Oxygen Isotope Fractionation between Carbonate Minerals and Carbonic Acid Systems and Constraints for Environmental Science and Geological Processes
The equilibrium oxygen isotope fractionation factor is widely used in geological thermometry. However, under most natural conditions, the oxygen isotope exchange is rare to reach equilibrium. Especially for the complex water–rock interaction process, the contribution of the H<sub>2</sub>...
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| Format: | Article |
| Language: | English |
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MDPI AG
2024-02-01
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| Series: | Molecules |
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| Online Access: | https://www.mdpi.com/1420-3049/29/3/698 |