Water use estimates and water returns for the ACF Basin were estimated and compiled by category and location during 2010. Categories included public supply, self-suppled domestic, self-supplied commercial, industrial, mining, agricultural (crop irrigation, livestock, and aquaculture), and thermoelectric-power generation. Methods for estimating irrigation water use were compared and evaluated against available metered data.
National Water Census • ACF Basin • Drought Impacts • Water Use • Estimating Streamflow • Groundwater/Surface-Water Interactions
In 2010, an average of 1,645 Mgal/d were withdrawn in the ACF Basin, with about 35 percent of withdrawals coming from groundwater sources and 65 percent from surface water. About 564 Mgal/d (34 percent of withdrawals) were returned to streams and rivers in the basin (mostly as treated wastewater) and less than 4 percent of withdrawals were for interbasin transfers outside of the ACF. Although population in the basin, particularly in the Atlanta metropolitan area, has increased by 45 percent from 1990 to 2010, surface-water use has declined during that period, most likely due to conservation measures. Conversely, groundwater use has steadily increased due to increases in pumping for agricultural irrigation with spikes in use during drought years.
Surface-water and groundwater withdrawals for the ACF Basin in 2010 by water-use category.
Key Findings and Results
- The largest use of surface water is for public supply (499 Mgal/d) and thermoelectric power supply (281 Mgal/d).
- More than 75 percent of groundwater is used for agriculture, the majority of which is used to irrigate crops in the lower Flint River Basin
- Read the report
Agriculture is the largest water use in the ACF Basin and estimates of agricultural water use are typically complex, with high levels of uncertainty. To address this uncertainty, three different methods were tested in the ACF FAS to compare their ability to match estimates of irrigation water use derived from metered wells. These methods include (1) crop-demand, (2) geostatistical with variography and conditional simulation, and (3) remote sensing technology to identify irrigated lands. Results are presented in a USGS Scientific Investigation Report (Painter and others, 2015) and indicate that information on local agricultural practices and spatial and temporal distribution of irrigated lands are critical for all three methods.
Key Findings and Results
- In all three methods evaluated to estimate irrigation water use, information was required on agricultural practices specific to the geographic location and season to produce useful results.
- Read the report
National Water Census • ACF Basin • Drought Impacts • Water Use • Estimating Streamflow • Groundwater/Surface-Water Interactions
Below are other science components of the Apalachicola-Chattahoochee-Flint River Basin Focus Area Study.
Apalachicola-Chattahoochee-Flint River Basin Focus Area Study
Apalachicola-Chattahoochee-Flint River Basin Focus Area Study: Drought Impacts on Streams and Groundwater
Apalachicola-Chattahoochee-Flint River Basin Focus Area Study: Estimating Streamflow
Apalachicola-Chattahoochee-Flint River Basin Focus Area Study: Groundwater/Surface-Water Interactions
Below are publications associated with the Apalachicola-Chattahoochee-Flint River Basin Focus Area Study.
Water use in the Apalachicola-Chattahoochee-Flint River Basin, Alabama, Florida, and Georgia, 2010, and water-use trends, 1985-2010
Evaluation and comparison of methods to estimate irrigation withdrawal for the National Water Census Focus Area Study of the Apalachicola-Chattahoochee-Flint River Basin in southwestern Georgia
Influence of septic systems on stream base flow in the Apalachicola-Chattahoochee-Flint River Basin near Metropolitan Atlanta, Georgia, 2012
- Overview
Water use estimates and water returns for the ACF Basin were estimated and compiled by category and location during 2010. Categories included public supply, self-suppled domestic, self-supplied commercial, industrial, mining, agricultural (crop irrigation, livestock, and aquaculture), and thermoelectric-power generation. Methods for estimating irrigation water use were compared and evaluated against available metered data.
National Water Census • ACF Basin • Drought Impacts • Water Use • Estimating Streamflow • Groundwater/Surface-Water Interactions
In 2010, an average of 1,645 Mgal/d were withdrawn in the ACF Basin, with about 35 percent of withdrawals coming from groundwater sources and 65 percent from surface water. About 564 Mgal/d (34 percent of withdrawals) were returned to streams and rivers in the basin (mostly as treated wastewater) and less than 4 percent of withdrawals were for interbasin transfers outside of the ACF. Although population in the basin, particularly in the Atlanta metropolitan area, has increased by 45 percent from 1990 to 2010, surface-water use has declined during that period, most likely due to conservation measures. Conversely, groundwater use has steadily increased due to increases in pumping for agricultural irrigation with spikes in use during drought years.
