Acta Geographica Sinica ›› 2014, Vol. 69 ›› Issue (3): 399-408.doi: 10.11821/dlxb201403011
Previous Articles Next Articles
WANG Suiji1, LI Ling1,2
Received:
2013-07-15
Revised:
2013-12-20
Online:
2014-03-20
Published:
2014-03-20
Supported by:
WANG Suiji, LI Ling. Lateral shift rate variation of the river banks in the Yinchuan Plain reach of the Yellow River and its causes[J].Acta Geographica Sinica, 2014, 69(3): 399-408.
Add to citation manager EndNote|Reference Manager|ProCite|BibTeX|RefWorks
[1] Zhao Wenlin. The Water Conservancy Technology Series of the Yellow River: Sediment of the Yellow River. Zhengzhou: Yellow River Water Conservancy Press, 1996. [赵文林. 黄河水利科学技术丛书: 黄河泥沙. 郑州: 黄河水利出版社, 1996.] [2] Yang Gensheng, Ta 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. 风沙对黄河内蒙古河段河道泥沙淤积的影响. 中国沙漠, 2003, 23(2): 152-159.] [3] Shen Guanqing, Zhang Yuanfeng, Hou Suzhen et al. Impact of water and sediment regulation by reservoirs in the upper Yellow River on Inner-Mongolia reaches. Journal of Sediment Research, 2007, (1): 67-75. [申冠卿, 张原锋, 侯素珍等. 黄河上游干流水库调节水沙对宁蒙河道的影响. 泥沙研究, 2007, (1): 67-75.] [4] Zhang Xiaohua, Pei Mingsheng, Pan Xiandi et al. Adjustment of alluvial reach in the Yellow River. Journal of Sediment Research, 2002, (3): 1-8. [张晓华, 裴明胜, 潘贤娣等. 黄河冲积性河道的调整. 泥沙研究, 2002, (3): 1-8.] [5] Yao Z Y, Ta W Q, Jia X P et al. Bank erosion and accretion along the Ningxia-Inner Mongolia reaches of the Yellow River from 1958 to 2008. Geomorphology, 2011, 127: 99-106. [6] Sun Dongpo. Analysis on energy distribution-dissipation relation on river system. Journal of Hydraulic Engineering, 1999, (3): 49-53. [孙东坡. 河流系统能量分配耗散关系分析. 水利学报, 1999, (3): 49-53.] [7] Sun Dongpo, Yang Zhenzhen, Zhang Li et al. Analysis of riverbed form adjustment based on energy dissipation in the Inner Mongolia reach of Yellow River. Advances in Water Science, 2011, 22(5): 653-661. [孙东坡, 杨真真, 张立等. 基于能量耗散关系的黄河内蒙段河床形态调整分析. 水科学进展, 2011, 22(5): 653-661.] [8] Yang Leifei. Analysis of the thaw flood discharge in the Ningxia-Neimenggu reach of the Yellow River. Journal of Sediment Research, 1992, (6): 62-68. [杨赉斐. 黄河宁蒙河段凌汛洪水流量分析研究. 泥沙研究, 1992, (6): 62-68.] [9] Wang Suiji. Analysis of river pattern transformations in the Yellow River Basin. Progress in Geography, 2008, 27(2): 10-17. [王随继. 黄河流域河型转化现象初探. 地理科学进展, 2008, 27(2): 10-17.] [10] Ran L S, Wang S J, Lu X X. Hydraulic geometry change of a large river: A case study of the upper Yellow River. Environmental Earth Sciences, 2012, 66: 1247-1257. [11] Wang S J, Yan Y X, Li Y K. Spatial and temporal variations of suspended sediment deposition in the alluvial reach of the upper Yellow River from 1952 to 2007. Catena, 2012, 92: 30-37. [12] Wang Suiji, Fan Xiaoli. Flood processes and channel responses in typical years of the different channel patterns in Neimenggu reaches of the upper Yellow River. Progress in Geography, 2010, 29(4): 501-506. [王随继, 范小黎. 