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OCR for page 46
Irrigation Today
Less than 1 percent of the nation's farmland was irrigated in 1900, but by
1982 irrigation accounted for 1 of every 8 acres under cultivation and nearly $4 of
every $10 of the value of crop production (U.S. Department of Agriculture,
1986~. This transition was driven by economic change: in the late nineteenth
century, western promoters turned to irrigation when mining, open range cattle,
and dry farming economies proved unable to sustain western settlement (Webb,
1931~. During this period, foundations were laid to support irrigation water
rights laws, advances in engineering, mutual water district organization and fi-
nancing and these supported early irrigation in areas such as California, Colo-
rado, and Utah. However, irrigation did not begin to expand rapidly until after
Congress passed the Reclamation Act of 1902, which established the Reclama-
tion Service (now the Bureau of Reclamation) to assist in developing the West
through irrigation.
The federal role in water development expanded further in the 1930s as
water development was also used to create new jobs. By the end of World War II,
four federal agencies the U.S. Army Corps of Engineers, the Bureau of Recla-
mation, the Tennessee Valley Authority, and the Soil Conservation Service (now
the Natural Resource Conservation Service of the Department of Agriculture)
NOTE: There are many sources of data that describe the status of irrigation in the
United States. However, the methods used to gather and interpret statistics vary
significantly, resulting in disparities among the different sources. Because many
references and sources were used in developing this chapter, there are occasions
where values may not be fully compatible.
46
OCR for page 47
IRRIGATION TODAY
47
had expanded their roles in the use and development of water resources (National
Research Council, 1992a). After World War II, irrigated agriculture expanded
rapidly in the far West and the central Great Plains. More recently, supplemental
irrigation has become important in the East, Southeast, and Midwest. Irrigated
agriculture remained an engine of western development until the 1970s. How-
ever, increasing development costs, reduced government financing, increasing
demand for municipal and industrial water supplies, diminishing sources of water
supply, and a growing concern for the environment have forced water managers
and planners to begin rethinking traditional approaches to water management
(National Research Council, 1992b).
This chapter provides background information about the current status of
irrigation the amount of land irrigated, types of crops, water withdrawals, and
consumptive use. It gives an overview of the technologies used and the econom-
ics of irrigated systems, including water pricing and marketing. It highlights key
issues in the relationship of irrigation to the environment and introduces an
increasingly important force in the water arena: the turfgrass sector. It also
highlights another element certain to be key in the future irrigation on Indian
lands. Together, these discussions are designed to provide a quick review of
irrigation today and thus set the stage for the committee's foray into irrigation's
future. Readers already well-versed in the status and trends of irrigation today
are encouraged to proceed to Chapter 4, where the committee explores the deeper
cause and effect relationships that underlie the statistics.
IRRIGATED AGRICULTURE
Irrigated Land in Farms
Irrigated agriculture occurs on just 14.8 percent of the harvested cropland
and yet produces 37.8 percent of the value of crops (Figure 3.1~. The relatively
Irrigation accounts for
4.8% of the land in farms
(total farm acreage = 964
million acres)
Irrigation accounts for
14.8% of the total
harvested cropland (282
million acres)
Irrigation accounts for
37.8% of the total crop
value ($68.8 billion)
FIGURE 3.1 Irrigation and farm production (1987 Census of Agriculture). Source:
Bajwa et al., 1992.
OCR for page 48
48
A NEW ERA FOR IRRIGATION
arge economic contribution of irrigated agriculture can be explained by the
sigher yields obtained for irrigated crops, the tendency to irrigate high-valued
Indoor specialty crops, and the improved product quality and consistency.
In 1959, 9 percent of all farms reported some irrigated land. By 1987, that
Hare had risen to 14 percent. During the 1980s, the total number of irrigated
acres and irrigated acres per farm fluctuated considerably because of the tempo-
~ary idling of land associated with annual commodity program acreage restric-
ions. Most (90 percent) of the nation's irrigated land is harvested cropland, but
many of the mountain states irrigate pasture and land from which wild hay is cut
;o sustain livestock through the winter.
In the United States, irrigation is used mainly in the 17 western states, plus
Arkansas, Florida, and Louisiana (see Box 3.1~. These 20 states account for 91
Percent of all U.S. irrigated acreage and 82 percent of all irrigated farms. The 17
western states alone contain over 81 percent of the total irrigated land; 85 to 90
Percent of total water withdrawn in the West is used for irrigation. Although
rrigated cropland provided a substantial portion of national farm income in 1987,
here were only about 292,000 individual irrigators, 14 percent of all farmers.
Our-fifths of the irrigators were located in the 17 western states.
The drought years of the 1950s and the development of centrifugal pumps
and more economical power sources stimulated irrigation development in the
southern Great Plains, where ground water is pumped from the Ogallala aquifer.
