[1]王仁超,孔纪名*,崔 云.西南山区长输油气管道坡面泥石流成灾特征与防治--以云南昆明水节箐高位溃决型泥石流为例[J].山地学报,2018,(05):813-820.[doi:10.16089/j.cnki.1008-2786.000377]
　WANG Renchao,KONG Jiming*,et al.Characteristics and Countermeasures of Slope Debris Flow in Kunming of Yunnan Province of China[J].Mountain Research,2018,(05):813-820.[doi:10.16089/j.cnki.1008-2786.000377]
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西南山区长输油气管道坡面泥石流成灾特征与防治--以云南昆明水节箐高位溃决型泥石流为例()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2018年05期
页码:
813-820
栏目:
研究简报
出版日期:
2018-09-30

文章信息/Info

Title:
Characteristics and Countermeasures of Slope Debris Flow in Kunming of Yunnan Province of China
文章编号:
1008-2786-(2018)5-813-08
作者:
王仁超1; 2; 孔纪名1*; 崔 云1
1.中国科学院、水利部成都山地灾害与环境研究所 中国科学院山地灾害与地表过程重点实验室, 成都 610041; 2.中国科学院大学,北京100049
Author(s):
WANG Renchao1;  2; KONG Jiming1*; CUI Yun1
1.Key Laboratory of Mountain Hazards and Earth Surface Processes of CAS, Institute of Mountain Hazards and Environment, CAS, Chengdu 610041,China; 2.University of Chinese Academy of Science, Beijing100049, China
关键词:
高位坡面泥石流;  油气管道;  成灾特征;  灾害链;  防治对策
Keywords:
high debris flow;  pipeline;  characteristic;  geohazards chain;  countermeasure
分类号:
P642.21
DOI:
10.16089/j.cnki.1008-2786.000377
文献标志码:
C
摘要:
云南省地处我国西南山区,地形复杂,斜坡地质灾害频发、多发。省内油气管道分布密集,近年来投产的长输油气管道主要有西南成品油管道、中缅油气管道、百色至昆明成品油管道等。油气管道的建设、运营和管理面临着不同类型山地灾害的挑战。本文基于2017年9月14日云南昆明市水节箐右岸管道泥石流现场调查,分析了高位溃决型坡面泥石流灾害的启动、演化、成灾基本特征以及油气管道防治对策,研究成果对推动西南山区长输油气管道沿线泥石流灾害工程治理具有积极意义。
Abstract:
Yunnan Province is in the southwest mountainous area of China, where slope debris flows are fully developed and clustered along slopes, posing great threats to the operating safety of oil and gas pipelines.The long-distance oil and gas pipelines, mainly consisted of the southwest oil product pipeline, the Sino-Myanmar oil and gas pipeline, and Baise to Kunming's refined oil pipelines, etc., had been installed in southwestern China in recent years.Their construction, operation and management are suffering the damages due to types of mountain disasters haunting the relieffed region.Based on field investigations, a sudden and severe slope debris flow on the right bank of the ShuiJiejing of Kunming City, Yunnan Province on September 14, 2017, was carefully investigated by jointly examining of geological and hydrometeorological data.The initiation, evolution and formation of high-position catastrophe-prone slope debris flow were performed for a case study.And the basic characteristics of slope debris flows and its prevention and control measures were concluded.This investigation would provide us an engineered insight into the understanding of the damage pattern of slope debris flow on oil and gas pipelines and enlighten the management of mountain pipeline geohazards.

参考文献/References:

