Characterization of surface and ground w
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Michael M. Reddy; Paul Schuster; Carol Kendall; Micaela B. Reddy
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Article
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2006
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John Wiley and Sons
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English
⚖ 349 KB
18 O is an ideal tracer for characterizing hydrological processes because it can be reliably measured in several watershed hydrological compartments. Here, we present multiyear isotopic data, i.e. 18 O variations (υ 18 O), for precipitation inputs, surface water and groundwater in the Shingobee Riv