Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10
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.
Citation Formats
Lawrence Livermore National Laboratory. (2013). Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10 [data set]. Retrieved from https://dx.doi.org/10.15121/1148811.
. Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10. United States: N.p., 27 Sep, 2013. Web. doi: 10.15121/1148811.
. Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10. United States. https://dx.doi.org/10.15121/1148811
. 2013. "Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10". United States. https://dx.doi.org/10.15121/1148811. https://gdr.openei.org/submissions/246.
@div{oedi_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.}, doi = {10.15121/1148811}, url = {https://gdr.openei.org/submissions/246}, journal = {}, number = , volume = , place = {United States}, year = {2013}, month = {09}}
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.Keywords
geothermal, chlorite dissolution rate law, geochemistry, geothermal kinetic database, chemical alteration, EGS, chlorite dissolution rate, chlorite dissolution, dissolution rate, data, raw data, processed dataDOE Project Details
Project Lead Greg Stillman
Project Number FY13 AOP 25727
