OwnerNational Renewable Energy Laboratory (NREL) - view all
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Last updatedabout 1 year ago
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OverviewCO2chloritegeothermalkineticstemperature
Chlorite dissolution kinetics were measured under far from equilibrium conditions using a mixed-flow reactor over temperatures of 100-275 degrees C at pH values of 3.0-5.7 in a background solution matrix of 0.05 m NaCl. Over this temperature range, magnesium was released congruently with respect to silica. The effect of variable pCO2 levels representative of engineered geothermal systems with CO2 as a heat-exchanging fluid (CO2-EGS) was explored by reacting chlorite with solutions containing a range of dissolved CO2 concentrations (0.1-0.5 M).
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dcat_issued2013-07-01T06:00:00Z
dcat_modified2017-05-25T15:24:10Z
dcat_publisher_nameLawrence Livermore National Laboratory
guidhttps://data.openei.org/submissions/3072
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- PDFChlorite Dissolution.pdf