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机构地区:[1]成都理工大学地质灾害防治与地质环境保护国家重点实验室,成都610059
出 处:《地质灾害与环境保护》2008年第4期25-28,共4页Journal of Geological Hazards and Environment Preservation
基 金:西部交通建设科技项目基金资助(项目编号:200431800003)
摘 要:溜砂坡是我国西部山区公路的主要地质灾害之一。由于对溜砂坡的形成发展机理认识不足,目前采用的治理措施不能很好地解决溜砂灾害,有些工程措施反而会加大灾害程度。通过对天山公路沿线溜砂坡的调查研究,以K612+750~K613+850段特大溜砂坡群为例,阐述该溜砂坡的最基本特性,分析溜砂坡的成灾机理和危害性特点,并对溜砂坡防治措施进行研究。Sand-sliding slope posed a main geological disaster during the highway construction in mountain areas of the west China. Due to ambiguity of formative mechanism of sand-sliding slope, countermeasure employed at p resent could not control the disaster, and some measures even aggravated destruction of slope. By means of investigation and Study of typical sand-- sliding slope along Tianshan Highway, taking the K612+750-K613-k850 section of especially big sand--sliding slope group as the example, the authors explained the constitutive features of sand--sliding slope, and analyzed its disaster formative mech- anism. Finally, some proper control countermeasures were researched against disaster of sand--sliding slope.
分 类 号:P642.22[天文地球—工程地质学]
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