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新藏公路新疆段泥石流灾害初探
引用本文:马东涛,崔鹏,杨坤,王掌军.新藏公路新疆段泥石流灾害初探[J].干旱区地理,2003,26(4):349-354.
作者姓名:马东涛  崔鹏  杨坤  王掌军
作者单位:1. 中国科学院、水利部成都山地灾害与环境研究所,成都,610041;中国科学院寒区旱区环境与工程研究所,兰州,730000
2. 中国科学院、水利部成都山地灾害与环境研究所,成都,610041
3. 交通部第一公路勘察设计研究院,西安,710068
基金项目:国家自然科学基金项目西部重大研究计划 (90 2 0 2 0 0 7),中国科学院知识创新项目“进藏公路铁路典型路段工程减灾理论与对策研究”(KZCX2 -3 0 6)资助
摘    要:新藏公路新疆段沿线共有泥石流灾害149处,直接危害线路53.05km。泥石流可分为暴雨型、冰雪融水型及雨水和冰雪融水混合型三个成因类型.其灾害集中分布于哈拉斯坦河、采拉克河、叶尔羌河及喀拉喀什河沿溪线路段。沿线泥石流具有松散堆积物丰富,水源不足,暴发频率低,规模火,受冰川和气候变化影响大等特点。在对泥石流成灾方式、活动现状和发展趋势分析研究的基础上.提出了灾害治理的基本原则和拟采取的主要工程措施及进一步工作的建议。

关 键 词:泥石流  新藏公路  形成条件  成灾方式  整治措施
文章编号:1000-6060(2003)04-0349-06
修稿时间:2003年5月8日

An Approach on Debris Flow Hazards Along the Xinjiang-Tibetan Highway Line in Xinjiang
MA Dong tao , CUI Peng YANG Kun WANG Zhang jun.An Approach on Debris Flow Hazards Along the Xinjiang-Tibetan Highway Line in Xinjiang[J].Arid Land Geography,2003,26(4):349-354.
Authors:MA Dong tao  CUI Peng YANG Kun WANG Zhang jun
Institution:MA Dong tao 1,2 CUI Peng 1 YANG Kun 1 WANG Zhang jun 3
Abstract:The Xinjiang Tibetan Highway line stretches over Tarim Basin and Kunlun Mountains with length of 654.5km in Xinjiang, which is one of the most important key national traffic lines to the western boundary of China. Along the highway line, geological tectonics are complex, Neo tectonic movement and seismic activity is quite extensive, glaciers and accumulated snow distribute broadly and rainstorm break out frequently, thus induce a great number of debris flows in Hanasitan River, Sailake River, Yarkant River and KaraKashi River valley. It is investigated that there are 149 debris flows along the highway line, among which 129 belong gully type and 20 belong to slope type; 53.05km long highway line is threatened by debris flow hazards. Debris flows are triggered by rainstorm, melt water of glaciers and accumulated snow or both of them. Debris flow fluid is major in sub viscous and rock water flow type due to shortage of fine granular in solid materials, which break out once in several or dozen years,with large scale and easily influenced by climate fluctuation and glacier changes. Debris flows often deposit and bury road surface, block bridges and culverts, erode and destroy roadbed and basement of bridges and culverts, and block transportation. With the global climate change and intensive seismic activities, debris flow will become more extensive and generate serious damages to the highway in near future. According to the active features and damage forms of debris flow on highway engineering, a series of disaster controlling principles and suggestions in the next step are put forward. The main mitigation measures in future highway construction are suggested , which are concrete road surface, bridge and culvert over crossing works, gully bed anti eroded works, blocked dams, drainage engineering and debris silting field et al.
Keywords:the Xinjiang  Tibetan Highway  debris flow hazards  formation condition  damage forms  controlling countermeasures
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