Mass transport and reaction in water-saturated and unsaturated rocks
Author:
Affiliation:
1. National Institute of Advanced Industrial Science and Technology, Geological Survey of Japan
Publisher
Japan Association of Mineralogical Sciences
Link
https://www.jstage.jst.go.jp/article/gkk/53/1/53_240123/_pdf
Reference41 articles.
1. Assouline, S. and Or, D. (2008): Air-entry based characteristic length for estimation of permeability of variably compacted earth materials. Water Resour. Res., 44, W11403.
2. Brace, W.F. (1980): Permeability of crystalline and argillaceous rocks. Int. J. Rock Mech. Min. Sci. & Geomech. Abstr., 17, 241-251.
3. Carman, P.C. (1956): Flow of Gases through Porous Media. Elsevier, New York.
4. Ehrenberg, S.N. (1990): Relationship between diagenesis andreservoir quality in sandstones of the Garn formation. Haltenbaken, mid-Norwegian continental shelf. A.A.P.G. Bull., 74, 1538-1558.
5. Ershov, A.P., Zorin, Z.M., Sobolev, V.D. and Churaev, N.V. (2001): Kinetics of gas bubble motion in a capillary. Colloid J., 63, 179-185.
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