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上方来水来沙的异位侵蚀效应研究进展
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  • 英文篇名:Review on the off-site erosion effect of up-slope runoff and sediment
  • 作者:王杉杉 ; 李占斌 ; 张乐涛 ; 马波
  • 英文作者:WANG Shanshan;LI Zhanbin;ZHANG Letao;MA Bo;State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau,Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources;University of Chinese Academy of Sciences;College of Environment and Planning,Henan University;
  • 关键词:上方来水来沙 ; 土壤侵蚀 ; 异位侵蚀效应 ; 水土保持措施 ; 研究进展
  • 英文关键词:up-slope runoff and sediment;;soil erosion;;off-site erosional effect;;soil and water conservation;;research advance
  • 中文刊名:STBC
  • 英文刊名:Science of Soil and Water Conservation
  • 机构:中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室;中国科学院大学;河南大学环境与规划学院;
  • 出版日期:2019-04-15
  • 出版单位:中国水土保持科学
  • 年:2019
  • 期:v.17
  • 基金:国家自然科学基金重点项目“黄土高原生态建设的生态—水文响应研究机理”(41330858)
  • 语种:中文;
  • 页:STBC201902017
  • 页数:7
  • CN:02
  • ISSN:10-1449/S
  • 分类号:143-149
摘要
上方来水来沙作为上下不同地貌部位之间水流能量传递的媒介和泥沙输移的载体,对下游侵蚀产沙过程具有重要影响,是土壤侵蚀研究的关键环节。以往研究多侧重于小流域泥沙来源以及上方来水来沙的异位沉积效应,对上方来水来沙的异位侵蚀效应研究相对较少。本文回顾了上方来水来沙异位侵蚀效应的研究方法,在总结归纳前人研究成果的基础上,首次提出了"异位侵蚀"的概念,从异位径流特征、侵蚀产沙等方面,分析了裸露坡面上方来水来沙的异位侵蚀效应,并对水土保持措施异位减蚀作用的研究进展进行了综述。在此基础上,进一步探讨了异位侵蚀研究中的热点和难点问题,提出可从明确异位侵蚀效应概念、探索异位侵蚀影响因素及其机理、阐明上方来水来沙异位侵蚀过程中水沙和能量传递特征、量化水土保持措施异位减蚀作用等4个方面进一步深入研究上方来水来沙的异位侵蚀效应。
        [Background] Up-slope runoff and sediment play an important role in energy deliver and sediment transport between the adjacent section. The change of up-slope runoff and sediment will affect the soil erosion process of down-slope. Thus,it is the vital content of soil erosion to study the up-slope runoff and sediment. However, previous studies mainly focused on the sediment sources of small watershed and the off-site depositional effects of up-slope runoff and sediment,while less studies focused on the off-site erosional effect of up-slope runoff and sediment. [Methods] This paper reviewed the study methods of the off-site erosional effect of up-slope runoff and sediment. Based on the previous research,the "off-site erosion"was firstly proposed in this paper. And then,it summarized the research achievements of predecessors. In terms of the characteristics of off-site runoff and sediment yield,the paper summarized the off-site erosional effect of up-slope runoff and sediment on the bare slope,and the research progress of the influence of soil and water conservation on the off-site erosional effect.Furthermore,it discussed the hotspots,challenges,and the future research directions of the off-site erosional effect. [Results]"Off-site erosion"refers to the change of downslope runoff characteristics and the sediment yield caused by up-slope runoff and sediment. The up-slope runoff and sediment joined into the down-slope and increased the runoff energy of down-slope. Besides,the runoff velocity,hydraulic radius,Reynolds number and Froude number increased,while resistance coefficient decreased. Based on the analysis of observed data and simulation experiments,the up-slope runoff and sediment would increase the sediment yield of down-slope. However,when the sediment concentration of runoff came to the sediment carrying capacity of runoff,the runoff with sediment couldn't erosive the down-slope soil,and even to deposit. The soil and water conservation measures on slope decreased runoff amount and sediment yield entering the down-slope. Some scholars thought soil and water conservation on slope decreased the off-site sediment yield,while others drew the opposite conclusion. Engineering measures,such as dams,drastically cut the runoff erosional energy,thus they had the decreased effect on off-site.[Conclusions]"Off-site erosion"is a relatively spatial concept,but how to reasonably define the upslope and down-slope regions,there is still no clear definition. Up-slope runoff and sediment,erosion pattern evolution process and erosion process interacted with each other. Meantime,off-site erosional effect of up-slope runoff and sediment would be impacted by the dynamic change,such as rainfall intensity,underlying surface,sediment concentration and sediment carrying capacity. Further research of the off-site erosional effect of up-slope runoff and sediment could be conducted in confirming the concept of "off-site erosion",exploring the influence factors and mechanism of off-site erosion,illuminating the transfer characteristics of sediment and runoff energy during the off-site erosional process of up-slope runoff and sediment, as well as quantitating the off-site less erosional effect of soil and water conservation.
