Spatial assessment of probable recharge areas –  investigating the hydrogeological controls of an  active deep-seated gravitational slope deformation

Pfeiffer, Jan; Zieher, Thomas; Schmieder, Jan; Bogaard, Thom; Rutzinger, Martin; Spötl, Christoph

doi:https://doi.org/10.5194/nhess-22-2219-2022

Articles | Volume 22, issue 7

Nat. Hazards Earth Syst. Sci., 22, 2219–2237, 2022

https://doi.org/10.5194/nhess-22-2219-2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Nat. Hazards Earth Syst. Sci., 22, 2219–2237, 2022

https://doi.org/10.5194/nhess-22-2219-2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 22, issue 7

Research article

06 Jul 2022

Research article | 06 Jul 2022

Spatial assessment of probable recharge areas – investigating the hydrogeological controls of an active deep-seated gravitational slope deformation

Jan Pfeiffer et al.

Data sets

Hydrogeological data of groundwater and precipitation monitored in the Vögelsberg landslide catchment (1.0) J. Pfeiffer, T. Zieher, J. Schmieder, T. Bogaard, M. Rutzinger, and C. Spötl https://doi.org/10.5281/zenodo.5817141

Short summary

The activity of slow-moving deep-seated landslides is commonly governed by pore pressure variations within the shear zone. Groundwater recharge as a consequence of precipitation therefore is a process regulating the activity of landslides. In this context, we present a highly automated geo-statistical approach to spatially assess groundwater recharge controlling the velocity of a deep-seated landslide in Tyrol, Austria.