Scour and Silting Evolution and Its Influencing Factors in Inner Mongolia Reach

Expand
  • 1. Key Laboratory of North-West Water Resources and Ecology Environment of Education Ministry, Xi'an University of Technology, Xi'an 710048, China;
    2. Water Conservancy Plan and Design Institute of Harbin, Harbin 150076, China

Received date: 2010-09-18

  Revised date: 2010-12-16

  Online published: 2011-03-20

Supported by

National Basic Research Program of China, No.2011CB403305

Abstract

Rivers with fluvial equilibrium are characterized by bed deformation adjustment. The erosion-deposition area in cross-section can reflect this characteristic. The time series of erosion-deposition area in BYGL and SHHK stations was obtained by quantifying change of section area during the period 1976-2006. After trend and mutation analysis, three different trends were identified in general: the quasi-equilibrium phase, rapid shrinkage phase and the new quasi-equilibrium phase. It was also found that once a big flood occurred in the ten tributaries, the trend of erosion-deposition area would change. The phenomenon was more obvious due to the decrease of deluge after the completion of upstream reservoir. After the time series had clear mutations in the late 1990s, the Inner Mongolia reach entered a new equilibrium phase. The conditions of incoming water and sediment were adapted to the bed boundary conditions. Therefore, how to control sedimentation in Inner Mongolia reach was worth discussing.

Cite this article

QIN Yi, ZHANG Xiaofang, WANG Fenglong, YAN Heng, HAN Haijun . Scour and Silting Evolution and Its Influencing Factors in Inner Mongolia Reach[J]. Acta Geographica Sinica, 2011 , 66(3) : 324 -330 . DOI: 10.11821/xb201103004

References

[1] Yao Huiming, Qin Fuxing, Shen Guochang et al. Ice regime characteristics in the Ningxia-Inner Mongolia reach of Yellow River. Advances in Water Science, 2007, 18(6): 893-899. [姚惠明, 秦福兴, 沈国昌等. 黄河宁蒙河段凌情特性研究. 水进展, 2007, 18(6): 893-899.]

[2] Zhao Wenlin, Cheng Xiuwen, Hou Suzhen et al. Analysis of scouring and sedimentation in the channel from Ningxia to Inner Mongolia in the upper Yellow River. Yellow River, 1999, 21(6): 11-14. [赵文林, 程秀文, 侯素珍等. 黄河上游宁道冲淤变化分析. 人民黄河, 1999, 21(6): 11-14.]

[3] Yang Gensheng, Tuo Wanquan, Dai Fengnian et al. Contribution of sand sources to the silting of riverbed in Inner Mongolia section of Huanghe River. Journal of Desert Research, 2003, 23(2): 152-159. [杨根生, 拓万全, 戴丰年等. 风沙对黄河古河段河道泥沙淤积的影响. 中国沙漠, 2003, 23(2): 152-159.]

[4] Liu Xiaoyan, Hou Suzhen, Chang Wenhua. Cause of main channel shrinkage occurred to the Inner-Mongolia reaches of Yellow River. Journal of Hydraulic Engineering, 2009, 40(9): 1048-1054. [刘晓燕, 侯素珍, 常温花. 黄河内蒙古河段主缩原因和对策. 水利学报, 2009, 40(9): 1048-1054.]

[5] Qian Ning, Zhang Ren, Zhou Zhide. Fluvial Process. Beijing: Science Press, 1987: 313-336. [钱宁, 张仁, 周志德. 河床演变学. 北京: 科学出版社, 1987: 313-336.]

[6] Wang Haibing, Jia Xiaopeng. Channel deposition and erosion processes of Inner Mongolian reach of Yellow River following upstream reservoirs operation. Journal of Desert Research, 2009, 29(1): 189-192. [王海兵, 贾晓鹏. 大型水库下内蒙古河道泥沙侵蚀淤积过程. 中国沙漠, 2009, 29(1): 189-192.]

[7] Wang Yancheng, Feng Xuewu, Wang Lunping et al. Influence of reservoirs in main stream of the upper Yellow River on the reach within Inner Mongolian Autonomous Region. Yellow River, 1996, (1): 5-11. [王彦成, 冯学武, 王伦平等. 黄河上流水库对内蒙古河段的影响. 人民黄河, 1996, (1): 5-11.]

[8] Feng Guohua, Chaolun Bagen, Gao Ruizhong et al. Hydrology, 2009, 29(1): 47-49. [冯国华, 朝伦巴根, 高瑞忠等. 黄河古段防凌对策研究. 水文, 2009, 29(1): 47-49.]

[9] Pedro Bernaola-Galván, Plamen Ch. Ivanov, Luís A. Nunes Amaral. Scale invariance in the nonstationarity of human heart rate. Physical Review Letters, 2001, 87(16): 168105.

[10] Wang Lina, Chen Xiaohong, Li Yue'an et al. Heuristic segmentation method for change-point analysis of hydrological time series. Yangtze River, 2009, 40(9): 68-69. [汪丽娜, 陈晓宏, 李粤安等. 水文时间序列突变点分析的启发式分割. 人民长江, 2009, 40(9): 68-69.]

[11] Wang Fenglong, Qin Yi, Zhang Xiaofang et al. Study on the deposition of Yellow River reach in Inner Mongolia. Journal ofWater Resources andWater Engineering, 2010, 21(1): 148-150. [王凤龙, 秦毅, 张晓芳等. 内蒙古河道淤积再探讨. 源与水工程学报, 2010, 21(1): 148-150.]

[12] Hong Roujia, Karim M F, John F Kennedy. Low-temperature effects on flow in sand-bed streams//Proceedings of the Second International Symposium on River Sedimentation. Beijing. China Water Resources and Electric Power Press, 1983: 128-136. [洪柔嘉, Karim M F, John F Kennedy. 低温对沙质河床水流的影响//第二次河流泥沙国际学术讨论会论文集. 北京: 水利电力出版社, 1983: 128-136.]

[13] Yellow River Conservancy Commission. Compilation of ice status data and its characteristics analysis. Zhengzhou, 2006. [水利部黄河水利委员会. 黄河凌情资料整编及特点分析. 郑州, 2006.]
Outlines

/