引文
[1]李景玉,张楠,王荣彬.黄河流域土壤侵蚀产沙模型研究进展[J].地理科学进展,2006,25(2):103.LI Jingyu,ZHANG Nan,WANG Rongbin.Soil erosion and sedimentation model in the Yellow River basin:Stateof-the art review[J].Progress in Geography,2006,25(2):103.
    [2]高均凯.土壤侵蚀的环境效应[J].生态农业研究,1993,1(4):19.GAO Junkai.The environmental impacts of soil erosion[J].Eco-Agriculture Research,1993,1(4):19.
    [3]PIMENTEL D,HARVEY C,RESOSUDARMO P,et al.Environmental and economic costs of soil erosion and conservation benefits[J].Science,1995,267(5201):1117.
    [4]刘婧春,岳大鹏,郭坤杰,等.20世纪60年代以来黄土高原小流域泥沙来源的方法与历史侵蚀过程研究进展[J].江西农业学报,2016,28(4):77.LIU Jingchun,YUE Dapeng,GUO Kunjie,et al.Research progress in methods for sediment source and historical erosion process of small watershed in loess plateau since 1960s[J].Acta Agriculturae Jiangxi,2016,28(4):77.
    [5]魏霞,李占斌,李勋贵.黄土高原坡沟系统土壤侵蚀研究进展[J].中国水土保持科学,2012,10(1):108.WEI Xia,LI Zhanbin,LI Xungui.Research progress on soil erosion of slope-gully systems in the Loess Plateau[J].Science of Soil and Water Conservation,2012,10(1):108.
    [6]MULLAN D.Soil erosion under the impacts of future climate change:Assessing the statistical significance of future changes and the potential on-site and off-site problems[J].Catena,2013,109(10):234.
    [7]BOARDMAN J,SHEPHEARD M L,WALKER E,et al.Soil erosion and risk-assessment for on-and off-farm impacts:A test case using the Midhurst area,West Sussex,UK[J].Journal of Environmental Management,2009,90(8):2578.
    [8]PETRI E,JOUNI L.Does control of soil erosion inhibit aquatic eutrophication?[J].Journal of Environmental Management,2012,93(1):140.
    [9]张乐涛,高照良,李永红,等.黄土丘陵区堆积体边坡对上方来水的侵蚀响应[J].水科学进展,2015,26(6):811.ZHANG Letao,GAO Zhaoliang,LI Yonghong,et al.Downslope erosion response of engineered landform to upslope runoff in loess hilly region[J].Advances in Water Science,2015,26(6):811.
    [10]陈浩.降雨特征和上坡来水对产沙的综合影响[J].水土保持学报,1992,6(2):17.CHEN Hao.The synthetic effect of rainfall characteristics and runoff from upper slope on sediment generation[J].Journal of Soil and Water Conservation,1992,6(2):17.
    [11]肖培青.上方来水来沙对坡面侵蚀过程影响的试验研究[D].陕西杨凌:西北农林科技大学,2001:1.XIAO Peiqing.An experimental study on effects of upslope runoff and sediment on down-slope erosion process[D].Yangling,Shaanxi:Northwest A&F University,2001:1.
