[1]宋丹青,梁收运,王志强,等.九甸峡库区地质灾害发育分布及影响因素[J].山地学报,2016,(01):84-91.[doi:10.16089/j.cnki.1008-2786.000104]
 SONG Danqing,LIANG Shouyun,WANG Zhiqiang,et al.Development, Distribution and Influencing Factors of Geohazards in Jiudian Gorge Reservoir[J].Mountain Research,2016,(01):84-91.[doi:10.16089/j.cnki.1008-2786.000104]
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九甸峡库区地质灾害发育分布及影响因素()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2016年01期
页码:
84-91
栏目:
山地灾害
出版日期:
2016-02-01

文章信息/Info

Title:
Development, Distribution and Influencing Factors of Geohazards in Jiudian Gorge Reservoir
作者:
宋丹青1梁收运2王志强23徐永福1*冯兴波1
1. 上海交通大学 船舶海洋与建筑工程学院,上海 200030; 2.兰州大学 土木工程与力学学院,甘肃 兰州 730000; 3.水利部 水利水电规划设计总院,北京 100081
Author(s):
SONG Danqing1LIANG Shouyun2WANG Zhiqiang23XU Yongfu1FENG Xingbo1
1. School of Naval Architecture, Ocean and Civil Engineering, Shanghai Jiaotong University, Shanghai 200030,China; 2. School of Civil Engineering and Mechanics, Lanzhou University, Lanzhou 730000,Gansu,China; 3. General Institute of Water Resources and Hydropower Planning and Design, Ministry of Water Resources, Beijing 100081, China
关键词:
地质灾害分布发育影响因素库区
Keywords:
geohazards factors development and distribute reservoir
分类号:
P642.2,P694
DOI:
10.16089/j.cnki.1008-2786.000104
文献标志码:
A
摘要:
九甸峡水库蓄水后库区地质环境发生较大程度上的改变,地质灾害发育。通过对库区的多次实地调查,分析了地质灾害的发育、分布特性及其影响因素,系统地分析了库区地质灾害的主要类型。结果表明:河流对库区地质灾害的分布具有重要影响,地质灾害点的分布基本位于距离库岸3 km范围内,约有50%位于1 km范围内,随着与库岸的距离增加,表现为递减趋势;地质灾害的分布与地貌有密切的关系, 大多数地质灾害发生在高程 2 200~2 500 m,尤其是坡度30°~50°的范围内;地质灾害在流域内分布范围广、灾害点多、具有带状分布特征, 主要沿库区沿岸发生,多呈线性分布;不同的岸坡结构控制着地质灾害的发育、分布,地质灾害的类型、发育分布也与坡体结构、岩土体性质密切相关;库区滑坡和泥石流主要类型分为3类,分析了灾害形成机制,为库区地质灾害的防治提供可靠依据。
Abstract:
The geological environment had changed in large extent after the Jiudian Gorge Reservoir in Zhuoni County of Gansu Province, China impoundment with the development of geological disasters. According to the detailed field investigation for many times, this paper has analyzed properties of the development and distribution and influencing factors of geological disasters with the main types of the geological disasters was systematically analyzed at the same time. The results show that the river had influence on the distribution of the geological disasters , the distribution of geological disasters were located within the range of 3 km from river approximately fifty percent being located in the range of 1 km with showing the decreasing trend with the increasing distance of the bank. The distribution of geological disasters has close relation with topography and geomorphology, and most of the geological disaster occurred in 2 200~2 500 m, especially the slope 30°~50°. The geological disasters were widely distribution, large number, and had the characteristics of zonal distribution. The main geological disasters occurred along coast of reservoir and most of them were showed linear distribution. The different geological structure controlled the development and distribution of geological disasters of the type and distribution, and it was also closely related to the slope structure, geotechnical liquid property. The main types of landslides and debris flows in reservoir area are divided into 3 types, and the disaster formation mechanism was analyzed for providing reliable basis for the geological disaster prevention.

