Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Ground water levels in the vicinity of the Miami well field, Montgomery County, Ohio

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5597811
 [1];  [2]
  1. Roy F. Weston, Inc., Cincinnati, OH (United States)
  2. Ohio Dept. of Natural Resources, Columbus, OH (United States)

During the early stages of the drought of 1987-88 in Ohio, a number of diminished capacity complaints were received from domestic well owners in northwestern Montgomery County. Most home owners blamed the nearby Dayton-Miami Well Field (MWF). The MWF is situated in a preglacial, bedrock valley filled with outwash deposits. In this area, sand and gravel outwash deposits from a buried valley aquifer. Glacial outwash also covers that uplands to the west, where a large number of domestic water wells are located. Recharge to the uplands is primarily by infiltration of precipitation. The buried valley aquifer is recharged via infiltration from the Great Miami River and precipitation. Recharge into the valley aquifer is enhanced from man-made recharge lagoons near the well field. Additional recharge to the well field occurs from ground water inflow from north of the well field, and inflow from the adjacent uplands to the east. Temporal changes in the extent of the cone of depression surrounding the well field are shown on potentiometric surface maps. Furthermore, the cone of depression extends into the glacial outwash deposits underlying the upland area, clearly indicating a hydraulic connection between the buried valley aquifer and these glacial outwash deposits beneath the upland area. This expanding cone of depression indicates that increased pumping is exceeding recharge and ground water is being removed from aquifer storage. Ground water levels in the MWF reached their lowest point during the drought of 1987-88. This was the period during which most domestic well failures occurred. If production from the MWF continues to increase and/or this region experience another prolonged drought, dewatering of domestic wells east of the MWF will likely reoccur.

OSTI ID:
5597811
Report Number(s):
CONF-921058--
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Journal Name: Geological Society of America, Abstracts with Programs; (United States) Vol. 24:7; ISSN GAAPBC; ISSN 0016-7592
Country of Publication:
United States
Language:
English

Similar Records

Complex interactions among glacial and bedrock aquifers in the River Styx basin, northeastern Ohio
Conference · Tue Dec 31 23:00:00 EST 1991 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:5806287

The bedrock topography of southwestern Ohio and its implications for Quaternary drainage changes
Conference · Tue Dec 31 23:00:00 EST 1991 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:5935776

Ground-water flow and recharge in the Mahomet Bedrock Valley Aquifer, east-central Illinois: A conceptual model based on hydrochemistry
Conference · Thu Mar 31 23:00:00 EST 1994 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:7123333