With the advent of the center pivot sprinkler irrigation systems, and with ground
hater readily available, irrigation expanded rapidly in the central Great Plains
luring the 1960s and 1970s. Irrigation also expanded in humid southeastern
states as a way to provide dependable and timely water. In California and the
Pacific Northwest, irrigated areas also expanded during the 1950s and 1960s as
many irrigation projects constructed by the Bureau of Reclamation and local
ntities were completed and put into service. The total irrigated area essentially
stabilized in the 1980s due to a combination of low farm commodity prices,
ncreased energy costs, and declining water resources. The percent of harvested
,ropland irrigated by state is given in Figure 3.2 (Bajwa et al., 1992~.
Figure 3.3 shows trends for irrigated land in farms and water applied per acre
From share of total acreage irrigated are rice (100 percent), orchards (81 percent),
OCR for page 49
IRRIGATION TODAY
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50-79
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FIGURE 3.2 Percentage of harvested cropland irrigated by state, 1987. Source:
Bajwa et al., 1992.
vegetables (64 percent), and cotton (38 percent). Crops with the largest total
irrigated acreages are hay, corn for grain, wheat, and cotton (U.S. Department of
Agriculture, 1986~. While much smaller percentages of grain acreages are irri-
gated (e.g., 14 percent of harvested core, 13 percent of sorghum, and 7 percent of
wheat), the combination of improved yields on irrigated farms and the increase in
the relative acreage devoted to irrigation accounted for 28 percent of the national
increase in corn production, 20 percent for sorghum, and 12 percent for wheat
from 1950 to 1977 (Frederick and Hanson, 1982~.
WATER USE FOR IRRIGATION
Irrigation water typically is measured in terms of withdrawals or consump-
tive use. Withdrawals represent the amount of water diverted from a surface
source or removed from the ground. Consumptive use is a measure of water lost
to the immediate water environment through evaporation, plant transpiration,
incorporation in products or crops, or consumption by humans and livestock.
Consumptive use in agriculture is primarily crop evapotranspiration, which is
influenced heavily by climate and the types of crops irrigated. Reasonably accu
OCR for page 50
so
Million acres
50
48
~6
~8
A NEW ERA FOR IRRIGATION
Inches
r ~- ~ - - r ~ IL-e ~ _ ~ u ~-- e
of b ·, ~
l ! ~ ~ r v ~ ~ v a~_r lob #~ ~ ~-~ d~ 51~ IN- L ~ I~ ~- ~ ~
1 · I Irrigated land in farms 1/
r (left scale)
/ ~ ~ ~ a- - ~ Water applied 2/
(right scale)
36 .; B~-L l --L,-~.l., J- I - -I ,.~ ,~ ~ ~llIs ~i ~ B ~1d~4- ~l ~ . ~It~ --1~ - ~r--l--l L8
-
~8 1972 1976 1980 19~ 1988 i992 1996
I/Based on Census and annual USDA data.
21Based on FRIS and changes in state/crop area
24
FIGURE 3.3 Trends in irrigated acres between 1969 and 1993. Source: U.S.
Department of Agriculture, 1993.
rate estimates of water withdrawn for irrigation can be made if the acreage
irrigated, water application rates, and conveyance losses are known. However,
reliable estimates for consumptive use and conveyance loss are not currently
available. Thus the available estimates are rough approximations of actual condi-
tions. These estimates reflect the importance of the four influential factors: irriga-
tion technology, crop prices, annual commodity program acreage restrictions,
and weather. Relaxed acreage restrictions, improved irrigation technology, and
high crop prices in the 1970s accelerated irrigation development, increasing total
irrigated area from 38 million acres in 1972 to 52 million acres in 1981. Irrigated
OCR for page 51
51
TABLE 3.1 Irrigated Area in the United States
Region1987 (thousand acres)1992 (thousand acres)Change (%)
Alabama8482-2
Arizona9149565
Arkansas2,4062,70212
California7,5967,5710
Colorado3,0163,1705
Connecticut76-19
Delaware61622
Florida1,6231,78310
Idaho3,2193,2601
Illinois20832858
Indiana17024142
Iowa9211625
Kansas2,4632,6809
Kentucky3828-27
Maine61069
Maryland515712
Massachusetts2020-1
Michigan31536817
Minnesota3543705
Mississippi63788339
Missouri53570933
Montana1,9971,976-1
Nebraska5,6826,31211
Nevada779556-29
New Hampshire32-41
New Jersey9180-12
New York5147-8
North Carolina138113-18
North Dakota16818711
Ohio3229-9
Oregon1,6481,622-2
Pennsylvania3023-22
Rhode Island33-15
South Dakota3623713
Tennessee3837-2
Texas4,2714,91215
Utah1,1611,143-2
Vermont2216
Virginia7962-22
Washington1,5191,6418
West Virginia33-12
Wisconsin28533116
Wyoming1,5181,465-4
Total (43 states)43,67146,3196.1
Source: U.S. Department of Commerce, 1994.
