Groundwater — The Invisible and Vital Resource. Details: 115 million people rely on groundwater for drinking water. 43 million people rely on groundwater from private wells. 1 of every 5 groundwater samples from parts of aquifers used for drinking water contained a contaminant from geologic or manmade sources at a level exceeding a potential human-health concern. 6,600 wells were sampled for this study. 1.3 million chemical analyses performed for this study.
“Through the WaterSMART initiative and the National Water-Quality Assessment Program, the Department of Interior is working to secure sustainable water supplies of sufficient quantity and quality and to identify measures needed to address climate change and future demands,” said Jennifer Gimbel, Principal Deputy Assistant Secretary of the U.S. Department of the Interior. “The integrated work that USGS is doing to map groundwater availability, groundwater quality, and the potential for contamination will give us the information we need to understand natural and human effects on groundwater and to take the actions needed to protect this vital natural resource.”
The recently completed national summary report of the quality of the Nation’s groundwater is now available online. Nine associated reports (USGS circulars) detail regional-scale assessments of groundwater quality in about 30 of the most heavily used principal aquifers across the United States.
A deep look at an unseen resourceOver the last two decades, USGS scientists have assessed water quality in source (untreated) water from 6,600 wells in extensive regional aquifers that supply most of the groundwater pumped for the Nation’s drinking water, irrigation, and other uses. This comprehensive sampling, along with detailed information on geology, hydrology, geochemistry, and chemical and water use, can be used to explain how and why aquifer vulnerability to contamination varies across the Nation.
Illustration: Map showing many charts indicating “Exceedances of human-health benchmarks by one or more contaminants”. For more details on exact numbers, please refer to the linked resources in this story.
- More than one in five (22 percent) groundwater samples contained at least one contaminant at a concentration of potential concern for human health.
- Contaminants from geologic sources—primarily manganese, arsenic, and radon—accounted for about 80 percent of contaminant concentrations that exceeded a human-health benchmark. Nitrate, which exceeded its benchmark in about 4 percent of wells sampled, was the only constituent from manmade sources that exceeded its human-health benchmark in more than 1 percent of samples.
- Differences in contaminant concentrations among aquifers, within an aquifer, and even between two nearby wells can be explained by large- and local-scale differences in geology, hydrology, geochemistry, and chemical and water use. Understanding how natural features and human activities affect groundwater quality helps to predict how and why aquifer vulnerability to contamination varies across the Nation.
- High-volume pumping and irrigation in many areas have profoundly changed groundwater flow and quality. By moving shallow groundwater deeper, into parts of aquifers used for drinking water, irrigation and pumping have increased the vulnerability of drinking-water supplies to contamination from nitrate, pesticides, and other manmade chemicals from the land surface.
- Irrigation, high-volume pumping, and artificial recharge can cause different types of waters to mix, with the unexpected consequence of causing the aquifer rocks and sediment to release naturally occurring contaminants, such as arsenic, selenium, or radium, into the groundwater.
Outlines of principal aquifers of the U.S. For details on the map, please use the linked resources available in this story.
Regional Principal Aquifer AssessmentsIn-depth, regional-scale assessments of groundwater quality focus on about 30 of the most heavily used Principal Aquifers in the Nation. Groundwater quality in these aquifers—and the factors that affect it—is described in nine new U.S. Geological Survey circulars.
Glacial Aquifer System (northern U.S.)
Western Volcanics (northwestern U.S., Hawaii)
Southwest Basin-fill Aquifers (southwestern U.S.)
Denver Basin Aquifer System (Colorado)
Piedmont, Blue Ridge, and Valley and Ridge Aquifers (eastern U.S.)
Northern Atlantic Coastal Plain Surficial Aquifer System (east coast of U.S.)
Upper Floridan Aquifer and Overlying Surficial Aquifer(southeastern U.S.)
Mississippi Embayment-Texas Coastal Upland Aquifer System and Mississippi River Valley Alluvial Aquifer (southeastern, southcentral U.S.)
High Plains Aquifer System (central U.S.)
Looking forwardOver the next decade, about 2,300 shallow wells and 1,400 deep public-supply wells will be sampled for a broad range of water-quality constituents as the National Water-Quality Assessment Program continues to address the three central questions:
1. What is the quality of the Nation’s groundwater,
2. Is it getting better or worse, and
3. What factors affect the quality of this vital resource.
In the future, USGS-led national and regional scale modeling will provide a three-dimensional perspective of the quality of the Nation’s groundwater that can be used to inform management decisions.
Learn moreUSGS National Summary Circular, Quality of the Nation’s Groundwater Quality, 1991-2010
Regional reports (nine) on principal aquifers of the U.S.
National Water-Quality Assessment (NAWQA) Program
USGS Groundwater Information