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Groundwater contamination at the Kesterson Reservoir, California. 1. Hydrogeologic setting and conservative solute transport

Journal Article · · Water Resources Research; (United States)
DOI:https://doi.org/10.1029/91WR00265· OSTI ID:5745963
; ; ;  [1];  [2]
  1. Lawrence Berkeley Lab., CA (United States)
  2. Geological Survey, Menlo Park, CA (United States)
Shallow groundwater under Kesterson Reservoir, Merced County, California, was contaminated over a period of 6 years while the reservoir was used for disposal of brackish subsurface agricultural drainage water from farmlands in the San Joaquin Valley. Drainage water contained an average of 10,000 mg/L total dissolved solids (TDS), high concentrations of selenium (300 {mu}g/L), nitrate (37 mg/L as nitrogen), boron (15 mg/L), and lesser amounts of mercury, chromium, and molybdenum. Infiltration and lateral migration of this water created a 20-m-deep plume of high-TDS, boron-rich water covering an area of about 5 km{sup 2}. Transport of selenium and nitrate was inhibited by biogeochemical reactions in the pond bottom sediments, so that migration of these two constituents into the aquifer was limited. This paper focuses on physical parameters affecting seepage and lateral migration of nonreactive solutes and on hydrogeological factors associated with selenium breakthrough into the shallow aquifer.
DOE Contract Number:
AC03-76SF00098
OSTI ID:
5745963
Journal Information:
Water Resources Research; (United States), Journal Name: Water Resources Research; (United States) Vol. 27:6; ISSN 0043-1397; ISSN WRERA
Country of Publication:
United States
Language:
English