Estimated hydrologic characteristics of shallow aquifer systems in the Valley and Ridge, the Blue Ridge, and the Piedmont Physiographic Provinces based on analysis of streamflow recession and base flow

A. T. Rutledge; T. O. Mesko

doi:10.3133/pp1422b

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Estimated hydrologic characteristics of shallow aquifer systems in the Valley and Ridge, the Blue Ridge, and the Piedmont Physiographic Provinces based on analysis of streamflow recession and base flow

A. T. Rutledge·T. O. Mesko

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Abstract

Inferences are drawn about properties of aquifer systems from the interpretation of streamflow records in the Appalachian Valley and Ridge, Piedmont, and Blue Ridge physiographic provinces. The analysis is divided into two parts--analysis of streamflow recession and base-flow analysis. Analysis of recession yields information about aquifer diffusivity and variation in specific yield. Base-flow analysis is used to develop water balances for representative basins in the study area.

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Source-reported bounding extent: 32.84267363195431° to 41.902277040963696° latitude; -87.73681640625° to -73.916015625° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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A. T. Rutledge, T. O. Mesko. 1996. Estimated hydrologic characteristics of shallow aquifer systems in the Valley and Ridge, the Blue Ridge, and the Piedmont Physiographic Provinces based on analysis of streamflow recession and base flow. https://doi.org/10.3133/pp1422b

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