OCR for page 52
52
A NEW ERA FOR IRRIGATION
acres then dipped from 1983 to 1987, primarily as a result of acreage restrictions
in commodity programs. Water applied per acre has declined from about 25
inches to less than 22 inches.
According to the 1992 Census of Agriculture (U.S. Department of Com-
merce, 1994) the total 1992 irrigated area was 46.3 million acres, up 2.6 million
acres from 1987 (Table 3.1~. During this period, there was no increase in irri-
gated acres in the West from surface water. The increase in irrigation from 1987
to 1992 occurred mostly in the Great Plains region, which relies primarily on
ground water. On the other hand, much of the East was dry in 1987, and the
return to more normal moisture levels in 1992 diminished a trend toward in-
creased irrigation in the East.
Irrigated Crops
Most major crops are irrigated to some degree, but the number of acres and
percentage of acres irrigated vary widely from crop to crop. Crops that have the
greatest estimates for consumptive use and conveyance loss are not currently
available. Thus the available estimates are rough approximations of actual con-
ditions.
Water Withdrawals
Irrigation is by far the largest consumptive water user in the United States,
particularly in the West. The quantity of water withdrawn for irrigation during
1990 was an estimated 137,000 million gallons per day, or 153 million acre-feet,
which represents 40 percent of total U.S. freshwater use for all offstream catego-
ries. Irrigation withdrawals as well as acres irrigated during 1990 were about the
same as during 1985. Water withdrawal and consumptive use information is
summarized by water resource region and by state in Tables 3.2 and 3.3, respec-
tively.
The nine western water resources regions, led by the Pacific Northwest
region, accounted for 90 percent of the total water withdrawn for irrigation during
1990 (Table 3.2~. In the eastern regions, most of the water withdrawn for irriga-
tion was in the Lower Mississippi and South Atlantic-Gulf regions, which to-
gether had about 2,400 million gallons per day more water withdrawn during
1990 than during 1985.
Most states rely on a combination of surface and ground water supplies for
irrigation purposes (see Table 3.3~. Surface water accounted for 63 percent of
total irrigation withdrawals in 1990. States with the highest share of surface
water withdrawals include California, Montana, Wyoming, Oregon, Washington,
and Utah.
Ground water is the primary supply source for irrigation in about half of the
states (Table 3.3~. Total ground water withdrawals were largest in California,
OCR for page 53
53
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OCR for page 54
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OCR for page 55
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OCR for page 56
56
A NEW ERA FOR IRRIGATION
Texas, and Idaho. Ground water as a share of irrigation withdrawals was highest
in Kansas, Mississippi, Arkansas, Oklahoma, and Nebraska. Irrigated agriculture
has contributed to declining aquifers in many areas.
In 1985, agriculture accounted for 42 percent of all freshwater withdrawals
in the United States, or a total of 141 billion gallons per day, of which 97 percent
was for irrigation and 3 percent was for livestock production. Freshwater with-
drawals for agriculture are used mainly for crop production, with 98.4 percent of
surface water and 93.8 percent of ground water used in irrigating cropland (Solley
et al., 1988).
The trend in water used for all purposes for 5-year intervals from 1950 to
1990 is shown in Table 3.4. Included are withdrawals, source of water, reclaimed
wastewater, consumptive use, and instream use (hydroelectric power). Table 3.4
also estimates the percentage increase or decrease in withdrawals between 1985
and 1990. After continual increases in the nation's water use from 1950 to 1980,
offstream and instream uses were less during 1985 than during 1980. Total
withdrawals were about 10 percent less during 1985 than during 1980, and the 2
percent increase from 1985 to 1990 is the result of increases in surface and
ground water withdrawals of 1 and 9 percent, respectively. The fact that the 1990
withdrawal estimates are only slightly higher than the 1985 estimates tends to
confirm the overall decline in water use from the peak of 1980.
The increase in estimated ground water withdrawals from 1985 to 1990 was
partly the result of decreased availability of surface water. Surface water with-
drawals for irrigation increased progressively for the years reported from 1960 to
1985 and decreased 6 percent from 1985 to 1990. It is expected that surface
water withdrawals in the Pacific Coast and Pacific Northwest will remain at
current levels or will decline as reallocations take place from agricultural use to
streamflow maintenance to restore anadromous fish populations.
