Control of silicate weathering by interface-coupled dissolutionprecipitation processes at the mineral-solution interface
The mechanism of surface coating formation (the so-called surface altered layers [SALs] or leached layers) during weathering of silicate minerals is controversial and hinges on understanding the saturation state of the fluid at the dissolving mineral surface. Here we present in-situ data on the evol...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Geological Society of America
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/22602 |