黄河内蒙古不同河型段对洪水过程的响应特征. 地理科学进展, 2010, 29(4): 501-506.] [13] Fan Xiaoli, Shi Changxing, Zhou Yuanyuan et al. Characteristics of flood regime in Ningxia-Inner Mongolia reaches of the upper Yellow River. Resources Science, 2012, 34(1): 65-73. [范小黎, 师长兴, 周园园等. 黄河宁蒙段洪水过程变化特点. 资源科学, 2012, 34(1): 65-73.] [14] Fan Xiaoli, Wang Suiji, Ran Lishan. Analysis of the channel evolution and influence factors in Ningxia reach of the Yellow River. Journal of Water Resources & Water Engineering, 2010, 21(1): 5-11. [范小黎, 王随继, 冉立山. 黄河宁夏河段河道演变及其影响因素分析. 水资源与水工程学报, 2010, 21(1): 5-11.] [15] Hou Suzhen, Chang Wenhua, Wang Ping et al. The characteristics of the channel shrinkage and reasons in the Neimenggu reach of the Yellow River. Yellow River, 2007, 29(1): 24-26. [侯素珍, 常温花, 王平等. 黄河内蒙古段河道萎缩特征及成因. 人民黄河, 2007, 29(1): 24-26.] [16] Ran Lishan, Wang Suiji, Fan Xiaoli. River channel change at Toudaoguai Section and its response to water and sediment supply of the upper Yellow River. Acta Geographica Sinica, 2009, 64(5): 531-540. [冉立山, 王随继, 范小黎等. 黄河内蒙古头道拐断面形态变化及其对水沙的响应. 地理学报, 2009, 64(5): 531-540.] [17] Petts G E. Changing river channels: The geographical tradition//Gurnell A, Petts G. Changing River Channels. New York: John Wiley & Sons, 1995: 1-23. [18] Wang Suiji. Variations of the channel sedimentation rate in the Yinchuan Plain reach of the Yellow River. Acta Sedimentologica Sinica, 2012, 30(3): 565-571. [王随继. 黄河银川平原段河床沉积速率变化特征. 沉积学报, 2012, 30 (3): 565-571.] [19] Khan N I, Islam A. Quantification of erosion patterns in the Brahmaputra-Jamuna River using geographical information system and remote sensing techniques. Hydrol. Process., 2003, 17: 959-966. [20] Yang Shuwen, Li Mingyong, Liu Tao et al. A method of alluvial fan automatic extraction from TM image. Remote Sensing for Land & Resources, 2011, (2): 65-69. [杨树文, 李名勇, 刘涛等. 一种利用TM 图像自动提取洪积扇的方法. 国土资源遥感, 2011, (2): 65-69.] [21] U.S. Geological Survey. http://earthexplorer.usgs.gov/. 2012. [美国地质勘查局. http://earthexplorer.usgs. gov/. 2012.] [22] Gurnell A M. Channel change on the River Dee meanders, 1946.1992, from the analysis of air photographs. Regul Rivers Res. Manag., 1997, 12: 13-26. [23] Winterbottom S. Medium and short-term channel planform changes of the Rivers Tay and Tummel, Scotland. Geomorphology, 2000, 34: 195-208. [24] Richard G A, Julien P Y, Baird D C. Statistical analysis of lateral migration of the Rio Grande, New Mexico. Geomorphology, 2005, 71: 139-155. [25] Yao Z, Xiao J, Ta W et al. Planform channel dynamics along the Ningxia-Inner Mongolia reaches of the Yellow River from 1958 to 2008: Analysis using Landsat images and topographic maps. Environ. Earth Sci., 2013, 70: 97-106. [26] Hudson P F, Kesel R H. Channel migration and meander-bend curvature in the lower Mississippi River prior to major human modification. Geology, 2000, 28(6): 531-534. |