Water application varies from about 30 inches per year for crops such as rice
and alfalfa to less than 10 inches per year for soybeans (Table 3.5~. The amounts
vary from region to region and from year to year depending on climatic condi-
tions (especially temperature), precipitation, and irrigation practices. There is no
direct annual measure of irrigation water applications, but 5 years of census and
postcensus survey data suggest some trends (U.S. Department of Commerce,
1994~. The east-west contrast in application rates has narrowed, with Atlantic
states using almost twice as much water per acre in 1988 as in 1969. Despite
increasing application rates in the East, national average application rates, as well
as application rates for several major crops, have declined.
Consumptive Use
Consumptive use of fresh water in the United States totaled about 105 mil-
lion acre-feet in 1990. Irrigation, the dominant consumptive water use, accounted
for 85 million acre-feet, or 81 percent of the U.S. total. Consumptive use as a
OCR for page 72
72
A NEW ERA FOR IRRIGATION
Instream Flows and Wetlands
Problems related to instream flows and wetland ecosystems occur in every
region of the country where significant quantities of surface and ground water are
withdrawn for irrigation. Dams and diversions for surface supplies reduce instream
flows, altering the natural hydrograph and affecting water temperature and flow
regimes, trapping sediments, and changing water quality. In addition to obstruct-
ing the passage of migratory fish, these changes degrade spawning and rearing
habitats in the stream and riparian areas. The draining and filling of wetlands for
irrigation have significant impacts on waterfowl and other aquatic species that
use these habitats for nesting and breeding and also increase the potential for
sedimentation and water pollution.
In California, for example, construction of the Friant Unit of the Central
Valley Project resulted in the dewatering of the San Joaquin River for a 50-mile
reach below Friant Dam. As a result of dams and diversions for irrigation, water
supplies available for fish and wildlife habitat have been greatly reduced. Ninety-
two percent of the historic wetland acreage in the San Joaquin Valley has been
converted to irrigated agriculture. (San Joaquin Valley Drainage Program, 1990~.
In Idaho, ground water pumping by irrigators along the Big Lost River over the
last 15 years has caused the dewatering of the lower reach of the river and
lowered ground water levels precipitously (High Country News, 1995~. Large-
scale irrigation projects constructed by the Bureau of Reclamation have drasti-
cally altered habitat conditions in major river basins across the West, including
the Platte River, the Colorado River, the Columbia River, and the Snake River.3
Many fish and other aquatic species that depend on habitat values in these rivers
are listed as threatened or endangered under federal and/or state endangered
species laws, although it must be noted that irrigation withdrawals are only one
factor among many (e.g., hydroelectric power generation) that contribute to
instream flow problems.
Salinity and Drainage
Salinity and drainage problems arise from natural hydrological and geochemi-
cal factors the earth's rocks and soils contain mineral salts, which are released
via normal chemical weathering processes. Irrigation in areas rich in such salts
can concentrate the salts in water and soils (surface evaporation and transpiration
by plants both act to move water into the atmosphere, leaving concentrated salts
behind). The major dissolved mineral salts at issue are sodium, calcium, magne-
sium, potassium, chorine, SO4, HCO3, CO3, and NO3. Over time, salts concen-
trated in soils can hinder plant germination, seeding, and growth and undermine
the yield and quality of plants. Saline drainage water can have adverse effects on
water quality and, in turn, harm wildlife populations and make the water less
desirable for other users.
OCR for page 73
IRRIGATION TODAY
73
About 30 percent of the land in the conterminous United States, much of it
concentrated in the West, has a moderate to severe potential for salinity problems
(Tanji, 1990~. The upper Colorado River basin, the northern Great Plains, and
California's San Joaquin Valley are examples of areas that suffer salinity and
drainage problems. The accumulation of salts in soils depends on the salinity of
the applied waters, the salinity of the native soil, and the rate at which salts are
leached out of the root zone. A related problem is waterlogging of the soil:
waterlogging in the root zone depends on the drainage characteristics of the soil,
whether there is a restricting layer in the soil, and the soil's capacity for deep
percolation. In poor conditions, waterlogging can occur relatively rapidly. In
good conditions, irrigation may be practiced for decades, and even centuries,
before surface drainage problems arise. Irrigation-induced salinization can be
avoided by providing adequate drainage, but drainage is expensive and exacts an
environmental price as well it degrades water quality along its disposal route
and in closed basins can render the terminus biologically uninhabitable (van
Schilfgaarde, 1990~.
