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USGS · 70241807

Hydraulics of sheetlike solution cavities

Gerald K. Moore
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Abstract

The sheetlike solution cavities that supply water to most wells in central Tennessee are 100 to 2,500 feet wide and less than 0.2 inch high. These dimensions have a scale similar to those in Hele-Shaw models. Both logical and mathematical evidence indicate laminar ground-water flow, except close to pumping wells. The Theis nonequilibrium formula may be used to analyze aquifer-test data and to calculate significant values for transmissivity and storage. The Navier-Stokes equation and the Darcy equation for steady-state conditions may be used to estimate cavity dimensions.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 34.982972° to 36.678118° latitude; -90.309877° to -81.6469° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Gerald K. Moore. 2006-07-06. Hydraulics of sheetlike solution cavities. https://doi.org/10.1111/j.1745-6584.1973.tb02976.x

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