[1] Cai Y-L (蔡运龙). Preliminary research on ecological reconstruction in karst mountain poverty areas of southwest China. Advance in Earth Sciences (地球科学进展), 1996, 11(6): 602-606 (in Chinese) [2] Chen H-S (陈洪松), Yang J (杨 静), Fu W (傅伟), et al. Characteristics of slope runoff and sediment yield on karst hill-slope with different land-use types in northwest Guangxi. Transactions of the Chinese Society of Agricultural Engineering (农业工程学报), 2012, 28(16): 121-126 (in Chinese) [3] Fu ZY, Chen HS, Zhang W, et al. Subsurface flow in a soil-mantled subtropical dolomite karst slope: A field rainfall simulation study. Geomorphology, 2015, 250: 1-14 [4] White C, Cook R, Lawrence R, et al. The D/H ratios of sap in trees: Implications for water sources and tree ring D/H ratios. Geochimica et Cosmochimica Acta, 1985, 49: 237-246 [5] Chen H-S (陈洪松), Wang K-L (王克林). Soil water research in karst mountain areas of Southwest China. Research of Agricultural Modernization (农业现代化研究), 2008, 29(6): 734-738 (in Chinese) [6] Jiang G-H (姜光辉), Chen K-K (陈坤琨), Yu S (于爽), et al. Separating karst slope runoff in peak cluster area. Journal of China Hydrology (水文), 2009(6): 14-19 (in Chinese) [7] Guo C-Q (郭纯青). Karst Ecohydrology in China. Beijing: Geological Press, 2007 (in Chinese) [8] Cao J-H (曹建华), Lu S-L (鲁胜力), Yang D-S (杨德生), et al. Process of soil and water loss and its control measures in karst regions, Southwestern China. Science of Soil and Water Conservation (中国水土保持科学), 2011, 9(2): 52-56 (in Chinese) [9] Bates BC, Aryal SK. A similarity index for storm runoff due to saturation excess overland flow. Journal of Hydrology, 2014, 513: 241-255 [10] Zhang ZC, Chen X, Ghadoani A, et al. Modelling hydrological processes influenced by soil, rock and ve-getation in a small karst basin of southwest China. Hydrological Processes, 2011, 25: 2456-2470 [11] Leh MD, Chaubey I, Murdoch J, et al. Delineating runoff processes and critical runoff source areas in a pasture hillslope of the Ozark Highlands. Hydrological Processes, 2008, 22: 4190-4204 [12] Peng T, Wang SJ. Effects of land use, land cover and rainfall regimes on the surface runoff and soil loss on karst slopes in southwest China. Catena, 2012, 90: 53-62 [13] Rui X-F (芮孝芳). Principle of Hydrology. Beijing: China Water Power Press, 2004: 131-152 (in Chinese) [14] Maloszewski P, Stichler W, Zuber A, et al. Identifying the flow systems in a Karstic-fissured-porous aquifer, the Schneealpe, Austria, by modelling of environmental 18O and 3H isotopes. Journal of Hydrology, 2002, 256: 48-59 [15] McDonnell JJ. Where does water go when it rains? Mo-ving beyond the variable source area concept of rainfall-runoff response. Hydrological Processes, 2003, 17: 1869-1875 [16] Klaus J, Zehe E, Elsner M, et al. Macropore flow of old water revisited: Experimental insights from a tile-drained hillslope. Hydrology & Earth System Sciences, 2013, 17: 103-118 [17] Dahlke HE, Easton ZM, Lyon SW, et al. Dissecting the variable source area concept: Subsurface flow pathways and water mixing processes in a hillslope. Journal of Hydrology, 2012, 420/421: 125-141 [18] Vogel T. Using oxygen-18 to study the role of preferential flow in the formation of hillslope runoff. Vadose Zone Journal, 2010, 9: 252-259 [19] Meng W (孟 薇). Soil Water Movement in Sloping Land of Red Region Based on Environmental Isotope Technologies. Master Thesis. Changsha: Institute of Subtropical Agriculture, Chinese Academy of Sciences, 2007 (in Chinese) [20] Zeng F-P (曾馥平), Peng W-X (彭晚霞), Song T-Q (宋同清), et al. Changes in vegetation after 22 years’ natural restoration in the Karst disturbed area in northwestern Guangxi, China. Acta Ecologica