How does groundwater pumping affect streamflow?

November 16th, 2012 in Earth / Environment

Groundwater provides drinking water for millions of Americans and is the primary source of water to irrigate cropland in many of the nations most productive agricultural settings. Although the benefits of groundwater development are many, groundwater pumping can reduce the flow of water in connected streams and rivers—a process called streamflow depletion by wells. The USGS has released a new report that summarizes the body of knowledge on streamflow depletion, highlights common misconceptions, and presents new concepts to help water managers and others understand the effects of groundwater pumping on surface water.

"Groundwater discharge is a critical part of flow in most streams—and the more we pump below the ground, the more we deplete water flowing down the stream," said USGS Director Marcia McNutt. "When viewed over the long term, it is one big zero-sum game."

Groundwater and surface-water systems are connected, and groundwater discharge is often a substantial component of the total flow of a stream. In many areas of the country, pumping wells capture groundwater that would otherwise discharge to connected streams, rivers, and other surface-water bodies. Groundwater pumping can also draw streamflow into connected aquifers where pumping rates are relatively large or where the locations of pumping are relatively close to a stream.

"Streamflow depletion caused by pumping is an important water-resource management issue across the nation because of the adverse effects that reduced flows can have on , the availability of surface water, and the quality and of streams and rivers," said Paul Barlow, USGS hydrologist and author on the report. "Managing the effects of streamflow depletion by wells is challenging, particularly because of the significant time delays that often occur between when pumping begins and when the effects of that pumping are realized in nearby streams. This report will help managers understand the many factors that control the timing, rates, and locations of streamflow depletion caused by pumping."

Major conclusions from the report:

"Conjunctive management of groundwater and surface-water resources is critical in New Mexico, where our limited surface-water supplies can be impacted by new uses that are predominantly dependent on pumping," said Mike Johnson, Chief of the Hydrology Bureau in the New Mexico Office of the State Engineer. "This new USGS publication consolidates our understanding of the connection between aquifers and streams and provides a clear, thorough and up-to-date explanation of the tools and techniques used to evaluate streamflow depletion by wells. This report will be very useful to New Mexico's in guiding technical analysis, dispelling common misconceptions, and explaining these complex concepts to decision makers and the public."

More information: The report, which is a product of the USGS Groundwater Resources Program, is titled "Streamflow Depletion by Wells—Understanding and Managing the Effects of Groundwater Pumping on Streamflow" and is available in print and online.

Provided by United States Geological Survey

"How does groundwater pumping affect streamflow?." November 16th, 2012. http://phys.org/news/2012-11-groundwater-affect-streamflow.html