OwnerNational Renewable Energy Laboratory (NREL) - view all
Update frequencyunknown
Last updatedover 1 year ago
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Overviewdissolution kineticsequationexperimentgeothermalilliteillite dissolutionrate
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.
Additional Information
KeyValue
dcat_issued2014-10-17T06:00:00Z
dcat_modified2017-06-27T14:27:37Z
dcat_publisher_nameLawrence Livermore National Laboratory
guidhttps://data.openei.org/submissions/3270
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Files
- XLSXResults.xlsx