The Ogallala Aquifer: A Case Study
Groundwater: What Can The Golf Course Industry Do to Protect This Valuable Natural Resource? The Ogallala Aquifer, also known as the High Plains Aquifer, is a vast yet shallow underground water table aquifer located beneath the Great Plains in the United States. One of the world's largest aquifers, it lies under about 174,000 square miles in portions of the eight states of South Dakota, Nebraska, Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and Texas. It was named in 1899 by N.H. Darton from its type locality near the town of Ogallala, Nebraska. It waters one fifth of U.S. irrigated land. In some parts of the Ogallala Aquifer that stretches across eight states in the Great Plains, aquifer depletion has caused increased pumping costs and decreased land values, forcing some farmers into bankruptcy. The Ogallala Aquifer is being depleted at a rate of 12 billion cubic meters per year. Some estimates say it will dry up in as little as 25 years. Many farmers in the Texas
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Industrial agriculture with its reliance on chemicals and its failure to adequately address soil erosion problems is guilty of depleting water resources. Ignorance and carelessness are in fact the main factors behind the increasing water quality deterioration. First, of course, any further ground water has to be pumped from deeper and deeper levels, and such water is not only more expensive to extract in terms of deeper wells and more powerful pumps, but is more likely to be chemically poor in quality. Second, the drop in the water table indicates that more ground water is being pumped than is being recharged, so that water supplies of the future are being mortgaged for present gain. Third, there are indirect effects of lowering the water table that are more insidious but more damaging. Natural vegetation may no longer be able to put down its roots deep enough to reach ground water, especially if there is a prolonged dry season, and it is
Industrial agriculture with its reliance on chemicals and its failure to adequately address soil erosion problems is guilty of depleting water resources. Ignorance and carelessness are in fact the main factors behind the increasing water quality deterioration. First, of course, any further ground water has to be pumped from deeper and deeper levels, and such water is not only more expensive to extract in terms of deeper wells and more powerful pumps, but is more likely to be chemically poor in quality. Second, the drop in the water table indicates that more ground water is being pumped than is being recharged, so that water supplies of the future are being mortgaged for present gain. Third, there are indirect effects of lowering the water table that are more insidious but more damaging. Natural vegetation may no longer be able to put down its roots deep enough to reach ground water, especially if there is a prolonged dry season, and it is