产沙模数与流域面积关系研究进展
A Review of the Relationship Between Specific Sediment Yield and Drainage Area
查看参考文献26篇
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文摘
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流域面积是综合地表一切要素的黑箱变量，而产沙模数是流域产沙强度的重要体现。自20世纪50年代以来，有关产沙模数随流域面积变化的研究受到了国内外学者的广泛关注。本文对多年来有关该方面的研究成果进行总结、提炼，在此基础上，把产沙模数与流域面积的变化关系划分为5种类型，即负相关关系，正相关关系，先增加后减小的非线性关系，先减小后增加的非线性关系以及无显著关系等，继而对每种类型出现的原因给出了合理的解释：在此基础上，指出产沙模数随流域面积变化的本质原因，即产沙模数随流域面积的变化是对流域内各种因素及因素间相互作用的响应，产沙模数与流域面积之间没有内在的联系，产沙模数随流域面积的增加可以出现任何变化。 |
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其他语种文摘
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Drainage area （A） is a lumped variable as all the environmental variables are involved within it, and specific sediment yield （Ys） is an index of soil erosion intensity of some drainage basin. Since the 1950s, study on the relationships between drainage area and specific sediment yield has attracted attention at home and abroad, and more and more work about Ys-A relationships has been conducted in recent years. Under this condition, the achievements of Ys-A relationships were summarized and analyzed in this paper, and then 5 types of Ys-A relationships were identified,including the direct, the reverse, the firstly increased and then decreased, the firstly decreased and then increased, and no specific relations, followed by reasonable explanations of the 5-typed relationships. The essential reason for the specific sediment yield changes with drainage area was pointed out that it is just the response to functions of the environmental variables in river basins, and there is no essential relationship between specific sediment yield and drainage area. It could be extended that all the possibilities could occur with the increase of the drainage area for the specific sediment yield if transport were changed for a certain river basin. variables influencing soil erosion and sediment |
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来源
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地理科学进展
,2008,27(6):63-69 【核心库】
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关键词
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产沙模数
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流域面积
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类型
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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, 中科院陆地水循环与地表过程重点实验室, 北京, 100101
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中国科学院烟台海岸带可持续发展研究所, 山东, 烟台, 264003
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1007-6301 |
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学科
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地球物理学;水利工程 |
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基金
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国家自然科学基金
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治黄专项基金项目（黄水保200651-02）
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文献收藏号
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CSCD:3452915
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参考文献 共
26
共2页
|
|
1.
王飞. 水土流失研究中尺度效应及其机理分析.
水土保持学报,2003,17(2):167-180
|
CSCD被引
23
次
|
|
|
|
|
2.
Renschler C S. Soil erosion assessment tools from point to regional scales:The role of geomorphologists in land management research and implementation.
Geomorphology,2002,47:189-209
|
CSCD被引
23
次
|
|
|
|
|
3.
Walling D E. Suspended sediment and solute response characteristics of river Exe.
Devon,1978:167-197
|
CSCD被引
1
次
|
|
|
|
|
4.
Sehumm S A.
The Fluvial System,1977
|
CSCD被引
1
次
|
|
|
|
|
5.
Brune G M. Sediment records in Midwestern United States.
International Association of Scientific Hydrology:Wallingford,1951:29-38
|
CSCD被引
1
次
|
|
|
|
|
6.
Dendy F E. Sediment yield-runoff-drainage area relationships in the United States.
Journal of Soil and Water Conservation,1976,31:264-266
|
CSCD被引
10
次
|
|
|
|
|
7.
Milliman J D. Geomorphic/tectonic control of sediment discharge to the ocean:the importance of small mountainous rivers.
Journal of Geology,1992,100:525-544
|
CSCD被引
202
次
|
|
|
|
|
8.
Summerfield M A. Natural controls of fluvial denudation rates in major world drainage basins.
Journal of Geophysical Research,1994,99:871-883
|
CSCD被引
1
次
|
|
|
|
|
9.
Einsele G. Terrestrial sediment yield and the lifetimes of reservoirs, lakes, and larger basins.
Geologische Randschan,1997,86:288-310
|
CSCD被引
1
次
|
|
|
|
|
10.
Lane J L. Processes controlling sediment yield from watersheds as functions of spatial scale.
Environmental Modeling and Software,1997,12:355-369
|
CSCD被引
14
次
|
|
|
|
|
11.
Xu J X. Scale effects on specific sediment yield in the Yellow River Basin and geomorphological explanations.
Journal of Hydrology,2005,307:219-232
|
CSCD被引
23
次
|
|
|
|
|
12.
Owens P. Late Holocene sediment yields in small alpine and subalpine drainage basins.
British Columbia,1992,209:147-154
|
CSCD被引
2
次
|
|
|
|
|
13.
Rondeau B. Budget and sources of suspended sediment transported in the St.Lawrence River, Canada..
Hydrological Processes,2000,14:21-36
|
CSCD被引
3
次
|
|
|
|
|
14.
Krishnaswamy J. Spatial patterns of suspended sediment yields in a humid tropical watershed in Costa Rica.
Hydrological Processes,2001,15:2235-2257
|
CSCD被引
1
次
|
|
|
|
|
15.
de Vente J. Predicting catchment sediment yield in Mediterranean environments:The importance of sediment source and connectivity in Italian drainage basins.
Earth Surface Processes and Landforms,2006,31:1017-1034
|
CSCD被引
2
次
|
|
|
|
|
16.
卢金发. 黄河中游流域地貌形态对流域产沙量的影响.
地理研究,2002,21(2):171-178
|
CSCD被引
26
次
|
|
|
|
|
17.
闫云霞. 黄土高原地区侵蚀产沙的尺度效应研究初探.
中国科学(D地球科学),2006,36:1-10
|
CSCD被引
2
次
|
|
|
|
|
18.
Osterkamp W R. Geomorphic considerations for erosion prediction.
Environmental Geology,1995,29:152-157
|
CSCD被引
1
次
|
|
|
|
|
19.
de Vente J. Predicting soil erosion and sediment yield at the basin scale.
Scale issues and semiquantitative models,2005,71:95-125
|
CSCD被引
1
次
|
|
|
|
|
20.
Church M. Disequilibrium of Hoiocene sediment yield in glaciated British Columbia.
Nature,1989,337:452-454
|
CSCD被引
11
次
|
|
|
|
|
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