Research progressin the effect of slope length on slope erosion, transportation and deposition processes
LIU Ran1, YU Xinxiao1, CAI Qiangguo2,3, SUN Liying2, FANG Haiyan2,3, JIA Guodong1, HE Jijun4
1. School of Soil Water Conservation in Beijing Forestry University, Key Laboratory of State Forestry and Grassland Administration on Soil and Water Conservation, 100083, Beijing, China; 2. Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Key Laboratory of Water Cycle and Related Land Surface Processes, 100101, Beijing, China; 3. College of Resources and Environment, University of Chinese Academy of Sciences, 100049, Beijing, China; 4. State Key Laboratory of Urban Environmental Processes and Numerical Simulation, Resources Environment and GIS Key Lab of Beijing, Capital Normal University, 100048, Beijing, China
Abstract:[Background] Slope length is one of the important geomorphological factors that affect the process of slope runoff erosion and sediment production. It determines the variation of slope water flow energy along the way, and affects sediment carrying capacity of the water flow, thereby affecting the process of soil erosion, transportation and deposition. In recent years, the research on impact of slope length on soil erosion has received considerable attention. Meanwhile, understanding the changing law of critical slope length provides an important theoretical basis for the study of sediment transport and deposition processes on slopes. [Methods] Based on the literature review, we summarized the influence of slope length on runoff erosion and sediment yield, the general law of erosion critical slope length, the calculation method of critical slope length and the influence of slope length on slope deposition. And we discussed the limitations of soil erosion in terms of slope length, and highlighted the focus of future research. The information for the methods comes from 46 core papers out of 2199 papers published in the web of science, CNKI, Baidu Academic and Science Direct in the past few decades with the keywords of "slope length soil erosion" and "slope surface deposition". [Results] 1)The relationship between slope length and soil erosion is very complicated. Due to the difference in experimental conditions, the erosion intensity varying with slope length has three dynamic forms: increasing, decreasing and fluctuating. 2) Through previous studies, we summarized the definition of the critical slope length for erosion, and pointed out that different critical slope lengths are obtained in different studies due to factors such as rainfall conditions, slope, and slope length. Moreover, the established calculation model of critical slope length is based on the experimental data of researchers, which causes certain limitations. 3)During the erosion, transportation, and deposition of the slope, the sediment is characterized by alternating strong and weak spatial changes. The existence of the critical slope length makes the influence of slope length on slope erosion and deposition more complicated. When the slope length does not reach the critical slope length, erosion and sedimentation activities cannot be fully developed.4)The key points of future research are described as follows. First of all, it is necessary to carry out further research and experiments on the sediment deposition process on the slope. Second, research on the critical slope length for erosion changes as well as experimental research on the relationship between slope lengths of different soil textures and soil erosion should be strengthened. Finally, slope length affects the wave form of slope erosion-sedimentation, and the coupling mechanism of slope length and slope erosion and sediment deposition process needs to be studied. [Conclusions] This paper summarizes the research progress and future research directions of slope length on slope erosion, transportation and deposition process, and aims to provide guidance for the research application and decision-making of soil erosion on slope length.
刘冉, 余新晓, 蔡强国, 孙莉英, 方海燕, 贾国栋, 和继军. 坡长对坡面侵蚀、搬运、沉积过程影响的研究进展[J]. 中国水土保持科学, 2020, 18(6): 140-146.
LIU Ran, YU Xinxiao, CAI Qiangguo, SUN Liying, FANG Haiyan, JIA Guodong, HE Jijun. Research progressin the effect of slope length on slope erosion, transportation and deposition processes. SSWC, 2020, 18(6): 140-146.
WISCHMERIER W H, SMITH D D, UHLAND R E. Evaluation of factors in the soil loss equation[J]. Agricultural Engineering, 1958, 39(8):458.
