USGS - science for a changing world

USGS Groundwater Information

Groundwater Resources Program

*  Home *  Regional GW Studies *  GW & Environment * Methods & Modeling *  Publications *  Data & Information [an error occurred while processing this directive] *  Intranet
 [Photo: Groundwater flowing out of well.]

New & Noteworthy

* Press Release: Study Explores Groundwater and Geothermal Energy in Drought-Stricken Eastern Oregon and Neighboring States

* Technical Announcement: USGS Issues Revised Framework for Hydrogeology of Floridan Aquifer

* Press Release: High Plains Aquifer Groundwater Levels Continue to Decline

* Regional Groundwater Availability Study Geospatial Data

* Press Release: USGS Assesses Current Groundwater-Quality Conditions in the Williston Basin Oil Production Area

Past listings...

USGS Groundwater Watch

USGS maintains a network of active wells to provide basic statistics about groundwater levels.

 [Image: USGS active water level wells location map.]

Other Water Topics

*  Water Resources

*  Groundwater

*  Surface Water

*  Water Quality

*  Water Use

USGS in Your State

USGS Water Science Centers are located in each state.

 [Map: There is a USGS Water Science Center office in each State.] Washington Oregon California Idaho Nevada Montana Wyoming Utah Colorado Arizona New Mexico North Dakota South Dakota Nebraska Kansas Oklahoma Texas Minnesota Iowa Missouri Arkansas Louisiana Wisconsin Illinois Mississippi Michigan Indiana Ohio Kentucky Tennessee Alabama Pennsylvania West Virginia Georgia Florida Caribbean Alaska Hawaii and Pacific Islands New York Vermont New Hampshire Maine Massachusetts South Carolina North Carolina Rhode Island Virginia Connecticut New Jersey Maryland-Delaware-D.C.

Water-Table Fluctuation (WTF) Method

Master Recession Curve (MRC) Approaches for Estimating Recharge Using the WTF Method

The MRC approach used in the WTF method is an automated or semi-automated procedure for calculating DH(tj) from water-level data. This approach develops an expression for the MRC that can be used to predict the slope of the hydrograph in the absence of recharge. Once the MRC is established, positive deviations of the hydrograph from the MRC are attributed to recharge, allowing recharge to be quantified even during periods of falling groundwater levels. Because of the need for daily water-level data, the MRC approach can be applied only at sites where water levels were continuously monitored.

Even though multiple steps are required, the MRC approaches are straightforward and easy to apply. The approaches avoid subjectivity after the estimation of the MRC parameters, but there remains the possibility that water-level rises that were not due to recharge may have been improperly included in the calculations. At least three different MRC approaches have been developed:

Accessibility FOIA Privacy Policies and Notices

Take Pride in America logo USA.gov logo U.S. Department of the Interior | U.S. Geological Survey
URL: http://water.usgs.gov/ogw/gwrp/methods/wtf/estimating_mrcapproach.html
Page Contact Information: Contact the Groundwater Resources Program
Page Last Modified: Tuesday, 03-Jan-2017 20:46:53 EST