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- W137398501 abstract "Twelve monthly measurements were made of the delta/sup 18/O of the water and of the dissolved sulfates in inlet streams and in outlet streams of lakes in three watersheds in the Adirondack Park region of New York. The average delta/sup 18/O/sub H/sub 2/O/ of the surface waters (streams and lakes) of the three watersheds was well within the typical range of seasonally varying delta/sup 18/O/sub H/sub 2/O/ of precipitation water; however, the delta/sup 18/O/sub SO/sub 4//sup 2 -// of the surface waters was significantly lower than the typical range of seasonally varying delta/sup 18/O/sub SO/sub 4//sup 2 -// in precipitation water. Two possible causes for the apparent alteration of delta/sup 18/O of the sulfates, during the water percolation of various ground strata in the ground link between the atmosphere and watershed lakes are: (1) bacteriological redox cycling, in which the sulfate is bacterially reduced, allowing isotopic equilibration between the HSO/sub 3//sup -/ ion and associated water, before catalytic reoxidation by air back to sulfate; and/or (2) ion exchange, in which the soil strata, containing chemically fixed sulfate, behave as a ''column'' which is not yet in sulfate-ion equilibrium with the sulfate in atmospheric recharge water." @default.
- W137398501 created "2016-06-24" @default.
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- W137398501 date "1985-01-01" @default.
- W137398501 modified "2023-09-27" @default.
- W137398501 title "Oxygen-18 study of the atmospheric-aquatic linkage in three Adirondack lake watersheds" @default.
- W137398501 hasPublicationYear "1985" @default.
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