Water Quality
Surface return flows and drainage from irrigation are a leading source of
water pollution in rivers, lakes, streams, and estuaries nationwide. According to
recent estimates, irrigated cropland in the West accounts for 89 percent of qual-
ity-impaired river mileage. Irrigated agriculture accounts for more than 40 per-
cent of the pollution in lakes with impaired water quality (U.S. Environmental
Protection Agency, 1992~. In the arid West, low river flows can exacerbate
pollution problems from irrigation because surface runoff and drainage often
provide a significant portion of these flows. Pollutants mobilized and transported
by irrigation return flows and drainage include naturally occurring trace elements
(e.g. selenium, boron, molybdenum), nitrogen, and salts, as well as pesticides,
herbicides, and other chemicals (U.S. Fish and Wildlife Service, 1992~. Signifi-
cantly, irrigation return flows are the most common source of pollution in na-
tional wildlife refuges (U.S. Environmental Protection Agency, 1992~. While
fewer data are available on the effects of agricultural drainage on species other
than waterfowl, agricultural runoff is believed to affect adversely fish popula-
tions in many river reaches in the country (U.S. Fish and Wildlife Service, 1992~.
The trend toward a greater public policy focus on irrigation's impact on the
environment is borne out by changes in various policies and institutions serving
both irrigation and environmental goals. The mission of the Soil Conservation
Service, now called the Natural Resources Conservation Service, has been modi-
fied and expanded over the past 50 years. It has gone from helping farmers
prevent soil erosion to conducting activities and providing technical and financial
support to farmers to conserve highly credible and environmentally sensitive
lands and protect water quality.4 In 1987 the Bureau of Reclamation, historically
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74
A NEW ERA FOR IRRIGATION
the supplier of one-fifth of all irrigation (agricultural) water in the United States
and manager of 45 percent of the West's water, announced the end of its mission
of helping to settle the West through the construction and operation of major
dams and diversions, and the beginning of a mission focused on resource man-
agement (Bureau of Reclamation, 1987~. In 1992, the Central Valley Project
Improvement Act (P.L.102-575, Title XXXIV, 106 Stat.4706) set aside 800,000
acre-feet of water previously delivered by the federal Central Valley Project to
agricultural users for fish and wildlife habitat.5 In addition, water users were
required to pay surcharges on irrigation water to be used to finance environmen-
tal restoration.
In 1987, amendments to the Clean Water Act required states to assess the
extent of nonpoint-source water quality impairment and to develop programs to
manage nonpoint-source pollution. Section 319 of the act authorized $400 mil-
lion in grants to states to assist in this effort (33 U.S.C. Section 1329~. In
addition, nonpoint-sources must be factored into the calculations that allocated
pollution reduction responsibilities among dischargers for each water body that
does not meet water quality standards (section 303; U.S.C. Section 1313~. In
1990, amendments to the Coastal Zone Management Act, administered by the
National Oceanic and Atmospheric Administration and the Environmental Pro-
tection Agency, required states with coastal zone management programs to de-
velop programs for the control of nonpoint sources, including agriculture (Coastal
Zone Act Reauthorization Amendments, 1990~.
Several states have adopted programs or passed legislation to protect aquatic
habitats and the species that depend on them. Minimum instream flow require-
ments, appropriations for instream rights, water transfer options, conservation
easements, and other mechanisms are being employed to address problems con-
cerning the quantity and quality of water available to fish and wildlife resources.
In the turfgrass sector, soil erosion and runoff during construction and the
potential for leaching and runoff of nutrients and pesticides from established sites
can lead to impacts on fish and wildlife habitats and aquatic systems. These
impacts likely will continue to fall under the urban stormwater provisions of the
Clean Water Act and sometimes state legislation.
Climate Change
The Second Scientific Assessment of Climate Change by the Intergovern-
mental Panel on Climate Change (IPCC) (1996) concludes for the first time that
a global warming attributable to human activities is now evident in the historic
record. Under a mid-range emission scenario, global mean surface temperature
relative to 1990 is expected to increase by about 2°C by 2100, when the effects of
greenhouse gas emissions and sulfate are considered.
Although beyond the time horizon that is the focus of this study, if it occurs,
greenhouse warming is certain to have a major impact on water supplies. A
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IRRIGATION TODAY
75
warmer climate would accelerate the hydrologic cycle, increasing both the rates
of precipitation and evapotranspiration. The regional impacts, however, are
highly uncertain. Regional precipitation patterns, evapotranspiration rates, the
timing and magnitude of runoff, and the frequency and intensity of storms would
be affected. But the magnitude and sometimes even the direction of the changes
for particular river basins and watersheds are uncertain. The range of likely
changes in average annual precipitation associated with an equivalent doubling
of atmospheric carbon dioxide for any given region might be on the order of plus
or minus 50 percent (Schneider et al., 1990~.
