Excerpt from Relation of Salinity and Selenium in Shallow Ground Water to Hydrologic and Geochemical Processes, Western San Joaquin Valley, California
Samples of shallow ground water were collected at 118 observation wells dis tributed throughout the study area (fig. Seventy-two of the wells were sam pled during an 18-day period in spring 1984. Forty-six wells were sampled in the spring of 1986. Samples collected at these 46 wells were analyzed for deuter ium and oxygen-18 (fig. The wells are 6 to 10 m deep and constructed of polyvinyl chloride pipe perforated over the entire depth of the well.
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