- document
- Charriere, M.K.M. (author), Bogaard, T.A. (author), Junier, S.J. (author), Malet, J.P. (author), Mostert, E. (author) journal article 2015
- document
- Charriere, M.K.M. (author), Bogaard, T.A. (author), Junier, S.J. (author), Malet, J.P. (author), Mostert, E. (author) journal article 2015
- document
- Charriere, M.K.M. (author), Bogaard, T.A. (author), Junier, S.J. (author), Malet, J.P. (author), Mostert, E. (author) lecture notes 2014
- document
-
Krzeminska, D.M. (author), Bogaard, T.A. (author), Debieche, T.H. (author), Cervi, F. (author), Marc, V. (author), Malet, J.P. (author)The unsaturated zone largely controls groundwater recharge by buffering precipitation while at the same time providing preferential flow paths for infiltration. The importance of preferential flow on landslide hydrology is recognised in the literature; however, its monitoring and quantification remain difficult. This paper presents a combined...journal article 2014
- document
- Charriere, M.K.M. (author), Sprague, T. (author), Bogaard, T.A. (author), Greiving, S. (author), Malet, J.P. (author), Mostert, E. (author) journal article 2013
- document
- Charriere, M.K.M. (author), Bogaard, T.A. (author), Malet, J.P. (author), Mostert, E. (author) journal article 2013
- document
- Charriere, M.K.M. (author), Bogaard, T.A. (author), Malet, J.P. (author), Mostert, E. (author) journal article 2013
- document
-
Krzeminska, D.M. (author), Bogaard, T.A. (author), Malet, J.P. (author), Van Beek, L.P.H. (author)The importance of hydrological processes for landslide activity is generally accepted. However, the relationship between precipitation, hydrological responses and movement is not straightforward. Groundwater recharge is mostly controlled by the hydrological material properties and the structure (e.g., layering, preferential flow paths such as...journal article 2013
- document
-
Krzeminska, D.M. (author), Bogaard, T.A. (author), Malet, J.P. (author), Van Beek, L.P.H. (author)The importance of hydrological processes for landslide activity is generally accepted. However, the relationship between precipitation, hydrological responses and movement is not straightforward. Groundwater recharge is mostly controlled by the hydrological material properties and the structure (e.g. layering, preferential flow paths such as...journal article 2012
- document
-
Van Asch, T.W.J. (author), Malet, J.P. (author)Forecasting the possibility of flow-type failures within a slow-moving landslide mass is rarely taken into account in quantitative hazard assessments. Therefore, this paper focuses on the potential transition of sliding blocks (slumps) into flow-like processes due to the generation of excess pore water pressure in undrained conditions. The...journal article 2009
- document
-
Van Asch, T.W.J. (author), Malet, J.P. (author), Bogaard, T.A. (author)Slow-moving landslides show complex mechanical and fluid interactions. They show among others non linear intrinsic viscosity of the shear zone, undrained loading effects and the generation of excess pore water pressure. The parameterization of hydrological and geomechanical factors by field and laboratory tests to describe the movement pattern...journal article 2009