Abstract
Large, slow-moving landslides with typical deformation rates of several centimetres per year often triggered by rainfall processes are very
common in Alpine regions. These events pose threats to various infrastructures such as railway tracks, roads, water power plants, and
residential areas, leading to potential risks and damages. In this paper, a recently developed analytical model that establishes a correlation
between precipitation, pore water pressure development in the slip zone and the deformation behaviour of the landslide is introduced. The
potential of the model is discussed based on data acquired from a landslide near Scheibbs in Eastern Austria.
common in Alpine regions. These events pose threats to various infrastructures such as railway tracks, roads, water power plants, and
residential areas, leading to potential risks and damages. In this paper, a recently developed analytical model that establishes a correlation
between precipitation, pore water pressure development in the slip zone and the deformation behaviour of the landslide is introduced. The
potential of the model is discussed based on data acquired from a landslide near Scheibbs in Eastern Austria.
| Original language | English |
|---|---|
| Title of host publication | Interpraevent 2024 - Conference Proceedings |
| Place of Publication | Vienna, Austria |
| Publisher | International Research Society Interpraevent |
| Chapter | C36 |
| Pages | 401-405 |
| Edition | Preliminary Version |
| ISBN (Print) | 978-3-901164-32-3 |
| Publication status | Published - 13 Jun 2024 |
| Event | Interpraevent 2024 - Vienna, Austria Duration: 10 Jun 2024 → 13 Jun 2024 |
Conference
| Conference | Interpraevent 2024 |
|---|---|
| Country/Territory | Austria |
| City | Vienna |
| Period | 10/06/24 → 13/06/24 |