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Title: Distribution and mobility of selenium and other trace elements in shallow ground water of the western San Joaquin Valley, California

Book ·
OSTI ID:6701431

Samples of shallow groundwater that underlies much of the irrigated area in the western San Joaquin Valley of California were analyzed for various major ions and trace elements, including selenium. Concentrations of the major ions generally were similar for groundwater collected in the two primary geologic zones - the alluvial fan and basin trough. Most of the variance in concentrations of major ions, as determined by principal components analysis, was associated with groundwater salinity and the dominant ions - magnesium, sodium, sulfate, and chloride. Most of the variance in trace elements was associated with concentrations of boron, molybdenum, selenium, and vanadium, which are present as mobile oxyanions. The concentrations of oxyanions trace elements were significantly correlated with groundwater salinity, but the correlations between selenium and salinity and molybdenum and salinity were significantly difference in the alluvial fan geologic zone compared with the basin-trough geologic zone. In addition, selenium concentrations are significant higher in the groundwater of the alluvial fan zone than in the basin-trough zone. The Evidence suggests that the main factors influencing selenium concentrations in the shallow groundwater are the degree of groundwater salinity and geologic source of the alluvial soil material. 31 refs., 5 figs., 3 tabs.

OSTI ID:
6701431
Resource Relation:
Related Information: USGS Open-File Report 86-538
Country of Publication:
United States
Language:
English