参考文献/References:
[1] 徐则民,黄润秋,范柱国等.滑坡灾害孕育-激发过程中的水-岩相互作用[J].自然灾害学报,2005,14(1):1-9 [XU Zemin, HUANG Runqiu, FANG Zhuguo, et al.Landslide disaster preparation-excitation process in water rock interaction[J].Journal of Natural Disasters, 2005, 14(1):1-9]
[2] SHOAEI Zieaoddin.Mechanism of the giant Seimareh Landslide, Iran, and the longevity of its landslide dams[J].Environmental Earth Sciences, 2014, 727: 2411-2422.
[3] FIORILLO Francesco.Geological features and landslide mechanisms of an unstable coastal slope(Petacciato, Italy)[J].Engineering Geology, 2002, 673:255-267.
[4] 张丽华,王成武.非饱和土壤优先流运动特性的染色示踪研究[J].节水灌溉,2010(5):35-36 [ZHANG Lihua, WANG Chengwu.Study on the flow characteristics of non-saturated soil referential flow characteristics[J].Water Saving Irrigation, 2010(5):35-36]
[5] HEIJS A W J,RITSEMA C J,DEKKER L W.Three-dimensional visualization of preferential flow patterns in two soils[J].Geoderma, 1996,702:101-116.
[6] MITCHELL A R, ELLSWORTH T R, MEEK B D.Effect of root systems on preferential flow in swelling soil[J].Communications in Soil Science and Plant Analysis, 1995, 2615-16:2655-2666.
[7] RONKANEN Anna-Kaisa, KLOVE Bjørn.Use of stabile isotopes and tracers to detect preferential flow patterns in a peatland treating municipal wastewater[J].Journal of Hydrology, 2007, 3473:418-429.
[8] SANDER Till, H.GERKE Horst.Modelling field-data of preferential flow in paddy soil induced by earthworm burrows[J].Journal of Contaminant Hydrology, 2008, 1041:126-136.
[9] SHIPITALO M J, NUUTINEN V, KEVIN R B.Interaction of earthworm burrows and cracks in a clayey, subsurface-drained, soil[J].Applied Soil Ecology, 2004, 263:209-217.
[10] 冯杰,郝振纯.CT扫描确定土壤大孔隙分布[J].水科学进展,2002,13(5):611-617 [FENG Jie, HAO Zhenchun.CT scan to determine the distribution of soil[J].Advances in Water Science,2002,13(5):611-617]
[11] 解河海,冯杰,冯青等.考虑大孔隙的土壤入渗模型[J].水利水电科技进展,2011,31(5):35-38[JIE Hehai, FENG Jie, FENG Qing, et al.Consider the macropore soil infiltration model[J].Advances in Science and Technology of Water resources, 2011,31(5):35-38]
[12] 王凤,邓念东,马逢清等.基于CT的黄土大孔隙形态三维分形研究[J].计算机工程, 2014,40(7):217-220 [WANG Feng, DENG Niandong, MA Fengqing, et al.Based on CT of the three dimensional fractal of the Loess Plateau[J].Computer Engineering, 2014, 40(7):217-220]
[13] 张家明,徐则民,裴银鸽.植被发育斜坡非饱和带大孔隙[J].山地学报,2012,30(4):439-449[ZHANG Jiaming, XU Zemin, Pei Yinge.Macropores of unsaturated zone in the slope of vegetation development[J].Mountain Research, 2012, 30(4):439-449]
[14] ALLAIRE S E, GUPTA S C, NIEBER J, MONCRIEF J F.Role of macropore continuity and tortuosity on solute transport in soils[J].Journal of Contaminant Hydrology, 2002, 583:299-321.
[15] CHRISTIANSEN Jesper Skovdal, THORSEN Mette, CLAUSEN Thomas, et al.Modelling of macropore flow and transport processes at catchment scale[J].Journal of Hydrology, 2004, 2991:136-158.
[16] 王帮团,徐则民,王帮圆.植被发育斜坡土体中根-土间隙的导流特性[J].山地学报, 2015,33(3):257-267[WANG Gang, XU Zemin, WANG Bangyuan.The diversion characteristics of soil in the soil of the slope of vegetation development[J].Mountain Research, 2015, 33(3):257-267]
[17] PANKHURST C E, PIERRET A, HAWKE B G, et al.Microbiological and chemical properties of soil associated with macropores at different depths in a red-duplex soil in NSW Australia[J].Plant and Soil, 2002, 238:11-20.
[18] 张霞,李凤滨,盛金昌等.格子Boltzmann方法模拟土体渗流场研究 [J].水电能源科学, 2012,30(10):61-64 [ZHANG Xia, LI Fengbin, SHENG Jinchang, et al.Lattice Boltzmann method simulation of seepage field [J].Water Resources and Power, 2012,30(10):61-64]