Abstract
It is important to examine the lateral shift rate variation of river banks in different periods. One of the challenges in this regard is how to obtain the shift rate of river banks, as gauging stations are deficient for the study of river reaches. The present study selected the Yinchuan Plain reach of the Yellow River with a length of 196 km as a case study, and searched each point of intersection of 153 cross-sections (interval between two adjacent cross-sections was 1.3 km) and river banks in 1975, 1990, 2010 and 2011, which were plotted according to remote sensing images in those years. Then the shift rates for the points of intersection during 1975–1990, 1990–2010 and 2010–2011 were calculated, as well as the average shift rates for different sections and different periods. The results show that the left bank of the river reach shifts mostly to the right, with the average shift rates being 36.5 m/a, 27.8 m/a and 61.5 m/a in the three periods, respectively. Contemporarily, the right bank shifts mostly to the right in the first period, while it shifts to the left in the second and third periods, with the average shift rates being 31.7 m/a, 23.1 m/a and 50.8 m/a in the three periods, respectively. The average shift rates for the left and right banks during the period 1975–2011 are 22.3 m/a and 14.8 m/a, respectively. The bank shift rates for sections A, B and C are different. The shift rate ratio of the left bank in the three sections is 1:7.6:4.6 for shift to the left and 1:1.7:3.8 for shift to the right, while that of the right bank is 1:1.8:1.2 for shift to the left and 1:5.6:17.7 for shift to the right during the period 1975–2011. Obviously, the average shift rate is the least in section A, while it is maximum in section B for shift to the left and in section C for shift to the right. The temporal variation of the shift rate is influenced by human activities, while the spatial variation is controlled by the local difference in bank materials.
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References
Baki A B M, Gan T Y, 2012. Riverbank migration and island dynamics of the braided Jamuna River of the Ganges Brahmaputra basin using multi-temporal Landsat images. Quaternary International, 263: 146–161.
Fan X, Shi C, Zhou Y et al., 2012. Characteristics of flood regime in Ningxia-Inner Mongolia Reaches of the upper Yellow River. Resources Science, 34(1): 65–73.
Fan X, Wang S, Ran L, 2010. Analysis of the channel evolution and influence factors in Ningxia Reach of the Yellow River. Journal of Water Resources and Water Engineering, 21(1): 5–11. (in Chinese)
Gurnell A M, 1997. Channel change on the River Dee meanders, 1946–1992, from the analysis of air photographs. Regulated Rivers: Research and Management, 13: 13–26.
Hossain M A, Gan T Y, Baki A B M, 2013. Assessing morphological changes of the Ganges River using satellite images. Quaternary International, 304: 142–155.
Hou S, Chang W, Wang P et al., 2007. Channel shrinking characteristics and cause of formation in the Neimenggu Reach of the Yellow River. Yellow River, 29(1): 24–26. (in Chinese)
Hudson P F, Kesel R H, 2000. Channel migration and meander-bend curvature in the lower Mississippi River prior to major human modification. Geology, 28(6): 531–534.
Kammu M, Lu X X, Rasphone A et al., 2008. Riverbank changes along the Mekong River: Remote sensing detection in the Vientiane-Nong Khai area. Quaternary International, 186: 100–112.
Khan N I, Islam A, 2003. Quantification of erosion patterns in the Brahmaputra-Jamuna River using geographical information system and remote sensing techniques. Hydrological Processes, 17: 959–966.
Nicoll T J, Hickin E J, 2010. Planform geometry and channel migration of confined meandering rivers on the Canadian prairies. Geomorphology, 116: 37–47.
Petts G E, 1995. Changing river channels: The geographical tradition. In: Gurnell A, Petts G (eds.). Changing River Channels. New York: John Wiley & Sons, 1–23.
Ran L, Wang S, Fan X, 2010. Channel change at Toudaoguai Station and its responses to the operation of upstream reservoirs in the upper Yellow River. Journal of Geographical Sciences, 20(2): 231–247.
