Coupled fluctuations in element release during dolomite dissolution
Atomic force microscopy has been used to determine more precisely the mechanism of the initial stages of dolomite dissolution. Analysis of outflow solutions initially shows fluctuations of both Ca and Mg release with concentrations of Ca >> Mg. The dolomite surface dissolves congruently in the...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Mineralogical Society
2014
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| Online Access: | http://hdl.handle.net/20.500.11937/45442 |