摘要 | 西藏是全国地质灾害最严重的省区之一, 地质灾害对经济社会发展的影响日趋显著。为研究西藏堆龙德庆区典型灾害泥石流的发育特征及孕灾地质条件, 本文基于1: 5万地质灾害风险调查评价成果, 在系统总结研究区泥石流灾害发育特征及时空分布规律的基础上, 选用ArcGIS空间分析方法探讨泥石流灾害与地形地貌、地质构造、工程地质岩组、水系密度、植被覆盖率等因素的关系。研究成果显示, 区内共发育泥石流灾害点117处, 灾害规模以小型为主, 主要集中发生在7-8月, 具有沿断裂构造、河流及深切河谷区集中分布的特征。地形地貌、地质构造、工程地质岩组、水系密度与泥石流表现出了不同程度的相关性, 流域面积越小, 沟道纵坡降越大, 流域内断层和水系 密度越大, 越有利于泥石流灾害的形成; 而易滑地层则为泥石流的发育提供有利的物源条件。泥石流灾害的形成与上述孕灾因子关系密切, 是多种因素耦合作用的结果, 可为研究区泥石流灾害的防治提供参考基础。 |
Abstract | Xizang is one of the provinces and regions with the most serious geological disasters in China. The impact of geological disasters on economic and social development is becoming increasingly significant. To study the development characteristics and geological conditions of typical disaster debris flows in the Deqing District of Duilong, this article is based on the results of a 1: 50000 geological hazard risk investigation and evaluation. Based on a systematic summary of the development characteristics and spatiotemporal distribution patterns of debris flow disasters in the research area, ArcGIS spatial analysis method is used to explore the relationship between debris flow disasters and factors such as topography, geological structure, engineering geological rock formations, water system density, and vegetation coverage. The research results show that there are a total of 117 debris flow disaster points developed in the area, the scale of disasters is mainly small-scale disasters, mainly occurring in July and August, which characterized by concentrated distribution along fault structures, rivers, and deep river valleys. There is a varying degree of correlation between topography, geological structure, engineering geological rock formations, water system density, and debris flow. The smaller the watershed area, the greater the longitudinal slope of the channel, and the higher the density of faults and water systems within the watershed, which is more conducive to the formation of debris flow disasters; And the easily slippery strata provide favorable source conditions for the development of debris flows. The formation of debris flow disasters is closely related to the above-mentioned disaster prone factors, and is the result of the coupling effect of multiple factors, which can provide a reference basis for the prevention and control of debris flow disasters in the study area. |
DOI | 10.48014/cesr.20240813002 |
文章类型 | 研究性论文 |
收稿日期 | 2024-08-13 |
接收日期 | 2024-08-24 |
出版日期 | 2024-12-28 |
关键词 | 泥石流, 孕灾地质条件, 分布规律, 堆龙德庆区 |
Keywords | Debris flow, geological conditions of disaster prone areas, distribution pattern, Duilong Deqing District |
作者 | 周鹏, 万忠焱*, 李强, 荣峰, 刘恭喜, 元旦措姆 |
Author | ZHOU Peng, WAN Zhongyan*, LI Qiang, RONG Feng, LIU Gongxi, YUAN Dancuomu |
所在单位 | 西藏自治区地勘局地热地质大队, 拉萨 850000 |
