Processes affecting the distribution of selenium in shallow ground water of agricultural areas, western San Joaquin Valley, California

Open-File Report 87-220
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Abstract

A study was undertaken to evaluate the processes affecting the chemistry of shallow ground water associated with agricultural drainage systems in the western San Joaquin Valley, California. The study was prompted by a need for an understanding of selenium mobility in areas having high selenium concentrations in shallow ground water. Groundwater samples were collected along transects in three artificially drained fields where the age of the drainage system varied (15, 6, and 1.5 years). Selenium concentrations in the drainage water also varied (0F30, 58, and 3700 micrograms per liter, respectively). Isotopic enrichment and chemical composition of the ground-water samples indicate that saline- and selenium-enriched water has evolved as a result of evaporation of ground water. This evaporated, isotopically enriched water is being displaced by more recent, less saline irrigation water percolating through the root zone. This displace-ment seems to be a process whereby sodium chloride and sodium sulfate water is being replaced by more dilute calcium sulfate and calcium bicarbonate water.

Publication type Report
Publication Subtype USGS Numbered Series
Title Processes affecting the distribution of selenium in shallow ground water of agricultural areas, western San Joaquin Valley, California
Series title Open-File Report
Series number 87-220
DOI 10.3133/ofr87220
Year Published 1987
Language English
Publisher U.S. Geological Survey
Description iv, 14 p.
Country United States
State California
Other Geospatial San Joaquin Valley
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