The hydrologic uncertainties are compounded because relatively small changes
in precipitation and temperature can have sizable effects on the volume and timing
of runoff, especially in arid and semiarid areas. For example, Nash and Gleick
(1993) have speculated on the estimated impacts of alternative temperature and
precipitation changes on annual runoff in several semiarid areas. In their sce-
nario, with no change in precipitation, estimated runoff in these study areas
declines by 3 to 12 percent with a 2°C increase in temperature and by 7 to 21
percent with a 4°C increase in temperature. A 10 percent increase in precipitation
does not fully offset the negative impacts on runoff attributable to a 4°C increase
in temperature in three of the five basins for which this climate scenario was
studied.
The CO2 fertilization effect will affect plant growth and possibly water sup-
plies. Research results suggest that the increasing levels of atmospheric carbon
dioxide (CO2) levels will increase the growth and yield of C3 plants (small grains,
legumes, root crops, and most trees) by 34~+/-6) percent and C4 plants (e.g.,
maize and sorghum) by 14 (+/-11) percent (Rosenberg et al., 1990~. The impacts
of the CO2 fertilization effect on water supplies is less certain because of two
counteracting effects. On the one hand, an increase in leaf and root areas has the
potential to increase transpiration and, thereby, reduce runoff. A simulation
analysis suggests that a 15 percent increase in the leaf area index (other things
being constant) would increase summertime evapotranspiration from a wheat
field in Nebraska by 5 percent. On the other hand, a rise in atmospheric CO2
levels would increase stomata! resistance, the primary plant factor controlling
evapotranspiration. Transpiration from a given leaf area declines as the stomata!
resistance rises. In another simulation of the impacts of climate variables on the
Nebraska wheat field, a 40 percent increase in stomata! resistance (other things
being equal) reduces summertime evapotranspiration by 12 percent (Rosenberg
et al., 1990~.
In summary, the prospect of a global greenhouse warming introduces major
new uncertainties and challenges for irrigators as well as for other farmers and
water users. The allocation of water supplies among competing uses in response
to any climate-induced shifts in hydrology and the response of irrigators to these
changes is likely to be an important determinant of the future of irrigation.
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76
A NEW ERA FOR IRRIGATION
THE TURFGRASS SECTOR
When precipitation is insufficient, turfgrass must be irrigated to provide the
desired turf appearance and recuperative ability. Problems arise when there is an
extended period of lack of precipitation or lack of availability of either ground
water or surface water to allow for turf irrigation. The importance of turfgrass
irrigation was most clearly realized during the drought period of 1976 to 1978 in
the western United States, when extensive damage occurred.
Although turf was commercially recognized before World War II, the rapid
growth and development of the turf industry occurred after the war. In 1965
turfgrass was a $4.3 billion industry (Turfgrass Times, 1965~. By 1992 it had
grown to a nearly $30 billion industry. The fixed asset value of turf is, of course,
many times that annual expenditure. California, Florida, Michigan, New York,
North Carolina, Pennsylvania, and South Carolina all have billion-dollar turf
industries, and Illinois and Texas are very near this level. A survey of 2,309 golf
courses in late 1984 by the Golf Course Superintendents Association of America
(GCSAA) and the National Golf Foundation (NGF) provided statistical data on
the acreage and cost of maintaining America's golf courses. Projecting the
financial data obtained from the sample, it is estimated that $1.7 billion is spent
each year for golf course maintenance and that the nation's courses had a mainte-
nance equipment inventory valued at more than $1.8 billion (Prusa and Beditz,
1985~. Even though the technology of turfgrass management has undergone
tremendous development, it is still labor intensive. It is estimated that 380,000
people make their living directly from the care and maintenance of turf in the
United States.
There are over 50 million home lawns and more than 14,000 golf courses in
this country (Schroeder and Sprague, 1994~. Water use rates for turfgrass vary
widely, from 0.1 inch per day for foggy coastal climates to 0.45 inch per day for
dry desert areas (Beard, 1982~. A golf course may require a water source capable
of supplying as much as 1.5 to 3.5 million gallons of water per week during the
golf season (Jones and Rando, 1974~.
Surface waters of all types are common direct sources of water for golf
courses and other larger turfgrass areas. Frequently, small streams and major
drainage channels may be dammed, excavated, or both, and the impounded water
used to irrigate the golf course. Small reservoirs (less than 50 acre-feet in size)
provide only 2 percent of the nation' s total storage capacity. However, they are
a significant source of water for golf courses and park areas. Water harvesting
and storage in small ponds and reservoirs are increasingly becoming a major
element in golf course design.
Treated effluent water, although not technically "surface water," is an alter-
native source of supplemental irrigation water. Because of its nutrient content, it
is a particularly valuable source of irrigation water for sod farms and golf courses.
The quality of the effluent depends on the source; therefore, it varies widely.
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IRRIGATION TODAY
77
Advantages and disadvantages are associated with use of effluent (Watson, 1978~.
