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          <dc:title>Anthropogenic and
Geogenic Factors Affecting Groundwater
Arsenic and Potential Drinking Water Exposure in the San Luis Valley,
Colorado</dc:title>
          <dc:creator>Ryan G. Smith (6255986)</dc:creator>
          <dc:creator>Alandra M. Lopez (9719690)</dc:creator>
          <dc:creator>Alexandder S. Honeyman (25138540)</dc:creator>
          <dc:creator>Dawson Carney (20737595)</dc:creator>
          <dc:creator>Scott Fendorf (415363)</dc:creator>
          <dc:creator>Melissa A. Lombard (9981454)</dc:creator>
          <dc:creator>Matthew O. Gribble (6556550)</dc:creator>
          <dc:creator>Abdullah Al Fatta (21688841)</dc:creator>
          <dc:creator>Katherine A. James (16017412)</dc:creator>
          <dc:subject>Biotechnology</dc:subject>
          <dc:subject>Environmental Sciences not elsewhere classified</dc:subject>
          <dc:subject>Ecology</dc:subject>
          <dc:subject>Biological Sciences not elsewhere classified</dc:subject>
          <dc:subject>Cancer</dc:subject>
          <dc:subject>Inorganic Chemistry</dc:subject>
          <dc:subject>test data sets</dc:subject>
          <dc:subject>serious health threat</dc:subject>
          <dc:subject>san luis valley</dc:subject>
          <dc:subject>including redox potential</dc:subject>
          <dc:subject>heterogeneous aquifer geochemistry</dc:subject>
          <dc:subject>driven data set</dc:subject>
          <dc:subject>many recent studies</dc:subject>
          <dc:subject>domestic wells changes</dc:subject>
          <dc:subject>including surface elevation</dc:subject>
          <dc:subject>grained aquifer sediments</dc:subject>
          <dc:subject>depth continuously across</dc:subject>
          <dc:subject>435 groundwater measurements</dc:subject>
          <dc:subject>model produces pseudo</dc:subject>
          <dc:subject>geothermal fluid influence</dc:subject>
          <dc:subject>colorado groundwater arsenic</dc:subject>
          <dc:subject>grained sediments</dc:subject>
          <dc:subject>private wells</dc:subject>
          <dc:subject>many regions</dc:subject>
          <dc:subject>geothermal influences</dc:subject>
          <dc:subject>well depth</dc:subject>
          <dc:subject>trace metals</dc:subject>
          <dc:subject>term subsidence</dc:subject>
          <dc:subject>spatial variability</dc:subject>
          <dc:subject>several known</dc:subject>
          <dc:subject>residents rely</dc:subject>
          <dc:subject>positive relationship</dc:subject>
          <dc:subject>major ions</dc:subject>
          <dc:subject>improving understanding</dc:subject>
          <dc:subject>important predictors</dc:subject>
          <dc:subject>global scales</dc:subject>
          <dc:subject>elemental indicators</dc:subject>
          <dc:subject>drinking water</dc:subject>
          <dc:subject>depth due</dc:subject>
          <dc:subject>dependent exposure</dc:subject>
          <dc:subject>biogeochemical conditions</dc:subject>
          <dc:subject>3d estimates</dc:subject>
          <dc:description>Groundwater arsenic is a serious health threat in many
regions
with limited surface water drinking supplies. In the San Luis Valley,
Colorado, USA, where most residents rely on groundwater for drinking
water, elevated groundwater arsenic concentrations (≥5 μg/L)
were observed in 19.8% of private wells. Many recent studies have
leveraged data science methods to estimate the spatial variability
of arsenic at local, regional, and global scales. These studies typically
predict depth-independent arsenic concentrations due to limited well
depth information. However, arsenic concentrations may vary greatly
with depth due to heterogeneous aquifer geochemistry, including redox
potential, pH, and biogeochemical conditions. In this study, we apply
random forest modeling to predict elevated groundwater arsenic concentrations
(≥5 μg/L) over space and depth continuously across the
San Luis Valley using a community-driven data set of 435 groundwater
measurements of major ions and trace metals. Our model reveals the
influence of several known or hypothesized drivers or proxy drivers
of arsenic in groundwater, including surface elevation, fraction of
fine-grained aquifer sediments, well depth, soil pH, long-term subsidence,
and geothermal influences. Elevation, percentage of fine-grained sediments,
and elemental indicators of geothermal fluid influence are some of
the most important predictors of arsenic, while long-term subsidence
is found to have a weak but positive relationship with arsenic. The
model has a specificity of 0.82 and a sensitivity of 0.81 on held-out
test data sets. In addition to improving understanding of drivers
of arsenic in the region, this model produces pseudo-3D estimates
of groundwater arsenic. The model can also be used to assess the time-dependent
exposure to arsenic as the depth of domestic wells changes over time.</dc:description>
          <dc:date>2026-09-29T00:00:00Z</dc:date>
          <dc:type>Text</dc:type>
          <dc:type>Journal contribution</dc:type>
          <dc:identifier>10.1021/acs.est.6c02761.s001</dc:identifier>
          <dc:relation>https://figshare.com/articles/journal_contribution/Anthropogenic_and_Geogenic_Factors_Affecting_Groundwater_Arsenic_and_Potential_Drinking_Water_Exposure_in_the_San_Luis_Valley_Colorado/34027276</dc:relation>
          <dc:rights>CC BY-NC 4.0</dc:rights>
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