Ran L, Wang S, Lu X, 2012. Hydraulic geometry change of a large river: A case study of the upper Yellow River. Environmental Earth Sciences, 66: 1247–1257.
Richard G A, Julien P Y, Baird D C, 2005. Statistical analysis of lateral migration of the Rio Grande, New Mexico. Geomorphology, 71: 139–155.
Shen G, Zhang Y, Hou S et al., 2007. Impact of water and sediment regulation by reservoirs in the upper Yellow River on Inner-Mongolia reaches. Journal of Sediment Research, (1): 67–75. (in Chinese)
Sun D, 1999. Analysis on energy distribution-dissipation relation on river system. Journal of Hydraulic Engineering, (3): 49–53. (in Chinese)
Sun D, Yang Z, Zhang L et al., 2011. Analysis of riverbed form adjustment based on energy dissipation in the Inner Mongolia Reach of Yellow River. Advances in Water Science, 22(5): 653–661. (in Chinese)
US Geological Survey, 2012. http://earthexplorer.usgs.gov/.
Wang S, 2008. Analysis of river pattern transformations in the Yellow River basin. Progress in Geography, 27(2): 10–17. (in Chinese)
Wang S, 2012. Variations of the channel sedimentation rate in the Yinchuan Plain reach of the Yellow River. Acta Seidmentologica Sinica, 30(3): 565–571. (in Chinese)
Wang S, Fan X, 2010. Flood processes and channel responses in typical years of the different channel patterns in Neimenggu reaches of the upper Yellow River. Progress in Geography, 29(4): 501–506. (in Chinese)
Wang S, Yan M, Yan Y et al., 2012a. Contributions of climate change and human activities to the changes in runoff increment in different sections of the Yellow River. Quaternary International, 282: 66–77.
Wang S, Yan Y, Li Y, 2012b. Spatial and temporal variations of suspended sediment deposition in the alluvial reach of the upper Yellow River from 1952 to 2007. Catena, 92: 30–37.
Winterbottom S, 2000. Medium and short-term channel planform changes of the Rivers Tay and Tummel, Scotland. Geomorphology, 34: 195–208.
Yang G, Ta W, Dai F et al., 2003. Contribution of sand sources to the silting of riverbed in Inner Mongolia section of Huanghe River. Journal of Desert Research, 23(2): 152–159. (in Chinese)
Yang L, 1992. Analysis on ice flood discharge in Ningmeng reach of the Yellow River. Journal of Sediment Research, 6: 62–68. (in Chinese)
Yang S, Li M, Liu T et al., 2011. A method of alluvial fan automatic extraction from TM image. Remote Sensing for Land & Resources, (2): 65–69. (in Chinese)
Yao Z, Ta W, Jia X et al., 2011. Bank erosion and accretion along the Ningxia-Inner Mongolia reaches of the Yellow River from 1958 to 2008. Geomorphology, 127: 99–106.
Yao Z, Xiao J, Ta W et al., 2013. 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.
Zhang X, Pei M, Pan X et al., 2002. Adjustment of alluvial reach in the Yellow River. Journal of Sediment Research, (3): 1–8. (in Chinese)
Zhao W, 1996. The Sediments in the Yellow River. Zhengzhou: Yellow River Water Conservancy Press. (in Chinese)
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Foundation: National Natural Science Foundation of China, No.41271027; National Basic Research Program of China, No. 2011CB403305
Author: Wang Suiji, PhD and Associate Professor, specialized in fluvial geomorphology, sedimentology and land surface processes.
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Wang, S., Li, L. & Cheng, W. Variations of bank shift rates along the Yinchuan Plain reach of the Yellow River and their influencing factors. J. Geogr. Sci. 24, 703–716 (2014). https://doi.org/10.1007/s11442-014-1114-2
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DOI: https://doi.org/10.1007/s11442-014-1114-2