Sinica (生态学报), 2007, 27(12): 5110-5119 (in Chinese) [21] Ohrstrom P, Persson M, Albergel J, et al. Field-scale variation of preferential flow as indicated from dye coverage. Journal of Hydrology, 2002, 257: 164-173 [22] Badoux A, Witzig J, Germann PF, et al. Investigations on the runoff generation at the profile and plot scales, Swiss Emmental. Hydrological Processes, 2006, 20: 377-394 [23] Jia H, Lei A, Lei J, et al. Effects of hydrological processes on nitrogen loss in purple soil. Agricultural Water Management, 2007, 89: 89-97 [24] Fu Z-Y (付智勇), Chen H-S (陈洪松), Wang K-L (王克林), et al. A micro soil hydrological monitoring system suitable for karst slope with high heterogeneity. China, 201310424726.3. 2013-12-18 (in Chinese) [25] Song T-Q (宋同清), Peng W-X (彭晚霞), Zeng F-P (曾馥平), et al. Spatial heterogeneity of surface soil moisture content in dry season in Mulun National Natural Reserve in Karst area. Chinese Journal of Applied Ecology (应用生态学报), 2009, 20(1): 98-104 (in Chinese) [26] Fu ZY, Chen H, Xu Q, et al. Role of epikarst in near-surface hydrological processes in a soil mantled subtropical dolomite karst slope: Implications of field rainfall simulation experiments. Hydrological Processes, 2015, 30: 795-811 [27] Yang J (杨 静). Rainfall-infiltration-runoff Characte-ristics and Their Influencing Factors in Karst Hillslopes. PhD Thesis. Institute of Subtropical Agriculture, Chinese Academy of Sciences, 2016 (in Chinese) [28] Luk S, Abrahams AD, Parsons AD. Methodology: A simple rainfall simulator and trickle system for hydro-geomorphological experiments. Physical Geography, 1986, 7: 344-356 [29] Fu Z-Y (付智勇), Chen H-S (陈洪松), Wang K-L (王克林), et al. A portable lifting rainfall simulator suitable for karst slope with high heterogeneity. China, 201310703990.0. 2014-04-20 (in Chinese) [30] Kendall C, McDonnell J. Isotope Tracers in Catchment Hydrology. Amsterdam: Elsevier, 1998 [31] Diner T, Payne BR, Florkowski T, et al. Snowmelt runoff from measurements of tritium and oxygen-18. Water Resources Research, 1970, 6: 110-124 [32] Buttle JM, Vonk AM, Taylor CH. Applicability of isotopic hydrograph separation in a suburban basin during snowmelt. Hydrological Processes, 1995, 9: 197-211 [33] Pearce AJ, Stewart MK, Sklash MG. Storm runoff ge-neration in humid headwater catchments. 1. Where does the water come from? Water Resources Research, 1986, 22: 1263-1272 [34] Klaus J, Zehe E, Elsner M, et al. Macropore flow of old water revisited: Experimental insights from a tile-drained hillslope. Hydrology & Earth System Sciences, 2013, 17: 103-118 [35] NIie Y-P (聂云鹏), Chen H-S (陈洪松), Wang K-L (王克林). Seasonal variation of water sources for plants growing on continuous rock outcrops in limestone area of Southwest China. Chinese Journal of Plant Ecology (植物生态学报), 2011, 35(10): 1029-1037 (in Chinese) [36] Dunne T. Field studies of hillslope flow processes// Kirkby MJ, ed. Hillslope Hydrology. Chichester: John Wiley & Sons, 1978: 227-289 [37] Peters DL, Buttle JM, Taylor CH, et al. Runoff production in a forested, shallow soil, Canadian Shield Basin. Water Resources Research, 1995, 31: 1291-1304 [38] Bodman GB, Colman EA. Moisture and energy conditions during downward entry of water into soils. Soil Science Society of America Journal, 1944, 8:Ⅱ6-Ⅱ6 [39] Guebert MD, Gardner TW. Macropore flow on a reclaimed surface mine: Infiltration and hillslope hydrology. Geomorphology, 2001, 39: 151-169 [40] Xie X-L (谢小立), Yin C-M (尹春梅), Chen H-S (陈洪松), et al. A study of water transportation on red soil slope based on environmental isotope technology. Bulletin of Soil and Water Conservation (水土保持通报), 2012, 32(3): 1-6 (in Chinese) |