METHODOLOGICAL ASPECTS OF LANDSLIDE RISK ASSESSMENT WITHIN URBAN AREAS (CASE STUDY OF THE MODEL SITE "LYSA GORA", KYIV)

O. Ivanik, O. Menshov, D. Kravchenko, K. Bondar, K. Hadiatska, L. Tustanovska, R. Khomenko
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Abstract

The integrated geological, geophysical, and GIS methods for the overall assessment of the geological hazards within the urbanized environment were considered. The principal gap in the understanding of the geologically hazardous areas in Ukraine (landslide, soil erosion, pollution, etc.) is the lack of information about the properties of rocks and soils as well as their interaction with the past and present natural and anthropogenic formation. The study area is the landslide activation territory of Lysa Gora in Kyiv, Ukraine (Golosiivsky district). The slope has the conditional stabilization. At the same time the landslides provide the real dangery to the infrastructure facilities. One of the examples is the deformation of the railway along the Stolychne Highway. Landslide susceptibility data have been collected. The proposed methodology consists of the geological, geophysical, thermography, and remote sensing. This methods provide the possibility for the monitoring of landslides at the model areas in Kyiv region. The electrical resistivity tomography at the Lysa Gora identified two local zones of activation of landslide displacements, which are located in the range of depths of 3-8 m from the ground surface. The random distribution of the soil magnetic susceptibility and frequency dependence of the magnetic susceptibility both on lateral and verical line (soil genetic horizons) identified the presence of the displacement, redistribution and deposition of the soil and underlaying rocks. All the mentioned factors are in the genetic relation to the soil erosion and initial landslides.
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城市地区滑坡风险评估的方法学方面(基辅“lysa gora”模型场地的案例研究)
研究了地质、地球物理和地理信息系统综合评价城市化环境地质灾害的方法。在了解乌克兰地质危险地区(滑坡、水土流失、污染等)方面的主要差距是缺乏关于岩石和土壤性质及其与过去和现在的自然和人为形成的相互作用的资料。研究区为乌克兰基辅市Lysa Gora滑坡活化区(Golosiivsky区)。该边坡具有条件稳定。与此同时,山体滑坡对基础设施构成了真正的威胁。其中一个例子是沿斯托利奇高速公路的铁路变形。收集了滑坡易感性资料。提出的方法包括地质、地球物理、热成像和遥感。这种方法为在基辅地区的示范地区进行滑坡监测提供了可能。在Lysa Gora的电阻率层析成像确定了两个局部滑坡位移激活区,它们位于距离地表3-8 m的深度范围内。土壤磁化率的随机分布和磁化率在横向和纵向(土壤成因层)上的频率依赖性表明了土壤和下垫岩的位移、重分布和沉积的存在。这些因素都与土壤侵蚀和初期滑坡有一定的成因关系。
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