Ogallala Aquifer

Saturated thickness of the Ogallala Aquifer in 1997 after several decades of intensive withdrawals: The breadth and depth of the aquifer generally decrease from north to south. Regions where the water level has declined in the period 1980-1995 are shown in yellow and red; regions where it has increased are shown in shades of blue. Data from the USGS Groundwater withdrawal rates (fresh water, all sources) by county in 2000. Source: National Atlas

The Ogallala Aquifer is a shallow water table aquifer located beneath the Great Plains in the United States. One of the world's largest aquifers, it underlies an area of approximately 174,000 mi² (450,000 km²) in portions of eight states: (South Dakota, Nebraska, Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and Texas). It was named in 1898 by N.H. Darton from its type locality near the town of Ogallala, Nebraska. The aquifer is part of the High Plains Aquifer System, and rests on the Ogallala Formation, which is the principal geologic unit underlying 80% of the High Plains.^[1]

About 27 percent of the irrigated land in the United States overlies the aquifer, which yields about 30 percent of the ground water used for irrigation in the United States. Since 1950, agricultural irrigation has reduced the saturated volume of the aquifer by an estimated 9%. Depletion is accelerating, with 2% lost between 2001 and 2009^[2] alone. Certain aquifer zones are now empty; these areas will take over 100,000 years to replenish naturally through rainfall.

The aquifer system supplies drinking water to 82 percent of the 2.3 million people (1990 census) who live within the boundaries of the High Plains study area.^[3]

General characteristics

The deposition of aquifer material dates back 2 to 6 million years, from the late Miocene to early Pliocene ages when the southern Rocky Mountains were still tectonically active. From the uplands to the west, rivers and streams cut channels in a generally west to east or southeast direction. Erosion of the Rockies provided alluvial and aeolian sediment that filled the ancient channels and eventually covered the entire area of the present-day aquifer, forming the water-bearing Ogallala Formation. In that respect, the process is similar to those currently prevailing in other modern rivers of the area, such as the Kansas River and its tributaries. The major differences are time and depth.

The depth of the Ogallala varies with the shape of then-prevailing surface, being deepest where it fills ancient valleys and channels. The Ogallala Formation consists mostly of coarse sedimentary rocks in its deeper sections, which transition upward into finer-grained material.^[4]

The water-saturated thickness of the Ogallala Formation ranges from a few feet to more than 1000 feet (300 m) and is generally greater in the northern plains.^[5] The depth of the water below the surface of the land ranges from almost 400 feet (120 m) in parts of the north to between 100 and 200 feet (30 and 60 m) throughout much of the south. Present-day recharge of the aquifer with fresh water occurs at an exceedingly slow rate, suggesting that much of the water in its pore spaces is paleowater, dating back to the most recent ice age and probably earlier.

Aquifer water balance

An aquifer is a groundwater storage reservoir in the water cycle. While groundwater is a renewable source, reserves replenish relatively slowly. The USGS has performed several studies of the aquifer, to determine what is coming in (groundwater recharge from the surface), what is leaving (water pumped out and baseflow to streams), and what the net changes in storage are (rise, fall or no change — see figure above).

Withdrawals from the Ogallala Aquifer for irrigation amounted to 26 km³ (21,000,000 acre·ft) in 2000. As of 2005, the total depletion since pre-development amounted to 253,000,000 acre feet (312 km³).^[6] Some estimates indicate a remaining volume sufficient for as little as 25 years. Many farmers in the Texas High Plains, which rely particularly on the underground source, are now turning away from irrigated agriculture as they become aware of the hazards of overpumping.^[7]

Groundwater recharge

The rate at which recharge water enters the aquifer is limited by several factors. Much of the plains region is semiarid, with steady winds that hasten evaporation of surface water and precipitation. In many locations, the aquifer is overlain, in the vadose zone, with a shallow layer of caliche that is practically impermeable; this limits the amount of water able to recharge the aquifer from the land surface. However, the soil of the playa lakes is different and not lined with caliche, making these some of the few areas where the aquifer can recharge. The destruction of playas by farmers and development decreases the available recharge area. The prevalence of the caliche is partly due to the ready evaporation of soil moisture and the semiarid climate; the aridity increases the amount of evaporation, which in turn increases the amount of caliche in the soil. Both mechanisms reduce the amount of recharge water that reaches the water table.

