ft high, reproducing by seeds and by many deep, very slender rhizomes, which form weak runners above the ground, and small tubers or nutlets at the tips of underground stems. The tubers are dark, unevenly globed shaped, 3/8 to 3/4-inch long, and edible, tasting somewhat like almonds. Near the base of the triangular yellow-green stem, a cluster of three-ranked, grasslike leaves arises which are often longer than the stems, and 1/8 to 1/3-inch broad. The umbrella-like flowering tops have a few threadlike stems of different lengths radiating out like spokes from the stem tip. These have numerous yellowish to golden-brown spikelets on the upper part. The spikelets are very narrow, flattened, 1/16 to 1/12-inch broad, and 1/4 to 1 1/2-inch long. The leaves beneath the flowering tops are 2 to 10 inches or more long, and some are much longer than the flowering stems. The brownish three-angled achene, about 1/16-inch long, is widest at the top. The nutlets are almost smooth at maturity and unevenly globe shaped. Yellow nutsedge grows from perennial tuber-bearing rootstocks; the tubers are approximately 2/5 to 4/5-inch long. The leaves are narrow and grass-like, growing in three vertical rows on the stem. Most of the leaves are clustered at the base of the stem. The small flowers are yellowish or yellowish-brown, and arranged in narrow spikelets on umbel-like inflorescences (group of flowers originating from a single point). Located immediately below the inflorescence are 3- to 9-inch long leaf-like structures (bracts). The flowers have three stamens and a three-cleft style. The yellowish-brown seeds are about 1/16-inch long and three-angled. |
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6.2.3. Growth and development
The yellow nutsedge plant forms tubers in the summer and autumn.
The tubers, which are formed at the apical ends of
indeterminate rhizomes, usually sprout the spring after they are formed.
Tubers generally produce one to three sprouts
(determinate rhizomes), which grow toward the soil surface and form a
primary basal bulb just below the surface.
Each primary basal bulb produces a vegetative plant. The basal bulb
produced by the original tuber has many fibrous roots and
indeterminate rhizomes; the indeterminate rhizomes may then develop
into secondary basal bulbs and tubers.
When a critical daylength or temperature is reached,
plants stop growing vegetatively and start to flower;
however, many populations do not produce viable seed.
Tubers are the only part of the plant that overwinter.
Winter conditions kill basal bulbs, rhizomes, fibrous roots, and all above-ground parts.
While tubers may be viable up to 3.5 years, most only survive one winter.
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6.2.4. Reproduction
Yellow nutsedge does produce seed; however, reproduction by
seed is of minimal importance in most areas in comparison to vegetative spread.
The species spreads primarily by tubers, rhizomes, and corn-like basal bulbs.
Tubers planted to soil depths of 80 cm produced new plants. Tubers survive soil temperatures
as cold as -5oC and require a period of chilling to
break dormancy and germinate. Tubers germinate when soil temperatures remain above
6oC. Under field conditions, tubers typically survive
approximately 3-4 years.
Yellow nutsedge is considered one of the world's worst weeds.
Well adapted to irrigated agriculture, yellow nutsedge is particularly problematic in row crops
because it competes with crops for water, light, and nutrients, thereby reducing crop yield.
It has also been known to spoil the quality of some crops. In some areas, yellow nutsedge tubers have been
known to grow into potato tubers causing them to be graded as culls.
They may also pass through shelled lima beans, requiring costly
hand sorting. It addition, there has been some suspicion that
this species may produce chemicals that are toxic to crops.
6.2.5. Economic importance
Yellow nutsedge is closely related to chufa (Cyperus esculentus variety sativus);
some taxonomists treat them as the same species. In parts of Africa, Europe and Asia,
chufa is grown for its edible tubers.
The tubers contain protein, carbohydrates, sugars, and lots of oil and fiber.
The chufa nut is good for human health, containing
high levels of iron and potassium, and no sodium. The Spanish produce a
drink called "horchata" made out of the nuts (tubers)
of yellow nutsedge. The popularity of this drink has recently extended
to other countries such as France, Great Britain, and Argentina.
Chufa tubers are ground into flour, as well as being used to produce a cold drink (horchata),
a coffee
substitute, vegetable oil, and cellulose.
In the United States, the primary use of chufa as a crop is to attract and feed game,
particularly wild turkeys. Turkeys love chufa tubers; as natural scratchers, once
discovering a plot of chufa,
they will return again and again, all winter long, or until spring arrives and other food
is readily available.
Chufa tubers have been planted so that pigs could be turned into the fields to fatten and improve
the taste of pork.
In the United States, chufa tubers have
been used as hog feed, pastured in the field in states such as Florida, Georgia, and Alabama.
Tubers of chufa have also been identified as valuable food for waterfowl and cranes.
Ducks dive for them when wetland fields are flooded.
Chufa is also used in seed mixes for wetland restoration, mitigation, and erosion control.
Currently, yellow nutsedge is merely regarded as another obnoxious weed; however,
historically, its small tuberous rhizomes were used both
as food and medicine by the Native Americans. Even today the Egyptians cultivate
a native species of Cyperus in moist soils or
sandy shores for their edible tubers. These are called "tiger nuts" and are first fried,
and then soaked in water. Reportedly, the
taste is similar to hazelnuts. It was another species (C. papyrus)
that the Egyptians used to make paper, sails, cloth. mats, ropes,
or plaited into sandals.
In the Peruvian Amazon, reportedly there is a native
species of Cyperus used widely by tribal women as a natural contraceptive.
This property has been attributed to a certain mold that grows on the root of the
Amazonian species that has oxytoxic (abortive)
properties similar to Ergot, a fungus that grows on rye.
In Maradi state, eastern Niger, C. esculentus is cultivated for
export to Nigeria. Revenues from this weed exceed those from the
typical cash crops such as cowpea and groundnut.
The tubers of C. esculentus may be consumed raw, roasted, or ground.
Nowadays, chufa is cultivated in Northern Nigeria and Ghana,
where it is made into a sweet meat, and Togo, where it is used uncooked as a side dish.
These countries, and others as the Ivory Coast, export 2300 tons of tubers every year to Spain.
The chufa is also a representative crop of the Spanish Mediterranean region, where tubers
are used to make a beverage called
horchata or horchata de chufas. The milky-looking
aqueous extract of chufa has a pleasant and characteristic flavor of vanilla and almonds.
Chufa is potentially a commercial source of high-oleic acid vegetable oil
and high-carbohydrate tuber cakes. Some authors believe that
tuber oil could be exploited in the same way as olive oil.
Chinese researchers have measured the
physical and fuel properties of oil extracted from the chufa,
and concluded that the physical properties are similar to those of
other vegetable oils. They have suggested that this oil may also be used as biodiesel fuel.
Products from the chufa tubers include aqueous solutions (as a base for non-alcoholic beverages),
milky solutions (as refreshing beverages or partial milk substitutes),
as well as cookies and ice-cream made with chufa.
The caramel from malted tubers of Cyperus esculentus may be used to
add body, flavor, or color to certain baked products,
non-alcoholic malt beverages and dark beers, and in the production of
condiments. The starches obtained from chufa and rice showed
similar properties; the solutions of the starch exhibited a good paste
stability, clarity, and adhesive strength.
The starch can be used in many starch-based foods as well as in the
cosmetic industry, and for laundry, glazing and stiffening.
The waste residue after oil extraction could be further modified
producing syrups, flours, or livestock feeds.
Chufa tubers have a relatively high total antioxidant capacity,
because they contain considerable amounts of
water-soluble flavonoid glycosides.
Consumption of antioxidants could protect the immune system of malnourished populations.
In addition, the intake of antioxidant-containing foods may
delay the progression of HIV infection to AIDS.
For many years, the chufa tubers have been considered to have adequate
properties to fight respiratory infections, and some stomach
illnesses. To this date, the "horchata de chufas" is considered
an effective remedy for diarrhea, according to popular tradition in
Valencia, Spain.
6.2.6. Cultivation
Chufa is planted in late spring to midsummer
by dropping the dried tubers 6-12 inches apart in rows spaced 2-3 feet apart.
The planting rate is 15-40 pounds per acre.
The tuber develops into a plant which has several
tubers bunched together directly beneath it, the plant and a few straglers some
distance away. Although bunched together, each nut
is attached to a thin underground stem that connects the single tuber to the growing shoot.
Chufas are easy to grow and require almost the same care as corn.
