Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C

Publicly accessible License 

Chemical reactions pose an important but poorly understood threat to EGS long-term success because of their impact on fracture permeability. This report summarizes the dissolution rate equations for layered silicates where data were lacking for geothermal systems. Here we report updated rate laws for chlorite (Carroll and Smith 2013), biotite (Carroll and Smith, 2015), illite (Carroll and Smith, 2014), and for muscovite. Also included is a spreadsheet with rate data and rate equations for use in reactive transport simulators.

Citation Formats

Lawrence Livermore National Laboratory. (2017). Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C [data set]. Retrieved from https://dx.doi.org/10.15121/1441454.
Export Citation to RIS
Carroll, Susan, Smith, Megan M., and Lammers, Kristin. Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C. United States: N.p., 24 Feb, 2017. Web. doi: 10.15121/1441454.
Carroll, Susan, Smith, Megan M., & Lammers, Kristin. Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C. United States. https://dx.doi.org/10.15121/1441454
Carroll, Susan, Smith, Megan M., and Lammers, Kristin. 2017. "Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C". United States. https://dx.doi.org/10.15121/1441454. https://gdr.openei.org/submissions/910.
@div{oedi_910, title = {Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C}, author = {Carroll, Susan, Smith, Megan M., and Lammers, Kristin.}, abstractNote = {Chemical reactions pose an important but poorly understood threat to EGS long-term success because of their impact on fracture permeability. This report summarizes the dissolution rate equations for layered silicates where data were lacking for geothermal systems. Here we report updated rate laws for chlorite (Carroll and Smith 2013), biotite (Carroll and Smith, 2015), illite (Carroll and Smith, 2014), and for muscovite. Also included is a spreadsheet with rate data and rate equations for use in reactive transport simulators.}, doi = {10.15121/1441454}, url = {https://gdr.openei.org/submissions/910}, journal = {}, number = , volume = , place = {United States}, year = {2017}, month = {02}}
https://dx.doi.org/10.15121/1441454

Details

Data from Feb 24, 2017

Last updated Jun 13, 2018

Submitted Feb 24, 2017

Organization

Lawrence Livermore National Laboratory

Contact

Susan Carroll

925.423.5694

Authors

Susan Carroll

Lawrence Livermore National Laboratory

Megan M. Smith

Lawrence Livermore National Laboratory

Kristin Lammers

Lawrence Livermore National Laboratory

DOE Project Details

Project Name The Viability of Sustainable, Self-Propping Shear Zones in Enhanced Geothermal Systems: Measurement of Reaction Rates at Elevated Temperatures

Project Lead Lauren Boyd

Project Number FY14 AOP 1422

Share

Submission Downloads