参考文献/References:

[1] 张春山,张业成,马寅生,等.黄河上游地区地质灾害分布规律与区划[J].地球学报,2003,24(2):155-160[Zhang Chunshan, Zhang Yecheng, Ma Yinsheng, et al. Distribution regularity and regionalization of geological hazards in the Upper Yellow River Valley[J]. Acta Geosicientia Sinica, 2003, 24(2):155-160]
[2] 张春山,张业成,胡景江,等.中国地质灾害时空分布特征与形成条件[J].第四纪研究,2000,20(6):559-566[Zhang Chunshan, Zhang Yecheng, Hu Jingjiang, et al. Spatial and temporal distribution characteristics and forming conditions of Chinese geological disasters[J]. Quaternary Sciences, 2000, 20(6):559-566]
[3] Paronuzzi P, Rigo E, Bolla A. Influence of filling- drawdown cycles of the Vajont reservoir on Mt.Toc slope stability [J]. Geomorphology, 2013,191:75-93
[4] 杨为民,吴树仁,张永双,等.降雨诱发坡面型泥石流形成机理[J].地学前缘,2007,14(6):197-204[Yang Weimin, Wu Shuren, Zhang Yongshuang, et al. Research on formation mechanism of the debris flowon slope induced by rainfall[J]. Earth Science Frontiers, 2007, 14(6):197-204]
[5] 甘肃省地质灾害防治工程勘察设计院.洮河九甸峡水利枢纽灾害危险性评估报告[R].兰州:甘肃省地质灾害防治工程勘察设计院,2003.[Gansu Province Geological Disaster Prevention Engineering Investigation and Design Institute. The disaster risk assessment report on Jiudianxia Water conservancy hub[R]. Lanzhou: Gansu Province Geological Disaster Prevention Engineering Investigation and Design Institute,2003.]
[6] 曾琳洁,张涛,冯文凯.河南南召县地质灾害形成条件与分布规律[J].中国地质灾害与防治学报,2014, 25(1):82-89[Zeng Linjie, Zhang Tao, Feng Wenkai. Formation conditions and distribution law about geological disasters in Nanzhao county, Henan Province [J]. The Chinese Journal of Geological Hazard and Control, 2014, 25(1): 82-89]
[7] Parsons T, Chen J, Kirby E. Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin [J].Nature,2008, 454:509-510
[8] Keefer D K. Statistical analysis of an earthquake induced landslide distribution the 1989 Loma Prieta, California eveat [J]. Engineering Geology, 2000, 58:231-249
[9] 巨能攀,侯伟龙,赵建军,等.安县雎水河流域地质灾害发育、分布及影响因素[J].山地学报,2010,28(6):732-740[Ju Nengpan, Hou Weilong, Zhao Jianjun, et al. Geohazards of Jushui Riverin the Wenchuan Earthquak Area [J]. Mountain Research, 2010, 28(6):732-740]
[10] 刘传正.中国崩塌滑坡泥石流灾害成因类型[J].地质评论,2014,60(4):858-868[Liu Chuanzheng. Genetic types of landslide and debris flow disasters in China [J]. Geological Review,2014, 60(4): 858-868]
[11] 卢书强,易庆林,易武,等.三峡库区树坪滑坡变形失稳机制分析[J].岩土力学,2014,35(4): 1123 -1130[Lu Shuqiang, Yi Qinglin, Yi Wu, et al. Analysis of deformation and failure mechanism of Shuping landslide in Three Gorges Reservoir Area [J]. Rock and Soil Mechanics, 2014,35(4): 1123-1130]
[12] 许冲,徐锡伟,于贵华.玉树地震滑坡分布调查及其特征与形成机制[J].地震地质,2012,34(1):47-62[Xu Chong, Xu Xiwei, Yu Guihua. Study on The characteristics, mechanism, and spatial distribution of Yushu Earthquake triggered landslides [J]. Seismology and Geology, 2012, 34(1): 47-62]
[13] 吴琼,唐辉明,王亮清.库水位升降联合降雨作用下库岸边坡中的浸润线研究[J].岩土力学,2009,30(10): 3025-3031[Wu Qiong, Tang Huiming, Wang Liangqing. Analytic solutions for phreatic line in reservoir slope with inclined impervious bed under rainfall and reservoir water level fluctuation [J]. Rock and Soil Mechanics, 2009, 30(10): 3025-3031]

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备注/Memo

备注/Memo:
收稿日期(Received date):2015-08-31;改回日期(Accepted):2015-09-09。 基金项目(Foundation item):国家自然科学基金项目(41272318,41472251);国家重点基础研究发展计划(973计划)(2014CB744701)。[ The National Natural Science Foundation of China (41272318,41472251);The national key basic research and development program (2014CB744701).] 作者简介(Biography):宋丹青(1989-),男,博士研究生,主要从事岩土工程方面的研究工作。[Song Danqing(1989-), male, Ph D, born in Zhengzhou City,Henan Province. Mainly engaged in the research of geotechnical engineering.]
更新日期/Last Update: 1900-01-01