Experience in Northwest Florida suggests that
chufa plots should be no less one acre, and preferably 2-5 acres.
Very small plots may be damaged or destroyed by
raccoons, crows, skunks, deer or squirrels. Raccoons, crows
and skunks will dig up young plants to eat the tubers.
Deer and squirrels will eat the tubers if they are exposed.
Chufa may be planted in woodlands to encourage populations of wild turkey and deer.
Planting time must allow 90-100 days frost-free growing time.
In Northwest Florida, chufa is planted from April to early August.
Earlier plantings seem to higher yield but require more
cultivation or herbicide protection. Later plantings tend to last longer
into the next winter, which is desirable. Chufas grow
best in sandy-loam soils but will grow even in the hardest clay.
At the end of the planting season, when chufa tops have died down,
a clumps should be turned over for the first-time turkeys to find.
After they have located the plot, they will scratch it up and
notify the next of kin, who will return to dig up and eat the tubers.
Since 1978, a number of research studies have been carried out
related to the cultivation of chufa.
The date of cultivation of chufa tubers has varied throughout time.
Formerly tubers were usually planted
at the beginning July, after the wheat harvest. Later, planting
started in June and more recently, the first fortnight of May.
In the early 1980s, most farmers preferred to plant tubers even
earlier in the year to increase production.
The influence of soil texture on the amount and quality of
tubers has also been studied. The most appropriate soil texture for
chufa cultivation is sandy loam.
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6.2.7. Chemical control
The chemical control of yellow nutsedge is described in the following tables.
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| Table 5. Chemical control of yellow nutsedge. | |||
| Herbicides | Turfgrass | Ornamentals | Cool-season grasses |
| Preemergence | Pennant | Pennant | Basagran T/O, Daconate 6 |
| Post-emergence | Basagran T/O, Daconate 6, Image | Basagran T/O, Roundup | Basagran T/O, Daconate 6 |
| Table 6. Chemical control of yellow nutsedge (continued). | ||||
| Herbicides | Bermuda grass | Centipede grass | St. Augustine grass | Zoysia grass |
| Preemergence: Metolachlor | yes | yes | yes | yes |
| Post-emergence: Bentazon | yes | yes | yes | yes |
| Post-emergence: Halosulfuron | yes | yes | yes | yes |
| Post-emergence: Imazaquin | yes | yes | yes | yes |
| Post-emergence: Imazaquin + MSMA | yes | no | no | yes |
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6.2.8. Other controls
It is best to target control efforts in the year before planting. Use of a cereal crop or cover crop that shades the soil is recommended, as nutsedge does not tolerate shade very well. Rotation to a crop where Dual or Frontier can be incorporated before planting is recommended. The incorporation into the soil puts the herbicide down where the tuber will germinate from, inhibiting new shoots. Preliminary results show that a single top burndown at 30 to 45 days is not enough to prevent further tuber development. However, if topgrowth is controlled for a full year, tuber numbers will be reduced up to 90%. The farmer needs to look for opportunities to burn down the nutsedge before the nutlets begin to form in July. For late-planted crops, the tops should be destroyed before planting, or after an early harvested crop, the topgrowth should be destroyed immediately after harvest. In the non-crop period, Gramoxone, Ignite, or Roundup will kill tops. Basagran is also effective in killing tops. Nutsedge is usually dragged into a field on tillage equipment. Nutsedge moves into crop fields from edges near ditches and roadsides. New patches should be targeted before they get to be a problem.
6.3. Purple Nutsedge
The native range of C. rotundus is Eurasia.
It is present in all southern states, in
most southwestern states, and in some northern states.
It is also present in the Pacific Islands, including Micronesia
and American Samoa, and elsewhere in Asia, including Australia, New Zealand,
Japan, Korea, Taiwan, China, Phillipines, Thailand, Cambodia,
Viet Nam, Malaysia, and Indonesia. It occurs elsewhere in the world in
regions with tropical to warm climates.
In Arizona, purple nutsedge is largely confined to the valleys; 100 to 4000 ft
in elevation; flowering from May to fall frosts.
It is present in all summer crops, in lawns, ditchbanks, and field borders.
The rhizomes, runners, and tubers make the nutsedges almost
impossible to erradicate.
Purple nutsedge is reportedly native to India, but has been introduced
around the World. The plant is a serious pest in the
U.S. Southeast ranging from Virginia to Texas. It has become established
in California and Arizona, and has the potential to invade
other Pacific states.
Purple nutsedge occasionally occurs in more temperate
regions, but it has not persisted in cold locales.
The northern limit of nutsedge in Japan is in a region where the average
minimum atmospheric temperature is
-5oC, below which the tubers will not germinate.
Temperature appears to limit the species
to more tropical and warm temperate regions.
Purple nutsedge is limited to areas where the average January temperature is above
-1oC.
6.3.1. Habitat
Purple nutsedge is prevalent in disturbed areas and lawns.
It grows best in moist, fertile soils; it does not grow well in shade,
and once established, it is very persistent.
In California, purple nutsedge occurs in the Central valley,
South Coast, and the Sonoran Desert, up to 250 m elevation.
In Papua New Guinea it grows to at least 1800 m elevation.
6.3.2. Characteristics
Purple nutsedge closely resembles yellow nutsedge, but the matures stems are usually
longer than the basal leaves.
The leaves below the flowering heads, 1 to 5 inches long, are about the same length
as the flower stems; few are longer.
The spikelets are dark brown-purple, and the runners are fewer,
woody, and thicker. The nutlets are oblong and covered by persistent reddish scales.
Purple nutsedge is a colonial, herbaceous, perennial, with
fibrous roots. It typically grows from 7-40 cm tall and reproduces
extensively by rhizomes and tubers.
The rhizomes are initially white and fleshy with scaly leaves,
and become fibrous, wiry, and very dark brown with age.
Rhizomes may grow in any direction in the soil.
Those growing upward and reaching the soil surface become enlarged,
forming a structure 2-25 mm in diameter variously
called a "basal bulb, a tuberous bulb, or a corn" that produces
shoots, roots, and other rhizomes. Rhizomes that grow
downward or horizontally form individual tubers or chains of tubers.
Individual tubers are dark reddish-brown when mature,
about 12 mm thick, and 10-35 mm long.
The dark green, shiny, three-ranked leaf blades arise from or near
the base of the plant. They are narrow and grass-like ranging
in size from 5-12 mm wide to 50-cm long and have a prominent channel
cross section. The leaf sheets are tubular and membranous
and attach to compact nodes at or near the base of the plant.
The upright culms or stems are 10-50 cm tall, smooth, triangular in
cross section, and support a much-branched inflorescence.
Two to four leaf-like bracts subtend the inflorescence which is
umble-like consisting of 3-9 unequal length branches
(sometimes referred to as rays) bearing spikes of 3-10 spikelets.
Spikelets are flattened and linear, ranging in length
from 10-30 mm long and generally dark reddish purple or reddish brown in color.
Each of the approximately twenty flowers (florets) in a
spikelet is subtended by a keeled scale (glumes) 2-5 mm long, having a green
midvein and membranous margin. The
flowers are bisexual, each with three stamens and a pistil bearing three stigmas.
Fruit, although rarely produced,
consists of a three-angled achene (nutlet).
The purple nutsedge is characterized by triangular, erect, solid, nodeless stems,
each 12-18 inches in height;
by basal leaves that are dark green and shorter than the stem;
and by dark brown rhizomes that produce chains of
irregularly shaped, hairy, dark brown to black tubers 1/4-1/2 inch in diameter.
The rhizomes become like thin wires
once the plant matures and serve to maintain dominance among tubers in that chain.
The inflorescence is an umbrella-like cluster of branches 1/2-1 inch long and
reddish brown to purple in color. Viable seed is produced, but
the plant propagates almost exclusively by tubers.
