Multi-physics simulation for predicting the permeability change of single rock fracture due to geochemical effect depending on pH condition
Author:
Affiliation:
1. Osaka University
2. Ehime University
3. Kyoto University
Publisher
The Japanese Geotechnical Society
Subject
General Computer Science
Link
https://www.jstage.jst.go.jp/article/jgssp/9/3/9_v09.cpeg045/_pdf
Reference8 articles.
1. 1) Bond, A., Brusky, I., Chittenden, N., Feng, X-T., Kolditz, O., Lang, P., Lu, R., McDermott, C., Neretnieks, I., Pan, P-Z., Sembera, J., Shao, H. and Yasuhara, H. (2016): Development of approaches for modelling coupled thermal–hydraulic–mechanical–chemical processes in single granite fracture experiments, Environ. Earth. Sci. 75: 1313.
2. 2) Kalinowski, BE. and Schweda, P. (1996): Kinetics of muscovite, phlogopite and biotite dissolution and alternation at pH 1-4, room temperature, Geochm. Cosmochim. Act, 60, 367-385.
3. 3) Kinoshita, N. and Yasuhara, H. (2012): Evolution of Fracture Permeability in Granite under High Temperature and High Confining Pressure Condition, Journal of MMIJ, 128, 72-78 (in Japanese).
4. 4) Ogata, S., Yasuhara, H., Kinoshita, N., Cheon, DS. and Kishida, K. (2018): Modeling of coupled thermal-hydraulic-mechanical-chemical process for predicting the evolution in permeability and reactive transport behavior within single rock fractures, Int. J. Rock Mech. Min. Sci, 107, 271-281.
5. 5) Palandri, JL. and Kharaka, YK. (2004): A compilation of rate parameters of mineral-water interaction kinetics for application to geochemical modelling, US Geological Survey open file report 2004–108, USA.
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1. Multi-physics numerical analyses for predicting the alterations in permeability and reactive transport behavior within single rock fractures depending on temperature, stress, and fluid pH conditions;SOILS FOUND;2022
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