    [12]ZUO Depeng,XU Zongxue,YAO Wenyi,et al.Assessing the effects of changes in land use and climate on runoff and sediment yields from a watershed in the Loess Plateau of China[J].Science of the Total Environment,2016,544:238.
    [13]ZHOU Yuanyuan,SHI Changxing,FAN Xiaoli,et al.The influence of climate change and anthropogenic activities on annual runoff of Huangfuchuan basin in northwest China[J].Theoretical and Applied Climatology,2015,120(1/2):137.
    [14]LIU Jieying,YU Ming,WU Yong,et al.Scenario analysis of soil and water conservation in Xiejia watershed based on improved CSLE model[C].IOP Conference Series:Earth and Environmental Science,2018:1.
    [15]LIU Xiaoyan,YANG Shengtian,DANG Suzhen,et al.Response of sediment yield to vegetation restoration at a large spatial scale in the Loess Plateau[J].Science China Technological Sciences,2014,57(8):1482.
    [16]曾伯庆.晋西黄土丘陵沟壑区水土流失规律及治理效益[J].人民黄河,1980(2):20.ZENG Boqing.Soil and ater loss law and control benefit in loess hilly region of west part of Shanxi province[J].Yellow River,1980(2):20.
    [17]陈浩.黄河中游小流域的泥沙来源研究[J].土壤侵蚀与水土保持学报,1999,5(1):19.CHEN Hao.Sediment source on small basin in middle reaches of Yellow River[J].Journal of Soil Erosion and Soil and Water Conservation,1999,5(1):19.
    [18]肖培青,郑粉莉.上方来水来沙对细沟侵蚀产沙过程的影响[J].水土保持通报,2001,21(1):23.XIAO Peiqing,ZHENG Fenli.Effect of run-on water and sediment on rill erosion process at down-slope section[J].Bulletin of Soil and Water Conservation,2001,21(1):23.
    [19]郭忠录,马美景,蔡崇法,等.模拟降雨径流作用下红壤坡面侵蚀水动力学机制[J].长江流域资源与环境,2017,26(1):150.GUO Zhonglu,MA Meijing,CAI Chongfa,et al.Soil erosion and flow hydraulics on red soil slope under simulated rainfall/runoff[J].Resources and Environment in the Yangtze Basin,2017,26(1):150.
    [20]孔亚平,张科利.黄土坡面侵蚀产沙沿程变化的模拟试验研究[J].泥沙研究,2003,(1):33.KONG Yaping,ZHANG Keli.The distribution of soil loss on the surface of loess slope[J].Journal of Sediment Research,2003,(1):33.
    [21]焦菊英,刘元保,唐克丽.小流域沟间与沟谷地径流泥沙来量的探讨[J].水土保持学报,1992,6(2):24.JIAO Juying,LIU Baoyuan,TANG Keli.An approach to runoff and sediment generation of gully and intergully land in small watershed[J].Journal of Soil and Water Conservation,1992,6(2):24.
    [22]肖培青,郑粉莉,张成娥.细沟侵蚀过程与细沟水流水力学参数的关系研究[J].水土保持学报,2001,15(1):54.XIAO Peiqing,ZHENG Fenli,ZHANG Cheng'e.Research on rill erosion process and rill flow hydraulics parameters[J].Journal of Soil and Water Conservation,2001,15(1):54.
    [23]车小力,王文龙,郭军权,等.上方来水来沙对浅沟侵蚀产沙及水动力参数的影响[J].中国水土保持科学,2011,9(3):26.CHE Xiaoli,WANG Wenlong,GUO Junquan,et al.Effects of up-slope runoff and sediment on ephemeral gully erosion sediment and hydraulic parameters[J].Science of Soil and Water Conservation,2011,9(3):26.
    [24]肖培青,郑粉莉,姚文艺.坡沟系统坡面径流流态及水力学参数特征研究[J].水科学进展,2009,20(2):236.XIAO Peiqing,ZHENG Fenli,YAO Wenyi.Flow pattern and hydraulic parameter characteristics in hillslopegullyslope system[J].Advances in Water Science,2009,20(2):236.
