Saline-water intrusion in the Floridan Aquifer in the Fernandina Beach area, Nassau County, Florida
Water-Resources Investigations Report
77-32
By: Roy W. Fairchild and C.B. Bentley
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Abstract
The Floridan aquifer is the major source of water for municipal and industrial use in northeastern Nassau County, Florida. Pumpage from the aquifer at Fernandina Beach has created a cone of depression in the potentiometric surface which is at or below sea level in a 35-square mile area. Since 1880 water levels have declined more than 120 feet near the center of pumping, and chloride concentrations have increased from about 20 to a maximum of 800 milligrams per liter in some deep wells. The saline water probably is connate water which comes from zones below 1,250 and 2,000 feet. Several alternate methods to control the migration of saline water are discussed. (Woodard-USGS)
Suggested Citation
Fairchild, R.W., Bentley, C., 1977, Saline-water intrusion in the Floridan Aquifer in the Fernandina Beach area, Nassau County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-32, iv, 27 p., https://doi.org/10.3133/wri7732.
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Saline-water intrusion in the Floridan Aquifer in the Fernandina Beach area, Nassau County, Florida |
| Series title | Water-Resources Investigations Report |
| Series number | 77-32 |
| DOI | 10.3133/wri7732 |
| Year Published | 1977 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Description | iv, 27 p. |
| Country | United States |
| State | Florida |
| County | Nassau County |