An experimental study of dolomite dissolution rates as a function of pH from −0.5 to 5 and temperature from 25 to 80°C
- 1 May 1999
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 157 (1-2) , 13-26
- https://doi.org/10.1016/s0009-2541(98)00193-4
Abstract
No abstract availableKeywords
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