Earth Science Frontiers ›› 2021, Vol. 28 ›› Issue (2): 58-70.DOI: 10.13745/j.esf.sf.2020.9.1

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Influence of natural dams on the river profile of the Yalong River Basin

LIU Weiming1(), ZHOU Liqin1,2, CHEN Xiaoqing1,*(), ZHOU Zhen3, Wolfgang SCHWANGHART4, HU Xudong5, LI Xuemei1, ZHANG Xiaogang1   

  1. 1. CAS Key Laboratory of Mountain Hazards and Earth Surface Processes, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China
    2. University of Chinese Academy of Sciences, Beijing 100149, China
    3. China Railway Eryuan Engineering Group Co., Ltd., Chengdu 610031, China
    4. Institute of Earth and Environmental Science, University of Potsdam, Potsdam 14476-14482, Germany
    5. Hubei Key Laboratory of Disaster Prevention and Mitigation, College of Civil Engineering and Architecture, China Three Gorges University, Yichang 443002, China
  • Received:2020-06-30 Revised:2020-09-10 Online:2021-03-25 Published:2021-04-03
  • Contact: CHEN Xiaoqing

Abstract:

Natural dams are known to impose pronounced and long-lasting perturbations on the river profiles in mountaineous areas. In some cases, the steepened profiles caused by natural dams are easily confused with the migrating knickpoints associated with relative base-level fall linked to tectonism. However, the degree to which natural dams may compromise geomorphometry-based tectonics has not been systematically investigated. In this research, we studied the Yalong River Basin on the eastern edge of the Tibetan Plateau. Our investigation of the relation between river dams and the river longitudinal profile relies on the interpretation and analysis of remote sensing imagery and digital elevation models (DEM). Through such analysis and field work, we identified 34 natural dams in the Yalong River Basin. We extracted the river longitudinal profile from 30 m SRTM DEM and calculated the locations of convex knickpoints, the channel steepness index, and other geomorphic parameters using TopoToolbox. Our analysis reveals 18 natural dams with locations coinciding with knickpoints that are over 30 m high. Among them, eight have a significant influence on the river longitudinal profile as they can form knickpoints with heights exceeding 100 m. Moreover, we show that landslide dams have bigger influence on the river profile than mudslide dams. Further analysis of the Yalong River and its tributary Liqiu River shows that the river steepness index attains higher values at the dams. Excluding the influence of variable lithology and fault activity on the river profile, there are several knickpoints along the river that can still be attributed to dams. Therefore, we conclude that to accurately and reliably extract and analyze information on regional tectonics from DEMs, the potential occurrence of river knickpoints due to dams must be taken into consideration.

Key words: river longitudinal profile, dam, river knickpoint, remote sensing interpretation, Yalong River Basin

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