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摘要:
Due to the complex geological processes of Qinghai-Tibet Plateau, numerous deposits, espe-cially the large-scale ancient landslide deposits, are characteristic features of the valleys incised in south-western China. Intense water level fluctuations since 2011 in Maoergai Reservoir, China, registered the reactivation of Xierguazi ancient landslide, and presented a significant risk to neighboring facilities. Based on detailed field survey and drilling exploration, the landslide was divided into Zone A and Zone B, and other characterizations of landslide were studied as well. To precisely measure the extent of landslide dis-placement during filling and drawdown stage, surface displacement monitoring system was deployed on the landslide. The monitoring analyses data reveal that reservoir fluctuation is the dominant factor influ-encing landslide displacement, especially during drawdown stage. Moreover, a future sliding is anticipated in Zone A, while a creep had already existed in Zone B. A reservoir regulation was then established using the lead-lag correlation between reservoir fluctuation and landslide displacement and landslide stability analysis. In the end, the follow-up deformation monitoring demonstrates that the reservoir regulation controlled the landslide effectively. Landslide control by reservoir regulation in Maoergai can serve as a case study for other settlements involved in similar construction activities.
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篇名 Reservoir Regulation for Control of an Ancient Landslide Reactivated by Water Level Fluctuations in Heishui River, China
来源期刊 地球科学学刊(英文版) 学科
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年,卷(期) 2020,(6) 所属期刊栏目
研究方向 页码范围 1058-1067
页数 10页 分类号
字数 语种 英文
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地球科学学刊(英文版)
双月刊
1674-487X
42-1788/P
大16开
武汉市洪山区鲁磨路388号
38-354
1990
eng
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