OwnerNational Renewable Energy Laboratory (NREL) - view all
Update frequencyunknown
Last updatedabout 1 year ago
Overviewbiotitechemistrychloritedissolutionegsenergyenhanced geothermal systemsfeldsparfracture permeabilitygeochemistrygeothermalillitekinetic datakineticsmuscoviterate equationssuccess
Chemical reactions pose an important but poorly understood threat to EGS long-term success because of their impact on fracture permeability. This report summarizes the dissolution rate equations for layered silicates where data were lacking for geothermal systems. Here we report updated rate laws for chlorite (Carroll and Smith 2013), biotite (Carroll and Smith, 2015), illite (Carroll and Smith, 2014), and for muscovite. Also included is a spreadsheet with rate data and rate equations for use in reactive transport simulators.
Additional Information
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dcat_issued2017-02-24T07:00:00Z
dcat_modified2018-06-13T17:05:44Z
dcat_publisher_nameLawrence Livermore National Laboratory
guidhttps://data.openei.org/submissions/3594
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