Fractionation of stable chlorine isotopes during transport through semipermeable membranes
The stable isotope ratio of chlorine is a potential hydrogeochemical tool. A recently-developed technique allows detection of differences in the isotope ratio of water samples. Measured variations cover a range of 3.0 ± 0.12 per mil. In deep aquifer brines, enrichment in 37C1 seems to increase with...
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| Language: | en |
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The University of Arizona.
1985
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| Online Access: | http://hdl.handle.net/10150/191280 |