Fractured Rock Permeability as a Function of Temperature and Confining Pressure-Reference-Cited by-同舟云学术

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Fractured Rock Permeability as a Function of Temperature and Confining Pressure

Published:2015-04-01 Issue:10 Volume:172 Page:2871-2889
ISSN:0033-4553
Container-title:Pure and Applied Geophysics
language:en
Short-container-title:Pure Appl. Geophys.

Author:

Alam A. K. M. Badrul,Fujii Yoshiaki,Fukuda Daisuke,Kodama Jun-ichi,Kaneko Katsuhiko

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00024-015-1073-2.pdf

Reference19 articles.

1. Alam, A.K.M. B., M. Niioka, Y. Fujii, D. Fukuda, and J. Kodama (2014), Effect of confining pressure on the permeability of three rock types under compression, Int. J. Rock Mech. Min. Sci., 65(1), 49–61.

2. Backblom, G., and C.D. Martin (1999), Recent experiments in hard rock to study the excavation response: Implication of the performance of a nuclear waste geological repository, Tunnel Undergr. Space Technol., 14(3), 377–394.

3. Brace, W.F., J.B. Walsh, and W.T. Frangos (1968) Permeability of granite under high pressure, J. Geophys. Res., 73, 2225–2236.

4. Darot, M., Y. Gueguen, M.-L. Baratin (1992), Permeability of thermally cracked granite. Geophys. Res. Letter, 19(9), 869–872.

5. Dhakal, G., T. Yoneda, M. Kato, and K. Kaneko (2002), Slake durability and mineralogical properties of some pyroclastic and sedimentary rocks, Eng. geol., 65(1), 31–45.

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