张伟朋, 谌文武, 叶飞, 王圣麟. 2016: 基于GIS的白龙江流域甘肃段滑坡分布规律研究. 工程地质学报, 24(s1): 1118-1126. DOI: 10.13544/j.cnki.jeg.2016.s1.161
    引用本文: 张伟朋, 谌文武, 叶飞, 王圣麟. 2016: 基于GIS的白龙江流域甘肃段滑坡分布规律研究. 工程地质学报, 24(s1): 1118-1126. DOI: 10.13544/j.cnki.jeg.2016.s1.161
    ZHANG Weipeng, CHEN Wenwu, YE Fei, WANG Shenglin. 2016: STUDY ON THE DISTRIBUTION RULES OF LANDSLIDES OF BAILONG RIVER BASIN IN GANSU PROVINCE. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 1118-1126. DOI: 10.13544/j.cnki.jeg.2016.s1.161
    Citation: ZHANG Weipeng, CHEN Wenwu, YE Fei, WANG Shenglin. 2016: STUDY ON THE DISTRIBUTION RULES OF LANDSLIDES OF BAILONG RIVER BASIN IN GANSU PROVINCE. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 1118-1126. DOI: 10.13544/j.cnki.jeg.2016.s1.161

    基于GIS的白龙江流域甘肃段滑坡分布规律研究

    STUDY ON THE DISTRIBUTION RULES OF LANDSLIDES OF BAILONG RIVER BASIN IN GANSU PROVINCE

    • 摘要: 白龙江流域是全国四大地质灾害高发地区之一,通过遥感影像解译及实地调查等手段共查明白龙江流域甘肃段境内发育各类规模滑坡1030处。本文基于GIS空间技术分析方法,分别使用滑坡数量和滑坡密度两个统计指标,对滑坡发育的地层岩性、高程、坡向、坡度、断层缓冲区、河流缓冲区、道路缓冲区、土地类型等8项参数进行统计分析,结果表明白龙江流域甘肃段滑坡发育主要呈现以下特征:(1)滑坡坡向主要集中在S和SE坡,坡度集中在0~20范围内,主要分布在薄层灰岩、板岩、千枚岩岩组区及板岩、中厚层灰岩岩组区;(2)1300~2000m高程段内滑坡数量最多,600~1300m高程段内滑坡密度最大;(3)滑坡数量及密度等分布特征与断裂、河流及道路的延伸关系密切,随着与断裂、河流及道路的距离减小,滑坡的数量及密度逐渐增大;(4)耕地区滑坡的数量及密度最大,其次为草地区,其他土地类型滑坡较少发育。

       

      Abstract: Bailongjiang Valley is one of the four major geological disaster prone areas.1030 landslides are found by the combination of remote sensing technology and on-the-spot investigation in the research areas. Based on the GIS space analysis method, two statistical indicators, namely landslide number and density, were used to count 8 parameters of formation lithology, slope height, slope direction, slope angle, the fault buffer, the river buffer, the road buffer and the land types. The statistical results of 1030 landslides distributed in 6 counties suggest that, landslide distribution of Bailongjiang valley in Gansu province mainly showed the following characteristics:(1) the landslides mainly distribute in the S and SE slope, the range of 0~20 degree, and mainly distribute in the phyllite, slate, thin limestone rock group and the thick layer of limestone, slate rock group district; (2) the height of 1300~2000m occupies in the largest number of landslide, while landslide density maximum in 600~1300m height; (3) the number and density of the landslide decreases with the increase of fracture, river and road distance; (4) the landslide mainly concentrated in the farming area, followed by the grass area.

       

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