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6.3.3. Growth and development
Rhizomes and tubers of purple nutsedge form extensive networks in the soil. While most tubers are found growing in the upper 15 to 20 cm, a few penetrate to a depth of 40 cm. The root system in heavy clay may extend more than 1-m deep. Under favorable conditions, a single tuber could produce 99 tubers in 90 days. Experimental planting of tubers set on 0.9-m centers resulted in their nearly five-fold increase by the end of the growing season. Tubers of purple nutsedge resist temperature extremes, but seem more sensitive to lower temperatures. Germination failed in tubers held for 12 hours at 50oC. However, greater than 80% germination occurred after exposure to 40oC. Tubers exposed to temperatures of -5oC did not survive more than 2 hours. Tubers and basal buds serve as vegetative propagules. They are carried on farm tillage implements and may be spread by erosion and running water. Severe storms may bring tubers to the surface and transport them to new areas. Such propagules may also be transported long distances with nursery stock. Even though purple nutsedge flowers abundantly, it rarely produces viable seeds. Seeds are disseminated by wind or water, transported in mud, or carried onto fields by flooding streams or with irrigation water. Purple nutsedge possesses the C4 photosynthetic apparatus, which is an adaptation to assimilating CO2 at higher temperature and higher light intensities compared to C3-pathway plants. C4 plants typically exhibit their best growth rates at temperatures characteristic of tropical and subtropical regions. The leaf anatomy for purple nutsedge is of the Krantz-type. Sheaths of cells that from around the vascular bundles serve to compartmentalize the photosynthetic events.
6.3.4. Reproduction
Tubers and rhizome production are important factors in the purple nutsedge's success as a weed.
Rhizomes provide the major means by which the plants may colonize an area.
Tubers offer a mechanism for asexual reproduction, and they are the major
dispersal unit capable of surviving extreme environmental conditions.
Tubers make the plant difficult to control, because only translocated
herbicides are potentially effective on this species.
Besides their competition for resources, evidence suggests that organic
substances released from the decay of dead subterranean tissues
may be allelopathic and reduce crop yields where purple nutsedge
infestations are severe.
Purple nutsedge may produce up to 40,000 kg of subterranean plant material per hectare.
Under experimental conditions, barley yield
was reduced by 15 to 25% by C. rotundus residues in the soil.
Tubers of purple nutsedge tolerate high temperatures, but not freezing.
They germinate when soil temperatures remain above 15oC.
Typically only one tuber in a chain germinates, unless the chain is severed.
Low oxygen and high carbon dioxide levels appear to
promote tuber dormancy. Tuber dormancy is high in undisturbed soils and deeper soil levels.
Tubers can remain dormant for long periods and can become dormant after sprouting.
Tuber dormancy often increases with age. New tubers
are initiated when flowers develop, often about 4-8 weeks after shoots emerge.
Tubers planted at a depth of 90 cm are usually unable to produce aerial shoots.
Tubers desiccate quickly when detached from the rhizome-root system under dry conditions and can
survive flooded soils for at least 200 days. Tuber longevity
is variable and depends on environmental conditions. In most cases, tubers
survive about 3-4 years, but under certain conditions, they can remain
viable for up to 10 years or more. Seedling survival is typically low.
Purple nutsedge has been called the world's worst weed. This is a
befitting designation for a species known from more countries (at least 92)
than any other weed and that infests at least fifty-two different crops worldwide.
It grows in all types of soils and can survive with the
highest temperature known in agriculture. In the United States, purple
nutsedge infests cultivated fields, waste areas, roadsides,
pastures, and natural areas. It is considered a headache for the Southern
gardener because of its insidious, rapid growth in flowerbeds
and vegetable gardens. Purple nutsedge produces an extensive system of
underground tubers from which they can regenerate. Nutsedge is very
difficult to control once it is established.
Purple nutsedge greatly impacts agriculture and has an unfavorable effect on
natural ecosystems by displacing native plants
or by changing the availability of food or shelter for native animals.
Although relatively small in nature, purple nutsedge provides
formidable resource competition for much larger crop plants and ornamentals.
This rapid growing plant can quickly form dense colonies
due to its ability to produce an extensive system of rhizomes and tubers.
Many studies document reduced yields in sugar cane, corn, cotton, rice,
vegetables, and numerous other crops. The abundantly produced tubers
present an efficient means of dispersal and reproduction. These
features, together with the ineffectiveness of herbicides, make this weed nearly
indestructible.
6.3.5. Economic Importance
Cyperus rotundus, reportedly originating in China, is used as a carminative
and energy and hormone regulating herb in Traditional
Chinese medicine. Purple nutsedge has also been used in landscaping in China.
There are reports of its use in India as a soil binder.
It is undesirable as fodder, because it quickly becomes fibrous with age, but
in the absence of more desirable plants, it can serve that purpose.
Extracts and compounds from purple nutsedge have medicinal properties such as
reduction of fever, inflammation, and pain.
The literature contains numerous references to the use of the roots of this plant for
essential oils and its seeds for food products. Tuber extracts
may reduce nausea and act as a muscle relaxant.
6.3.6. Chemical Control
There are no herbicides registered for use on all vegetables that will
control purple nutsedge.
While there are herbicides that can be used safely to control purple
nutsedge in lawns, these herbicides
should not be used on vegetables, unless so specified on the label.
Herbicides such as Image, Manage, or MSMA
can be used to successfully control purple nutsedge in the lawn; however,
these herbicides will severely injure
or kill most vegetables or may result in herbicide residue in the produce.
The chemical control of purple nutsedge is described in the following tables.
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Table 7. Chemical control of purple nutsedge.
| Herbicides | Turfgrass |
Ornamentals | Warm-season grasses | Cool-season grasses | Preemergence | None available | None available | None available | None available | Post-emergence | Basagran T/O, Daconate 6, Image |
Basagran T/O, Roundup | Image, Daconate 6 | None available | | ||||
| Table 8. Chemical control of purple nutsedge (continued). | ||||
| Herbicides | Bermuda grass | Centipede grass | St. Augustine grass | Zoysia grass |
| Preemergence: None | N.A. | N.A. | N.A. | N.A. |
| Post-emergence: Halosulfuron | yes | yes | yes | yes |
| Post-emergence: Imazaquin | yes | yes | yes | yes |
| Post-emergence: Imazaquin + MSMA | yes | no | no | yes |
| 6.4. Comparison |
| The following table shows a comparison between yellow nutsedge and purple nustsedge. |
| Table 9. Comparison between yellow nutsedge and purple nutsedge. | ||
| Characteristics | Yellow nutsedge | Purple nutsedge |
|---|---|---|
| 1. Scientific name | Cyperus esculentus L. | Cyperus rotundus L. |
| 2. Common names | Chufa, coquillo, yellow nutgrass, Northern nutgrass, nutsedge,
earth almond, groundnut, tigernut, | Nutgrass, cocograss, mustaka, musta, motha, coquillo |
| 3. Life cycle | Perennial | Perennial |
| 4. Growth habit | Graminoid | Graminoid |
| 5. Basal leaves | Three ranked | Three ranked |
| 6. Leaves | Flat, slightly corrugated, usually as long or longer than flowering stem | Flat, slightly corrugated, usually shorter than flowering stem |
| 7. Leaf color | Light green | Dark green |
| 8. Leaf width | 4-9 mm | 3-6 mm |
| 9. Leaf tip | Abruptly tapered, very pointed, pinched together | Long attenuated, keeled |
| 10. Flowering stem | Triangular | Triangular |
| 11. Stem height | Up to 0.9 m | Up to 0.4 m |
| 12. Flower color | Yellowish-brown, gold-brown or straw color | Purple to reddish brown |
| 13. Flower size | 5-30 mm long, about 2-3 mm wide | 8-25 mm long, about 1-2 mm wide |
| 14. Tubers | Round, unevenly globe-shaped, 0.3-1.5 cm in diameter, brown to black, hard, hairless, smooth (scales shed with maturity), with buds only at apex, formed at ends of whitish rhizomes | Irregularly shaped, oblong to nearly round, up to 2.5 cm long, usually less than 1 cm thick, covered with persistent reddish or reddish brown papery scales or hairs, with buds scattered on the surface, tubers in chains, wiry rhizomes |
| 15. Tuber taste | sweet, almond-like | bitter |
| 16. Rhizomes | Terminate with a tuber, break easily; not connected among plants | Develop chains of up to 15 tubers at intervals of 5-25 cm along their length; interconnected among plants |
| 17. Uses of plants | Wetland restoration, mitigation, and erosion control | Carminative and energy and hormone regulating herb in traditional Chinese medicine; landscaping in China |
| 18. Uses of tubers | Edible, earthy-almond flavor | Medicinally in China and India; tuber extracts may reduce nausea and act as a muscle relaxant |
| 19. Reproduces | Primarily by tubers | Primarily by tubers |
| 20. Climate | Temperate to tropical | Tropical to warm |
| 21. Habitat | Disturbed soils, wide range of soil types; margins of lakes, rivers, streams, and marshes; riparian | Disturbed soils, moist fertile soil, full sun |
| 22. U.S. distribution | All states, excluding Wyoming, Montana, and Alaska, and including Hawaii and Puerto Rico | All Southern states, most Southwestern states, a few other northern states, plus Hawaii and Puerto Rico |
|
6.5. Sustainable Control Strategies
6.5.1. Soil solarization
Soil solarization is a simple, cheap, and highly efficient method to control weeds effectively.
