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Risk assessment of highways affected by debris flows in Wenchuan earthquake area
  • ISSN号:1672-6316
  • 期刊名称:Journal of Mountain Science
  • 时间:2013.4
  • 页码:173-189
  • 分类:P642.23[天文地球—工程地质学;天文地球—地质矿产勘探;天文地球—地质学] P333.2[天文地球—水文科学;水利工程—水文学及水资源;天文地球—地球物理学]
  • 作者机构:[1]Key Laboratory of Mountain Hazards and Earth Surface Processes / Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China, [2]School of Environment and Resources, Southwest University of Sciences and Technology, Mianyang 621010, China
  • 相关基金:supported by the Key Program of National Natural Science Found of China(Grant No.41030742); the Grand Program of National Natural Science Found of China(Grant No.41190084)
  • 相关项目:川藏交通干线环境灾害演化规律与工程风险
中文摘要:

碎片流动和山崩,广泛地沿着 Parlung Zangbo 发展并且经常发生,严重在 Bomi 从四川损坏高速公路到 Tiebt (G318 ) 县。灾难性的碎片在2007年9月4日 Tianmo 分水岭流动,2010年7月25日和2010年9月4日,堵住的 Parlung Zangbo 河和生产的建水坝的湖,其爆发流动由于在平台的脚上的强烈搜索在相反的河岸使 50 m 成为了高平台倒塌。作为结果,因为那 900 m 高速公路底是 destructed, 430 m 破产了,交通在 2010 被打断 16 天。这些碎片流动被冰川的融化开始它被连续更高的温度和下列集中的降雨导致,并且沿着隧道由冰碛膨胀了然后堵住了 Parlung Zangbo。在分水岭,密度,速度和碎片流动的山峰分泌物的插头是 2.06 t/m < 啜 class= “ a-plus-plus ” > 3 , 12.7 m/s 和 3334 m < 啜 class= “ a-plus-plus ” > 3 /s, 分别地。在进河的插头和免职体积的分泌物什么时候超过 2125 m <啜class=“ a-plus-plus ”> 3 /s 和 126 潩?景ㄠ?代???杩?潣牲汥瑡潩獮爠湡楧杮映潲???″潴???椠摮捩瑡?桴瑡???瑮牥浩挠畯摬挠灡畴敲琠敨愠湮慵?祣汣?敶祲眠汥??睯癥牥?湡愠敶慲敧爠潯?敭湡猭畱牡?牥潲?爨獭?漠??鰷????鈿???辮?鶝岑???额???鸿銾铌?

英文摘要:

Debris flows and landslides, extensively developing and frequently occurring along Parlung Zangbo, seriously damage the Highway from Sichuan to Tiebt(G318) at Bomi County. The disastrous debris flows of the Tianmo Watershed on Sept. 4, 2007, July 25, 2010 and Sept. 4, 2010, blocked Parlung Zangbo River and produced dammed lakes, whose outburst flow made 50 m high terrace collapse at the opposite bank due to intense scouring on the foot of the terrace. As a result, the traffic was interrupted for 16 days in 2010 because that 900 m highway base was destructed and 430 m ruined. These debris flows were initiated by the glacial melting which was induced by continuous higher temperature and the following intensive rainfall, and expanded by moraines along channels and then blocked Parlung Zangbo. At the outlet of watershed,the density, velocity and peak discharge of debris flow was 2.06 t/m3, 12.7 m/s and 3334 m3/s, respectively. When the discharge at the outlet and the deposition volume into river exceeds 2125 m3/s and 126×103 m3, respectively, debris flow will completely blocked Parlung Zangbo. Moreover,if the shear stress of river flow on the foot of terrace and the inclination angel of terrace overruns 0. 377 N/m2 and 26°, respectively, the unconsolidated terrace will be eroded by outburst flow and collapse. It was strongly recommended for mitigation that identify and evade disastrous debris flows, reduce the junction angel of channels between river and watershed, build protecting wall for highway base and keep appropriate distance between highway and the edge of unconsolidated terrace.

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期刊信息
  • 《山地科学学报:英文版》
  • 主管单位:
  • 主办单位:中国科学院山地灾害与环境研究所
  • 主编:
  • 地址:四川成都一环路南二段16号
  • 邮编:610041
  • 邮箱:yudf@imde.ac.cn
  • 电话:028-85252110 85252044
  • 国际标准刊号:ISSN:1672-6316
  • 国内统一刊号:ISSN:51-1668/P
  • 邮发代号:
  • 获奖情况:
  • 国内外数据库收录:
  • 英国农业与生物科学研究中心文摘,荷兰文摘与引文数据库,美国地质文献预评数据库,美国剑桥科学文摘,美国科学引文索引(扩展库)
  • 被引量:84