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Illite Dissolution Rates and Equation (100 to 280 dec C)
The objective of this suite of experiments was to develop a useful kinetic dissolution expression for illite applicable over an expanded range of solution pH and temperature conditions representative of subsurface conditions in natural and/or engineered geothermal reservoirs. Using our new data, the resulting rate equation is dependent on both pH and temperature and utilizes two specific dissolution mechanisms (a “neutral” and a “basic” mechanism). The form of this rate equation should be easily incorporated into most existing reactive transport codes for to predict rock-water interactions in EGS shear zones.
- Publication Date:
- Report Number(s):
- DOE Contract Number:
- FY14 AOP 126.96.36.199
- Product Type:
- Research Org(s):
- DOE Geothermal Data Repository; Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
- Lawrence Livermore National Laboratory
- Sponsoring Org:
- USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Office (EE-4G)
- 15 Geothermal Energy; geothermal; illite; dissolution kinetics; illite dissolution
- OSTI Identifier:
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