Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10

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We have calculated a chlorite dissolution rate equation at far from equilibrium conditions by combining new data (20 experiments at high temperature) with previously published data Smith et al. 2013 and Lowson et al. 2007. All rate data (from the 127 experiments) are tabulated in this data submission. More information on the calculation of the rate data can be found in our FY13 Annual support (Carroll LLNL, 2013) which has been submitted to the GDR and is linked below.

The rate equation fills a data gap in geothermal kinetic data base and can be used directly to estimate the impact of chemical alteration on all geothermal processes. It is especially important for understanding the role of chemical alteration in the weakening for shear zones in EGS systems.

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TY - DATA AB - We have calculated a chlorite dissolution rate equation at far from equilibrium conditions by combining new data (20 experiments at high temperature) with previously published data Smith et al. 2013 and Lowson et al. 2007. All rate data (from the 127 experiments) are tabulated in this data submission. More information on the calculation of the rate data can be found in our FY13 Annual support (Carroll LLNL, 2013) which has been submitted to the GDR and is linked below. The rate equation fills a data gap in geothermal kinetic data base and can be used directly to estimate the impact of chemical alteration on all geothermal processes. It is especially important for understanding the role of chemical alteration in the weakening for shear zones in EGS systems. DB - Geothermal Data Repository DP - Open EI | National Renewable Energy Laboratory DO - 10.15121/1148811 KW - geothermal KW - chlorite dissolution rate law KW - geochemistry KW - geothermal kinetic database KW - chemical alteration KW - EGS KW - chlorite dissolution rate KW - chlorite dissolution KW - dissolution rate KW - data KW - raw data KW - processed data LA - English DA - 2013/09/27 PY - 2013 PB - Lawrence Livermore National Laboratory T1 - Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10 UR - https://doi.org/10.15121/1148811 ER -
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. Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10. Lawrence Livermore National Laboratory, 27 September, 2013, Geothermal Data Repository. https://doi.org/10.15121/1148811.
. (2013). Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10. [Data set]. Geothermal Data Repository. Lawrence Livermore National Laboratory. https://doi.org/10.15121/1148811
. Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10. Lawrence Livermore National Laboratory, September, 27, 2013. Distributed by Geothermal Data Repository. https://doi.org/10.15121/1148811
@misc{GDR_Dataset_246, title = {Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10}, author = }, abstractNote = {We have calculated a chlorite dissolution rate equation at far from equilibrium conditions by combining new data (20 experiments at high temperature) with previously published data Smith et al. 2013 and Lowson et al. 2007. All rate data (from the 127 experiments) are tabulated in this data submission. More information on the calculation of the rate data can be found in our FY13 Annual support (Carroll LLNL, 2013) which has been submitted to the GDR and is linked below.

The rate equation fills a data gap in geothermal kinetic data base and can be used directly to estimate the impact of chemical alteration on all geothermal processes. It is especially important for understanding the role of chemical alteration in the weakening for shear zones in EGS systems.}, url = {https://gdr.openei.org/submissions/246}, year = {2013}, howpublished = {Geothermal Data Repository, Lawrence Livermore National Laboratory, https://doi.org/10.15121/1148811}, note = {Accessed: 2025-05-07}, doi = {10.15121/1148811} }
https://dx.doi.org/10.15121/1148811

Details

Data from Sep 27, 2013

Last updated Jul 6, 2021

Submitted Sep 27, 2013

Organization

Lawrence Livermore National Laboratory

Contact

Susan Carroll

925.423.5694

Authors

This submission does not list any authors.

DOE Project Details

Project Lead Greg Stillman

Project Number FY13 AOP 25727

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