Geophysical monitoring of landslides can provide insights into spatial and temporal
variations of subsurface properties associated with slope failure. Recent improvements in …

In the context of in-situ geophysical methods the Electrical Resistivity Tomography (ERT) is
widely used for the near-surface exploration of landslide areas characterized by a complex …

A geoelectrical investigation of a slow moving earth slide–earth flow in Lower Jurassic Lias
Group rocks of the Cleveland Basin, UK, is described. These mudrock slopes are particularly …

黄土高原地区受构造活动及河流侵蚀形成的大量黄土斜坡, 在降雨及农业灌溉等条件影响下,
每年会有大量黄土滑坡发生, 因此, 准确揭示黄土斜坡内部水分空间分布规律及运移特征对于 …

A ground model of an active and complex landslide system in instability prone Lias
mudrocks of North Yorkshire, UK is developed through an integrated approach, utilising …

Landslides developed on clay-rich slopes are controlled by the soil water regime and the
groundwater circulation. Spatially-distributed and high frequency observations of these …

The hydrological state of a hillslope prior to a sprinkling‐induced shallow landslide was
monitored using electrical resistivity tomography (ERT) along a 47 m long transect …

If electrodes move during geoelectrical resistivity monitoring and their new positions are not
incorporated in the inversion, then the resulting tomographic images exhibit artefacts that …

Measurement sensors permanently installed on landslides will inevitably change their
position over time due to mass movements. To interpret and correct the recorded data, these …

Shallow landslides are among the most frequent natural hazards in the Pays d'Auge plateau
(Normandy, France) but no study has yet focused on the functioning of these phenomena at …