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- W2030485440 abstract "Deuterium and oxygen-18 were used as passive tracers to separate streamflow into “old” or “pre-event” and “new” or “event” components during spring snowmelt in 1987 in a small catchment in the southern Laurentians of Quebec. The old water component of flow appeared to respond to the diurnal snowmelt cycle, accounting for up to 85% of the hydrograph rise from morning to late afternoon. Assumptions concerning constancy of new water concentrations and homogeneity of old water were not satisfied; however, sensitivity analyses indicated that it can be concluded that old water was a major component of streamflow. Mobilization of old vadose storage may have been an important process in runoff generation. Sampling variability of new water concentrations is documented and consequent uncertainty in separations is discussed." @default.
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- W2030485440 date "1989-12-01" @default.
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- W2030485440 title "Tracing runoff sources with deuterium and oxygen-88 during spring melt in a headwater catchment, southern Laurentians, Quebec" @default.
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- W2030485440 doi "https://doi.org/10.1016/0022-1694(89)90185-6" @default.
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