[1] |
XU Y, ZHANG L M. Breaching parameters of earthand rockfill dams [J]. Journal of Geotechnical andGeoenvironmental Engineering, 2009, 135(12): 1957-1970.
|
[2] |
TALBOT J R, DEAL C E. Rehabilitation of crackedembankment dams [C]//Proceedings of GeotechnicalPractice in Dam Rehabilitation. North Carolina, USA:ASCE, 1993: 267-283.
|
[3] |
YAO H L, ZHENG S H, CHEN S Y. Analysis of theslope stability of expansive soils considering cracksand infiltration of rainwater [J]. Chinese Journal ofGeotechnical Engineering, 2001, 23(5): 606-609 (inChinese).
|
[4] |
LI J H. Field experimental study and numerical simulationof seepage in saturated/unsaturated cracked soil[D]. Hong Kong, China: Department of Civil and EnvironmentalEngineering, The Hong Kong Universityof Science and Technology, 2009.
|
[5] |
ZHANG L M, FREDLUND D G. Characteristics ofwater retention curves for unsaturated fractured rocks[C]//Proceedings of the Second Asian Conference onUnsaturated Soils. Osaka, Japan: ASIA, 2003: 425-428.
|
[6] |
BURGER C A, SHACKELFORD C D. Soil-watercharacteristic curves and dual porosity of sanddiatomaceousearth mixtures [J]. Journal of Geotechnicaland Geoenvironmental Engineering, 2001, 127(9):790-800.
|
[7] |
MILLER C J, MI H, YESILLER N. Experimentalanalysis of desiccation crack propagation in clay liners[J]. Journal of the American Water Resources Association,1998, 34(3): 677-686.
|
[8] |
VOGEL H J, HOFMANN H, ROTH K. Studies ofcrack dynamics in clay soil: Experimental methods, results,and morphological quantification [J]. Geoderma,2005, 125: 203-211.
|
[9] |
TANG C S, SHI B, LIU C, et al. Influencing factorsof geometrical structure of surface shrinkage cracks inclayey soils [J]. Engineering Geology, 2008, 101(3/4):204-217.
|
[10] |
PETERS R R, KLAVETTER E A. A continuummodel for water movement in an unsaturated fracturedrock mass [J]. Water Resources Research, 1988, 24(3):416-430.
|
[11] |
XU Y F, DONG P. Fractal approach to hydraulic propertiesin porous media [J]. Chaos, Solitons and Fractals,2004, 19(2): 327-337.
|
[12] |
RIEU M, SPOSITO G. Fractal fragmentation, soilporosity, and soil water properties: Theory [J]. SoilScience Society of America Journal, 1991, 55 (5):1231-1238.
|
[13] |
GUARRACINO L. A fractal constitutive model forunsaturated flow in fractured hard rock [J]. Journalof Hydrology, 2006, 324(1/2/3/4): 154-162.
|
[14] |
LE′ ON C A L Y. New perspectives in mercuryporosimetry[J]. Advances in Colloid and IntefaceScience, 1998, 76: 341-372.
|
[15] |
SHENG Y G, XU Y, LI Z H, et al. Determination offractal dimensions of silicon dioxide xerogel by meansof gas-adsorption [J]. Acta Physica Sinica, 2005, 54(1):221-227 (in Chinese).
|
[16] |
PHAM H Q, FREDLUND D G, BARBOUR S L. Astudy of hysteresis models for soil-water characteristiccurves [J]. Canadian Geotechnical Journal, 2005,42(6): 1548-1568.
|
[17] |
REITAM S, KUPER B H. Laboratory measurementof capillary pressure-saturation relationships in a rockfracture [J]. Water Resources Research, 1994, 30(4):865-878.
|
[18] |
REN Q, XU W Y. Fractal model for unsaturated seepageflow in fractured rock masses [J]. Rock and SoilMechanics, 2008, 29(10): 2735-2740 (in Chinese).
|
[19] |
National Research Council. Conceptual model of flowand transport in the fractured vadose zone [M]. Washington:National Academy Press, 2001.
|
[20] |
ZHANG Y T. Rock hydraulics and engineering [M].Beijing: China Water Power Press, 2005: 243-244 (inChinese).
|
[21] |
CURRIE I G. Fundamental mechanics of fluids [M].New York: McGraw-Hill, 1993.
|