Recharge in the aquifer ranges from 0.024 inches (0.61 mm) per year in parts of Texas and New Mexico to up to 6 inches (150 mm) per year in south-central Kansas.^[8]

Groundwater discharge

NASA ASTER image of an approx. 557 mi² area of fields (1443 km²) in Kansas which are watered from the Ogallala aquifer with center pivot irrigation systems.

The regions overlying the Ogallala aquifer are some of the most productive regions in the United States for ranching livestock, and growing corn, wheat, and soybeans. The success of large-scale farming in areas that do not have adequate precipitation and do not always have perennial surface water for diversion has depended heavily on pumping groundwater for irrigation.

Early settlers of the semiarid High Plains were plagued by crop failures due to cycles of drought, culminating in the disastrous Dust Bowl of the 1930s. It was only after World War II when center pivot irrigation became available, that the land mass of the High Plains aquifer system was transformed into one of the most agriculturally productive regions in the world.

Change in groundwater storage

Ground water levels decline when the rate of extraction by irrigation exceeds the rate of recharge. At places, the water table was measured to drop more than five feet (1.5 m) per year at the time of maximum extraction. In extreme cases, the deepening of wells was required to reach the steadily falling water table. In the 21st century, recognition of the significance of the aquifer has led to increased coverage from regional and international journalists.^{[9][10][11][12]}

The USGS estimated that total water storage was about 2,925,000,000 acre feet (3,608 km³) in 2005. This is a decline of about 253,000,000 acre feet (312 km³), or 9%, since substantial ground-water irrigation development began in the 1950s.^[6]

Water conservation practices (terracing and crop rotation), more efficient irrigation methods (center pivot and drip), and reduced area under irrigation have helped to slow depletion of the aquifer, but levels are generally still dropping in areas including southwestern Kansas and the Texas Panhandle. In other areas, such as parts of eastern and central Nebraska and of the region south of Lubbock, Texas, water levels have risen since 1980.

The center-pivot irrigator was described as the "villain" ^[13] in a New York Times article, "Wells Dry, Fertile Plains Turn to Dust" recounting the relentless decline of parts of the Ogallala Aquifer. Sixty years of intensive farming using huge center-pivot irrigators has emptied parts of the High Plains Aquifer.^[13] It would take hundreds to thousands of years of rainfall to replace the groundwater in the depleted aquifer. In 1950, irrigated cropland covered 250,000 acres. With the use of center-pivot irrigation, nearly three million acres of land were irrigated.^[13] In some places in the Texas Panhandle, the water table has been drained (dewatered). "Vast stretches of Texas farmland lying over the aquifer no longer support irrigation. In west-central Kansas, up to a fifth of the irrigated farmland along a 100-mile swath of the aquifer has already gone dry."^[13]

The center-pivot irrigation system is considered to be a highly efficient system which helps conserve water. However, by 2013 it was shown that as the water consumption efficiency of the center-pivot irrigator improved over the years, farmers chose to plant more intensively, irrigate more land and grow thirstier crops rather than reduce water consumption.^[13] One approach to reducing the amount of groundwater used is to employ treated recycled water for irrigation; another approach is to change to crops that require less water, such as sunflowers.^[14]

Several rivers, such as the Platte, run below the water level of the aquifer. Because of this, the rivers receive groundwater flow (baseflow), carrying it out of the region rather than recharging the aquifer.

Accelerated decline in aquifer storage

According to a 2013 report by research hydrologist, Leonard F. Konikow, at the United States Geological Survey (USGS), the depletion between 2001–2008, inclusive, is about 32 percent of the cumulative depletion during the entire 20th century.^[15] In the United States, the biggest users of water from aquifers include agricultural irrigation and oil and coal extraction.^[16]"Cumulative total groundwater depletion in the United States accelerated in the late 1940s and continued at an almost steady linear rate through the end of the century. In addition to widely recognized environmental consequences, groundwater depletion also adversely impacts the long-term sustainability of groundwater supplies to help meet the Nation’s water needs."^[15]

Environmental controversies

In the 1980s, Texas Panhandle organic foods farmer and spokesman Frank Ford successfully prevented the location of a nuclear waste repository in his native Deaf Smith County. He opposed the site on the grounds that the material could poison the Ogallala Aquifer.^{[citation needed]} The repository was proposed to be located, instead, in Yucca Mountain in Nevada.

