TY - DATA AB - 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). AU - Carroll, Susan A. AU - Smith, Megan M. AU - Wolery, Thomas J. DB - Open Energy Data Initiative (OEDI) DP - Open EI | National Renewable Energy Laboratory DO - KW - geothermal KW - chlorite KW - kinetics KW - CO2 KW - temperature LA - English DA - 2013/07/01 PY - 2013 PB - Lawrence Livermore National Laboratory T1 - Kinetics of Chlorite Dissolution at Elevated Temperatures and CO2 Conditions UR - https://data.openei.org/submissions/ ER -