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Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C
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.
Complete Metadata
| @type | dcat:Dataset |
|---|---|
| accessLevel | public |
| bureauCode |
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| contactPoint |
{
"fn": "Susan Carroll",
"@type": "vcard:Contact",
"hasEmail": "mailto:carroll6@llnl.gov"
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| dataQuality |
true
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| description | 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. |
| distribution |
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{
"@type": "dcat:Distribution",
"title": "Dissolution Kinetics at Variable pH and Temperatures.docx",
"format": "docx",
"accessURL": "https://gdr.openei.org/files/910/CarrollFY17LLNL_25Feb2017_IM.docx",
"mediaType": "application/vnd.openxmlformats-officedocument.wordprocessingml.document",
"description": "Report summarizing dissolution of biotite, chlorite, illite, muscovite, and feldspar at variable pH and temperatures up to 280 degrees C."
},
{
"@type": "dcat:Distribution",
"title": "Dissolution Rates.xlsx",
"format": "xlsx",
"accessURL": "https://gdr.openei.org/files/910/KineticRates_10Feb2017.IM.xlsx",
"mediaType": "application/vnd.openxmlformats-officedocument.spreadsheetml.sheet",
"description": "Biotite, chlorite, illite, muscovite, and feldspar dissolution rates and data in spreadsheet format. Includes raw data, dissolution rate equations, and a derivation of kinetic dissolution rate and rate parameters."
}
]
|
| DOI | 10.15121/1441454 |
| identifier | https://data.openei.org/submissions/7086 |
| issued | 2017-02-24T07:00:00Z |
| keyword |
[
"biotite",
"chemistry",
"chlorite",
"dissolution",
"egs",
"energy",
"enhanced geothermal systems",
"feldspar",
"fracture permeability",
"geochemistry",
"geothermal",
"illite",
"kinetic data",
"kinetics",
"muscovite",
"rate equations",
"success"
]
|
| landingPage | https://gdr.openei.org/submissions/910 |
| license | https://creativecommons.org/licenses/by/4.0/ |
| modified | 2018-06-13T17:05:44Z |
| programCode |
[
"019:006"
]
|
| projectLead | Lauren Boyd |
| projectNumber | FY14 AOP 1422 |
| projectTitle | The Viability of Sustainable, Self-Propping Shear Zones in Enhanced Geothermal Systems: Measurement of Reaction Rates at Elevated Temperatures |
| publisher |
{
"name": "Lawrence Livermore National Laboratory",
"@type": "org:Organization"
}
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|
| title | Chlorite, Biotite, Illite, Muscovite and Feldspar Dissolution Kinetics at Variable pH and Temperatures up to 280 deg C |
