Feldspar dissolution kinetics and equilibrium: Implications for natural and engineered systems
The chemical composition of groundwater is controlled largely by subsurface mineral/fluid interactions. Experimental measurement of plagioclase dissolution rates provides a critical means of understanding the relationship between groundwater composition and reservoir characteristics. This thesis foc...
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| Format: | Others |
| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/1911/18736 |