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

Carroll, Susan

doi:10.15121/1148811

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

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Abstract

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.

Authors:: Carroll, Susan

Publication Date:: Fri Sep 27 00:00:00 EDT 2013

Research Org.:: USDOE Geothermal Data Repository (United States); Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)

Sponsoring Org.:: USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Program (EE-4G)

Contributing Org.:: Lawrence Livermore National Laboratory

OSTI Identifier:: 1148811

Report Number(s):: 246

DOE Contract Number:: FY13 AOP 25727

Resource Type:: Data

Country of Publication:: United States

Availability:: GDRHelp@ee.doe.gov

Language:: English

Subject:: 15 Geothermal Energy; geothermal; chlorite dissolution rate law; geochemistry; geothermal kinetic database; chemical alteration; EGS; chlorite dissolution rate; chlorite dissolution; dissolution rate; data; raw data; processed data

Citation Formats


                    Carroll, Susan. Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10.  United States: N. p., 2013. 
        Web.  doi:10.15121/1148811.

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                    Carroll, Susan. Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10.  United States.  https://doi.org/10.15121/1148811

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                    Carroll, Susan. 2013.  
        "Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10".  United States.  https://doi.org/10.15121/1148811.  https://www.osti.gov/servlets/purl/1148811.

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@article{osti_1148811,

  title        = {Chlorite Dissolution Rates From 25 to 275 degrees and pH 3 to 10},

  author       = {Carroll, Susan},

  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://www.osti.gov/biblio/1148811},
  journal      = {},
number       = ,

  volume       = ,

  place        = {United States},

  year         = {Fri Sep 27 00:00:00 EDT 2013},

  month        = {Fri Sep 27 00:00:00 EDT 2013}

}

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