川藏铁路拉萨—加查段泥石流发育特征及防治对策
详细信息 查看官网全文
- 英文论文题名：Development Characteristics and Control Measures of Debris Flows in Lhasa-Jiacha Section of Sichuan-Tibet Railway
- 论文作者：游勇 ; 蒋良文 ; 张广泽 ; 张敏 ; 陈兴长 ; 柳金峰
- 英文论文作者：You Yong ; Jiang Liangwen ; Zhang Guangze ; Zhang Min ; Chen Xingzhang ; Liu Jinfeng ; Key Laboratory of Mountain Hazards and Earth Surface Process ; Chinese Academy of Sciences ; Institute of Mountain Hazards and Environment ; Chinese Academy of Sciences ; Chengdu Geotechnical Engineering Co.Ltd of China Railway Eryuan Engineering Group Co.Ltd ; School of Environment and Resource ; Southwest University of Science and Technology
- 年：2016
- 作者机构：中国科学院山地灾害与地表过程重点实验室;中国科学院水利部成都山地灾害与环境研究所;中铁二院成都地勘岩土工程有限责任公司;西南科技大学环境与资源学院;
- 论文关键词：泥石流 ; 发育特征 ; 防治对策 ; 川藏铁路 ; 雅鲁藏布江
- 英文论文关键词：debris flow ; development characteristics ; control measures ; the Sichuan-Tibet railway ; Yarlung Zangbo River
- 会议召开时间：2016-10-14
- 会议录名称：“川藏铁路建设的挑战与对策”2016学术交流会论文集
- 语种：中文
- 分类号：P642.23;U212.22
- 学会代码：ZGTD
- 会议名称：“川藏铁路建设的挑战与对策”2016学术交流会
- 会议地点：中国四川成都
- 主办单位：中国铁道学会、中国铁道学会工程分会、中国中铁股份有限公司、中铁二院工程集团有限责任公司
- 学会名称：中国铁道学会
- 页数：7
- 文件大小：1687k
- 原文格式：O
- 会议级别：全国
摘要
川藏铁路拉萨—加查段泥石流普遍发育,对铁路选线和运营影响很大。本文通过遥感解译、现场调查和实地勘测,对研究区泥石流发育的环境背景条件、泥石流类型及其发育特征进行了系统研究。研究区共发育泥石流沟225条,坡面型泥石流122条,沟谷型泥石流沟103条;对拟建铁路有直接影响的泥石流沟83条。研究区独特的地理位置和气候条件,形成了如下的泥石流发育特征:①分布密度大,具有广泛性;②流域面积较小,汇流条件好;③堆积扇规模宏大,以混杂堆积为主;④流体性质单一,均为稀性泥石流;⑤沟谷型和坡面型泥石流均普遍发育。泥石流的防治,建议采取以防为主、防治结合的原则;积极开展泥石流灾害的预报,预防人为泥石流灾害,针对性地开展泥石流治理工作。
Debris flows are widespread in Lhasa-Jiacha section of the Sichuan-Tibet Railway,as has a great influence on selection and operation of the proposed railway.The research on environmental conditions,types and development characteristics of debris flows in the study area was conducted by the remote sensing interpretation and field investigation.Results show that there are 225 debris flows,122 of which are slope debris flows and the others are gully debris flows.There are 83 debris flows have a direct impact on the proposed railway.Due to the unique geographical location and climatic conditions of the study area,the debris flows have the following development characteristics:①widespread and distribution density;②small catchment areas and good confluence conditions;③large-scale accumulation fan mainly with mixed accumulation;④all being turbulent debris flows;⑤valley and slope debris flows being common development.It is suggested that the control counteirneasure should obey the principle of "prevention and treatment integrated,mainly in prevention".So the following works should be strengthened:forecasting debris flow disaster,preventing man-made debris flow,and controlling debris flow.
Debris flows are widespread in Lhasa-Jiacha section of the Sichuan-Tibet Railway,as has a great influence on selection and operation of the proposed railway.The research on environmental conditions,types and development characteristics of debris flows in the study area was conducted by the remote sensing interpretation and field investigation.Results show that there are 225 debris flows,122 of which are slope debris flows and the others are gully debris flows.There are 83 debris flows have a direct impact on the proposed railway.Due to the unique geographical location and climatic conditions of the study area,the debris flows have the following development characteristics:①widespread and distribution density;②small catchment areas and good confluence conditions;③large-scale accumulation fan mainly with mixed accumulation;④all being turbulent debris flows;⑤valley and slope debris flows being common development.It is suggested that the control counteirneasure should obey the principle of "prevention and treatment integrated,mainly in prevention".So the following works should be strengthened:forecasting debris flow disaster,preventing man-made debris flow,and controlling debris flow.
引文
[1]刘志飞,王成善,李祥辉.西藏南部雅鲁藏布江缝合带的沉积—构造演化[J].同济大学学报,2000,28(5):537-541.Liu Zhifei,WANG Chengshan,LI Xianghui.Sedimentary-tectonic Evolution of the Yarlung Zangbo Suture Zone,Southern Tibet[J].Journal of Tongji University,2000,28(5):537-541.
[2]苏学军,段国玺,彭兴阶。等.西藏乃东—米林地区雅鲁藏布江结合带的地质特征及构造演化[J].地质通报,2006,25(6):700-707.Su Xuejun,Duan Guoxi,PENG Xingjie,et al.Geological characteristics and tectonic evolution of the Yarlung Zangbo junction belt in the Nedong-Mainling area,Tibet,China[J].Geological Bulletin of China,2006,25(6):700-707.
