Crop production was simulated under four different groundwater use scenarios, ranging from most optimistic to pessimistic. The most optimistic scenario assumes that the maximum amount of recharge can be used for irrigation. The less optimistic scenarios, which are based on safe aquifer yield, assume that only a fraction of the recharge goes into the aquifer and just that restricted amount of water can be used for irrigation. The less optimistic scenarios account for uncertainty in groundwater availability as well as preserving some water to maintain healthy ecosystems. The four sustainable groundwater use scenarios are based on safe aquifer yields of 100%, 75%, 50%, and 25%.
Under the most optimistic sustainable groundwater use scenario, U.S. irrigated production of corn, soybean and winter wheat is reduced by 20%, 6% and 25%, respectively. Under the most pessimistic scenario, corn, soybean and winter wheat production is reduced by 45%, 37% and 36%, respectively.
“Our findings underscore how corn, soybean and winter wheat production could be affected if we chose to stop depleting aquifers across the United States,” says co-lead author Jonathan Winter, an associate professor of geography and principal investigator of the Applied Hydroclimatology Group at Dartmouth. “However, future precipitation, which affects groundwater resources, is difficult to predict, and improved irrigation technology, more water-efficient crops, and better agricultural water management could reduce the production losses from a transition to sustainable groundwater use.”
The findings show that Nebraska, Kansas, and Texas, which rely on groundwater from the High Plains Aquifer (also known as the Ogallala Aquifer) to grow corn, soybeans and winter wheat, would experience some of the greatest production losses as a result of sustainable groundwater use. This region is particularly vulnerable due to its lack of rainfall, which limits rainfed agriculture and groundwater recharge. Prior research found that the High Plains extracts three times as much groundwater as its aquifer’s recharge rate.
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