    [25]西峰水土保持实验站.南小河沟流域综合治理增产减沙效益[J].山西水土保持科技,1976(2):29.Xifeng Water and Soil Conservation Experimental Station.The production increase and sediment reduction benefits of comprehensive treatment in Nanxiaohe basin[J].Soil and Water Conservation Science and Technology in Shanxi,1976(2):29.
    [26]肖培青,郑粉莉,贾媛媛.基于双土槽试验研究的黄土坡面侵蚀产沙过程[J].中国水土保持科学,2003,1(4):10.XIAO Peiqing,ZHENG Fenli,JIA Yuanyuan.Loess hill slope erosion and sediment yield process using a dual box system[J].Science of Soil and Water Conservation,2003,1(4):10.
    [27]王文龙,雷阿林,李占斌,等.黄土区坡面侵蚀时空分布与上坡来水作用的实验研究[J].水利学报,2004,35(5):25.WANG Wenlong,LEI Alin,LI Zhanbin,et al.Experimental study on spatial and temporal distribution of erosion on loess slope[J].Journal of Hydraulic Engineering,2004,35(5):25.
    [28]郑粉莉,康绍忠.黄土坡面不同侵蚀带侵蚀产沙关系及其机理[J].地理学报,1998,53(5):40.ZHENG Fenli,KANG Shaozhong.Erosion and sediment yield in different zones of loess slopes[J].Acta Geographica sinica,1998,53(5):40.
    [29]武敏,郑粉莉,黄斌.黄土坡面汇流汇沙对浅沟侵蚀影响的试验研究[J].水土保持研究,2004,11(4):74.WU Min,ZHENG Fenli,HUANG Bin.Experimental study on upslope runoff effects on ephemeral gully erosion processes at loessial hillslope[J].Research of Soil and Water Conservation,2004,11(4):74.
    [30]ZHANG Xinhe,ZHENG Fenli,WANG Xiaoyong.Effects of up-slope runoff on erosion processes at down slope shallow gully erosion areas[J].Journal of Northwest Sci-Tech University of Agriculture and Forestry,2008,36(3):105.
    [31]肖培青,郑粉莉.上方汇水汇沙对坡面侵蚀过程的影响[J].水土保持学报,2003,17(3):25.XIAO Peiqing,ZHENG Fenli.Effects of runoff and sediment from upslope on downslope erosion process[J].Journal of Soil and W ater Conservation,2003,17(3):25.
    [32]ZHENG Fenli,GAO Xuetian.Effects of upslope runoff and sediment on erosion process at downslope area[C].Soil Erosion,2001:163.
    [33]谭贞学,王占礼,马春艳,等.黄土坡面下坡位土壤侵蚀过程的模拟试验[J].中国水土保持科学,2009,7(2):12.TAN Zhenxue,WANG Zhanli,MA Chunyan,et al.Simulated-rainfall experimental research on soil erosion processes on downslope segment of loess hillslope[J].Science of Soil and Water Conservation,2009,7(2):12.
    [34]蔡强国,陆兆熊,王贵平.黄土丘陵沟壑区典型小流域侵蚀产沙过程模型[J].地理学报,1996,51(2):108.CAI Qiangguo,LU Zhaoxioang,WANG Guiping.Process-based soil erosion and sediment yieid model in a small basin in the hilly loess region[J].Acta Geographica Sinica,1996,51(2):108.
    [35]ZHANG Guanghui,LIU Yumei,HAN Yanfang,et al.Sediment transport and soil detachment on steep slopes:II.Sediment feedback relationship[J].Soil Science Society of America Journal,2009,73(4):1298.
    [36]HUANG C,WELLS L K,NORTON L D.Sediment transport capacity and erosion processes:Model concepts and reality[J].Earth Surface Processes and Landforms,1999,24(6):503.
    [37]王文龙,莫翼翔,雷阿林,等.黄土区土壤侵蚀链各垂直带水沙流时空分布特征研究[J].水动力学研究与进展(A辑),2003,18(5):540.WANG Wenlong,MO Yixiang,LEI Alin,et al.Temporal and spatial distribution characteristic of water-sand flow in vertical belts of soil erosion chain in loess region[J].Journal of Hydrodynamics(Ser A),2003,18(5):540.