Proposed Keystone XL Pipeline

In 2008, TransCanada Corporation proposed the construction of the 1,661-mile (2,673 km) Keystone XL pipeline to carry oil from the Athabasca oil sands of Alberta to refineries near Houston, Texas.^[17][18] The proposed route of the pipeline crosses the eastern part of the Nebraska Sandhills; opponents of the route cite the risk to the Ogallala Aquifer posed by the possibility of contamination from spilled dilute bitumen.^[19][20]

Research hydrogeologist James Goeke, professor emeritus at the University of Nebraska, who has spent more than 40 years studying the Ogallala Aquifer, phoned TransCanada officials and quizzed them on the project, and satisfied himself that danger to the aquifer was small, because he believes that a spill would be unlikely to penetrate down into the aquifer, and if it did, he believes that the contamination would be localized. He noted: “A lot of people in the debate about the pipeline talk about how leakage would foul the water and ruin the entire water supply in the state of Nebraska and that’s just a false,” ^[21] Goeke said "... a leak from the XL pipeline would pose a minimal risk to the aquifer as a whole."^[22]

Pipeline industry spokesmen have noted that thousands of miles of existing pipelines carrying crude oil and refined liquid hydrocarbons have crossed over the Ogallala Aquifer for years, in southeast Wyoming, eastern Colorado and New Mexico, western Nebraska, Kansas, Oklahoma, and Texas.^{[23][24][25][26][27]} The Pioneer crude oil pipeline crosses east-west across Nebraska, and the Pony Express pipeline, which crosses the Ogallala Aquifer in Colorado, Nebraska, and Kansas, was being converted as of 2013 from natural gas to crude oil, under a permit from the Federal Energy Regulatory Commission.^[28]

As the lead agency in the transboundary pipeline project, the U.S. State Department commissioned an environmental-impact assessment as required by the National Environmental Policy Act of 1969. The Environmental Impact Statement concluded that the project posed little threat of "adverse environmental impacts",^[19][29] the report was drafted by Cardno Entrix, a regular TransCanada subcontractor. While it is "common for companies applying to build government projects to be involved in assigning and paying for the impact analysis",^[30] U.S. President Barack Obama cited the apparent conflict of interest in his January 2012 decision to await further environmental review.^[31] On February 17, 2013, a rally at the National Mall drew an estimated 40,000 in protest of Keystone XL.^[31]

On 1 March 2013, the U.S. State Department released its Keystone pipeline Draft Supplemental Environmental Impact Statement, which concluded that a large crude oil spill from the pipeline that reached the Ogallala could spread as far as 1,214 feet, with dissolved components spreading as much as 1,050 feet further.^[32] Secretary of State John Kerry is reviewing the permit application and the White House is expected to announce its decision after the Secretary has familiarised himself with the project.^[31]

Conservation

Since 2010, the North Plains Groundwater Conservation District, which encompasses eight counties north of Amarillo, including Moore and Dallam counties, has offered a $300,000 annual demonstration project to conserve water that farmers pump from the Ogallala Aquifer. Participating farmers grow corn with just over half of the water that they would normally require to irrigate the fields, or they plant several weeks later than customary. Pivot sprinklers are used in the project, rather than the more expensive drip irrigation. According to district manager Steve Walthour, conservation is essential considering declining levels of the aquifer.^[33]

Eleven farmers in 2013 participated in the conservation program, with some planting in dry earth, rather than pre-watered soil. They are leaving more space between plants a technique that retains moisture for a longer period of time. Soil sensors permit farmers to gather accurate information about the moisture level of their crops. The motivation to save water comes from the district's regulations on extracting water from the aquifer. The United States Geological Survey determined the water level in the aquifer has dropped more in Texas than in any other state in the basin.^[33]

Farmers on their own land may draw water without charge from the aquifer. Pumping costs are low because the fuel used, natural gas, is inexpensive. The North Plains district first established limits on pumping limits in 2005 and tightened the regulations four years later. Certain wells are now required to have meters. Yet another challenge facing the district is that higher prices for crops have prompted some to plant additional fields and further increase the use of water from the aquifer.^[33]

See also

References

External links

Wikimedia Commons has media related to Ogallala Aquifer.

• "The Ogallala Aquifer" Manjula V. Guru, Agricultural Policy Specialist and James E. Horne, President & CEO, The Kerr Center for Sustainable Agriculture, Poteau, Oklahoma
• USGS High Plains Regional Groundwater Study
• A Legal Fight in Texas over the Ogallala Aquifer
• Kansas Geological Survey information on the High Plains / Ogallala Aquifer
• Rapid Recharge of Parts of the High Plains Aquifer Indicated by a Reconnaissance Study in Oklahoma

Coordinates: 36°59′26″N 101°26′52″W / 36.99056°N 101.44778°W / 36.99056; -101.44778