细沟侵蚀影响因素和临界条件研究进展
Reviewing on Factors and Critical Conditions of Rill Erosion
查看参考文献65篇
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文摘
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细沟侵蚀是坡耕地时常发生的一种侵蚀形式.细沟侵蚀对坡面土壤侵蚀产沙有重要贡献,而且是坡面侵蚀由面蚀向沟蚀发展的过渡.本文分析了细沟侵蚀影响因素和临界条件研究取得的进展和存在的不足.影响细沟侵蚀的主要因素有降雨径流,土壤,地形,土壤表面特征和土地管理等因素,其中,前4者有多种指标来表征其效应,而土壤表面特征的影响还处于定性研究阶段.坡面需要达到特定的临界条件才可能发育细沟,细沟发生临界条件的研究主要从临界径流条件,临界土壤条件和临界地形条件等角度出发,各临界条件并非定值,而是关乎其他因素的综合指标.最后,本文对今后细沟侵蚀影响因素和临界条件研究可能的研究内容和方向进行了展望 |
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其他语种文摘
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Rill erosion plays an important role in soil erosion process in loess hillslopes. It is a quantum leap during the process of soil erosion on slopes, and also is the beginning of a qualitative change in the process of soil erosion. On the basis of studying many papers, the authors review the study of factors and critical conditions of rill erosion. Rainfall and runoff, soil, topography, soil surface characteristics and land management all have their impact on rill erosion. On the one hand, researches use a variety of parameters to represent the impact of rainfall and runoff, soil, topography and land management. On the other hand, there are two forms of soil surface characteristics, namely, surface roughness and surface soil crust. The studies on the impacts of both of them are still in a qualitative research stage, and some studies have shown they can weaken rill erosion, the other studies concluded that they would exacerbate the occurrence of rill erosion. The generation of rill on the slopes needs certain conditions, and the critical runoff, soil and terrain conditions have their corresponding research results. The critical conditions for the generation of rill are not numbers, but are related to many factors. Critical conditions for rill erosion are not fixed values, but all of them should be a comprehensive index of other factors. At the same time, the future possible research direction and contents of the influencing factors and the critical conditions of rill erosion are pointed out. More experiments and field observation data are needed. In rill erosion factors research, the following points need further works:(1)the quantitative analysis of the impact of rainfall and runoff on the joint action of rill erosion;(2)screening key indicators to represent the effect of soil, topography and land management factors;(3)an in-depth study on how the soil surface characteristics affect rill erosion, and a quantitative analysis of the impact of surface roughness and soil crust on rill erosion;(4)the interaction of various factors with the impact of rill erosion. Meanwhile, the studies of critical conditions of rill erosion need more investments, which include:(1)exploring the critical rainfall conditions for rill erosion, and finding out its relationship with critical runoff conditions,(2)a systematic study on the critical conditions in different areas,to obtain a judgment with strong applicability about whether rill erosion will occur |
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来源
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地理科学进展
,2010,29(11):1319-1325 【核心库】
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关键词
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细沟侵蚀
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影响因素
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临界条件
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土壤特征
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地址
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1.
中国科学院地理科学与资源研究所, 中国科学院陆地水循环与地表过程重点实验室, 北京, 100101
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中国科学院地理科学与资源研究所, 中国科学院陆地水循环与地表过程重点实验室;;黄土高原土壤侵蚀与旱地农业国家重点实验室, 北京, 100101
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语种
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中文 |
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ISSN
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1007-6301 |
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学科
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自然地理学 |
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基金
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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基金
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国家自然科学基金重点项目
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国家自然科学基金
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文献收藏号
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CSCD:4051258
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参考文献 共
65
共4页
|
|
1.
陈永宗.
黄土高原现代侵蚀与治理,1988
|
CSCD被引
121
次
|
|
|
|
|
2.
FAO.
Soil erosion by water:some measures for its control on cultivated lands,1965:141-156
|
CSCD被引
1
次
|
|
|
|
|
3.
Meyer L D. Effect or flow rate and canopy on rill erosion.
Transactions of the ASAE,1975,18(5):905-911
|
CSCD被引
23
次
|
|
|
|
|
4.
朱显谟. 黄土高原流水侵蚀的主要类型及有关因素.
水土保持通报,1982(1):1-9
|
CSCD被引
9
次
|
|
|
|
|
5.
郑粉莉. 坡耕地细沟侵蚀影响因素的研究.
土壤学报,1989,26(2):109-116
|
CSCD被引
67
次
|
|
|
|
|
6.
黄秉维. 谈黄河中游土壤保持问题.
中国水土保持,1983(1):8-13
|
CSCD被引
7
次
|
|
|
|
|
7.
雷廷武.
细沟侵蚀物理模型,2009
|
CSCD被引
18
次
|
|
|
|
|
8.
Foster G R. A closed form erosion equation for upland areas.
Sedimentation. Ft Collins. 210,1972
|
CSCD被引
1
次
|
|
|
|
|
9.
Foster G R. Transport of soil particles by shallow flow.
Transaction of the ASAE,1972,15(1):99-102
|
CSCD被引
38
次
|
|
|
|
|
10.
刘宝元. WEPP水蚀预报流域模型.
水土保持通报,1998,18(5):6-12
|
CSCD被引
41
次
|
|
|
|
|
11.
张玉斌. WEPP模型概述.
水土保持研究,2004,11(4):146-149
|
CSCD被引
27
次
|
|
|
|
|
12.
Foster G R. Modeling the soil erosion process.
Hydrologic modeling of Small Watersheds,ASAE, St, Joseph,MI(Chapter 8),1982:297-382
|
CSCD被引
1
次
|
|
|
|
|
13.
丁文峰. 坡面细沟侵蚀过程的水动力学特征试验研究.
水土保持学报,2002,16(3):72-75
|
CSCD被引
44
次
|
|
|
|
|
14.
陈力. 坡面细沟侵蚀的冲刷试验研究.
水动力学研究与进展,2005,20(6):761-766
|
CSCD被引
12
次
|
|
|
|
|
15.
R?mkens M J M. Soil erosion under different rainfall intensities, surface roughness, and soil water regimes.
Catena,2002,46(2):103-123
|
CSCD被引
1
次
|
|
|
|
|
16.
王治国. 黄土残塬区人工降雨条件下坡耕地水蚀的研究.I：影响细沟侵蚀因素的综合分析.
水土保持学报,1995,9(2):51-57
|
CSCD被引
17
次
|
|
|
|
|
17.
Yen B C. Dynamic equations for steady spatially varied flow.
Journal of Hydraulics Division,ASCE,1970,96(3):801-814
|
CSCD被引
9
次
|
|
|
|
|
18.
刘青泉. 坡面流及土壤侵蚀动力学(Ⅰ)--坡面流.
力学进展,2004,34(3):360-370
|
CSCD被引
37
次
|
|
|
|
|
19.
Emmett W W. Overland flow.
Hillslope Hydrology,1978:145-176
|
CSCD被引
20
次
|
|
|
|
|
20.
Yoon Y N. Spatially varied flow from controlled rainfall.
Journal of the Hydraulics Division, ASCE,1962,97(9):1367-1386
|
CSCD被引
5
次
|
|
|
|
|
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