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publication > water resources investigations > report 83-4249


U.S. Department of the Interior
US Geological Survey
WRI 83-4249

Hydrogeology of a Zone of Secondary Permeability in the Surficial Aquifer of Eastern Palm Beach County, Florida

Water-Resources Investigations Report 83-4249

By

Leo J. Swayze and Wesley L. Miller

ABSTRACT

The surficial aquifer is the primary source of fresh water for the heavily developed coastal area in eastern Palm Beach County. Well fields are generally located in a discontinuous zone of high secondary permeability in the surficial aquifer that extends from the Juno Beach area south to Broward County and varies in width from about 4 to 15 miles. This zone is the northernmost extension of the Biscayne aquifer. The zone, formed by varying dissolution of aquifer limestone materials during Pleistocene changes in sea level, ranges in depth from about sea level to 220 feet below sea level. Because of proximity to the Atlantic Ocean and saltwater estuaries on the east and diluted residual seawater to the west, the aquifer is susceptible to saltwater intrusion.

The ground water is predominantly a calcium bicarbonate type. Dissolved solids, calcium carbonate hardness, and chloride are greatest along the saltwater - intruded coastline and in the western part of the study area where diluted residual seawater exists. Total organic carbon increases inland because of infiltration of rainwater through thicker layers of organic soils.

Ground-water levels in the surficial aquifer in eastern Palm Beach County are strongly influenced by controlled levels in canals of the South Florida Water Management and the Lake Worth Drainage Districts. In March 1981 after 12 months of below-average rainfall, ground-water levels ranged from about 2 feet above sea level along the coast to nearly 21 feet above sea level, 15 miles inland in the northwest section of the study area.



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Last updated: 12 January, 2005 @ 03:14 PM (KP)