The only price input is the plastic sheets.
To solarize the soil, first the soil must be in moist condition and covered
with 0.125-mm thick black polyethylene
or 0.1-mm thick transparent polyethylene sheet for 4 to 6 weeks. The sheet should
be in a full stretched condition, and the edges
buried in the soil to hold the sheet in place.
Solar radiation heats the soil under the plastic sheets and the temperature rises
to 45-50oC.
The heavy heat affects the weed seeds present in the soil under the polyethylene cover.
The effectiveness of the soil solarization
depends on the exposure time and the prevailing temperature.
In addition to weed control, soil solarization controls plant diseases, and it alters
some of the physical and chemical properties
of the soil to promote better crop yield.
6.5.2. Tuber marketing
Parts of the nutsedge, particularly the tubers of the yellow nutsedge,
have been marketed as food for animals and even humans. Other parts of the purple nutsedge may also have
economic uses.
Additional research will determine whether this is a feasible control strategy for the
Ojos Negros
and neighboring valleys of Baja California.
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6.5.3. Feed for pigs and wildlife
There is evidence that pigs can be used effectively to control coquillo. Pigs will search and eat the tubers, particularly those of the yellow nutsedge. Wildlife such as ducks and turkeys are also fond of the tubers of the yellow nutsedge. Research is needed to determine whether use of the nutsedge as animal feed is a feasible control strategy for the Ojos Negros and neighboring valleys of Baja California.
6.5.4. Shading
The coquillo requires plenty of sunlight and water for its continued growth and development.
One strategy for coquillo control that is being used in
Ojos Negros is to rotate alfalfa into a coquillo-infested
field. Alfalfa effectively shades the ground, inhibiting the coquillo aerial parts from growing.
Control is effective while the alfalfa is being cultivated, although there is no experience
to indicate that the coquillo
will not come back after the field is rotated back to vegetables.
6.5.5. Experience in Valencia, Spain
It is perhaps in Valencia, Spain, that the yellow nutsedge (C. esculentus L.) is best valued
for the quality of its tubers (Pascual et al, 2000).
Researchers at the Universidad Politécnica de Valencia (Polytechnic University of Valencia)
have studied the economic uses of C. esculentus since 1981. In particular,
Pascual España and Maroto (1984) have published a book on the agronomy of the
chufa (Cyperus esculentus L.). Their findings are reported here.
The principal use of the chufa in Spain is as the main ingredient of the beverage
called "horchata de chufas," which is common in Valencia. However, it is recognized
that the chufa has other uses in other parts of the world, primarily
as pig and wildlife feed. Great Britain and France import the tubers for the manufacture of sweets.
The chufa tubers are very rich in carbohydrates and fats.
Additionally, a very high-quality oil can be extracted from the tubers. This oil has been
used in human consumption in Italy and Egypt.
The chufa crop, although small compared to other popular staples,
has increased steadily in Spain.
The main reason appears to be the increase in the consumption of horchata,
coupled with the increased profits associated with the mechanical collection of the tubers.
The majority of the chufa grown in Spain is in Valencia.
The chufa is grown during the spring, since its aerial parts are very much affected by cold
weather. The sprouting of tubers
requires a temperature of at least 12oC. The chufa is
adapted to sandy and silty-sandy soils; it does not do well in clayey soils.
One tuber can produce from 25 to 150 plants (Vaya, 1981).
In one instance, one tuber produced 1900 plants
and 6900 tubers, all within an area of 2.1 m diameter and 0.23 m depth (Tumbleson and Kommendahl, 1961).
The Valencian growers distinguish two types of chufa tubers: "Ametlla," of rounded tubers,
and "Largueta,"
of elongated tubers. Planting is done at the beginning of May, and sometimes as early as
April. The number of water applications varies with the local rainfall, from between 10 to 15
per crop. The watering interval is
one month during the spring and one week during the summer.
The chufa plants are better adapted to cultivation in soils of sandy and silty-sandy texture. In clayey soils, the tubers
are of thicker skin, less pleasing taste, and feature a greater number of roots.
Fertilization studies of chufa has been accomplished with positive results. The Valencian study
used two types of liquid fertilizers, and concluded that the chufa responds adequately to target fertilization.
Fertilization increased the number and quantity of tubers, and the size of the aerial parts.
"Bedding" is a mechanical or physiological accident which
consists of the bending of the aerial parts from nearly vertical to nearly horizontal. Late
bedding usually
starts in August, when the plants have grown considerably. Prolonged bedding interrupts
photosynthesis, and the plants turn brownish in color and start to wilt. Late bedding is normal;
however, early bedding, which occurs around July, has the effect of lowering productivity. It
appears that agronomic practices that delay bedding, either late or early, have the net effect of
increasing tuber productivity.
In general, chufa is not fertilized because of the rotation with other crops,
among which are potatoes and artichokes,
which are fertilized. While there is no rule for chufa fertilization,
there is a belief that too much nitrogen
could lead to excessive aerial growth and intensify bedding,
at the cost of reduced tuber productivity.
Nitrogenous fertilizers have shown to reduce the dry weight of tubers,
as compared to fertilization with non-nitrogenous
fertilizers.
Tuber collection is performed during the second half of November and the first half of December,
although it may extend until January.
The aerial components
of the plant are usually burned. Tuber collection used to be accomplished manually,
but at present it is done by mechanical means.
Manual collection consists of a revolving hopper with a screen that separates soil and other impurities, leaving the tubers
almost clean, ready for the wash.
Mechanical collection is accomplished with a tractor that pulls two bodies;
the first body collects the soil, transporting it to a sloping and rotating cylindrical hopper,
where the tubers are separated from the soil, and collected at the end of the cylinder.
After collection, the chufas are washed to eliminate rocks, earth, and other impurities. The chufas are
bagged and allowed to dry for about 4-6 hours. Production varies between 15 and 18
metric tons per hectare,
when the tubers are weighted 4-6 hours after washing, and in rare occasions, it can reach
22 metric tons per hectare. Dry weight is about 60% of the initial weight.
Studies at Valencia have shown that the substrate texture has a bearing on the type of tubers
that are likely to develop in a chufa crop. Sandy substrates produces tubers of larger
size than those produced in other substrates. However, there is little difference on the total
weight of tubers under various types of substrates.
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6.6. Strategies for the Ojos Negros Valley
6.6.1. Botanical description
The botanical description corresponds to the species Cyperus esculentus collected in
the valleys of Ojos Negros,
Maneadero and La Trinidad. The description of Cyperus rotundus is not included
because the field samples did not show
differences, being all Cyperus esculentus.
The genus Cyperus esculentus is an annual or perennial with flowers of various arrangements,
frequently in compound inflorescences
sustained by bracts resembling leaves.
Its plants generally have rizomes, the plants are not dioic (with both sexes in the same plant),
perfect flowers,
stems generally rooted from the base of the inflorescence, even though in contact with the soil;
rhizomes with presence of tubers, fruits
of 1.5 to 1.8 mm of length, of brown-grayish color, shiny; thin scales,
reddish, acute; the tubers of more than 1 cm diameter.
The height of this plant in the region is from 30 to 60 cm.
Yellow nutsedge is found close to arroyos and channels, and its flowering is from June to October.
In the northwestern region of Baja California, it is known as "coquillo,"
which competes with high-yield irrigated crops.
It is considered a weed, and is subject to control with herbicides with little success.
6.6.2. Affected producers
The following table shows a list of agricultural producers (ejidatarios) in the Ojos Negros valley,
whose parcels are affected with the coquillo weed.
