The hydrogen isotopic fractionation factor between brucite and water has been determined in the temperature range of 100~ ~ C. Brucite is always depleted in deuterium relative to the coexisting water, and the degree of depletion becomes larger with decreasing temperature. The fractionation factor ch
β¦ LIBER β¦
Experimental studies of oxygen and hydrogen isotope fractionations between brucite and water at low temperatures
β Scribed by Baolong Xu; Yong-Fei Zheng
- Book ID
- 105644406
- Publisher
- Springer
- Year
- 1998
- Tongue
- English
- Weight
- 57 KB
- Volume
- 43
- Category
- Article
- ISSN
- 1001-6538
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