陈卓, 梁收运. 2016: 兰州地区黄土-基岩不整合面与滑坡的关系研究. 工程地质学报, 24(s1): 681-686. DOI: 10.13544/j.cnki.jeg.2016.s1.099
    引用本文: 陈卓, 梁收运. 2016: 兰州地区黄土-基岩不整合面与滑坡的关系研究. 工程地质学报, 24(s1): 681-686. DOI: 10.13544/j.cnki.jeg.2016.s1.099
    CHEN Zhuo, LIANG Shouyun. 2016: RESEARCH ON THE RELATIONS BETWEEN LOESS-BEDROCK UNCONFORMITY SURFACE AND LANDSLIDE IN LANZHOU AREA. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 681-686. DOI: 10.13544/j.cnki.jeg.2016.s1.099
    Citation: CHEN Zhuo, LIANG Shouyun. 2016: RESEARCH ON THE RELATIONS BETWEEN LOESS-BEDROCK UNCONFORMITY SURFACE AND LANDSLIDE IN LANZHOU AREA. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 681-686. DOI: 10.13544/j.cnki.jeg.2016.s1.099

    兰州地区黄土-基岩不整合面与滑坡的关系研究

    RESEARCH ON THE RELATIONS BETWEEN LOESS-BEDROCK UNCONFORMITY SURFACE AND LANDSLIDE IN LANZHOU AREA

    • 摘要: 黄土地区普遍发育的滑坡灾害与黄土-基岩不整合面的关系密切,深入分析该类不整合面对黄土滑坡的控制作用是灾害防治的需要。本文以兰州地区为例,在分析滑坡的分布规律和一般特征的基础上,探讨了黄土-基岩不整合面与滑坡的发育密度和体积之间的空间关系。结果表明:(1)滑坡的发育长度、宽度、面积及体积,总体表现出随滑坡规模的增加,具有在特定范围集中分布的趋势;(2)滑坡的宽度与体积之间的相关性较差,滑坡长度与体积之间的相关性较好,描述滑坡规模指标间的拟合关系都表现出随滑坡规模的增大,离散性增加的特点;(3)滑坡在不整合面两侧近对称分布,且在该类不整合面附近,以黄土-基岩滑坡较为发育,滑坡规模大且数量多,而远离不整合面的滑坡规模小且数量少;(4)滑坡的数量、体积与该类不整合面间的距离服从分段幂律分布。

       

      Abstract: Landslides are commonly in loessland which has close relation to loess-bedrock unconformity surface. Furthermore, it is very necessary to conduct prevention and controlling of geological disasters by deeply analyzing the controlling effect of the unconformity surface on loess landslides. Taking Lanzhou area as the research object, this paper discusseed the spatial relationship between density and volume of landslide and the loess-bedrock unconformity surface through the analysis of landslide distribution and general characteristics. The results show that:(1) the length, width, area and volume of landslide present a concentration on certain range along with the increasing of the landslide scale; (2) the correlation between width and volume of the landslide is worse, whereas better correlation presents between length and volume of the landslide, and the fitting relationship between landslide scale indicates that the characteristic of discrete increase with the increasing of landslide scale; (3) landslides are almost symmetrically distributed on the both sides of unconformity surface, moreover a large quantity of loess-bedrock landslides in great size are relatively developed near the unconformity surface; (3) between amount and volume of landslide and the distance of loess-bedrock unconformity surface obeys piecewise power-law distribution.

       

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