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6.6.3. Field observations
The following observations have been made after several field inspections:
6.6.4. Bromatological analysis A sample of Cyperus esculentus was taken to the UABC Laboratory of Animal Nutrition in Mexicali for a bromatological analysis. The results are shown in the following table. |
| Table 11. Bromatological analysis of yellow nutsedge. | |||||||
| Sample | Dry material % | Moisture % | Volatile extract % | Protein % | Ash % | Fiber % | Free Extract of Nitrogen % |
| Cyperus esculentus | 89.09 | 11.91 | 4.82 | 5.94 | 3.45 | 9.60 | 63.56 |
| Laboratorio de Nutrición Animal, UABC Mexicali | 02 August 2002 |
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6.6.5. Control strategies
The research has determined that the coquillo is a weed that thrives in irrigated lands such as those of the Ojos Negros valley, in sandy soils, and that it is a crop which is difficult to kill by mechanical or chemical means. The research has also revealed a potential for a positive use of the coquillo tubers as food for animals and humans. The tubers have been effectively used as pig feed, and for feeding wildlife such as cranes and wild turkeys. An alternative use of the yellow nutsedge, which holds promise for the Ojos Negros valley, is the marketing of the coquillo tubers for the preparation of the horchata drink ("horchata de chufas"). This will require a change in the local attitude toward coquillo, from a weed to a beneficial plant. Research is needed to explore the possibility of applying this concept in the Ojos Negros valley, and in neighboring valleys such as the Maneadero valley, near Ensenada, and the Trinidad valley. The extent of the coquillo infestation in these valleys appears to be greater than in the Ojos Negros valley.
6.6.6. Interviews with affected producers
In June 2002, the affected producers (listed in section 6.1) were interviewed
to gather their perceptions on the
causes, extent, and strategies to deal with the coquillo problem.
Thirteen interviews were conducted with
owners (ejidatarios) and renters.
A summary of the responses is given below.
Most affected producers attribute the presence of coquillo to
land or machinery rental; some point out that the coquillo has been brought in
with seed mix for pasture.
There appears to be a strong link between the presence of coquillo
and the cultivation of green onions (cebollin).
Propagation is aided by the sharing of equipment and dispersion by animals (birds or groundhogs).
Vegetable crops are most affected by coquillo; these include
green onions, onions, hot peppers, tomatillo, beans, watermelon,
melon, and pumpkin. Among the affected crops, the green onion
shows the greatest vulnerability, competing very poorly with the coquillo.
Taller and denser crops such as
alfalfa, wheat, tall grass and prairie grass are not as vulnerable because
they tend to shade the coquillo, inhibiting its growth.
Farmers who have rented their fields to the agricultural companies
(Agroindustrias Vigor, Estrella Nueva,
Agricola el Sol and Agricola el Toro)
have reported coquillo infestations in the years following the rental period.
It appears that the companies are shying away
from continuing to rent infested parcels.
The coquillo has been recognized as a problem in the valley for the past 6 years,
but some have mentioned longer periods,
up to 16 years. Most people interviewed agree that the extent of coquillo infestation
has been increasing, while consistently being fought with
cultural practices and other means, including mechanical and chemical. In general, the affected producers
are not aware of the type of coquillo, although the evidence suggests that the yellow
nutsedge predominates over the purple nutsedge.
The extent of the
infestation varies from moderate to severe, typically ranging from 10% to 30% of aerial
coverage. In some fields, the infestation
appears in dense patches, while in others it covers most of the field with low density.
One particular parcel
close to a packing plant was severely infested, with the coquillo seen in patches
as well as distributed throughout the land.
In two cases the infestation was minimal, being restricted to small areas.
The affected producers have tried to control the coquillo in many ways.
Some have used herbicides like Bueno 6, Dual, Gramopol and
Sempra, but these herbicides provide a temporary solution and do not
eliminate the tuber. The herbicides tend to kill only the aerial part of
the coquillo and are expensive and inefficient. Nonetheless, the majority of the
producers will keep using this strategy for lack of a better
alternative. A solution that has been tried is to rest the field for
one year or more in an attempt to kill the tuber. Manual and mechanical
removal of the aerial parts is a common way to attack the coquillo,
but it increases the cost of operation, reducing profits. Infested
parcels are being weeded mechanically to discourage and eliminate
competition with the planted crop. A novel approach consists of
removing a depth of soil, say 30-50 cm, when the infested area is
new and of limited extent; the extracted soil is quarantined and the
field is then leveled for cultivation. Little if any support
has been forthcoming from the various levels of government to
control the coquillo weed.
The use of pigs to dig out and eat the tubers has been recognized,
but there are some drawbacks, including the unsanitary conditions
and the apparent impracticality of the procedure; two of the producers interviewed
recognized this alternative as a solution.
Solarization is expensive, it has not been tried, and there is no experience with it.
The affected producers were suprised when told that the coquillo is grown
commercially in other parts of the world.
Reactions ranged from positive to negative.
A few farmers wholeheartedly supported the concept of growing coquillo as a crop,
if further research clarified its
feasibility and if the economic benefits
could be clearly defined. Other farmers tended to regard the coquillo more as a
menace than anything else, and were
reluctant to consider it as a crop.
More research is recommended on this issue.
6.7. Summary
The following conclusions are derived from this study:
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7. RESEARCH FINDINGS: DROUGHT
7.1. Definition of Drought
Drought is a weather-related natural disaster.
It affects vast regions for months or years. It has an impact on food production
and it reduces life expectancy and the economic performance of large regions or entire countries.
Drought is a recurrent feature of the climate. It occurs in virtually
all climatic zones, and its characteristics vary significantly among regions.
Drought differs from aridity in that drought is temporary; aridity is a permanent
characteristic of regions with low rainfall.
Drought is an insidious hazard of nature.
It is related to a deficiency of precipitation over an extended period of time, usually for a season or more.
This deficiency results in a water shortage for some activity, group, or environmental sector.
Drought is also related to the timing of precipitation.
Other climatic factors such as high temperature,
high wind, and low relative humidity are often associated with drought.
Drought is more than a physical phenomenon or natural event.
Its impact results from the relation between a
natural event and demands on the water supply, and it is often exacerbated by human activities.
The experience from droughts has underscored the vulnerability of
human societies to this natural hazard.
Drought definitions are of two types: (1) conceptual, and (2) operational.
Conceptual definitions help understand the meaning of drought and its effects.
For example, drought is a protracted period of deficient precipitation which causes extensive
damage to crops, resulting in loss of yield.
Operational definitions help identify the drought's beginning, end, and degree of severity.
To determine the beginning of drought,
operational definitions specify the degree of departure from the precipitation average
over some time period. This is usually accomplished
by comparing the current situation with the historical average. The threshold
identified as the beginning of a drought (e.g., 75% of average precipitation over a
specified time period) is usually established somewhat arbitrarily.
An operational definition for agriculture may compare daily
precipitation to evapotranspiration to determine the rate of soil-moisture
depletion, and express these relationships in terms of drought effects on plant behavior.
Operational definitions are used to analyze drought frequency,
severity, and duration for a given historical period.
Such definitions, however, require weather data on hourly, daily, monthly, or other time
scales and, possibly, impact data (e.g., crop yield). A climatology of
drought for a given region provides a greater understanding
of its characteristics and the probability of recurrence at various levels of severity.
Information of this type is beneficial in the formulation of mitigation strategies.
The various types of droughts are listed below.
Meteorological drought is defined on the basis of the degree of dryness, in comparison to a normal or average amount, and the duration of the dry period. Definitions of meteorological drought must be region-specific, since the atmospheric conditions that result in deficiencies of precipitation are highly region-specific. The variety of meteorological definitions in different countries illustrates why it is not possible to apply a definition of drought developed in one part of the world to another. For instance, the following definitions of drought have been reported:
Data sets required to assess meteorological drought are daily rainfall information, temperature, humidity, wind velocity and pressure, and evaporation.
Agricultural drought links various characteristics of meteorological drought to agricultural impacts,
focusing on precipitation shortages, differences between actual and
potential evapotranspiration, soil-water deficits,
reduced groundwater or reservoir levels, and so on.
Plant water demand depends on prevailing weather conditions,
biological characteristics of the specific plant, its stage of growth, and
the physical and biological properties of the soil.
A good definition of agricultural drought should account for the
susceptibility of crops during different stages of crop development.
Deficient topsoil moisture at planting may hinder germination,
leading to low plant populations per hectare and a reduction of yield.
Data sets required to assess agricultural drought are soil texture, fertility and soil
moisture, crop type and area, crop water requirements, pests and climate.
Hydrological drought refers to a persistently low discharge and/or volume of
water in streams and reservoirs, lasting months or years.
Hydrological drought is a natural phenomenon, but it may be exacerbated by human activities.