[3]彭小龙,王道永.雅鲁藏布江断裂带活动构造特征与活动性分析[J].长江大学学报:自科科学版,2013,10(26):41-44.Peng Xiaolong,Wang Daoyong.Analysis on the structure characteristics and activities of the yarlung zangbo river fault zone[J].Journal of Yangtze University(Nat SCi Edit),2013,10(26):41-44.
[4]李森,王跃,哈斯,等.雅鲁藏布江河谷风沙地貌分类与发育问题[J].中国沙漠,1997,17(4):342-350.Li Sen,Wang Yue,Ha Si,et al.Classification and development of aeolian sand landform in the Yurling Zangbo valley[J].Journal of Desert Research,1997,17(4):342-350.
[5]赵银兵,何政伟。倪忠云,等.雅鲁藏布江曲水-乃东段沙化空间特征研究[J].干旱区资源与环境,2012,26(8):135-140.Zhao Yinbing,He Zhengwei,Ni Zhongyun,et al.Spatial feature of desertification in Qushui-Naidong area of Yarlung Zangbo River[J].Journal of Arid Land Resources and Environment,2012,26(8):135-140.
[6]邹陈.新建拉林铁路主要工程地质问题探讨[J].铁道工程学报,2016,(4):26-30.Zou Chen.Exploration on the Engineering Geological Problems of the New Lhasa-Linzhi railway[J].Journal of Railway Engineering Society,,2016,(4):26-30.
[7]崔鹏,陈晓清,程尊兰,等.西藏泥石流滑坡监测与防治[J].自然杂志,2010,32(1):19-25.Cui Peng,Chen Xiaoqing,CHENG Zunlan,et al.Monitoring and prevention of debris-flows and landslides in Tibet[J].Chinese Journal of Nature,,2010,32(1):19-25.
[8]袁磊,沈渭寿,李海东,等.雅鲁藏布江中游河谷区域风沙化土地演变趋势及驱动因素[J].生态与农村环境学报,2010,26(4):301-305.Yuan Lei,Shen Weishou,LI Haidong,et al.Evolution and causes of aeolian desertification of the middle reaches of Yarlung Zangbo River,China[J].Journal of Ecology and Rural Environment,2010,26(4):301-305.
[9]刘连友,刘志民,张甲珅,等.雅鲁藏布江江当宽谷地区沙源物质与现代沙漠化过程[J].中国沙漠,1997,17(4):377-382.Liu Lianyou,Liu Zhimin,Zhang Jiashen,et al.Sand source of sand dune and modern desertification process in Jiandang wide valley area of Yarlung Zangbo river[J].Journal of Desert Research,1997,17(4):377-382.
[2]苏学军,段国玺,彭兴阶。等.西藏乃东—米林地区雅鲁藏布江结合带的地质特征及构造演化[J].地质通报,2006,25(6):700-707.Su Xuejun,Duan Guoxi,PENG Xingjie,et al.Geological characteristics and tectonic evolution of the Yarlung Zangbo junction belt in the Nedong-Mainling area,Tibet,China[J].Geological Bulletin of China,2006,25(6):700-707.
[3]彭小龙,王道永.雅鲁藏布江断裂带活动构造特征与活动性分析[J].长江大学学报:自科科学版,2013,10(26):41-44.Peng Xiaolong,Wang Daoyong.Analysis on the structure characteristics and activities of the yarlung zangbo river fault zone[J].Journal of Yangtze University(Nat SCi Edit),2013,10(26):41-44.
[4]李森,王跃,哈斯,等.雅鲁藏布江河谷风沙地貌分类与发育问题[J].中国沙漠,1997,17(4):342-350.Li Sen,Wang Yue,Ha Si,et al.Classification and development of aeolian sand landform in the Yurling Zangbo valley[J].Journal of Desert Research,1997,17(4):342-350.
[5]赵银兵,何政伟。倪忠云,等.雅鲁藏布江曲水-乃东段沙化空间特征研究[J].干旱区资源与环境,2012,26(8):135-140.Zhao Yinbing,He Zhengwei,Ni Zhongyun,et al.Spatial feature of desertification in Qushui-Naidong area of Yarlung Zangbo River[J].Journal of Arid Land Resources and Environment,2012,26(8):135-140.
[6]邹陈.新建拉林铁路主要工程地质问题探讨[J].铁道工程学报,2016,(4):26-30.Zou Chen.Exploration on the Engineering Geological Problems of the New Lhasa-Linzhi railway[J].Journal of Railway Engineering Society,,2016,(4):26-30.
[7]崔鹏,陈晓清,程尊兰,等.西藏泥石流滑坡监测与防治[J].自然杂志,2010,32(1):19-25.Cui Peng,Chen Xiaoqing,CHENG Zunlan,et al.Monitoring and prevention of debris-flows and landslides in Tibet[J].Chinese Journal of Nature,,2010,32(1):19-25.
[8]袁磊,沈渭寿,李海东,等.雅鲁藏布江中游河谷区域风沙化土地演变趋势及驱动因素[J].生态与农村环境学报,2010,26(4):301-305.Yuan Lei,Shen Weishou,LI Haidong,et al.Evolution and causes of aeolian desertification of the middle reaches of Yarlung Zangbo River,China[J].Journal of Ecology and Rural Environment,2010,26(4):301-305.
[9]刘连友,刘志民,张甲珅,等.雅鲁藏布江江当宽谷地区沙源物质与现代沙漠化过程[J].中国沙漠,1997,17(4):377-382.Liu Lianyou,Liu Zhimin,Zhang Jiashen,et al.Sand source of sand dune and modern desertification process in Jiandang wide valley area of Yarlung Zangbo river[J].Journal of Desert Research,1997,17(4):377-382.