Altitude of the potentiometric surface in the Mississippi River Valley alluvial aquifer, spring 2018

Virginia L. McGuire; Ronald C. Seanor; William H. Asquith; Anna M. Nottmeier; David C. Smith; Roland W. Tollett; Wade H. Kress; Kellan R. Strauch

doi:10.3133/sim3453

USGS · sim3453

Altitude of the potentiometric surface in the Mississippi River Valley alluvial aquifer, spring 2018

Virginia L. McGuire·Ronald C. Seanor·William H. Asquith·Anna M. Nottmeier·David C. Smith·Roland W. Tollett·Wade H. Kress·Kellan R. Strauch

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Abstract

A potentiometric-surface map for spring 2018 was created for the Mississippi River Valley alluvial (MRVA) aquifer using available groundwater-altitude data from 1,126 wells completed in the MRVA aquifer and from the altitude of the top of the water surface in area rivers from 66 streamgages. Personnel from Arkansas Natural Resources Commission, Arkansas Department of Health, Arkansas Geological Survey, Illinois Department of Agriculture, Illinois State Water Survey, Louisiana Department of Natural Resources, Louisiana Department of Transportation and Development, Mississippi Department of Environmental Quality, Missouri Department of Natural Resources, Yazoo Mississippi Delta Joint Water Management District, U.S. Department of Agriculture-Natural Resources Conservation Service, and U.S. Geological Survey (USGS) routinely collect groundwater-level data from wells screened in the MRVA aquifer. The USGS and the U.S. Army Corps of Engineers routinely collect data on river stage and streamflow for the rivers overlying the MRVA aquifer area. The potentiometric-surface map for 2018 was created utilizing existing groundwater and surface-water altitudes to support investigations to characterize the MRVA aquifer as part of the USGS Water Availability and Use Science Program. Sufficient data were available to map the potentiometric surface of the MRVA aquifer for spring 2018 for about 87 percent of the aquifer area. The potentiometric contours ranged from 10 to 340 feet above North American Vertical Datum of 1988. The regional direction of groundwater flow was generally to the south-southwest, except in areas of groundwater-altitude depressions, where groundwater flowed into the depression, and near rivers, where flow can be from aquifer to the river or from the river into the aquifer. There are large depressions in the potentiometric-surface map in the lower one-half of the Cache region and in most of the Grand Prairie and Delta regions.

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Source-reported bounding extent: 28.92163128242129° to 37.33522435930639° latitude; -92.3291015625° to -87.978515625° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Virginia L. McGuire, Ronald C. Seanor, William H. Asquith, Anna M. Nottmeier, David C. Smith, Roland W. Tollett, Wade H. Kress, Kellan R. Strauch. 2020-05-12. Altitude of the potentiometric surface in the Mississippi River Valley alluvial aquifer, spring 2018. https://doi.org/10.3133/sim3453

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