Hydrological droughts are usually related to meteorological droughts,
and their recurrence interval varies accordingly. Changes in land use and
land degradation can affect the magnitude and frequency of hydrological droughts.
Data sets required to assess hydrological drought are surface-water area and volume,
surface runoff, streamflow measurements, infiltration, water-table fluctuations, and aquifer
parameters.
Socioeconomic definitions of drought associate the supply and demand of some
economic good with elements of meteorological,
hydrological, and agricultural drought. It differs from the other types
of drought in that its occurrence depends on the processes of supply and demand.
The supply of many economic goods, such
as water, forage, food grains, fish, and hydroelectric power, depends on the weather.
Due to the natural variability of climate,
water supply is ample in some years, but insufficient to meet human and environmental
needs in other years.
Socioeconomic drought occurs when the demand for an economic good exceeds the supply as a result of a
weather-related shortfall in water supply.
The drought may result in significantly reduced hydroelectric power production
because power plants were dependent on streamflow rather than storage for power generation. Reducing hydroelectric power
production may require the government to convert to more
expensive petroleum alternatives, and to commit to stringent energy conservation measures to
meet its power needs.
The demand for economic goods is increasing as a result of
population growth and economic development.
The supply may also increase because of improved production efficiency, technology,
or the construction of reservoirs. When both supply and demand increase,
the critical factor is their relative rate of change. Socioeconomic drought is
promoted when the demand for water for economic activities far exceeds the supply.
Data sets required to assess socioeconomic drought are human and animal population
and growth rate, water and fodder requirements, severity of crop failure, and industry type
and water requirements.
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7.2. Impacts of Drought
Drought produces a complex web of impacts that spans many sectors of the economy and reaches well beyond the area experiencing physical drought. This complexity exists because water is integral to society's ability to produce goods and provide services. Impacts are commonly referred to as direct and indirect. Direct impacts include reduced crop, rangeland, and forest productivity, increased fire hazard, reduced water levels, increased livestock and wildlife mortality rates, and damage to wildlife and fish habitat. The consequences of these direct impacts illustrate indirect impacts. For example, a reduction in crop, rangeland, and forest productivity may result in reduced income for farmers and agribusiness, increased prices for food and timber, unemployment, reduced tax revenues because of reduced expenditures, foreclosures on bank loans to farmers and businesses, migration, and disaster relief programs. The types of drought impacts are described below.
Many economic impacts occur in agriculture and related sectors, because of the reliance of these sectors on surface and groundwater supplies. In addition to losses in yields in both crop and livestock production, drought is associated with insect infestations, plant disease, and wind erosion. The incidence of forest and range fires increases substantially during extended periods of droughts, which in turn places both human and wildlife populations at higher levels of risk. Income loss is another indicator used in assessing the impacts of drought. Reduced income for farmers has a ripple effect. Retailers and others who provide goods and services to farmers face reduced business. This leads to unemployment, increased credit risk for financial institutions, capital shortfalls, and eventual loss of tax revenue for local, state, and federal governments. Prices for food, energy, and other products increase as supplies are reduced. In some cases, local shortages of certain goods result in importing these goods from outside the drought-stricken region. Reduced water supply impairs the navigability of rivers and results in increased transportation costs because products must be transported by alternative means. Hydropower production may also be significantly affected.
Environmental losses are the result of damages to plant and animal species, wildlife habitat,
and air and water
quality, forest and range fires, degradation of landscape quality, loss of biodiversity,
and soil erosion. Some of
these effects are short-term, conditions returning to normal following the end of the drought.
Other environmental effects last for some time and may even become permanent.
Wildlife habitat, for example, may be degraded through the loss
of wetlands, lakes, and vegetation. However, many species eventually recover from
this temporary aberration.
The degradation of landscape quality, including increased soil erosion, may lead to a
more permanent loss of biological productivity.
Social impacts involve public safety, health, conflicts between water users,
reduced quality of life,
and inequities in the distribution of impacts and disaster relief. Many of the
impacts identified as economic
and environmental have social components as well. Population migration is a
significant problem in many
countries, often stimulated by a greater supply of food and water elsewhere.
Migration is usually to urban
areas within the stressed area, or to regions outside the drought area.
Migration may even be to adjacent countries.
When the drought has abated, the migrants seldom return home, depriving rural
areas of valuable human resources. The drought migrants
place increasing pressure on the social infrastructure of the urban areas,
leading to increased poverty and social unrest.
7.3. Characteristics of Drought
The characteristics of droughts are expressed in terms of: (1) drought index,
(2) intensity-duration-frequency.
7.3.1. Drought Index
A drought index assimilates thousands of data on rainfall, snowpack,
streamflow and other water-supply indicators into a comprehensible picture.
A drought index is typically a single number,
far more useful than raw data for decision making.
There are several indices that measure how much precipitation for a given
period of time has deviated
from historically established norms.
Some indices are better suited than others for certain uses. For example,
the Palmer Drought Severity Index (PDSI) has been widely used by the U.S. Department
of Agriculture to determine
when to grant emergency drought assistance. The PDSI is better suited for
large areas with uniform topography.
Western states, with mountainous terrain and the resulting complex regional
microclimates, find it useful to supplement the PDSI with other indices
such as the Surface Water Supply Index (SWSI),
which takes snowpack and other unique conditions into account.
The National Drought Mitigation Center is using a new index, the Standardized
Precipitation Index (SPI),
to monitor moisture-supply conditions. The distinguishing features of this index are
that it identifies emerging droughts months sooner than the Palmer Index, and that it is computed on
various time scales.
Most water-supply planners find it useful to evaluate one or more indices before making a decision.
Important drought indices used in the United States and elsewhere (Australia) are detailed below.
The percent of normal precipitation is the ratio of actual to normal precipitation for a given location
and a given period, expressed as a percentage.
Analyses using the percent of normal are effective when used for a single
region and a single season.
In other applications, the index can vary depending on the choice of period,
including monthly, seasonal, or annual.
The Standardized Precipitation Index (SPI) was developed in the understanding that a certain deficit of precipitation has different impacts on the soil moisture, ground water, reservoir storage, snowpack, and streamflow. The SPI was designed to quantify the precipitation deficit for multiple time scales. These time scales reflect the impact of drought on the availability of the various types of water resources. Soil moisture conditions respond to precipitation anomalies on a relatively short scale, while ground water, streamflow, and reservoir storage reflect long-term precipitation anomalies. For these reasons, the SPI was originally calculated for 3-, 6-,12-, 24-, and 48-month time periods. The SPI is an index based on the precipitation record for a location and chosen period (months or years). The record is fitted to a probability distribution which is then transformed into a normal distribution so that the mean SPI for the location and period is zero. The index is negative for drought and positive for non-drought conditions. Table 12 shows a classification system linking SPI's with drought intensities. A drought event occurs any time the SPI is continuously negative and reaches an intensity less than or equal to -1.0. The event ends when the SPI becomes positive. Each drought event has a duration defined by its beginning and end, and an intensity for each month that the event lasts. The sum of the SPI's for all the months within a drought event is the drought magnitude. |
| 2.0 or more | Extremely wet |
| 1.5 to 1.99 | Very wet |
| 1.0 to 1.49 | Moderately wet |
| -0.99 to 0.99 | Near normal |
| -1.0 to -1.49 | Moderately dry |
| -1.5 to -1.99 | Severely dry |
| -2.0 and less | Extremely dry |
In 1965, Palmer developed an index to measure the departure of the moisture supply. Palmer based his index on the supply-and-demand concept of the water-balance equation, taking into account the precipitation deficit. The objective of the Palmer Drought Severity Index (PDSI) is to provide standardized measurements of moisture conditions, so that comparisons can be made between locations and between durations. The PDSI is a meteorological drought index that is responsive to abnormal weather conditions, either on the dry or wet side. For example, when conditions change from dry to normal or wet, the drought measured by the PDSI ends without taking into account streamflow, lake and reservoir levels, and other long-term hydrological aspects. The PDSI is calculated based on precipitation and temperature data, as well as the local Available Water Content (AWC) of the soil. From the inputs, all the basic terms of the water balance equation can be determined, including evapotranspiration, soil recharge, runoff, and moisture loss from the surface layer. Human impacts on the water balance, such as irrigation, are not considered. Palmer developed the PDSI to include the duration of a drought or a wet spell. An abnormally wet month in the middle of a long-term drought should not have a major impact on the index, or a series of months with near-normal precipitation following a serious drought does not mean that the drought is over. Therefore, Palmer developed criteria for determining when a drought or a wet spell begins and ends, and to adjust the PDSI accordingly. In near-real time, Palmer's index is no longer a meteorological index but becomes a hydrological index, properly referred to as the Palmer Hydrological Drought Index (PHDI). This index is based on moisture inflow (precipitation), outflow, and storage, and does not take into account the long-term trend. |
| 4 or more | Extremely wet |
| 3.0 to 3.99 | Very wet |
| 2.0 to 2.99 | Moderately wet |
| 1.0 to 1.99 | Slightly wet |
| 0.5 to 0.99 | Incipient wet spell |
| 0.49 to -0.49 | Near normal |
| -0.5 to -0.99 | Incipient dry spell |
| -1.0 to -1.99 | Mild drought |
| -2.0 to -2.99 | Moderate drought |
| -3.0 to -3.99 | Severe drought |
| -4.0 or less | Extreme drought |
The Surface Water Supply Index (SWSI) complements the Palmer Index for moisture condition. The Palmer Index is basically a soil-moisture algorithm calibrated for relatively homogeneous regions. It is not designed for large topographic variations across a region and it does not account for snow accumulation and subsequent runoff. The SWSI was designed to be an indicator of surface water conditions, including mountain snowpack. The objective of the SWSI is to incorporate both hydrological and climatological features into a single index resembling the Palmer Index, and applicable to major river basins. The SWSI values are standardized to allow comparisons between basins. Four inputs are required: snowpack, streamflow, precipitation, and reservoir storage. The SWSI is dependent on the season; therefore, it is computed with only the snowpack, precipitation, and reservoir storage in the winter. During the summer months, streamflow replaces snowpack as a component of the SWSI. The procedure to determine the SWSI for a particular basin is as follows. Monthly data are collected and summed up for all precipitation stations, reservoirs, snowpack and streamflow measuring stations across the basin. Each summed component is normalized using a frequency analysis gathered from a long-term data set. The probability of nonexceedence is determined for each component based on the frequency analysis. This allows comparisons of the probabilities between the components. Each component has a weight assigned to it depending on its typical contribution to the surface water within that basin. These weighted components are summed to determine a SWSI value representing the entire basin. Like the Palmer Index, the SWSI is centered on zero and has a range between -4.2 and +4.2.