Company | Geothermal and Geological Party, Tibet Bureau of Mineral Resource Exploration and Development, Lhasa 850000, China |
浏览量 | 137 |
下载量 | 43 |
基金项目 | 西藏自治区地质灾害防治体系项目(项目编号:54000021210200001372) |
参考文献 | [1] 潘懋, 李铁峰. 灾害地质学[M]. 北京: 北京出版社, 2002. [2] 吴树仁, 石菊松, 张春山, 等. 地质灾害风险评估技术指南初伦[J]. 地质通报, 2009, 28(8): 995-1005. https://doi.org/10.3969/j.issn.1671-2552.2009.08.001 [3] 齐信, 唐川, 陈州丰, 等. 地质灾害风险评价研究[J]. 自然灾害学报, 2012, 21(5): 33-40. https://doi.org/10.13577/j.jnd.2012.0506 [4] 高峰, 高秀. 近20a来我国地质灾害链研究综述[J]. 地质灾害与环境保护, 2024, 35(1): 55-62. https://doi.org/10.3969/j.issn.1006-4362.2024.01.010 [5] 刘德民, 王杰, 姜淮, 等. 青藏高原形成演化动力机制及其远程效应[J]. 地学前缘, 2024, 31(1): 154-169. https://doi.org/10.13745/j.esf.sf.2024.1.146 [6] 王世金, 魏彦强, 牛春华, 等. 青藏高原多灾种自然灾害综合风险管理[J]. 冰川冻土, 2021, 43(6): 1848-1860. https://doi.org/10.7522/j.issn.1000-0240.2021.0116 [7] 西藏地勘局第二地质大队. 西藏自治区1: 5万地质灾害详细调查综合研究报告[R]. 2020. [8] 西藏地勘局地热地质大队. 西藏自治区堆龙德庆区1: 50000地质灾害详细调查报告[R]. 2019. [9] 西藏地勘局地热地质大队. 西藏自治区堆龙德庆区1: 50000地质灾害风险调查评价报告[R]. 2021. [10] 徐琳, 罗邵强, 胡林, 等. 基于GIS的拉萨堆龙德庆区地质灾害易发性评价[J]. 四川地质学报, 2023, 43(1): 147-151. https://doi.org/10.3969/j.issn.1006-0995.2023.01.025 [11] 徐琳, 达娃, 罗邵强, 等. 堆龙德庆区比西沟泥石流特征及成因机制分析[J]. 四川地质学报, 2021, 41(3): 448-452. https://doi.org/10.3969/j.issn.1006-0995.2021.03.019 [12] 杜榕桓, 段金凡. 中国泥石流形成环境剖析[J]. 云南地理环境研究, 1990, 2(2): 8-18. [13] 杜榕桓, 李鸿琏, 唐邦兴, 等. 三十年来的中国泥石流研究[J]. 自然灾害学报, 1995, 4(1): 64-73. [14] 符文熹, 聂德新, 任光明, 等. 中国泥石流发育分布特征研究[J]. 中国地质灾害与防治学报, 1997, 8(4): 39-43. [15] 崔鹏, 韦方强, 谢洪, 等. 中国西部泥石流及其减灾对策[J]. 第四纪研究, 2003, 23(2): 142-151. https://doi.org/10.3321/j.issn:1001-7410.2003.02.004 [16] 贾铁飞, 何雨, 李容全. 中国东部山地泥石流发育的第四纪环境背景及减灾对策[J]. 山地学报, 2000, 18(2): 104-109. https://doi.org/10.16089/j.cnki.1008-2786.2000.02.002 [17] 杨成林, 陈宁生, 李战鲁. 汶川地震次生泥石流形成模式与机理[J]. 自然灾害学报, 2011, 20(3): 31-37. https://doi.org/10.13577/j.jnd.2011.0306 [18] 吴凯, 倪万魁, 袁志辉, 等. 宁夏隆德县泥石流形成条件[J]. 南水北调与水利科技, 2016, 14(2): 159-164. https://doi.org/10.13476/j.cnki.nsbdqk.2016.02.028 [19] 张书豪. 基于GIS与人工智能的区域泥石流、地震滑坡易发危险性评价方法研究———以丽香铁路金沙江桥址减灾选线应用为例[D]. 成都: 西南交通大学, 2014. https://doi.org/10.27414/d.cnki.gxnju.2022.003866 [20] 王高峰, 王爱军, 田运涛, 等. 基于图幅调查的六盘山镇孕灾地质条件分析[J]. 水土保持研究, 2016, 23(5): 364-369. https://doi.org/10.13869/j.cnki.rswc.2016.05.050 [21] 刘腾, 任蕊, 匡野, 等. 四川省北川县崩滑灾害孕灾地质条件分析[J]. 中国地质调查, 2022, 9(6): 59-66. https://doi.org/10.19388/j.zgdzdc.2022.06.08 [22] 齐信. 四川松潘水沟墩沟泥石流成因和动力学特征及其对铁路工程的影响评价[J]. 中国地质灾害与防治学报, 2014, 25(2): 13-18. https://doi.org/10.19388/10.16031/j.cnki.issn.1003-8035.2014.02.005 |
引用本文 | 周鹏, 万忠焱, 李强, 等. 西藏堆龙德庆区泥石流发育特征及孕灾地质条件分析[J]. 中 国地球科学评论, 2024, 3(4): 177-184. |
Citation | ZHOU Peng, WAN Zhongyan, LI Qiang, et al. Analysis on the development characteristics and geological conditions of debris flow in Duilong Deqing District, Xizang[J]. Chinese Earth Sciences Review, 2024, 3(4): 177-184. |