Monday, March 23, 2009

The Ogallala Aquifer: Saving a Vital U.S. Water Source


On America’s high plains, crops in early summer stretch to the horizon: field after verdant field of corn, sorghum, soybeans, wheat and cotton. Framed by immense skies now blue, now scarlet-streaked, this 800-mile expanse of agriculture looks like it could go on forever.

It can’t.

The Ogallala Aquifer, the vast underground reservoir that gives life to these fields, is disappearing. In some places, the groundwater is already gone. This is the breadbasket of America—the region that supplies at least one fifth of the total annual U.S. agricultural harvest. If the aquifer goes dry, more than $20 billion worth of food and fiber will vanish from the world’s markets. And scientists say it will take natural processes 6,000 years to refill the reservoir.

The challenge of the Ogallala is how to manage human demands on the layer of water that sprawls underneath parts of eight states from South Dakota to Texas. As landowners strive to conserve what’s left, they face a tug-of-war between economic growth and declining natural resources. What is happening here—the problems and solutions—is a bellwether for the rest of the planet.

High Plains farmers were blissfully unaware a generation ago that a dilemma was already unfolding. In the early 1950s, when Rodger Funk started farming near Garden City, Kan., everyone believed the water was inexhaustible. “People were drilling wells,” he says. “You could pump all the water you wanted to pump.”

And they did. What changed everything for Funk, now age 81, was a public meeting in the late 1960s at Garden City Community College. State and federal geologists, who had been studying where all that water was coming from, announced grim findings. “They said it’s geologic water. When it’s gone, it’s gone,” Funk says. “I remember coming home and feeling so depressed.”

Today his community in southern Kansas, 180 miles west of Wichita, is one of the High Plains areas hardest hit by the aquifer’s decline. Groundwater level has dropped 150 feet or more, forcing many farmers to abandon their wells. The cause is obvious, says Mark Rude, executive director of the Southwest Kansas Groundwater Management District: overuse.

more from Scientific American

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