Surface-Water Withdrawals by Use Category: Total is 1,069 million gallons per day. Groundwater Withdrawals by Use Category: Total is 576 millon gallons per day. Surface-water and groundwater withdrawals for the ACF Basin in 2010 by water-use category.
Key Findings and Results
- The largest use of surface water is for public supply (499 Mgal/d) and thermoelectric power supply (281 Mgal/d).
- More than 75 percent of groundwater is used for agriculture, the majority of which is used to irrigate crops in the lower Flint River Basin
- Read the report
Agriculture is the largest water use in the ACF Basin and estimates of agricultural water use are typically complex, with high levels of uncertainty. To address this uncertainty, three different methods were tested in the ACF FAS to compare their ability to match estimates of irrigation water use derived from metered wells. These methods include (1) crop-demand, (2) geostatistical with variography and conditional simulation, and (3) remote sensing technology to identify irrigated lands. Results are presented in a USGS Scientific Investigation Report (Painter and others, 2015) and indicate that information on local agricultural practices and spatial and temporal distribution of irrigated lands are critical for all three methods.
Geostatistical techniques used to estimate irrigation depth. Key Findings and Results
- In all three methods evaluated to estimate irrigation water use, information was required on agricultural practices specific to the geographic location and season to produce useful results.
- Read the report
National Water Census • ACF Basin • Drought Impacts • Water Use • Estimating Streamflow • Groundwater/Surface-Water Interactions
- Science
Below are other science components of the Apalachicola-Chattahoochee-Flint River Basin Focus Area Study.
Apalachicola-Chattahoochee-Flint River Basin Focus Area Study
As one of several National Focus Area Studies within the USGS National Water Census (NWC) the USGS completed a 3-year study of water availability and use in the Apalachicola-Chattahoochee-Flint (ACF) River Basin.Apalachicola-Chattahoochee-Flint River Basin Focus Area Study: Drought Impacts on Streams and Groundwater
During 2011 drought conditions in the ACF basin provided an opportunity to document streamflow and groundwater levels under these extreme conditions. Over 350 water levels were measured in wells and streamflow was measured at 212 streams or springs.Apalachicola-Chattahoochee-Flint River Basin Focus Area Study: Estimating Streamflow
A hydrologic model that simulates streamflow conditions in the ACF Basin was constructed using the Precipitation Runoff Modeling System. The model simulated development by including withdrawals and returns, interbasin transfers, storage in unmanaged reservoirs, and impervious surface.Apalachicola-Chattahoochee-Flint River Basin Focus Area Study: Groundwater/Surface-Water Interactions
In the lower Chattahoochee and Flint River Basin, a groundwater flow model was developed to simulate the effects of groundwater withdrawals on streamflow. This model was linked with the streamflow model to improve estimates of baseflow conditions during critical times, such as droughts. - Publications
Below are publications associated with the Apalachicola-Chattahoochee-Flint River Basin Focus Area Study.
Water use in the Apalachicola-Chattahoochee-Flint River Basin, Alabama, Florida, and Georgia, 2010, and water-use trends, 1985-2010
The Apalachicola-Chattahoochee-Flint (ACF) River Basin encompasses about 20,230 square miles in parts of Alabama, Florida, and Georgia. Increasing population growth and agricultural production from the 1970s to 2010 has prompted increases in water-resources development and substantially increased water demand in the basin. Since the 1980s, Alabama, Florida, Georgia, and the U.S. Army Corps of EngiAuthorsStephen J. LawrenceEvaluation and comparison of methods to estimate irrigation withdrawal for the National Water Census Focus Area Study of the Apalachicola-Chattahoochee-Flint River Basin in southwestern Georgia
Methods to estimate irrigation withdrawal using nationally available datasets and techniques that are transferable to other agricultural regions were evaluated by the U.S. Geological Survey as part of the Apalachicola-Chattahoochee-Flint (ACF) River Basin focus area study of the National Water Census (ACF–FAS). These methods investigated the spatial, temporal, and quantitative distributions of watAuthorsJaime A. Painter, Lynn J. Torak, John JonesInfluence of septic systems on stream base flow in the Apalachicola-Chattahoochee-Flint River Basin near Metropolitan Atlanta, Georgia, 2012
Septic systems were identified at 241,733 locations in a 2,539-square-mile (mi2) study area that includes all or parts of 12 counties in the Metropolitan Atlanta, Georgia, area. Septic system percolation may locally be an important component of streamflow in small drainage basins where it augments natural groundwater recharge, especially during extreme low-flow conditions. The amount of groundwateAuthorsJohn S. Clarke, Jaime A. Painter