不同流路时期黄河下游河道的冲淤变化过程

doi:10.11821/xb201005010

地理学报 ›› 2010, Vol. 65 ›› Issue (5): 613-622.doi: 10.11821/xb201005010

不同流路时期黄河下游河道的冲淤变化过程

彭俊; 陈沈良; 刘锋; 陆勤; 陈一强

华东师范大学河口海岸学国家重点实验室，上海200062

收稿日期:2010-01-08 修回日期:2009-02-25 出版日期:2010-05-25 发布日期:2010-05-25
通讯作者: 陈沈良, 男, 博导, 教授, 主要从事河口海岸动力地貌和沉积动力学研究。E-mail: slchen@sklec.ecnu.edu.cn
作者简介:彭俊(1981-), 男, 博士研究生, 讲师, 主要从事海洋地质和沉积动力学研究。E-mail: ipengjun2010@sina.com
基金资助:
海洋公益性行业科研专项经费项目(200805063); 河口海岸学国家重点实验室科研业务课题(2008KYYW06)

Erosion and Siltation Processes in the Lower Yellow River during Different River Courses into the Sea

PENG Jun; CHEN Shen-liang; LIU Feng; LU Qin; CHEN Yi-qiang

State Key Laboratory of Estuarine and Coastal Research; East China Normal University; Shanghai 200062; China

Received:2010-01-08 Revised:2009-02-25 Online:2010-05-25 Published:2010-05-25
Supported by:
Special Expenses Program of Scientific Research in Marine Commonweal Industry, No.200805063; Scientific Research Program of State Key Laboratory of Estuarine and Coastal Research, No.2008KYYW06

摘要/Abstract

摘要：

运用统计学方法对1950-2007年的水沙数据以及不同流路各水文站同流量(3000m³/s)水位变化进行了分析,结果表明:黄河下游河道表现出淤积—冲刷交替出现的变化过程,当进入下游的含沙量为18.6kg/m³时,河道冲淤表现为动态平衡。艾山以下河道的冲淤变化过程除受水沙条件控制外,还受到流路变迁的影响。流路变迁初期河道发生溯源冲刷作用,中后期河道发生溯源淤积作用。各站同流量水位变化,神仙沟流路主要为下降,河道以冲刷为主;刁口河流路主要为升高,河道以淤积为主;清水沟流路有升有降,河道冲淤互有,总体表现为淤积。流路变迁对河道横断面形态的影响主要在利津以下。

关键词: 黄河, 水沙, 流路, 水位, 淤积, 冲刷

Abstract:

There are distinctive responses of the lower Yellow River to water-sediment variation, and river course transfer into the lower reaches have been changed notably since 1950 due to the water-sediment conditions, which is the result of human activities and climate changes, and the river course into the sea has been transferred several times. The paper analyzed the water-sediment data (1950-2007) and the water level variation under the same flow (3000 m³/s) at hydrological stations in different courses into the sea. Results show that the lower Yellow River has displayed an alternation between siltation and scouring. It would keep a dynamic balance when the suspended sediment concentration into the lower reaches is about 18.6 kg/m³. Besides controlled by water-sediment with siltation or scouring, the variation process of reaches downwards Aishan has been affected by river course transfer. The reaches have experienced upriver scouring in early days of river course transfer and it has exhibited upriver siltation as the extension of river mouth in mid-and late periods of transfer. During the survival time of Shenxiangou course, the water level variation under the same flow at hydrological stations has descended mainly with the characteristic of erosion in the reaches.

Key words: Yellow River, water-sediment, river course, water level, siltation, erosion

中图分类号:

P333.4

彭俊; 陈沈良; 刘锋; 陆勤; 陈一强. 不同流路时期黄河下游河道的冲淤变化过程[J]. 地理学报, 2010, 65(5): 613-622.

PENG Jun; CHEN Shenliang; LIU Feng; LU Qin; CHEN Yiqiang. Erosion and Siltation Processes in the Lower Yellow River during Different River Courses into the Sea[J]. Acta Geographica Sinica, 2010, 65(5): 613-622.

