Approximately 3.4 million acres of Idaho farmland are irrigated with water that a growing urban population competes to use instead.
An aquifer is an underground “reservoir” of water contained in one or more layers or strata of permeable rock or unconsolidated materials. Groundwater from aquifers can then be pumped from water wells and distributed for use on farms, in factories, and across municipalities, whether to cook food, take a bath, or irrigate exterior landscaping. (Read the full section on aquifers here.)
Three of Idaho’s aquifers are classified by the Environmental Protection Agency (EPA) as “sole source aquifers”. That means they are the only or principal source of drinking water for the hundreds of thousands of residents in those regions.
Just as human demands on the SVRP Aquifer are increasing, a changing climate is also putting pressure on the aquifer by creating earlier springs and drier summers. Higher temperatures for longer periods lead to more evaporation; increased evaporation results in more intensive storms and faster melt of the snowpack; this in turn means less water infiltrating into soil and the aquifer; finally, less soil moisture leads to an increase in summer water use, as well as more drought and wildland fires.
Projected future population growth in the SVRP Aquifer counties will increase the number of water consumers. At what point the increasing population will begin to overdraft and draw down the aquifer is uncertain. At the same time, what is certain is that increasing land development, impervious surfaces (pavement and roofs), and human and industrial activities will expose this unconfined aquifer to an increasing amount and variety of pollutants. (Read Here.)
The authors of the study concluded in 2023:
For now, when Idaho citizens are confronted with a choice of diverting water from the state’s agriculture to provide water for drinking or any other urban use, they side with agriculture, according to polling done for this study.