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Barometric fluctuations in wells tapping deep unconfined aquifers.

Water Resources Research

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Abstract

Barometric effects on water levels in unconfined aquifers can be computed by solution of the differential equation governing the flow of gas in the unsaturated zone subject to the appropriate boundary conditions. Solutions to this equation for two sets of boundary conditions were applied to compute water level response in a well tapping the Ogallala Formation near Lubbock, Texas from simultaneous microbarograph records. -from Author

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Barometric fluctuations in wells tapping deep unconfined aquifers.
Series title:
Water Resources Research
Volume
15
Issue:
5
Year Published:
1979
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Water Resources Research
First page:
1167
Last page:
1176