Effluent water or wastewater is used to irrigate several golf courses, including the
Eisenhower Course at the Air Force Academy; Innisbrook at Tarpon Springs,
Florida; Randolph Park at Tucson, Arizona; and some military courses. Develop-
ment of multiple-plumbing systems to accommodate regular and effluent water
for turf facilities is inevitable. Many golf courses already use such systems, and
use of effluent water for golf course irrigation is mandatory in California where it
is available (Thomas, 1994~.
The availability of sufficient water of adequate quality and price in the future
will pose a challenge to the turfgrass industry. In humid and subhumid areas,
watering of home lawns often is restricted because municipal distributive sys-
tems have not kept up with the rapid expansion of suburban areas. For the same
reasons, watering of turfgrass areas may be restricted in semiarid and arid re-
gions. Alternative water sources that may be useful to the turfgrass industries
include wastewaters, including treated sewage effluents; capture and impound-
ment of runoff waters; and dual water systems for turf facilities, including home
lawns, to accommodate potable and nonpotable waters (Watson, 1985~.
THE SPECIAL CASE OF INDIAN IRRIGATION
The legal, historical, and political framework for Indian irrigation and natu-
ral resource use is rooted firmly in the history and development of the United
States. American Indians have a unique relationship with the United States
which stems from the Constitution, Treaties, Executive Orders, Court decisions,
and legislation enacted since the late eighteenth century through the present. The
body of law created by these mechanisms establishes a framework for the imple-
mentation of the U.S. trust responsibility for the protection of Indian natural
resources. As the twenty-first century approaches, the increased implementation
of these treaty rights through the development of water for agricultural or nonag-
ricultural enterprises is central to Indian economic development activity.
While much of the treaty making was completed more than a century ago, it
is only now that many of the provisions of the treaties are coming to fruition. The
securing of water supplies and other natural resources has implications for irri-
gated agriculture in the United States, particularly in the Northwest, Southwest
and Missouri River basin. Today, American Indians own 2.7 million acres of
cropland, of which 64 percent is irrigated. The total estimated income from
Indian irrigation, both in private systems and BIA-administered programs ex-
ceeds $1 billion annually.6
The development of irrigated agriculture on Indian reservations and the
forced transformation of Indian culture in the mid to late nineteenth century
formed the core development vision of U.S. policy regarding American Indians.
Reservations were set aside as homelands, whose purpose was envisioned as
agricultural. Most tribal irrigation projects were authorized congressionally. Un
OCR for page 78
78
A NEW ERA FOR IRRIGATION
der the general appropriations for irrigation authorized by Congress, the irriga-
tion systems that were built for tribes were refinements of earlier irrigation sys-
tems constructed by the tribes themselves prior to any assistance from the federal
government (Bureau of Indian Affairs, 1975~. In several instances, existing non-
Indian projects were extended to meet the needs of the Indians. While all of this
work was designed to "fulfill treaty stipulations with various Tribes," many
irrigation systems on Indian reservations were constructed, improved, or ex-
tended by the federal government without consideration as to economic feasibil-
ity and repayment capability, a fact that is common to all irrigation projects
constructed with federal funds during this century. In many cases, such projects
were constructed without the consent of the Indians involved.
Table 3.10 presents a partial listing of the 71 statutorially authorized Indian
irrigation projects. The Pick-Sloan program of the 1944 Flood Control Act also
authorized the construction of Indian irrigation projects. To date, few Indian
irrigation projects have been constructed under the Pick-Sloan program. It is
significant to note that initial appropriations authorized were in most cases not
sufficient to finish the project, nor to design the project for effective water deliv-
ery. In addition, funding did not cover routine operation, maintenance, and
replacement activities. Nearly all of these projects have serious replacement,
operations, and maintenance costs and other problems that have inhibited full
agricultural development and effective water delivery.
There are also statutorily authorized power projects in conjunction with
irrigation projects, which were established by Congress to provide power for
pumping of water to supplement gravity-flow systems on reservation. These
include Colorado River, Flathead, San Carlos, and the Wapato irrigation projects.
In addition to these formally designated projects, approximately half of the
irrigated cropland in Indian Country is irrigated by tribal individuals or tribal
government operators. Many of these systems are private ditch systems which
retain the essential character and disposition of the original design. Because of
the lack of formal funding for the operation, maintenance, and repair of these
systems, some private systems are in disrepair. Nevertheless, several Tribal
operations, such as Gila River, Navajo, Yankton, Winnebago, Standing Rock,
and Lower Brute have fully operating and sophisticated irrigation systems.
