Untersuchungen über das Gleichgewicht zw
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H. E. Usdowski; H. L. Barnes
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Article
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1972
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Springer
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English
⚖ 753 KB
During equilibration of K-feldspar, quartz and muscovite with dilute KCl-solutions, the change in pH of the solution was measured as a function of time. The resulting equilibrium constant, K T = a K +/att +, is 104-~14-0.08, 105.s6 • and 106.~ at 300, 60 and 30 ~ C respectively (standard states at 1