2002
DOI: 10.3133/ofr02354
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Lithologic and ground-water data for monitoring sites in the Mojave River and Warren Valley basins, San Bernardino County, California, 1992-1998

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Cited by 7 publications
(2 citation statements)
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“…Dissolved oxygen concentrations begin to decrease at this depth (Figure 3) and arsenic concentrations in this area may be controlled by geochemical factors, such as pH and redox at deeper depths, rather than geologic factors, such as the source of the alluvial deposits. Increasing arsenic concentrations with depth agrees with water-quality data for arsenic concentrations reported in Mojave River basin monitoring wells [6].…”
Section: Water-chemistry Datasupporting
confidence: 84%
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“…Dissolved oxygen concentrations begin to decrease at this depth (Figure 3) and arsenic concentrations in this area may be controlled by geochemical factors, such as pH and redox at deeper depths, rather than geologic factors, such as the source of the alluvial deposits. Increasing arsenic concentrations with depth agrees with water-quality data for arsenic concentrations reported in Mojave River basin monitoring wells [6].…”
Section: Water-chemistry Datasupporting
confidence: 84%
“…Arid regions of the southwestern United States often depend on groundwater resources to supply rapidly growing populations. Arsenic is in water from some wells in the Mojave River basin in the western Mojave Desert of southern California at concentrations in excess of the MCL for arsenic [5][6][7][8].…”
Section: Introductionmentioning
confidence: 99%