Kinetics of Chlorite Dissolution at Elevated Temperatures and CO2 Conditions
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).
Citation Formats
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.
A2 - Smith, Megan M.
A3 - 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/6567
ER -
Carroll, Susan A., et al. Kinetics of Chlorite Dissolution at Elevated Temperatures and CO2 Conditions. Lawrence Livermore National Laboratory, 1 July, 2013, GDR. https://gdr.openei.org/submissions/222.
Carroll, S., Smith, M., & Wolery, T. (2013). Kinetics of Chlorite Dissolution at Elevated Temperatures and CO2 Conditions. [Data set]. GDR. Lawrence Livermore National Laboratory. https://gdr.openei.org/submissions/222
Carroll, Susan A., Megan M. Smith, and Thomas J. Wolery. Kinetics of Chlorite Dissolution at Elevated Temperatures and CO2 Conditions. Lawrence Livermore National Laboratory, July, 1, 2013. Distributed by GDR. https://gdr.openei.org/submissions/222
@misc{OEDI_Dataset_6567,
title = {Kinetics of Chlorite Dissolution at Elevated Temperatures and CO2 Conditions},
author = {Carroll, Susan A. and Smith, Megan M. and Wolery, Thomas J.},
abstractNote = {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).},
url = {https://gdr.openei.org/submissions/222},
year = {2013},
howpublished = {GDR, Lawrence Livermore National Laboratory, https://gdr.openei.org/submissions/222},
note = {Accessed: 2025-04-30}
}
Details
Data from Jul 1, 2013
Last updated May 25, 2017
Submitted Jul 1, 2013
Organization
Lawrence Livermore National Laboratory
Contact
Authors
Original Source
https://gdr.openei.org/submissions/222Research Areas
Keywords
geothermal, chlorite, kinetics, CO2, temperatureDOE Project Details
Project Name Chemical Impact of Elevated CO2 on Geothermal Energy Production
Project Lead Greg Stillman
Project Number AID 19980
