摘要:Landslides occur frequently all over the world, causing
at times considerable economic damage, injuries
and even death. In order to improve hazard assessment, common landslide types of a given region
need to be investigated in detail. While traditional
techniques of subsurface investigation are expensive
and only provide point information, geophysical
methods are suitable tools for gathering 2D and 3D
information on the subsurface quickly, reliably and
cost-effectively.
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In this study, the suitability and limitations of 2D
resistivity for the determination of landslide extent,
structure and soil moisture conditions are presented.
For this purpose, two identical profiles were taken
during a two-month period. Significant differences in
electrical resistivity (>1000 Ωm) due to varying soil
moisture conditions were observed. Using various
inversion parameters, it was possible to model two
distinct subsurface images. Regrettably, the sliding
plane could not be detected reliably, possibly due to
the homogeniety of the landslide material and underlying bedrock.