[1]
Finn R. Equilibrium Capillary Surfaces: Mathematical theory. New York: Springer, 17-18. (1986).
Google Scholar
[2]
Fredlund D. G. and Rahardjo H. Soil mechanics for unsaturated soils. New York: Wiley& Sons Inc, 120-156. (1993).
Google Scholar
[3]
Dullien F.A.L. Porous media: fluid transport and pore structure. New York: Academic Press, 23-100. (1979).
Google Scholar
[4]
Stenitzer E., Diestel H., Zenker T. et al. Assessment of capillary rise from shallow groundwater by the simulation model SIMWASER using either estimated pedotransfer functions or measured hydraulic parameters. Water Resources Management, 21(9): 1567-1584. (2007).
DOI: 10.1007/s11269-006-9113-4
Google Scholar
[5]
Jacob Bear, Alexander H. -D. Cheng. Modeling Groundwater Flow and Contaminant Transport[M]. New York: Springer, (2010).
Google Scholar
[6]
Wessolek G., Bohne K., Duijnisveld W., et al. Development of hydro-pedotransfer functions to predict capillary rise and actual evapotranspiration for grassland sites. Journal of Hydrology. 400 (3/4): 429-437. (2011).
DOI: 10.1016/j.jhydrol.2011.01.059
Google Scholar
[7]
Lu N. and Likos W.J. Rate of capillary rise in soil. Journal of Geotechnical and Geoenvironmental Engineering, 130(6): 646-650. (2004).
DOI: 10.1061/(asce)1090-0241(2004)130:6(646)
Google Scholar
[8]
Lehmann P., Stauffer F., and Hinz C. Effect of hysteresis on water flow in a sand column with a fluctuating capillary fringe. Journal of Contaminant Hydrology, 33(1-2): 81-100. (1998).
DOI: 10.1016/s0169-7722(98)00066-7
Google Scholar
[9]
Ronen Daniel, Scher H. and Blunt M. Field observations of a capillary fringe before and after a rainy season. Journal of Contaminant Hydrology, 44(2): 103-118. (2000).
DOI: 10.1016/s0169-7722(00)00096-6
Google Scholar
[10]
Zhang H., Baray D. A. and Hocking G. C. Analysis of continuous and pulsed pumping of a phreatic aquifer. Advances in Water Resources, 22 (6): 623-632. (1999).
DOI: 10.1016/s0309-1708(98)00038-4
Google Scholar
[11]
Mixon F. O. Saturated and capillary fringe ground water behavior near an excavation. Ground Water, 26(2): 148-155. (1984).
DOI: 10.1111/j.1745-6584.1988.tb00377.x
Google Scholar
[12]
Dixon S. The effects of settlement and pastoral occupation in Australia upon the indigenous vegetation. Transactions of the Royal Society of South Australia, 15: 195-206. (1892).
Google Scholar
[13]
Snyder K. A and Tartowski S.L. Multi-scale temporal variation in water availability: Implications for vegetation dynamics in arid and semi- arid ecosystems. Journal of Arid Environments, 65(2): 219-234. (2006).
DOI: 10.1016/j.jaridenv.2005.06.023
Google Scholar
[14]
Wu Aihong, Gu qiangkang and Li Wan. Laboratory experiment on migration of capillary water of saline soil of airport. Subgrade Engineering, 6: 137-141. (2008).
Google Scholar
[15]
Gao Jiangping, Wu Jiahui and Yang Rongshang. Analysis of the interaction laws of all influencing factors upon salt heaving properties of the sulphate salty Soil. China Journal of Highway and Transport, 10 (1): 10-15. (1997).
Google Scholar
[16]
Chen Yimin, Zhang Xifa, Zhang Dongqing and SUN. An integrated experimental study of harmful rising height of capillary water of highway subgrade in seasonally frozen ground regions. Journal of Glaciology and Geocryology, 30(4): 641-645. (2008).
Google Scholar
[17]
Li rui, Zhao Wenguang and Chen Shanxiong. Capillary water upward movement analysis of expansive soil roadbed based on GEO-SLOPE. Journal of Huazhong University of Science and Technology (Urban Science Edition), 23(S1): 36-39. (2006).
Google Scholar
[18]
Tan Yunzhi, Kong Lingwei, Guo Aiguo et al. Capillary effect of moisture transfer and its numerical simulation of compacted late rite soil. Rock and Soil Mechanics, 31 (7): 2289-2294. (2010).
Google Scholar
[19]
Wang Youchang and Fu qiang. Comparison experimental study on the influence factors about capillary water upward movement of red clay. Highways & Automotive Applications, 3: 100-104. (2011).
Google Scholar
[20]
Xu Jian, Niu Fujun, Niu Yonghong et al. Forcast on the effect height of frost damage of clayey loess in Northeast China. Journal of Xi'an University of Architecture & Technology (Natural Science Edition), 43(4): 501-506. (2011).
Google Scholar
[21]
Kowalik P. J. Drainage and capillary rise components in water balance of alluvial soils. Agricultural Water Management, 86(1/2): 206-211. (2006).
DOI: 10.1016/j.agwat.2006.08.003
Google Scholar
[22]
Zhang Ping, Wu Hao, Yin Hongjian, Li Baogang and Wang Haikun. Research on influence of construction of soil layer on height of capillary water upward movement and evaporation of groundwater. Water Saving Irrigation, 3: 6-8. (2011).
Google Scholar
[23]
Shi Wenjuan, Shen Bing, Wang Zhirong et al. Maximum height of upward capillary water movement in layered soil. Agricultural Research in the Arid Areas, 25(1): 94-97. (2007).
Google Scholar
[24]
Li Xianwen, Zhou Jinlong, Zhao Yujie and Liu Yanfeng. Effects of high-TDS on capillary rise of phreatic water in sand soil. Transactions of the CSAE, 27(8): 84-89.(2011).
Google Scholar
[25]
Zhuang Li, Chen Yaning, Li Weihong, and Zhao Hongyan. Relationship of the protective enzymes of desert vegetations with water table in the lower reaches of tarim river. Acta Botanica Boreali-occidentalia Sinica, 25 (7): 1287-1294. (2005).
Google Scholar
[26]
Chen Hesheng. The influence of water resources system exploitation on vegetation arid northwest area. Journal of Arid Land Resources & Environment, 5(1): 57-65. (1991).
Google Scholar
[27]
Qiao Yunfeng, Wang Xiaohong, Shen Bing et al. Groundwater characters and their effects on vegetation in Hotian oasis. Journal of Yangtze River Scientific Research Institute, 12(2): 28-31. (2004).
Google Scholar
[28]
Deng Julong. Essential methods of grey system. Wuhan: Huazhong University of Science and Technology Press, 17-165. (1987).
Google Scholar
[29]
Miao Qiangqiang, Chen Zhenghan, Tian Qingyan et al. Experimental study of capillary rise of unsaturated clayey sand. Rock and Soil Mechanics, 32 (S1): 327-322. (2011).
Google Scholar
[30]
Li X., Zhang L.M., and Fredlund D.C. Wetting front advancing column test for measuring unsaturated hydraulic conductivity. Canadian Geotechnical Journal, 46: 1431-1445. (2009).
DOI: 10.1139/t09-072
Google Scholar
[31]
Ma Yuan. The characteristics of the capillary water rise and its plant ecological significance in northwest desert lake-basin region—take the Jilantai lake-basin of Ulan Buh. Chang'an University (2012).
DOI: 10.4028/www.scientific.net/amr.955-959.3671
Google Scholar