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Geology and hydrology of the shallow alluvial aquifer, West Sharrard Gulch, Colorado

Technical Report ·
OSTI ID:6182630
Interactions between the alluvial groundwater and the surface water in West Sharrard Creek were studied during a series of investigations prompted by concerns over former waste disposal sites along the drainage. West Sharrard Gulch is adjacent to the former site of the Anvil Points Facility. The investigations involved well installations, groundwater monitoring and surface water studies. The studies revealed that surface water and groundwater along West Sharrard Gulch are linked by a series of recharge and discharge zones. These zones are in turn directly related to the gradients controlled by the differential erosion of various bedrock layers. Groundwater seeps were found at predictable locations based on the intersection of alluvial groundwater at streambed nickpoints. The nickpoints result when streambed erosion exposes sandstone lenses in the underlying Wasatch Formation. Information from well logs, groundwater monitoring records, and topographic maps was combined to form a conceptual model of the flow relationships. Similar models may have application for siting future waste disposal facilities related to oil shale development in the Piceance Creek Basin. 20 refs., 8 figs., 1 tab.
Research Organization:
Oak Ridge National Lab., TN (USA)
Sponsoring Organization:
DOE; USDOE, Washington, DC (USA)
DOE Contract Number:
AC05-84OR21400
OSTI ID:
6182630
Report Number(s):
ORNL/TM-11467; ON: DE91009046
Country of Publication:
United States
Language:
English

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