Fluvial diversity in relation to valley setting in the source region of the Yangtze and Yellow Rivers
查看参考文献59篇
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文摘
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The spatial distribution of valley setting (laterally-unconfined, partly-confined, or confined) and fluvial morphology in the source region of the Yangtze and Yellow Rivers is contrasted and analyzed.The source region of the Yangtze River is divided into 3 broad sections (Ⅰ, Ⅱ and Ⅲ) based on valley setting and channel gradient, with the upstream and downstream sections being characterized by confined (some reaches partly-confined) valleys, while the middle section is characterized with wide and shallow, laterally-unconfined valleys.Gorges are prominent in sections Ⅰ and Ⅲ, while braided channel patterns dominate section Ⅱ.By contrast, the source region of the Yellow River is divided into 5 broad sections (sections Ⅰ-Ⅴ) based on valley characteristics and channel gradient.Sections Ⅰ, Ⅱ and Ⅳ are alluvial reaches with mainly laterally-unconfined (some short reaches partly-confined) valleys.Sections Ⅲ and Ⅴ are mainly confined or partly-confined.Greater morphological diversity is evident in the source region of the Yellow River relative to the upper Yangtze River.This includes braided, anabranching, anastomosing, meandering and straight alluvial patterns, with gorges in confined reaches.The macro-relief (elevation, gradient, aspect, valley alignment and confinement) of the region, linked directly to tectonic movement of the Qinghai-Tibet Plateau, tied to climatic, hydrologic and biotic considerations, are primary controls upon the patterns of river diversity in the region. |
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来源
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Journal of Geographical Sciences
,2013,23(5):817-832 【核心库】
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DOI
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10.1007/s11442-013-1046-2
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关键词
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valley setting
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fluvial morphology
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river patterns
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spatial distribution
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source region of the Yangtze and Yellow Rivers
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地址
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1.
Institute of Geographic Sciences and Natural Resources Research, CAS, Key Laboratory of Water Cycle and Related Land Surface Processes, CAS, Beijing, 100101
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Tsinghua University, State Key Laboratory of Hydroscience and Engineering, Beijing, 100084
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School of Environment, University of Auckland, New Zealand, Auckland, 92019
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Changjiang River Scientific Research Institute, Wuhan, 430010
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语种
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英文 |
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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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1009-637X |
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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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国家自然科学基金
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International Science & Technology Cooperation Program of China
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文献收藏号
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CSCD:5021273
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参考文献 共
59
共3页
|
|
1.
An Z S. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since Late Miocene times.
Nature,2001,411:62-66
|
CSCD被引
691
次
|
|
|
|
|
2.
Ashworth P J. How do big rivers come to be different?.
Earth Science Reviews,2012,114:84-107
|
CSCD被引
4
次
|
|
|
|
|
3.
Blue B. Geodiversity in the Yellow River source zone.
Journal of Geographical Sciences,2013,23(5):775-792
|
CSCD被引
10
次
|
|
|
|
|
4.
Brierley G J. River styles, a geomorphic approach to catchment characterization: Implications for river rehabilitation in Bega catchment, New South Wales, Australia.
Environmental Management,2000,25:661-679
|
CSCD被引
7
次
|
|
|
|
|
5.
Brierley G J.
Geomorphology and River Management: Applications of the River Styles Framework,2005:398
|
CSCD被引
1
次
|
|
|
|
|
6.
Corenblit D. Reciprocal interactions and adjustments between fluvial landforms and vegetation dynamics in river corridors: A review of complementary approaches.
Earth Science Review,2007,84:56-86
|
CSCD被引
5
次
|
|
|
|
|
7.
Coulthard T J. Effects of vegetation on braided stream pattern and dynamics.
Water Resources Research,2005,41:W04003
|
CSCD被引
4
次
|
|
|
|
|
8.
Craddock W H. Rapid fluvial incision along the Yellow River during headward basin integration.
Nature Geoscience,2010,3:209-213
|
CSCD被引
54
次
|
|
|
|
|
9.
Crosato A. Simple physics-based predictor for the number of river bars and the transition between meandering and braiding.
Water Resources Research,2009,45(3):W03424
|
CSCD被引
6
次
|
|
|
|
|
10.
Davies N S. Evolution of fixed-channel alluvial plains in response to Carboniferous vegetation.
Nature Geoscience,2011,4:629-632
|
CSCD被引
2
次
|
|
|
|
|
11.
Deng X F. Evolution of Quaternary glaciers and environment on the eastern side of the Geladandong Peak.
Journal of Glaciology and Geocryology,1992,14(2):153-160
|
CSCD被引
3
次
|
|
|
|
|
12.
Eaton B C. Assessing the effect of vegetation-related bank strength on channel morphology and stability in gravel-bed streams using numerical models.
Earth Surface Processes and Landforms,2008,34:712-724
|
CSCD被引
3
次
|
|
|
|
|
13.
Eaton B C. Channel patterns: Braided, anabranching, and single-thread.
Geomorphology,2010,120(3/4):353-364
|
CSCD被引
21
次
|
|
|
|
|
14.
Fotherby L M. Valley confinement as a factor of braided river pattern for the Platte River.
Geomorphology,2009,103(4):562-576
|
CSCD被引
5
次
|
|
|
|
|
15.
Fryirs K. Antecedent controls on river character and behaviour in partly-confined valley settings: Upper Hunter catchment, NSW, Australia.
Geomorphology,2010,117:106-120
|
CSCD被引
3
次
|
|
|
|
|
16.
Fu B. Displacement and timing of left-lateral faulting in the Kunlun Fault Zone, northern Tibet, inferred from geologic and geomorphic features.
Journal of Asian Earth Sciences,2007,29(2/3):253-265
|
CSCD被引
11
次
|
|
|
|
|
17.
Graf W L. Fluvial adjustments to the spread of tamarisk in the Colorado Plateau region.
Geological Society of America Bulletin,1978,89:1491-1501
|
CSCD被引
2
次
|
|
|
|
|
18.
Gran K. Riparian vegetation controls on braided stream dynamics.
Water Resources Research,2001,37(12):3275-3283
|
CSCD被引
6
次
|
|
|
|
|
19.
Gregory K J. Vegetation and river channel form and process.
Biogeomorphology,1988:11-42
|
CSCD被引
1
次
|
|
|
|
|
20.
Guccione M J. Stream response to repeated coseismic folding, Tiptonville dome, New Madrid seismic zone.
Geomorphology,2002,43:313-349
|
CSCD被引
1
次
|
|
|
|
|
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