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Earth’s “critical zone,” the zone of the planet from treetops to base of groundwater, is critical because it is a sensitive region, open to impacts from human activities, while providing water necessary for human consumption and food production. Quantifying water movement in the subsurface is critical to predicting how water-driven critical zone processes respond to changes in climate and human perturbation of the natural system. Here, Prof. Singha specifically focuses on the efficacy of the hyporheic zone—the zone of surface water and groundwater mixing— in two ~1 km stream reaches within the Bonita Peak Mining District, a U.S. Environmental Protection Agency Superfund site located near Silverton, Colorado, USA. High concentrations of trace metal(loid)s exported from abandoned mine wastes and acid-rock drainage pose a risk to the health of aquatic ecosystems. To determine if and when the hyporheic zone mediates metal(loid) export, her team investigated the relationship between streamflow, groundwater-stream connectivity, and subsurface metal(loid) concentrations.
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