Calcite dissolution by mixing waters: geochemical modeling and flow-through experiments
Dissolution of carbonates has been commonly predicted by geochemical models to occur at the seawater-freshwater mixing zone of coastal aquifers along a geological time scale. However, field evidences are inconclusive: dissolution vs. lack of dissolution. In this study we investigate the process of c...
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| Vydáno v: | Geologica Acta: an international earth science journal |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universitat de Barcelona
2011
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=50522124007 |
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