黄河小北干流汛期和非汛期冲淤过程模拟
Simulation of sedimentation processes in dry and wet seasons in the Xiaobeiganliu reach of the Yellow River
查看参考文献23篇
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文摘
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滞后性是河流系统自动调整的重要特征之一。根据河道演变的滞后响应机制,在考虑上游来水来沙和下游侵蚀基准面(潼关高程)共同影响的基础上,建立了能够模拟河道汛期和非汛期冲淤过程的滞后响应模型,并采用黄河小北干流1960-2015年的冲淤资料进行参数率定(1960-2001年)和模型验证(2002-2015年)。结果表明该模型能较好地模拟小北干流汛期和非汛期的冲淤过程。汛期和非汛期累计冲淤量的模拟效果优于单个冲淤量;累计冲淤量和单个冲淤量的模拟效果汛期要优于非汛期。三门峡水库修建后,1960-2015年间小北干流汛期和非汛期的冲淤过程表现出时段差异。根据建立的滞后响应模型,本文分析了来水来沙和潼关高程对小北干流汛期和非汛期各个特征时段冲淤的贡献率,汛期和非汛期的第一时段(1960-1970年,1960-1968年)主要受到潼关高程的影响,但是后续时段主要受到来水来沙的影响。 |
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其他语种文摘
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Delayed response is one of important characteristics of self-adjustment in fluvial processes. Based on the mechanism of delayed response in fluvial processes, a delayed response model, considering the effects of water-sediment regime and the base level (Tongguan elevation), was developed to simulate the sedimentation processes in wet and dry seasons. The measured data in the period of 1960-2001 was used to estimate the parameters, and the measured data in the period of 2002-2015 was used to validate this model. Results showed that the proposed model could reasonably simulate the sedimentation processes in wet and dry seasons in the Xiaobeiganliu reach. This model performed better for cumulative sediment storage than single sediment storage in wet and dry seasons. Besides, this model also performed better for cumulative and single sediment storage in wet season than in dry season. Since the closure of Sanmenxia Dam, the sedimentation processes in wet and dry seasons in the Xiaobeiganliu has changed obviously in different periods during 1960-2015. Using this model, the contributions of water-sediment regime and the Tongguan elevation on sedimentation in different periods were analyzed. The sedimentation process was mainly affected by the Tongguan elevation in the period of 1960-1970(wet season) and 1960-1968(dry season). However, it was dominated by water-sediment regime after 1970(wet season) and 1968(dry season). |
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来源
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地理学报
,2018,73(5):880-892 【核心库】
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DOI
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10.11821/dlxb201805008
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关键词
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小北干流
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冲淤
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潼关高程
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滞后响应模型
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汛期和非汛期
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地址
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清华大学, 水沙科学与水利水电工程国家重点实验室, 北京, 100084
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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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0375-5444 |
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学科
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水利工程 |
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基金
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国家重点研发计划
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国家自然科学基金重点项目
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文献收藏号
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CSCD:6229011
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参考文献 共
23
共2页
|
|
1.
Schumm S A.
The Fluvial System,1977
|
CSCD被引
42
次
|
|
|
|
|
2.
Viles H A. Biogeomorphological disturbance regimes: Progress in linking ecological and geomorphological systems.
Earth Surface Processes and Landforms,2008,33(9):1419-1435
|
CSCD被引
3
次
|
|
|
|
|
3.
Lane S N. Interactions between sediment delivery, channel change, climate change and flood risk in a temperate upland environment.
Earth Surface Processes and Landforms,2007,32(3):429-446
|
CSCD被引
7
次
|
|
|
|
|
4.
Mackin J H. Concept of the graded river.
Geological Society of America Bulletin,1948,59(5):463-512
|
CSCD被引
14
次
|
|
|
|
|
5.
钱宁.
河床演变学,1987
|
CSCD被引
304
次
|
|
|
|
|
6.
Surian N. Morphological response to river engineering and management in alluvial channels in Italy.
Geomorphology,2003,50(4):307-326
|
CSCD被引
31
次
|
|
|
|
|
7.
Wu B. A general framework for using the rate law to simulate morphological response to disturbance in the fluvial system.
Progress in Physical Geography,2012,36(5):575-597
|
CSCD被引
5
次
|
|
|
|
|
8.
Knighton D.
Fluvial Forms and Processes: A New Perspective,1998
|
CSCD被引
7
次
|
|
|
|
|
9.
Owens P N. Sediment response to catchment disturbances.
Journal of Soils and Sediments,2010,10(4):591-596
|
CSCD被引
1
次
|
|
|
|
|
10.
Schumm S A. Sediment yield from disturbed earth systems.
Geology,1995,23(5):391-394
|
CSCD被引
1
次
|
|
|
|
|
11.
Dang M H. Long-term riverbed response of lower Tedori River, Japan, to sediment extraction and dam construction.
Environmental Earth Sciences,2014,72(8):2971-2983
|
CSCD被引
4
次
|
|
|
|
|
12.
Graf W L. The rate law in fluvial geomorphology.
American Journal of Science,1977,277(2):178-191
|
CSCD被引
18
次
|
|
|
|
|
13.
王兆印. 潼关高程对渭河河床演变的影响.
水利学报,2004(9):1-8
|
CSCD被引
15
次
|
|
|
|
|
14.
吴保生. 冲积河流河床演变的滞后响应模型-Ⅰ模型建立.
泥沙研究,2008(6):1-7
|
CSCD被引
34
次
|
|
|
|
|
15.
吴保生. 冲积河流河床演变的滞后响应模型-Ⅱ模型应用.
泥沙研究,2008(6):30-37
|
CSCD被引
23
次
|
|
|
|
|
16.
郑珊. 黄河小北干流和渭河下游淤积过程模拟.
水利学报,2014,45(2):150-162
|
CSCD被引
11
次
|
|
|
|
|
17.
任美锷. 黄河的输沙量：过去、现在和将来——距今15万年以来的黄河泥沙收支表.
地球科学进展,2006,21(6):551-563
|
CSCD被引
30
次
|
|
|
|
|
18.
王均平.
黄河中游晚新生代地貌演化与黄河发育,2006
|
CSCD被引
6
次
|
|
|
|
|
19.
张金良. 关于三门峡水库若干问题认识与思考.
泥沙研究,2001(2):66-69
|
CSCD被引
1
次
|
|
|
|
|
20.
程龙渊.
三门峡库区水文泥沙实验研究,1999
|
CSCD被引
13
次
|
|
|
|
|
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