邓小龙, 李丽慧, 李星星, 谭玉芳. 2015: 北京市平谷区地质灾害易发性评价研究. 工程地质学报, 23(s1): 266-277. DOI: 10.13544/j.cnki.jeg.2015.s1.043
    引用本文: 邓小龙, 李丽慧, 李星星, 谭玉芳. 2015: 北京市平谷区地质灾害易发性评价研究. 工程地质学报, 23(s1): 266-277. DOI: 10.13544/j.cnki.jeg.2015.s1.043
    DENG Xiaolong, LI Lihui, LI Xingxing, TAN Yufang. 2015: GEOHAZARD SUSCEPTIBILITY ASSESSMENT OF PINGGU DISTRICT. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 266-277. DOI: 10.13544/j.cnki.jeg.2015.s1.043
    Citation: DENG Xiaolong, LI Lihui, LI Xingxing, TAN Yufang. 2015: GEOHAZARD SUSCEPTIBILITY ASSESSMENT OF PINGGU DISTRICT. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 266-277. DOI: 10.13544/j.cnki.jeg.2015.s1.043

    北京市平谷区地质灾害易发性评价研究

    GEOHAZARD SUSCEPTIBILITY ASSESSMENT OF PINGGU DISTRICT

    • 摘要: 地质灾害的易发性评价是区域地质灾害预警的基础, 具有重要的指导意义。文章基于北京市平谷区1: 5万地质灾害详细调查, 对其地质灾害的发育特征、分布规律及影响因素进行了详细地分析。运用GIS空间分析功能, 对影响地质灾害演变的区域构造断裂、工程地质岩组、植被覆盖率、地形坡度和人类工程活动等因素进行了综合分析, 采用频率比模型完成了地质灾害易发评价区划。结果显示:平谷区地质灾害分布主要与地形地貌、构造断裂及人类工程活动相关, 这与实际情况较为一致。根据评价结果可将平谷区地质灾害易发性划分为4个等级。其中, 地质灾害高易发区面积125.6km2, 占11.7%, 中易发区面积273.02km2, 占25.4%, 低易发区总面积为326.89km2, 占30.4%, 不易发区面积349.49km2, 占32.5%。评价结果可为平谷区地质灾害防治规划提供依据。

       

      Abstract: A scientific and rational knowledge of geohazard susceptibility assessment is of vital importance to the warning of regional geohazard. Based on geohazard field investigation of Pinggu District at 1:50000 scale and geohazard database established subsequently, the development characteristics, spatial distribution and influence factors of geohazards were obtained. Factors such as engineering geological strata, slope gradient, tectonic fault, human engineering activities and vegetation coverage have a significant impact on the evolution of geohazard, they was comprehensively analyzed through the spatial tool in GIS.Using frequency ratio evaluation, geohazard susceptibility assessment of Pinggu District was carried out. Results showed the distribution of geohazard in Pinggu District had a close relationship to regional landform, faults and human engineering activities, which was consistent with actual conditions. According to the evaluation, the whole area can be divided into four areas: the high susceptibility of geohazards area, which covers 125.6km2, accounting for 27.3% of the total studied area the medium susceptibility of geohazards area, which is calculated 273.02km2, accounting for 13.3% the low susceptibility of geohazards area, which is measured 326.89km2, taking up 22.7% and the stable area covers 349.49km2, accounting for 36.7%.The results can provide a guideline for the mitigation and prevention of geohazard in Pinggu District.

       

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