Sebastian Uhlemann

TL;DR: Whiteley et al. as discussed by the authors presented a review of the state of the art of geophysical monitoring applied to moisture-induced landslides, focusing on technical and practical uses of time-lapse methods in geophysics applied to monitoring moistureinduced landslide.

TL;DR: In this paper, the authors compared the performance of a combination of monitoring techniques that have been employed together for the first time on an active landslide in the Whitby Mudstone Formation at Hollin Hill, North Yorkshire, UK.

TL;DR: In this article, the authors describe a system and methods for monitoring temporal and spatial moisture content changes in clay embankments using electrical resistivity tomography (ERT) imaging, based upon the development of a robust relationship between fill resistivity and moisture content and its use in the transformation of resistivity image differences in terms of relative moisture content change.

TL;DR: In this article, a 3D time-lapse resistivity imaging on an active landslide was used to provide long-term data highlighting the evolution of moisture content prior to landslide reactivation and showing its decline post reactivation.

TL;DR: In this paper, the authors used geophysics to characterize spatial and temporal variability in the subsurface region proximal to SW bodies, the GW-SW interface, which is crucial as it actively regulates the transfer of nutrients, contaminants, and water between GW systems and SW environments.