[1] 张楠,方志伟,韩笑,等.近年来我国泥石流灾害时空分布规律及成因分析[J],地学前缘,2018,25(02):299-308[ZHANG Nan, FANG Zhiwei, HAN Xiao, et al.The spatial and temporal distribution law and cause analysis of debris flow disasters in China in recent years [J].Frontiers of Geology,2018,25(02):299-308]
[2] 费祥俊,舒安平.泥石流运动机理与灾害防治[M].北京:清华大学出版社,2004:182-186 [FEI Xiangjun, SHU Anping.Disaster prevention and movement mechanism of debris flow[M].Beijing: Press of Tsinghua University,2004:182-186]
[3] 中国科学院、水利部成都山地灭害与环境研究所.中国泥石流[M].北京:北京商务印书馆,2000 [Institute of Mountain Hazards and Environment, Chinese Academy of Sciences.Debris flows in China[M].Beijing: The Commercial Press,2000]
[4] 陈洪凯,唐红梅,叶四桥.中国公路泥石流研究[J],中国地质灾害与防治学报,2008,19(1):1-5[CHEN Hongkai, TANG Hongmei[J], YE Siqiao.Study on debris flows along highways in China [J],The Chinese Journal of Geological Hazard and Control,2008,19(1):1-5]
[5] 崔鹏.泥石流起动条件及机理的实验研究[J],科学通报,1991,21:1650-1652[CUI Peng.Study on conditions and mechanisms of debris flow initiation by means of experiment[J].Chinese Science Bulletin,1991,21:1650-1652]
[6] 潘华利,欧国强,柳金峰.泥石流沟道侵蚀初探[J],灾害学,2009.24(1):39-43[PAN Huali, OU Guoqiang, LIU Jinfeng.A study on debris flow gully erosion[J].Journal of Catastrophology,2009,24(1):39-43]
[7] 贺拿,陈宁生,曾超.泥石流起动机理研究现状及趋势[J],灾害学,2013.28(1):121-125[HE Na, CHEN Ningsheng, ZENG Chao.Current situation and tendencies of debris flow initiation mechanism[J].Journal of Catastrophology,2013,28(1):121-125]
[8] 唐红梅,陈洪凯,唐兰.坡面泥石流演化模式及其试验[J],山地学报,2014,32(1):98-104[TANG Hongmei, CHEN Hongkai, TANG Lan.Evolution model and test of slope debris flow[J],Mountain Research,2014,32(1):98-104]
[9] 曾凡伟,徐刚,李青,等.坡度阀值与坡面泥石流-以重庆市北碚区为例[J],山地学报,2004,22(5):568-571[ZENG Fanwei, XU Gang, LI Qing, et al.Critical gradient and debris flow on slope a case study in Beibei, Chongqing[J].Mountain Research,2004,22(5):568-571]
[10] M.A.卡森,M.J.柯克拜著,窦葆璋译.坡面形态与形成过程[M].北京:科学出版社,1984:28-66[CARSON M.A., KIRKBY M.J.Translated by DOU Baozhang.Hillslop form and process[M].Beijing: Science Press,1984:28-66]
[11] 崔鹏,杨坤,陈杰.前期降雨对泥石流形成的贡献一以蒋家沟泥石流形成为例[J],中国水土保持科学,2003,1(1):11-15[CUI Peng, YANG Kun, CHEN Jie.Relationship between occurrence of debris flow and antecedent precipitation: taking the Jiangjia Gully as an example[J].Science of Soil and Water Conservation,2003,1(1):11-15]
[12] 谭万沛,韩庆玉.四川省泥石流预报的区域临界雨量指标研究[J],灾害学,1992,7(2):37-12[TAN Wanpei, HAN Qingyu.Study on regional critical rainfall indices of debris flow in Sichuan province[J].Journal of Catastrophology,1992,7(2):37-42]
[13] 唐川,李为乐,丁军,等.汶川震区映秀镇“8·14”特大泥石流灾害调查[J],地球科学-中国地质大学学报,2011,36(1):172-180[TANG Chuan.LI Weile.DING Jun, et al.Field investigation and research on giant debris flow on august 14,2010 in Yingxiu Town epicenter of Wenchuan Earthquake [J].Earth Science-Journal of China University of Geosciences,2011,36(1):172-180]
[14] DZ/T0220-2006泥石流灾害防治工程勘查规范[S].北京:中国标准出版社,2006[Ministry of Land and Resources of the People's Republic of China.DZ/T0220-2006.Specification of geological investigation for debris flow stabilization[S].Beijing: China Standard Press,2006]
[15] 胡桂胜,尚彦军,曾庆利,等.新疆叶城“7.6”特大灾害性泥石流应急科学调查[J],山地学报,2017,35(1):112-116[HU Guisheng, SHANG Yanjun, ZENG Qingli,et al.The emergency scientific investigation of catastrophic debris flow in Yecheng County of Xinjiang on July 6th,2016[J].Mountain Research,2017,35(1):112-116]
[16] 唐邦兴.中国泥石流[M].北京:商务印书馆,2000:72-95[TANG Bangxing.Debris flow in China[M].Beijing: The Commercial Press,2000:72-95]

备注/Memo

备注/Memo:
收稿日期(Received date):2018-06-11; 改回日期(Accepted date): 2018-10-22
基金项目(Foundation item):中国石油化工股份有限公司科研基金(318022-8); 国家自然科学基金(41401608)。 [Research project of China Petrochemical Corporation(318022-8); National Natural Science Foundation of China(41401608)]
作者简介(Biography):王仁超(1989-),男,湖南湘潭人,博士研究生,主要研究方向:山地灾害综合防治技术。[WANG Renchao(1989-), male, born in Xiangtan, Hunan Province, Ph.D.candidate, research on integrated prevention and control of mountain disasters.]E-mail:renchao1225@sina.com
*通讯作者(Corresponding author):孔纪名(1956-),男,四川成都人,研究员,主要研究方向:斜坡变形破坏规律与综合防治技术。[KONG Jiming(1956-),male,born in Chengdu, Sichuan Province, professor, research on Law of slope failure and integrated prevention technology]E-mail: jimingk@imde.ac.cn
更新日期/Last Update: 2018-11-30