[2]
秦伟, 朱清科, 张岩. 通用土壤流失方程中的坡长因子研究进展[J]. 中国水土保持科学, 2010, 8(2):117. QIN Wei, ZHU Qingke, ZHANG Yan. Advance in researches on slop length factor in Universal Soil Loss Equation[J]. Science of Soil and Water Conservation, 2010, 8(2):117.
[3]
COOK H L. The nature and controlling variables of the water erosion process[J].Soil Science Society of American Proceeding, 1936, 1:60.
[4]
孔亚平, 张科利, 曹龙熹. 土壤侵蚀研究中的坡长因子评价问题[J]. 水土保持研究, 2008, 15(4):43. KONG Yaping, ZHANG Keli,CAO Longxi. Appraise slope length factors in soil erosion study[J]. Research of Soil and Water Conservation, 2008, 15(4):43.
[5]
GOVERS G. Rill erosion on arable land in central Belgium:Rates, controls and predictability[J]. Catena,1991,18(2):133.
[6]
AGASSI M, BENHUR M. Effect of slope length, aspect and phosphogypsum on runoff and erosion from steep slopes[J]. Soil Research,1991, 29(2):197.
[7]
BRYAN R B, POESEN J. Laboratory experiments on the influence of slope length on runoff, percolation and rill development[J]. Earth Surface Processes & Landforms, 1989, 14(3):227.
[8]
朱显谟. 黄土高原水蚀的主要类型及有关因素[J]. 水土保持通报, 1981, 1(3):13. ZHU Xianmo. Main types and related factors of water erosion in the Loess Plateau[J]. Bulletin of Soil and Water Conservation, 1981, 1(3):13.
[9]
孔亚平, 张科利, 唐克丽, 等. 坡长对侵蚀产沙过程影响的模拟研究[J]. 水土保持学报, 2001,15(2):17. KONG Yaping, ZHANG Keli, TANG Keli, et al. Impacts of slope length on soil erosion process under simulated rainfall[J]. Journal of Soil and Water Conservation, 2001,15(2):17.
[10]
方海燕, 蔡强国, 李秋艳. 黄土丘陵沟壑区坡面产流能力及影响因素研究[J]. 地理研究, 2009, 28(3):589. FANG Haiyan, CAI Qiangguo, LI Qiuyan. Study on the runoff generation capacity of slope surface and its influencing factors in a hilly loess region on the Loess Plateau[J]. Geographical Research, 2009, 28(3):589.
[11]
LAWS J O, PARSONS D A. The relationship of raindrop site to intensity[J]. Eos,Transactions American Geophysical Union, 1943(24):452.
[12]
ZINGG A W. Degree and length of land slope as it affects soil loss in runoff[J]. Agricultural Engineering, 1940, 21(2):59.
[13]
LANGBEIN W B, SUCHUMM S A. Yield of sediment in relation to mean precipitation[J]. Eos,Transactions American Geophysical Union, 1958(39):230.
[14]
王玲玲, 范东明, 王文龙, 等. 水蚀风蚀交错区不同坡长坡面产流产沙过程[J]. 人民黄河, 2016, 38(3):74. WANG Lingling, FAN Dongming, WANG Wenlong, et al. A field experiment of runoff and sediment yielding processes of different slopes in water and wind erosion crisscross region[J]. Yellow River, 2016, 38(3):74.
[15]
SMETS T, POESEN J, BOCHET E. Impact of plot length on the effectiveness of different soil-surface covers in reducing runoff and soil loss by water[J]. Progress in Physical Geography, 2008, 32(6):654.
[16]
KINNELL P I A. A review of the design and operation of runoff and soil loss plots[J]. Catena, 2016(145):257.
[17]
LIU Jianbo, GAO Guangyao, WANG Shuai,et al. Combined effects of rainfall regime and plot length on runoff and soil loss in the Loess Plateau of China[J]. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 2019, 3(109):397.
[18]
郑粉莉. 发生细沟侵蚀的临界坡长与坡度[J]. 中国水土保持, 1989(8):23. ZHENG Fenli. Critical slope length and slope for rill erosion[J]. Soil and Water Conservation in China, 1989(8):23.
