δ18O, δD and 3H measurements constrain groundwater recharge patterns in an upland fractured bedrock aquifer, Vermont, USA

Michael D. Abbott; Andrea Lini; Paul R. Bierman

doi:10.1016/s0022-1694(00)00149-9

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δ18O, δD and 3H measurements constrain groundwater recharge patterns in an upland fractured bedrock aquifer, Vermont, USA

Michael D. Abbott Andrea Lini Paul R. Bierman

Year: 2000 Journal: Journal of Hydrology Vol: 228 (1-2)Pages: 101-112 Publisher: Elsevier BV

DOI: 10.1016/s0022-1694(00)00149-9

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Keywords:

Groundwater recharge Groundwater Aquifer Evapotranspiration Bedrock Hydrology (agriculture) δ18O Geology Precipitation Meteoric water Environmental science Stable isotope ratio Geomorphology Geography Ecology

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Groundwater and Isotope Geochemistry

Physical Sciences → Earth and Planetary Sciences → Geochemistry and Petrology

Groundwater flow and contamination studies

Physical Sciences → Environmental Science → Environmental Engineering

Hydrology and Watershed Management Studies

Physical Sciences → Environmental Science → Water Science and Technology

δ18O, δD and 3H measurements constrain groundwater recharge patterns in an upland fractured bedrock aquifer, Vermont, USA

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