Model evaluation of the hydrogeology of the Morris Bridge well field and vicinity in West-Central Florida

Water-Resources Investigations Report 80-29
Prepared in cooperation with the Southwest Florida Water Management District
By: , and 

Links

Abstract

The Morris Bridge well field in west-central Florida, which is being developed may have a maximum well-field withdrawal of 40 million gallons per day. The water will be pumped from the Floridan aquifer--a sequence of carbonate rocks about 1,100 feet thick underlying surficial sand and clay deposits. A highly fractured and transmissive zone about 500 feet below National Geodetic Vertical Datum of 1929 will supply a large proportion of the water. Two-dimensional and three-dimensional digital flow models were used to evaluate the hydrogeology of the area. The model-derived leakance distribution (a property of the confining bed) for a 285-square-mile area ranged from 0.00002 to 0.008 per day. Model-derived transmissivity values for the Floridan aquifer ranged from 37,000 to 600,000 feet squared per day. Model-derived specific yield values for the surficial aquifer ranged from 0.05 to 0.30. The three-dimensional model was used to predict drawdowns in both the Floridan and surficial aquifers in response to a 40 million gallon per day stress. Mass-balance data from a 30-day simulation with no recharge from rainfall show percentage of withdrawn water that is derived from: (1) aquifer storage, (2) the Hillsborough River, and (3) reduction of evapotranspiration losses. (USGS)

Study Area

Publication type Report
Publication Subtype USGS Numbered Series
Title Model evaluation of the hydrogeology of the Morris Bridge well field and vicinity in West-Central Florida
Series title Water-Resources Investigations Report
Series number 80-29
DOI 10.3133/wri8029
Year Published 1980
Language English
Publisher U.S. Geological Survey
Description vi, 92 p.
Country United States
State Florida
Google Analytic Metrics Metrics page
Additional publication details