Three decades of data have informed a new Nebraska-led study that shows how the depletion of groundwater – the same that many farmers rely on for irrigation – can threaten food production amid drought and drier climes.
The study found that, due in part to the challenges of extracting groundwater, an aquifer’s depletion can curb crop yields even when it appears saturated enough to continue meeting the demands of irrigation. Those agricultural losses escalate as an aquifer dwindles, the researchers reported, so that its depletion exerts a greater toll on corn and soybean yields when waning from, say, 100 feet thick to 50 than from 200 feet to 150.
That reality should encourage policymakers, resource managers, and growers to reconsider the volume of crop-quenching groundwater they have at their disposal, the team said, especially in the face of fiercer, more frequent drought.
“As you draw down an aquifer to the point that it’s quite thin, very small changes in the aquifer thickness will then have progressively larger and larger impacts on your crop production and resilience,” said Nick Brozović, director of policy at the Daugherty Water for Food Global Institute. “And that’s a thing that we don’t predict well, because we tend to predict based on the past. So if we base what’s going to happen on our past experience, we’re always going to underpredict. We’re always going to be surprised by how bad things get.”
As you draw down an aquifer to the point that it’s quite thin, very small changes in the aquifer thickness will then have progressively larger and larger impacts on your crop production and resilience.
Nick Brozović
The team came to its conclusions after analyzing yields, weather, and groundwater data from the High Plains Aquifer, which, as the largest in the United States, underlies portions of eight states — including nearly all of Nebraska. Some areas of the aquifer, especially those beneath Texas and Kansas but also the Cornhusker State, have diminished considerably over the past several decades, pumped for the sake of irrigating land that would otherwise stand little chance of sustaining crops.
“In terms of things that let you address food security under extreme conditions – in particular, drought and climate change — we really can’t do without irrigation,” said Brozović, professor of agricultural economics at the University of Nebraska-Lincoln. “If we want to feed the world with high-quality, nutritious food and a stable food supply, we need to irrigate.”
Brozović and Husker colleague Taro Mieno had already constructed plenty of models, and run plenty of simulations, on how the High Plains Aquifer responds to drought and dry conditions. But talking with farmers revealed that the models were not addressing their primary concern: well yield, or the amount of groundwater that growers can expect to continuously draw when trying to buffer their crops against drought.
“Everybody’s interested in how aquifer depletion affects the resiliency of irrigated agriculture in the region,” said Mieno, an associate professor of agricultural economics and lead author of the study, which was published in the journal Nature Water.
So the researchers consulted annual estimates of the High Plains Aquifer’s thickness, which date back to 1935, along with county-level yields of corn and soybean from 1985 through 2016. Meteorological data, meanwhile, allowed the team to calculate seasonal water deficits or the difference between the water gained from precipitation and the amount that crops lost via evaporation and transpiration.
When the latter exceeds the former, farmers often turn to aquifers for help in making up the difference, the researchers knew. What they didn’t know: Under what conditions, and to what extent, would an aquifer’s depletion make pumping its water too difficult or expensive to undertake? And how much would the resulting decisions — to reduce the amount of irrigation per acre, to cease irrigating certain plots altogether – influence corn and soybean yields?
Farmers fortunate enough to be growing corn and soybean above the most saturated swaths of the High Plains Aquifer — roughly 220 to 700 feet thick — continued to enjoy high irrigated yields even in times of extreme water deficits, the team found. By contrast, those depending on the least saturated areas — between 30 and 100 feet – saw their irrigated yields begin trending downward when water deficits reached just 400 millimeters, a common occurrence in Nebraska and other Midwestern states.
In years when the deficit approached or exceeded 700 millimeters, irrigated fields residing above the thickest groundwater yielded markedly more corn than those sitting above the thinnest. The results were starker during a 950-millimeter water deficit, which corresponds with extreme drought: Fields atop the least saturated stretches of aquifer yielded roughly 19.5 fewer bushels per acre.
“Because of the way that aquifers work, even if there’s a lot of water there, as they deplete, you actually lose the ability to meet those crop water needs during the driest periods, because well yield tends to decline as you deplete an aquifer,” Brozović said. “That has an economic consequence and a resilience consequence.”
The study captured another telling link between the water residing underground and that applied at the surface. When atop groundwater roughly 330 feet thick, farmers irrigated 89% of their acres dedicated to growing corn. Where the aquifer was a mere 30 feet thick? Just 70% of those acres received irrigation. That’s likely a result of lower well yield driving farmers to irrigate only some of their fields, Taro said, or even give up on irrigation.
To better understand how that reduced irrigation was contributing to agricultural losses amid dry conditions, the researchers then factored in yields from both irrigated and non-irrigated fields, the latter of which rely on precipitation alone. That analysis pegged yields as even more sensitive to even smaller water deficits, suggesting that the decline in irrigated land was compounding the losses endured on still-irrigated plots.
And it illustrated the runaway threat posed when an aquifer’s average thickness drops below certain thresholds. At a water deficit of 950 millimeters, reducing an aquifer’s thickness from roughly 330 to 230 feet was estimated to initiate an average loss of about 2.5 corn bushels per acre, what the authors called a “negligible difference.” The same absolute decrease, but from 230 to 130 feet, led to an estimated loss of 15 bushels per acre.
“As a consequence, your resilience to climate decreases rapidly,” Mieno said. “So when you’re operating on an aquifer that is very thick right now, you’re relatively safe. But you want to manage it in a way that you don’t go past that threshold because from there, it’s all downhill.
“And the importance of aquifers is going to increase as climate change progresses in the future, for sure. As it gets hotter, you typically need more water. That means you need more irrigation, and you’re going to deplete the aquifer even faster, and things can get worse and worse.”
Nebraska is lucky, Brozović said, in that it sits above such a massive reservoir and has established a governance system designed to conserve it at a local scale. However most regulations focus on mandating how much and when groundwater gets pumped, not safeguarding the aquifer’s saturation level or the corresponding ability to extract water from it.
Brozović conceded that convincing policymakers to consider revising those parameters now, when much of the state still boasts sufficient groundwater, is “perhaps a tough sell.” He’s hopeful that the new study can at least help put that conversation on the table.
