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Application of geophysical methods in the study of landslides

机译:地球物理方法在山体滑坡研究中的应用

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The paper discusses the results of the study of landslide processes by geophysical methods. In examining of landslides it is important to find out the features of their structure but it should always remember that landslides, as a rule, have the various combination of contrasted boundaries sometimes with a high gradient of physical properties. Analysis of landslide blocks various types suggests that it is not always possible to obtain reliable and sufficient information using just one geophysical parameter. Therefore, to study landslides, it is expedient to use a set of geophysical methods and to determine complex indicators. The study of landslide processes is one of the most difficult tasks for engineering geophysics, because the researches must be performed on rather steep slopes with physical heterogeneous of slip area. Size of study area (commonly used a lateral lengths of landslide) is usually limited, which the standard geophysical methods had thereby been m ade more difficult. In this paper there is an example, we present some results of geophysical studies performed in the district of Vytachiv. Geophysical methods are proved to be efficient for studying landslides.
机译:本文通过地球物理方法讨论了对滑坡过程研究的结果。在检查Landslides时,重要的是要了解它们的结构的特征,但应始终记住,通常具有与物理性质高梯度的对比边界的各种组合。山体滑坡块的分析各种类型表明,只有一个地球物理参数,并不总是可以获得可靠和充分的信息。因此,为了研究山体滑坡,有利的是使用一组地球物理方法并确定复杂的指标。对滑坡过程的研究是工程地球物理最困难的任务之一,因为必须在相当陡峭的滑坡上进行研究,具有滑块的物理异构。学习区域的大小(常用横向长度的滑坡)通常是有限的,因此标准的地球物理方法由此达到较困难。在本文中,有一个例子,我们展示了在Vytachiv区进行的地球物理研究的一些结果。证明了地球物理方法效率为研究山体滑坡。

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