Oxygen isotope fractionation during smithsonite formation from aqueous solutions
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چکیده
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Hydrogen Isotope Fractionation in Aqueous Alkali Halide Solutions
The D/H ratios of hydrogen gas in equilibrium with aqueous alkali halide solutions were determined at 25 °C, using a hydrophobic platinum catalyst. The hydrogen isotope effect between the solution and pure water changes linearly with the molality of the solution at low concentrations, but deviates from this linearity at higher concentration for all alkali halide solutions. The magnitude of the ...
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ژورنال
عنوان ژورنال: Chemical Geology
سال: 2018
ISSN: 0009-2541
DOI: 10.1016/j.chemgeo.2018.08.005