Influence of the Three-Gorges Reservoir on Geomorphic Process on Bank Slope of the Yangtze River
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Influence of the Three-Gorges Reservoir on Geomorphic Process on Bank Slope of the Yangtze River
Bulletin of Soiland Water ConservationVol. 25, Issue 5, Pages: 23-25(2006)
作者机构:
1. 南京大学 城市与资源学系,江苏,南京,210093
2. 南京师范大学 地理科学学院,江苏,南京,210097
3. 南京水利科学研究院,江苏,南京,210024
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Published:2006
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XU Yong-hui, YANG Da-yuan, CHEN Ke-feng, et al. Influence of the Three-Gorges Reservoir on Geomorphic Process on Bank Slope of the Yangtze River[J]. Bulletin of Soiland Water Conservation, 2006, 25(5): 23-25.
DOI:
XU Yong-hui, YANG Da-yuan, CHEN Ke-feng, et al. Influence of the Three-Gorges Reservoir on Geomorphic Process on Bank Slope of the Yangtze River[J]. Bulletin of Soiland Water Conservation, 2006, 25(5): 23-25.DOI:
Influence of the Three-Gorges Reservoir on Geomorphic Process on Bank Slope of the Yangtze River
After the completion of the Three Gorges reservoir
a series of changes in fluvial geomorphology processes will inevitably occur on bank slope of the reservoir.Two parallel permanent fluctuating belts will form on bank slope
and thus the power of reservoir water will fluctuate with changed water level.Changes in groundwater and reservoir water may affect bank slope surface and rock medium.The changes have physical
chemical and mechanics effects on rock materials
and influence loose deposits and rocky bank slope
differently.The major geomorphic processes may shift from gravitational geomorphic processes to creep
slide
collapse
erosion and washing processes
which transforms bank slope in turn.The geomorphic transformation and retransformation processes on bank slope will last for a long time.