参考文献

[1] Ye Qingchao, Lu Zhongchen, Yang Yifen et al. Fluvial Landforms of the Lower Yellow River. Beijing: Science Press, 1990. [叶青超, 陆中臣, 杨毅芬等. 黄河下游河流地貌. 北京: 科学出版社, 1990.]
[2] Shi Changxing. Causes for continuous siltation of the lower Yellow River. Geomorphology, 2005, 68: 213-223.
[3] Xu Jiongxin. Sediment fluxes to the sea as influenced by sediment delivery of the lower Yellow River. Oceanologia et Limnologia Sinica, 2003, 34(6): 663-670. [许炯心. 黄河下游泥沙输移特征对入海泥沙通量的影响. 海洋与湖沼, 2003, 34(6): 663-670.]
[4] Xu Jiongxin. Temporal variation in sediment transferring function of the lower Yellow River and the formative causes. Geographical Research, 2006, 25(2): 276-284. [许炯心. 黄河下游河道输沙功能的时间变化及其原因. 地理研究, 2006, 25(2): 276-284.]
[5] Xu Baosheng. Analysis on sediment transport in the lower Yellow River. Journal of Sediment Research, 2007, (1): 30-35. [吴保生. 黄河下游输沙量的沿程变化规律和计算方法. 泥沙研究, 2007, (1): 30-35.]
[6] Xu Jiongxin. Deposition in the lower Yellow River. Geographical Research, 1997, 16(1): 23-30. [许炯心. 黄河下游泥沙淤积的经验统计关系. 地理研究, 1997, 16(1): 23-30.]
[7] Xu Jiongxin, Sun Ji. Sedimentation rate change in the lower Yellow River in the past 2300 years. Acta Geographica Sinica, 2003, 58(2): 247-254. [许炯心, 孙季. 黄河下游2300 年以来沉积速率的变化. 地理学报, 2003, 58(2): 247-254.]
[8] Xu Jiongxin. Effect of sediment sink of lower Yellow River on grain size of sediment flux to the sea. Journal of Sediment Research, 2005, (6): 21-28. [许炯心. 黄河下游泥沙沉积汇对入海悬浮质泥沙粒度的影响. 泥沙研究, 2005, (6): 21-28.]
[9] Yang Jishan, Xu Jiongxin, Wang Zhaoyin et al. Influencing factors of the shrinkage of the braided reach of the Yellow River. Geographical Research, 2007, 26(5): 915-921. [杨吉山, 许炯心, 王兆印等. 黄河下游游荡段河床萎缩的影响因素分析. 地理研究, 2007, 26(5): 915-921.]
[10] Hu Chunhong, Chen Jianguo, Sun Xuelan et al. Health assessment of river course in lower Yellow River and measures for regulation. Journal of Hydraulic Engineering, 2008, 39(10): 1189-1196. [胡春宏, 陈建国, 孙雪岚等. 黄河下游河道健康状况评价与治理对策. 水利学报, 2008, 39(10): 1189-1196.]
[11] Xu Jiongxin. Study on sediment transport in the lower Yellow River during flood period. Advances in Water Science, 2002, 13(5): 562-568. [许炯心. 黄河下游洪水的泥沙输移特征. 水科学进展, 2002, 13(5): 562-568.]
[12] Zhang Ouyang, Xu Jiongxin. Channel deformation at the wandering-braided reaches of the lower Yellow River at rising and falling stages during the period of flood events. Advances in Water Science, 2003, 14(4): 401-406. [张欧阳, 许炯心. 黄河下游花园口河段洪水涨落过程中河床横断面形态的调整. 水科学进展, 2003, 14(4): 401-406.]
[13] Shen Guanqing, Zhang Yuanfeng, Qu Shaojun et al. Influence of flood wave type on sediment transport in lower reaches of Yellow River. Journal of Hydraulic Engineering, 2008, 39(1): 7-13. [申冠卿, 张原锋, 曲少军等. 黄河下游不同峰型洪水对泥沙输移的影响. 水利学报, 2008, 39(1): 7-13.]
[14] Zhu Zhaoyu, Ding Zhongli. The Climatic and Tectonic Evolution in the Loess Plateau of China during the Quaternary. Beijing: Geological Press, 1994. [朱照宇, 丁仲礼. 中国黄土高原第四纪古气候与新构造演化. 北京: 地质出版社, 1994.]
[15] Ren M E, Zhu X M. Anthropogenic influences on changes in the sediment load of the Yellow River, China, during the Holocene. The Holocene, 1994, (4): 314-320.
[16] Saito Y, Yang Z S, Hori K. The Huanghe (Yellow River) and Changjiang (Yangtze River) deltas: A review on their characteristics, evolution and sediment discharge during the Holocene. Geomorphology, 2001, (41): 219-231.
[17] Milliman J D, Qin Y S, Ren M et al. Man's influence on the erosion and transport of sediment by Asian rivers: The Yellow River (Huanghe) example. Journal of Geology, 1987, (95): 751-762.
[18] Shi Changxing, Dian Zhang, You Lianyuan. Changes in sediment yield of the Yellow River basin of China during the Holocene. Geomorphology, 2002, 46: 267-283.
[19] Wang Kaichen. Relation between the lower Yellow River and the estuary and its regulation. Journal of Sediment Research, 1982, (2): 1-9. [王恺忱. 黄河河口与下游河道的关系及治理问题. 泥沙研究, 1982, (2): 1-9.]
[20] Jia Shaofeng. On the statistical test of the parallel raising of the profile of the lower Yellow River. Geographical Research, 1994, 13 (2): 1-10. [贾绍凤. 黄河下游河流纵剖面平行抬升的统计检验. 地理研究, 1994, 13(2): 1-10.]
[21] Yin Xueliang. Riverbed Evolution of the Yellow River Mouth. Beijing: China Railway Publishing House, 1997. [尹学良. 黄河口的河床演变. 北京: 中国铁道出版社, 1997.]
[22] Zhou Wenhao, Fan Zhao. Changes of the recent longitudinal profile of the lower Yellow River bed. Journal of Sediment Research, 1983, (4): 14-25. [周文浩, 范昭. 黄河下游河床近代纵剖面的变化. 泥沙研究, 1983, (4): 14-25.]

不同流路时期黄河下游河道的冲淤变化过程

Erosion and Siltation Processes in the Lower Yellow River during Different River Courses into the Sea

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