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K.W. Causseaux

Publications and source records attributed to K.W. Causseaux.

4 recordsLinked to original sources

The surficial aquifer in Pinellas County, Florida

The surficial aquifer in Pinellas County, Florida, contains potable water throughout most of the county and is a potential source of water to augment the public supply that is presently imported from adjacent counties. The county accounts for 38 percent of the public supply consumption of ground water in the 11-county area of west-central Florida and 68 percent of this water is imported from two adjacent counties. The surficial aquifer has a saturated thickness of more than 30 feet throughout most of the county. Specific capacity per foot of screen for wells is less than 0.1 gallon per minute per foot of drawdown in some parts of the county, but yield is sufficient in most of the county for many small uses with shallow-well pumps. Minimum potential yield varies from 5 gallons per minute in the northern part of the county to more than 30 gallons per minute in the south. Concentrations of iron are high enough in parts of the county to cause staining. Chloride concentrations are less than 100 milligrams per liter in most of the county and do not pose a problem for many uses. (USGS)

Water-Resources Investigations Report↗

Chloride concentrations in the coastal margin of the Floridan Aquifer, southwest Florida

The Floridan aquifer is the principal source of freshwater supply in southwest Florida. The freshwater part of the aquifer is underlain by saltwater in lower formations and is bounded on the west by saltwater in the coastal parts of the aquifer. A zone of mixing lies between the saltwater and freshwater. The saltwater and freshwater boundaries are defined by chloride concentrations of 19,000 milligrams per liter on the coastward side and 250 milligrams per liter on the landward side. Lateral intrusion of saltwater can occur along the coast in areas where the hydraulic gradient declines and upconing can occur in inland areas of heavy ground-water withdrawals. Safeguards against saltwater intrusion in these areas are necessary because flushing of the aquifer is a very slow process. A network of chloride monitor wells is proposed for the zone of mixing in the upper producing zone of the floridan aquifer. Seventy wells were selected at 54 sites to monitor chloride concentrations along the 250-milligram-per-liter line of equal chloride concentration. One-fourth of the wells are located in areas of increasing chloride concentrations or heavy ground-water withdrawals and the remaining wells are intended to improve delineation of the interface and to monitor long-term changes in chloride concentrations. (USGS)

Water-Resources Investigations Report↗

Position of the saltwater-freshwater interface in the upper part of the Floridan Aquifer, southwest Florida, 1979

Ground-water withdrawals in southwest Florida are increasing because of urban growth, industrial expansion and increased agricultural irrigation. As a result, the potentiometric surface of the Floridian aquifer has been lowered in some areas, allowing seawater to encroach into the aquifer and threaten the freshwater resources of the area. Effective management of groundwater is needed to control the encroachment and protect the freshwater aquifer.

Florida↗

Summary of U.S. Geological Survey investigations and hydrologic conditions in the Southwest Florida Water Management District for 1977

This report summarizes the activities of the Southwest Florida Subdistrict of the U.S. Geological Survey, Water Resources Division for fiscal year 1977. The organization and mission of the subdistrict office are described. The cooperative program for fiscal year 1977 included 41 interpretive investigations. Abstracts of twenty reports released by the subdistrict during 1977 and an extensive bibliography of reports released from 1933 to 1977 are included. The hydrologic setting of southwest Florida is outlined followed by discussions of surface-water, ground-water, and quality-of-water conditions. Hydrologic conditions in southwest Florida in 1977 are shown by the presentation of hydrographs from selected surface-water, ground-water, and lake-stage data collection sites.

Florida↗