Dissolved-solids concentration in water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States
Open-File Report
82-94
By: Craig L. Sprinkle
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Abstract
The Tertiary limestone aquifer system of the southeastern United States is a thick sequence of carbonate rocks that range from Paleocene to Miocene in age and are hydraulically connected in varying degrees. The upper permeable zone of the aquifer system consists of the Tampa, Suwannee, Ocala, and Avon Park Limestones. Based on analyses of water samples from 591 selected wells, a map is presented which shows dissolved-solids concentration in ranges of 0-250, 251-500, 501-1,000, and greater than 1,000 mg/. Dissolved-solids concentrations and hydrochemical facies developed within the aquifer system are related to the predevelopment and modern-day ground-water flow system.
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Dissolved-solids concentration in water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States |
| Series title | Open-File Report |
| Series number | 82-94 |
| DOI | 10.3133/ofr8294 |
| Year Published | 1982 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Description | 1 Plate: 33.95 x 43.95 inches |
| Country | United States |
| State | Alabama, Florida, Georgia, South Carolina |
| Google Analytic Metrics | Metrics page |