Abstract
The use of natural and anthropogenic isotopic tracers — both stable and radioactive — is a well-developed biogeochemical technique used in evaluating water-borne chemical fluxes (see Broecker and Peng 1982; Fry and Sherr 1984; Rundel et al. 1988; Griffiths 1991). Watersheds in temperate regions have been studied extensively using stable isotopes (oxygen-18 and deuterium) to follow water flow paths (e.g., Dinçer et al. 1970; Sklash and Farvolden 1979; Bottomley et al. 1986; Hooper and Shoemaker 1986; Kennedy et al. 1986; Obradovic and Sklash 1976; Pearce et al. 1986; Sklash et al. 1986; DeWalle et al. 1988; Swistock et al. 1989; Wels et al. 1991). However, there are few examples of simultaneous work tracing the fate of particle-reactive isotopes in snow, and even fewer isotopic applications in watersheds underlain by permafrost.
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Cooper, L.W. et al. (1996). Isotopic Tracers for Investigating Hydrological Processes. In: Reynolds, J.F., Tenhunen, J.D. (eds) Landscape Function and Disturbance in Arctic Tundra. Ecological Studies, vol 120. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-01145-4_8
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DOI: https://doi.org/10.1007/978-3-662-01145-4_8
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