    [38]陈浩,蔡强国.坡面植被恢复对沟道侵蚀产沙的影响[J].中国科学(D辑:地球科学),2006,36(1):69.CHEN Hao,CAI Qiangguo.Impact of hillslope vegetation restoration on gully erosion induced sediment yield[J].Science in China:Series D Earth Sciences,2006,36(1):69.
    [39]丁文峰,李勉.放水冲刷条件下坡面植被空间布局对坡沟系统侵蚀产沙的影响研究[J].土壤学报,2011,48(5):1103.DING Wenfeng,LI Mian.Effect of downslope vegetation distribution on sediment yield of slope-gully system exposed to runoff scouring[J].Acta Pedologica Sinica,2011,48(5):1103.
    [40]郑明国,蔡强国,王彩峰,等.黄土丘陵沟壑区坡面水保措施及植被对流域尺度水沙关系的影响[J].水利学报,2007,38(1):47.ZHENG Mingguo,CAI Qiangguo,WANG Caifeng,et al.Effect of vegetation and other measures for soil and water conservation on runoff-sediment relationship in watershed scale[J].Journal of Hydraulic Engineering,2007,38(1):47.
    [41]YAGHMAEI H,SADEGHI S H,MORADI H,et al.Effect of Dam operation on monthly and annual trends of flow discharge in the Qom Rood Watershed,Iran[J].Journal of Hydrology,2017,557:254.
    [42]方学敏,万兆惠,匡尚富.黄河中游淤地坝拦沙机理及作用[J].水利学报,1998,29(10):49.FANG Xuemin,WAN Zhaohui,KUANG Shangfu.Mechanism and effect of silt-arrest dams for sediment reduction in the middle Yellow River basin[J].Journal of Hydraulic Engineering,1998,29(10):49.
    [43]冉大川,罗全华,刘斌,等.黄河中游地区淤地坝减洪减沙及减蚀作用研究[J].水利学报,2004,35(5):7.RAN Dachuan,LUO Quanhua,LIU Bin,et al.Effect of soil-retaining dams on flood and sediment reduction in middle reaches of Yellow River[J].Journal of Hydraulic Engineering,2004,35(5):7.
    [44]LI X H,YANG J,ZHAO C Y,et al.Runoff and sediment from orchard terraces in southeastern China[J].Land Degradation&Development,2014,25(2):184.
    [45]HE Jijun,CAI Qiangguo,LI Guoqiang,et al.Integrated erosion control measures and environmental effects in rocky mountainous areas in northern China[J].International Journal of Sediment Research,2010,25(3):294.
    [46]MAETENS W,POESEN J,VANMAERCKE M.How effective are soil conservation techniques in reducing plot runoff and soil loss in Europe and the Mediterranean?[J].Earth-Science Reviews,2012,115(1/2):21.
    [47]张新和,郑粉莉,汪晓勇,等.上方汇水对黄土坡面侵蚀方式演变及侵蚀产沙的影响[J].西北农林科技大学学报(自然科学版),2008,36(3):105.ZHANG Xinhe,ZHENG Fenli,WANG Xiaoyong,et al.Effects of upslope runoff on loessial hillslope erosion pattern evolution process and erosion sediment[J].Journal of Northwest A&F University(Natural Science Eolition),2008,36(3):105.
    [48]王文龙,雷阿林,李占斌,等.土壤侵蚀链内细沟浅沟切沟流动力机制研究[J].水科学进展,2003,14(4):471.WANG Wenlong,LEI Alin,LI Zhanbin,et al.Study on dynamic mechanism of rills,shallow furrows and gully in the soil erosion chain[J].Advances in Water Science,2003,14(4):471.
    [49]ZHANG Letao,GAO Zhaoliang,LI Zhanbin,et al.Downslope runoff and erosion response of typical engineered landform to variable inflow rate patterns from upslope[J].Natural Hazards,2016,80(2):775.

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