[19]
张科利, 唐克丽, 王斌科. 黄土高原坡面浅沟侵蚀特征值的研究[J]. 水土保持学报, 1991, 5(2):8. ZHANG Keli, TANG Keli, WANG Binke. A study on characteristic value of shallow gully erosion genesis on slope farmland in the Loess Plateau[J]. Journal of Soil and Water Conservation, 1991, 5(2):8.
[20]
陈晓安, 蔡强国, 张利超, 等. 黄土丘陵沟壑区不同降雨强度下坡长对坡面土壤侵蚀的影响[J]. 土壤通报, 2011, 42(3):724. CHEN Xiaoan, CAI Qiangguo, ZHANG Lichao. Impact of slope length on soil erosion under different rainfall intensity in a hilly loess region on the Loess Plateau[J]. Chinese Journal of Soil Science, 2011, 42(3):724.
[21]
罗来兴. 甘肃华亭粮食沟坡侵蚀量的野外观测及其初步分析结果[J]. 地理学资料, 1958(2):118. LUO Laixing. Field observation and preliminary analysis results of grain gully slope erosion in Huating, Gansu[J]. Geographical Information, 1958(2):118.
[22]
蔡强国. 坡长在坡面侵蚀产沙过程中的作用[J]. 泥沙研究, 1989(4):90. CAI Qiangguo. Role of slope length in the process of slope erosion and sediment yield[J]. Journal of Sediment Research, 1989(4):90.
[23]
HAN Zhen, ZHONG Shouqin, NI Jiupai, et al. Estimation of soil erosion to define the slope length of newly reconstructed gentle-slope lands in hilly mountainous regions[J]. Scientific Reports, 2019(9):4676.
[24]
CUI Ming, CAI Qiangguo, ZHU Axing, et al. Soil erosion along a long slope in the gentle hilly areas of black soil region in Northeast China[J]. Journal of Geographical Sciences. 2007, 17(3):375.
[25]
汪晓勇, 郑粉莉. 黄土坡面坡长对侵蚀-搬运过程的影响研究[J]. 水土保持通报, 2008, 28(3):4. WANG Xiaoyong, ZHENG Fenli. Effects of slope length on detachment and transport processes on a loessial hillslope[J]. Bulletin of Soil and Water Conservation, 2008, 28(3):4.
[26]
付兴涛, 张丽萍. 坡长对红壤侵蚀影响人工降雨模拟研究[J]. 应用基础与工程科学学报, 2015, 23(3):474. FU Xingtao, ZHANG Liping. Impact of slope length on red soil erosion under simulated rainfall[J]. Journal of Basic Science and Engineering, 2015, 23(3):474.
[27]
曹银真. 土壤侵蚀过程中的地貌临界[J]. 中国水土保持, 1987(10):21. CAO Yinzhen. Landform criticality in soil erosion process[J]. Soil and Water Conservation in China, 1987(10):21.
[28]
GHAHRAMANI A, ISHIKAWA Y, GOMI T. Slope length effect on sediment and organic litter transport on a steep forested hillslope:Upscaling from plot to hillslope scale[J]. Hydrol Res Lett, 2011(5):16.
[29]
SADEGHI S H R, BASHARI S M, RANGAVAR A S. Plot sizes dependency of runoff and sediment yield estimates from a small watershed[J]. Catena,2013(102):55.
[30]
陈永宗, 景可, 蔡强国. 黄土高原现代侵蚀与治理[M]. 北京:科学出版社, 1988:112. CHEN Yongzong, JING Ke, CAI Qiangguo. Modern erosion and management of the Loess Plateau[M]. Beijing:Science Press, 1988:112.
[31]
雷廷武, 张晴雯, 赵军, 等. 细沟侵蚀动力过程输沙能力试验研究[J]. 土壤学报, 2002, 39(4):480. LEI Tingwu, ZHANG Qingwen, ZHAO Jun, ea al. Laboratory study on sediment transport capacity in the dynamic process of rill erosion[J]. Acta Pedologica Sinica, 2002, 39(4):480.
