Digital model simulation of the glacial-outwash aquifer at Dayton, Ohio

Water-Resources Investigations Report 75-18
Prepared in cooperation with The Miami Conservancy District
By:

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Abstract

Dayton, Ohio and its environs obtain most of their water from wells which penetrate highly productive glacial-outwash deposits underlying the Great Miami River and its tributaries and receive recharge by induced streambed leakage. Combined municipal and industrial use of ground water in the 90-square-mile area has increased from about 180 cubic feet per second in 1960 to nearly 250 cubic feet per second in 1972. The increased pumpage has resulted in continuing water-level declines in some parts of the area.

A digital model which uses a finite-difference approximation technique to solve partial differential equations of flow through a porous medium was used to evaluate the effects of pumping stresses on water levels. The simulated head values presented in map form generally are in good agreement with potentiometric-surface maps prepared from field measurements.

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Additional publication details

Publication type Report
Publication Subtype USGS Numbered Series
Title Digital model simulation of the glacial-outwash aquifer at Dayton, Ohio
Series title Water-Resources Investigations Report
Series number 75-18
DOI 10.3133/wri7518
Year Published 1975
Language English
Publisher U. S. Geological Survey
Publisher location Columbus, OH
Contributing office(s) Ohio Water Science Center
Description iv, 25 p.
Country United States
State Ohio
City Dayton
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