The Reclamation Drought Index (RDI) was developed as a tool for defining
drought severity and duration, and for predicting the beginning
and end of a drought period.
As with the SWSI, the RDI is calculated at a river basin level.
It incorporates the supply components of precipitation, snowpack, streamflow,
and reservoir levels. The RDI differs from the SWSI in that it builds a temperature-based
demand component and a duration into the index. The RDI is
adaptable to each particular region and its main strength is its ability to account for
both climate and water supply factors. As shown in Table 14, the RDI values and severity designations
are similar to the SPI, PDSI, and SWSI.
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| 4 or more | Extremely wet |
| 1.5 to 4 | Moderately wet |
| 0 to 1.5 | Normal to mild wetness |
| 0 to -1.5 | Normal to mild drought |
| -1.5 to -4 | Moderate drought |
| -4 or less | Extreme drought |
Another drought-monitoring technique consists of arranging the monthly precipitation data into deciles. This technique was developed to avoid some of the weaknesses of the "percent-of-normal" approach. The technique divides the distribution of occurrences over a long-term precipitation record into tenths of the distribution. Each of these categories is a "decile." The first decile is the rainfall amount not exceeded by the lowest 10% of the precipitation occurrences. The second decile is the precipitation amount not exceeded by the lowest 20% of occurrences. These deciles continue until the rainfall amount identified by the tenth decile is the largest precipitation amount within the long-term record. By definition, the fifth decile is the median, and it is the precipitation amount not exceeded by 50% of the occurrences over the period of record. The deciles are grouped into five classifications. |
| Deciles 1-2 Lowest 20% | Much below normal |
| Deciles 3-4 Next lowest 20% | Below normal |
| Deciles 5-6 Middle 20% | Near normal |
| Deciles 7-8 Next highest 20% | Above normal |
| Deciles 1-10 Highest 20% | Much above normal |
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7.3.2. Intensity-duration-frequency relations
The relations between drought intensity, duration and frequency can be
studied with conceptual models, which deal with meteorological droughts lasting at least one year,
with specific applicability to subtropical and midlatitudinal regions.
The climate types are defined across the climatic spectrum
in terms of the ratio
of mean annual precipitation to annual global terrestrial precipitation
Pma/Pagt , and additionally,
on the ratio of annual potential evapotranspiration to mean annual precipitation
Eap/Pma. To complete the description, the length
of rainy season Lrs across the climatic spectrum is also indicated.
For any year with precipitation P,
drought intensity is defined as the ratio of the deficit (Pma - P)
to the mean (Pma) .
For drought events longer than one year, intensity is the summation of the annual intensities.
The conceptual model of drought intensity-duration-frequency is shown in Table 16.
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7.4. Drought Mitigation
Drought is a natural hazard, it has a slow onset, and it evolves over months or even years. It may affect a large region and causes little structural damage. The impacts of drought can be reduced through preparedness and mitigation. The components of a drought preparedness and mitigation plan are the following:
Prediction can benefit from climate studies which use coupled ocean/atmosphere models, survey of snow packs, anomalous circulation patterns in the ocean and atmosphere, soil moisture, assimilation of remotely sensed data into numerical prediction models, and knowledge of stored water available for domestic, stock, and irrigation uses. Monitoring exists in countries which use ground-based information such as rainfall, weather, crop conditions and water availability. Satellite observations complement data collected by ground systems. Satellites are necessary for the provision of synoptic, wide-area coverage. Impact assessment is carried out on the basis of land-use type, persistence of stressed conditions, demographics and existing infrastructure, intensity and areal extent, and its effect on agricultural yield, public health, water quantity and quality, and building subsidence. Response includes improved drought monitoring, better water and crop management, augmentation of water supplies with groundwater, increased public awareness and education, intensified watershed and local planning, reduction in water demand, and water conservation. Drought preparedness and mitigation can be accomplished with the following practices:
7.4.1. Soil and water conservation
Conservation practices minimize the disruption of the soil's
structure, composition and natural biodiversity, thereby reducing
erosion and soil degradation, surface runoff, and water pollution.
The following are established practices of soil and water conservation:
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Soil and water conservation can be approached through agronomic and engineering measures.
Agronomic measures include contour farming, off-season tillage, deep
tillage, mulching and providing vegetative barriers on the contour. These measures
prevent soil erosion and increase soil moisture.
Engineering measures differ with location, slope of the land, soil type, and amount and intensity of rainfall. Measures commonly used are the following:
These features prevent soil erosion and obstruct the flow of runoff. The retained water increases soil moisture and recharges the groundwater.
Check dams are temporary structures constructed with locally available materials. Types of check dams are the brush-wood dam (Fig. 2 a), the loose-rock dam (Fig. 2 b) and the woven-wire dam.
These features store water for livestock and recharge the groundwater. They are constructed by excavating a depression to form a small reservoir, or by constructing an embankment in a natural ravine or gully to form an impoundment. Water-supply projects can also be implemented for drought mitigation, with a view to strengthen drought preparedness. Activities such as water-use planning, rain-water harvesting, runoff collection using surface and underground structures, improved management of channels and wells, exploration of additional water resources through drilling and dam construction, are implemented as a part of a drought-mitigation plan. To increase moisture availability, the following in-situ moisture-conservation practices can be adopted:
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Farmers can prepare for drought by developing plans which cover all
aspects of farm management and take into account variable climatic conditions.
Sustainable strategies
include appropriate fencing to control overgrazing,
pest-control measures,
planting drought-resistant crops and pasture,
stabilization of eroded soils,
pruning plants to reduce leaf area,
removing weak plants and thinning dense beds to reduce competition,
and the protection of native plant species.
7.4.2. Herd management
Herd management is an important strategy for drought mitigation.
Factors to be considered include the expected drought duration,
the current water and feed supplies,
the composition and body condition of the herd,
and the financial resources available.
Herd management practices include the following:
When feed resources are getting short, one solution is to critically evaluate the members
of the herd and eliminate those that are less useful.
Sale or agistment (relocating herd to non-affected pastures)
are the two options available to reduce stock numbers.
During a drought, the production of milk rapidly depletes a cow's body reserves, while
the calf derives little benefit.
