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Retention time and flow patterns in Lake Marion, South Carolina, 1984

Water-Resources Investigations Report 95-4145
By:  and 
https://doi.org/10.3133/wri954145

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Abstract

In 1984, six dye tracer tests were made on Lake Marion to determine flow patterns and retention times under conditions of high and low flow. During the high-flow tests, with an average inflow of about 29,000 cubic feet per second, the approximate travel time through the lake for the peak tracer concentration was 14 days. The retention time was about 20 days. During the low-flow tests, with an average inflow of about 9,000 cubic feet per second, the approximate travel time was 41 days, and the retention time was about 60 days. The primary factors controlling movement of water in the lake are lake inflow and outflow. The tracer cloud moved consistently downstream, slowing as the lake widened. Flow patterns in most of the coves, and in some areas along the northeastern shore, are influenced more by tributary inflow than by factors attributable to water from the main body of the lake.

Suggested Citation

Patterson, G.G., Harvey, R., 1995, Retention time and flow patterns in Lake Marion, South Carolina, 1984: U.S. Geological Survey Water-Resources Investigations Report 95-4145, vi, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954145.

Study Area

Publication type Report
Publication Subtype USGS Numbered Series
Title Retention time and flow patterns in Lake Marion, South Carolina, 1984
Series title Water-Resources Investigations Report
Series number 95-4145
DOI 10.3133/wri954145
Year Published 1995
Language ENGLISH
Publisher U.S. Dept. of the Interior, U.S. Geological Survey ; Earth Science Information Center, Open-File Services Section,
Contributing office(s) South Atlantic Water Science Center
Description vi, 52 p. :ill., maps ;28 cm.
Country United States
State South Carolina
Other Geospatial Lake Marion
Additional publication details