During the course of development of irrigation in Indian Country, there has
been considerable controversy over the construction, payment, and repayment of
construction costs associated with Indian irrigation projects. The controversy has
greatly affected the condition of Indian irrigation projects today. Beginning in
1914, 20 years after the Dawes Allotment Act,7 irrigation construction costs
were deemed reimbursable to the federal government either by the Indians or
non-Indian successors in interest. In 1921, these debts became a lien on the
property. Because of the inability of Indians or their non-Indian successors to
repay the government, many irrigation systems fell into disrepair and lands fell
out of Indian ownership. Acts of Congress in 1928, 1933, and 1936 either
OCR for page 79
IRRIGATION TODAY
TABLE 3.10 Partial list of Indian Irrigation Projects Authorized by Statue
79
Year Statute State
Blackfeet Project 1907 34 Stat. 1035 Montana
Coachella Valley 1950 64 Stat. 470 California
Colorado River Reservation 1935 49 Stat. 240 Arizona/California
Crow Indian Irrigation 1891 26 Stat. 1040 Montana
Flathead Project 1904 33 Stat. 365 Montana
Fort Hall Project 1894 28 Stat. 305 Indiana
Fort Peck Project 1908 35 Stat. 558 Montana
Middle Rio Grande Pueblos 1928 45 Stat. 383 New Mexico
Navajo Project 1962 70 Stat. 96 New Mexico
San Carlos Project 1924 43 Stat. 457 Arizona
Soboba Project 1970 84 Stat. 1465 California
Uintah Project 1906 34 Stat. 375 Utah
Valve Vo Project 1965 79 Stat. 1071 Arizona
Wapato Project 1904 33 Stat. 595 Washington
Wind River 1905 33 Stat. 1016 Wyoming
deferred payment of debts or canceled inappropriate debts or liens against Indian
and non-Indian property. The inconsistency in funding has contributed to the
current deteriorated condition of many Indian irrigation projects.
The Bureau of Indian Affairs (BIA) currently has the primary management
responsibility for Indian irrigation projects, although some tribes have contracted
this authority from the BIA using provisions of the 1973 Indian Self Determina-
tion and Education Assistance Act. BIA management of irrigation projects has
been severely constrained by institutional problems, lack of funding, and the
interplay between land laws, repayment requirements, and land ownership pat
terns.
A 1975 report to the Senate Committee on Interior and Insular Affairs on the
status of construction of Indian irrigation projects documented the need for more
than $200 million just to complete and rehabilitate the 71 Congressionally autho-
rized Indian irrigation projects currently administered by the BIA (Report to the
U.S. Senate Committee on Interior and Insular Affairs on the Construction of
Indian Irrigation Porjects, 1975~. Estimates of the costs for OM&R on private
systems are not readily available. OM&R needs on formal projects could repre-
sent a substantial liability to the United States as trustee for Indian Tribes. As a
result, policy decisions related to Indian irrigation projects and water resources
may significantly affect water resources available to irrigated agriculture.
NOTES
1. This section draws extensively on the following sources: U.S. Department of Commerce
(1987), Bajwa et al. (1992), Solley, et al. (1993), Boggus et al. (1993), and Gollehon et al. (1994).
2. It should be noted that irrigation runoff is some cases is responsible for creating and maintain-
ing wetland habitats, and curtailment of irrigation may on occasion actually harm or eliminate such
wetlands.
3. Numerous studies by federal agencies document these impacts. See, for example, Bowman,
David. 1994. Instream Flow Recommendations for Central Platte River, Nebraska. U.S. Fish and
Wildlife Service, Denver, Colorado. May 23, 1994; U.S. Fish and Wildlife Service. Final Recovery
Implementation Program for Endangered Fish Species in the Upper Colorado River Basin. Denver,
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80
A NEW ERA FOR IRRIGATION
Colorado., September 29, 1987; Department of Interior, Bureau of Reclamation. 1993. Operation of
Glen Canyon Dam, Draft Environmental Impact Study. Washington, D.C. May; Northwest Power
Planning Council. 1994. Columbia River Fish and Wildlife Program. Portland, Oregon, December;
National Marine Fisheries Service, 1995. Proposed Recovery Program for Snake River Salmon,
Washington, D.C., March.
4. In 1994 the USDA expenditures on conservation and related programs affecting agriculture
were estimated as follows: Conservation Reserve Program, $3.5 billion; wetlands programs, $56
million; water quality programs, $212 million; and other conservation, $1.5 billion (USDA, Agricul-
tural Resources and Environmental Indicators, 1994).
5. The Central Valley Project Improvement Act also includes requirements that water districts
and individuals who use federally supplied water assume responsibility for control and management
of drainage discharges in order to comply with federal and state water quality standards (Section
3405(c)).
6. Unpublished BIA preliminary estimates for 1994.
7. 25 USC 348.
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Representative terms from entire chapter:
ground water