Weaning the calf gives the cow a better chance of survival.
However, the decision to wean must be made in relation to the time of year and age of the calf.
In normal years, the nutritive value of pasture falls towards the end of autumn, at which time,
beef cows may be producing as little as 1 liter of milk per day. If the calf is 5 to 6 months of age,
weaning by the end of autumn will maintain or improve the cow's condition.
In drought years, early weaning is recommended.
However, calves should not be weaned before 3 months of age unless absolutely necessary.
Young calves need to be fed some true protein meal or preferably milk powder.
Most calves over three months of age will survive on grain and Lucerne hay
or molasses and protein meal diets.
Segregating animals into classes gives the herd a better chance of getting needed feed supplies.
Segregation makes possible the preferential treatment of vulnerable classes.
The older dry cows can be moved to the poorer forage fields.
Pregnancy testing is a useful tool to identify heavily pregnant cows for special feeding,
especially young cows that are pregnant for a second time.
Cattle under nutritional and other stresses are less resistant to parasites than in normal
conditions. Worms can be a serious problem with young cattle. During drought conditions,
all cattle under 18 months of age should be treated for worms.
Cattle do not graze well areas located far away from watering points.
Use of a drought-affected paddock can be encouraged by providing local water facilities,
with supplementary hand feeding as an attractant.
Polluted surface waters represent a death trap for drought-weakened cattle.
Fencing may be necessary to separate cattle from undesirable water holes.
Salinity may increase with the depletion of the water table,
with the water becoming too salty for the herd.
The upper limit of total soluble salts should not exceed 8500 ppm.
In addition, the sum of chlorides and sulphates of calcium and magnesium should not exceed 1400 ppm.
Potential problems arising from drought conditions are:
7.5. Strategies for the Ojos Negros Valley
The Ojos Negros valley is located in the state of Baja California, Mexico, approximately 40 km east of Ensenada,
along the Mexico 3 highway (Fig. 4).
The valley has an arid climate, with rainy season in the winter (November to April) and extreme temperature variability.
Agriculture and animal husbandry are the primary economic activities in the valley. The valley has approximately
3100 ha under irrigation and about 5000 head of cattle.
Irrigated agriculture is supported by groundwater;
however, a sizable portion of the total cultivated area is operated by
dryland farming, and consequently, it is subject to droughts. Droughts are a recurrent feature
of the landscape, primarily affecting the dryland farming and related animal-husbandry operations.
The climatological records for ten (10) stations located in Baja California, in the vicinity of the Ojos Negros valley,
were analyzed to establish drought intensity-duration-frequency relations.
The results of the analysis are shown in Table 17.
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While the average drought intensity for all stations is 0.83 (moderate), the intensity at Ojos Negros is 1.23 (severe). This shows that drought intensity is likely to be severe in the immediate vicinity of the Ojos Negros valley, while remaining moderate for the rest of the study region. When the data is taken all together, 48% of the drought events are moderate (intensity less than 0.625), 34% are severe (intensity between 0.625 and 1.25), and 18% are extreme (intensity greater than 1.25). Average drought duration is 2 yr at Ojos Negros, and 2.46 yr for the region. Average drought frequency is 3.54 yr at Ojos Negros, and 3.96 yr for the region. It is concluded that droughts in the Ojos Negros valley and vicinity are likely to be moderate to severe, to recur every 4 yr, and to last about 2 yr. Strategies for coping with droughts in the Ojos Negros valley include drought preparedness and mitigation. The following strategies have been identified:
7.5.1. Herd management
In principle, herd numbers should be related to the climate. The local climate is subject to variability, and the dry periods
(droughts) may last more than one year. In the Ojos Negros valley in particular, drought is likely to be moderate to severe,
last 2 yr, and recur every 4 yr. Therefore, ranchers must consider this climatic constraint
when planning the size of their herds. In general, herds should expand during
periods of wet weather, and contract during drought periods. Forecasting the climate on an annual basis is the responsibility
of the national water agency.
During a drought, the herd manager should evaluate the members of the herd to eliminate the inefficient individuals.
The herd size should be reduced to a number that can be supported by the available resources.
The physical attributes of the individual animals should be evaluated critically.
Animals with bad physical attributes or diminished reproduction ability should be considered for culling.
The replacement heifer crop should be critically evaluated.
In a drought year, the minimum number of heifers should be retained, and the rest should be sold.
Bull should be evaluated to select those that are getting old and in need of replacement.
Old bulls should be eliminated during drought years, and replaced as soon as practicable.
All cattle are affected by a host of internal and external parasites. Cattle under nutritional
and heat stress are less resistant to parasites than under normal conditions.
Strategic deworming during a drought will relieve some of the nutritional stress on the animals.
Heifers and calves are not able to compete with mature cattle for pasture or supplemental feed.
Drought feed is costly and it is important to feed only those animals who really need it.
Segregating animals gives each class a better chance of getting needed feed supplies.
Vulnerable classes can be segregated and given preferential treatment.
The older dry cows can be moved to the poorer forage fields.
Contract grazing or renting pasture is another drought strategy.
However, the cost of hauling or renting the pasture should not be more than the cost of purchasing feed.
Use of a drought-affected paddock can be optimized by providing local water facilities and supplemental hand feeding.
7.5.2. Conservation practices
Water retention and detention structures capture storm-water runoff which can be used
for a variety of purposes, including groundwater recharge, irrigation, and drinking water
for livestock.
Windbreaks and shelterbelts help in reducing wind velocity and, therefore,
evaporation and evapotranspiration, aiding in coping with drought.
Rainwater harvesting can be accomplished for immediate or eventual use in irrigation or drinking water for livestock.
Landscape contouring and terracing can be implemented where feasible to reduce runoff and direct excess moisture
into areas planted with trees, shrubs, and grass.
7.5.3. Interviews with local actors
During June 2002, several interviews were performed with local cattle ranchers.
The interviews sought to collect perceptions about drought, drought characteristics,
and drought mitigation, to serve as a basis for the development of policy.
Most people interviewed said that rain appears to have have been steadily decreasing.
Some ranchers observed that in the 1950's it rained all-year round and
the pastures were always green.
Since the 1970's, drought appears to have intensified.
Rain was plentiful in 1978, 1981, 1992 and 1998.
In other years, rain has been limited, and some years have not had any rain.
Ranchers do not consult outside sources (i.e., weather agencies) to learn whether is it going to rain or not.
They feel reluctant to ask these sources because they feel they could be wrong.
The ranchers agree that there is a recurrence interval between the drought years
and the rainy years, but the periodicity of the cycle is unknown. Some say the rainy periods
last from 4 to 7 yr, while the drought periods last from 2 to 4 yr. Yet others
believe that drought recurs every 4 yr on the average.
Furthermore, there are those that believe that even years are rainy while odd years are dry.
During drought years, there is not enough moisture for normal dryland pasture growth.
Irrigation is an option for those that can rely on groundwater, and this is typically the case of
Ojos Negros; but those ranchers which have no wells or small wells are significantly affected by drought.
Herd reduction to 50% or less is a common strategy to cope with drought. Some ranchers move their cattle to
rented land, while others are forced to purchase hay to feed their lot.
The last resort is to undersell the herd, with consequent loss of profitability.
When selecting the cattle to be sold or removed, farmers usually go first for the older animals,
then they separate the newborn herd to reduce competition for food.
Other drough-related effects are fires, erosion and groundwater depletion.
The Comisión Nacional del Agua (National Water Commission) has supplied farmers with statistical facts,
seminars and some additional help. SAGARPA and other government agencies have subsidized the shipping of hay from Mexicali to Ojos Negros
during droughts.
Retention walls, or structures such as dykes or dams, as well as natural obstructions to runoff
are yet to be used to retain precious water during drought.
Water reservoirs are an option, but water would be retained only for a limited amount of time.
Most ranchers believe that it is important to ration the water supply;
otherwise, the valley is going to eventually lose its economic potential.
7.6. Summary
The following conclusions are derived from this study:
8. CONCLUSIONS
The following conclusions are obtained from this study:
8.1. Sand Mining
8.2. Coquillo
8.3. Drought
9. RECOMMENDATIONS FOR FURTHER RESEARCH
The following recommendations are offered for further research:
10. RESEARCH BENEFITS
The following research benefits have been identified:
11. ACKNOWLEDGMENTS
The authors wish to acknowledge the assistance of the following persons:
12. REFERENCES
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