[32]
姚璟, 付兴涛. 坡长对离石黄土坡面径流含沙量影响的模拟降雨研究[J]. 应用基础与工程科学学报, 2018, 26(3):493. YAO Jing, FU Xingtao. Impact of slope length on sediment concentration in runoff under simulated rainfall in Lishi loess region[J]. Journal of Basic Science and Engineering, 2018, 26(3):493.
[33]
李君兰, 蔡强国, 孙莉英, 等. 降雨强度、坡度及坡长对细沟侵蚀的交互效应分析[J]. 中国水土保持科学, 2011,9(6):8. LI Junlan, CAI Qiangguo, SUN Liying, et al. Analysis of interaction effects of rainfall intensity, slope degree and slope length on rill erosion[J]. Science of Soil and Water Conservation, 2011, 9(6):8.
[34]
LEI T W, NEARING M A, HAGHIGHI K, et al. Rill erosion and morphological evolution:A simulation model[J]. Water Resources Research, 1998, 34(11):3157.
[35]
WISCHMERIER W H, SMITH D D, UHLAND R E.Evaluation of factors in the soil loss equation[J]. Agricultural Engineering, 1958, 39(8):458.
[36]
田培, 潘成忠, 许新宜, 等. 坡面流速及侵蚀产沙空间变异性试验[J]. 水科学进展, 2015, 26(2):178. TIAN Pei, PAN Chengzhong, XU Xinyi, et al. Field experiment investigation into the spatial variability of overland flow velocity and soil erosion[J]. Advance in Water Science, 2015, 26(2):178.
[37]
杨维鸽, 郑粉莉, 王占礼,等. 地形对黑土区典型坡面侵蚀-沉积空间分布特征的影响[J]. 土壤学报, 2016, 53(3):572. YANG Weige, ZHENG Fenli1, WANG Zhanli, et al. Effects of topography on spatial distribution of soil erosion and deposition on hillslope in the typical of black soil region[J]. Acta Pedologica Sinica, 2016, 53(3):572.
[38]
ZHANG X C, NEARING M A, GARBRECHT J D. Gaining insights into interrill erosion processes using rare earth element tracers[J]. Geoderma, 2017(299):63.
[39]
李鹏, 李占斌, 郑良勇. 黄土陡坡径流侵蚀产沙特性室内试验研究[J]. 农业工程学报, 2005, 21(7):44. LI Peng, LI Zhanbin, ZHENG Liangyong. Indoor experiment of characteristics of runoff erosion in loess steep slope[J].Transactions of the CSAE, 2005, 21(7):44.
[40]
田均良. 侵蚀泥沙坡面沉积研究初报[J]. 水土保持研究, 1997, 4(2):58. TIAN Junliang. A primary report for a study on deposition of erosion sediments on slope[J]. Research of Soil and Water Conservation, 1997, 4(2):58.
[41]
董元杰, 史衍玺, 孔凡美, 等. 基于磁测的坡面土壤侵蚀空间分布特征研究[J]. 土壤学报, 2009, 46(1):148. DONG Yuanjie, SHI Yanxi, KONG Fanmei, et al. Magnetic-measurement-based spatial distribution of soil erosion on slope[J]. Acta Pedologica Sinica, 2009, 46(1):148.
[42]
李勉, 杨剑锋, 侯建才,等. 137Cs示踪法研究黄土丘陵区坡面侵蚀空间变化特征[J]. 核技术, 2009, 32(1):52. LI Mian, YANG Jianfeng, HOU Jiancai, et al. The spatial variance of hill slope erosion in loess hilly area by 137Cs tracing method[J]. Nuclear Techniques, 2009, 32(1):52.
[43]
PARSONS A J, BRAZIER R E, WAINWRIGHT J. Scale relationships in hillslope runoff and erosion[J]. Earth Surface Processes and Landforms, 2006, 31(11):1384.