THE BANK CAVING ALONG HEILONGJIANG AND WUSHULIJIANG RIVERS: GEOLOGIC HAZARD AND COUNTERMEASURES
JIN Shong-pei1, ZOU Shu-fang2, SUN Wei3,4
1. Qiqihar Station, Monitoring Center for Geological Environment of Heilongjiang Province, Qiqihar 161005, China; 2 Shenyang Institute of Geology and Mineral Resources, Shenyang 110033, China; 3. Institute of Water Resources and Environment, China University of Geosciences, Beijing 100083, China; 4. Monitoring Center for Geological Environment of Heilongjiang Province, Harbin 150090, China
Abstract：Affected by geographic, geologic and morphologic factors, the banks of Heilongjiang and Wusulijiang Rivers have been suffering erosions from river water. Serious bank caving occurs along the rivers, and a large area of land was washed away. The reasons for the environmental hazards involve river and rainstorm erosions, freezing and melting, as well as human activities. This paper discusses the current situation, types, origins and developing trends of the bank caving, and then puts forwards countermeasures to prevent the geologic hazard by protecting natural vegetation, construction to conserve the banks and restoring grass and forests.
金松培, 邹淑芳, 孙伟. 黑龙江、乌苏里江塌岸地质灾害及防治措施[J]. 地质与资源, 2006, 15(2): 125-128.
JIN Shong-pei, ZOU Shu-fang, SUN Wei. THE BANK CAVING ALONG HEILONGJIANG AND WUSHULIJIANG RIVERS: GEOLOGIC HAZARD AND COUNTERMEASURES. GEOLOGY AND RESOURCES, 2006, 15(2): 125-128.
2006, Vol. 15 
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