46 citations as recorded by crossref.

1. Stability Analysis of a Two‐Layered Slope with Cracks by Finite Element Limit Analysis A. Zhou et al. 10.1155/2020/8812277
2. Quantification of the influence of preferential flow on slope stability using a numerical modelling approach W. Shao et al. 10.5194/hess-19-2197-2015
3. Conceptualization of preferential flow for hillslope stability assessment K. Kukemilks et al. 10.1007/s10040-017-1667-0
4. Comparison of single- and dual-permeability models in simulating the unsaturated hydro-mechanical behavior in a rainfall-triggered landslide W. Shao et al. 10.1007/s10346-018-1059-0
5. The hydrological and the hydrogeological framework of the Lottenbachtal, Bochum, Germany M. Alhamed 10.1007/s13201-014-0247-x
6. Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) G. Bièvre et al. 10.1155/2018/9593267
7. Groundwater—Surface waters interactions at slope and catchment scales: implications for landsliding in clay‐rich slopes V. Marc et al. 10.1002/hyp.11030
8. Influence of Benggang slope cracks on soil water regimes: Comparison of model simulation and time‐domain reflectometry X. Duan et al. 10.1111/ejss.13302
9. Influence of tension cracks on moisture infiltration in loess slopes under high-intensity rainfall conditions X. Ren et al. 10.1038/s41598-025-88865-w
10. Determining the influencing factors of preferential flow in ground fissures for coal mine dump eco-engineering Y. Li et al. 10.7717/peerj.10547
11. Rain and small earthquakes maintain a slow-moving landslide in a persistent critical state N. Bontemps et al. 10.1038/s41467-020-14445-3
12. Predicting subsurface stormflow response of a forested hillslope – the role of connected flow paths J. Wienhöfer & E. Zehe 10.5194/hess-18-121-2014
13. A modified Green–Ampt model for water infiltration and preferential flow D. Liu et al. 10.2166/nh.2016.160
14. Parametric study of a physically-based, plot-scale hillslope hydrological model through virtual experiments R. Sarkar & S. Dutta 10.1080/02626667.2014.897407
15. Kinematic behaviour of a large earthflow defined by surface displacement monitoring, DEM differencing, and ERT imaging R. Prokešová et al. 10.1016/j.geomorph.2014.06.029
16. Deep Hydraulically‐Active Fractures in Sensitive Clay Deposits: Implications for Groundwater Flow and Slope Stability N. Young et al. 10.1029/2023GL103156
17. 土体-大气相互作用下土质边坡稳定性研究 C. Sun et al. 10.3799/dqkx.2022.275
18. Life and death of slow-moving landslides P. Lacroix et al. 10.1038/s43017-020-0072-8
19. Modelling the impact of deep fractures on groundwater flow and slope stability in post-glacial marine clays (Quebec, Canada) J. Ospina et al. 10.1139/cgj-2023-0463
20. Effects of Anisotropy of Preferential flow on the Hydrology and Stability of Landslides E. Cristiano et al. 10.1016/j.proeps.2016.10.022
21. Unsteady sediment discharge in earth flows: A case study from the Mount Pizzuto earth flow, southern Italy L. Guerriero et al. 10.1016/j.geomorph.2017.07.011
22. Processes and factors controlling the groundwater flow in a complex landslide: A case study in the northern Italy E. Petrella et al. 10.1002/hyp.14891
23. The relationship between the landslide frequency and hydrogeological aspects: a case study from a hilly region in Northern Bavaria (Germany) J. Wiedenmann et al. 10.1007/s12665-016-5451-6
24. Detection of Preferential Water Flow by Electrical Resistivity Tomography and Self-Potential Method K. Kukemilks & J. Wagner 10.3390/app11094224
25. Erosion Failure of Slope in a Dump with Ground Fissure under Heavy Rain Y. Li et al. 10.3390/w14213425
26. A model of hydrological and mechanical feedbacks of preferential fissure flow in a slow-moving landslide D. Krzeminska et al. 10.5194/hess-17-947-2013
27. The influence of preferential flow on pressure propagation and landslide triggering of the Rocca Pitigliana landslide W. Shao et al. 10.1016/j.jhydrol.2016.10.015
28. Characterization of groundwater dynamics in landslides in varved clays J. van der Spek et al. 10.5194/hess-17-2171-2013
29. Shallow slope stability evolution during rainwater infiltration considering soil cracking state J. Zhang et al. 10.1016/j.compgeo.2019.103285
30. Surface temperature controls the pattern of post-earthquake landslide activity M. Loche et al. 10.1038/s41598-022-04992-8
31. Using high-resolution UAV imagery and artificial intelligence to detect and map landslide cracks automatically I. Sandric et al. 10.1007/s10346-024-02295-9
32. Deformation responses of slow moving landslides to seasonal rainfall in the Northern Apennines, measured by InSAR B. Bayer et al. 10.1016/j.geomorph.2018.02.020
33. 3D Discrete Fracture Network Modelling from UAV Imagery Coupled with Tracer Tests to Assess Fracture Conductivity in an Unstable Rock Slope: Implications for Rockfall Phenomena E. Mammoliti et al. 10.3390/rs15051222
34. Characterizing groundwater flow in a translational rock landslide of southwestern China H. Lv et al. 10.1007/s10064-017-1212-3
35. Semiempirical modeling of the transient response of pore pressure to rainfall and snowmelt in a dormant landslide H. Osawa et al. 10.1007/s10346-023-02158-9
36. Multidisciplinary non-invasive investigations to develop a hydrogeological conceptual model supporting slope kinematics at Fontana Cornia landslide, Northern Apennines, Italy A. Aguzzoli et al. 10.1007/s12665-022-10613-4
37. How to Use COMSOL Multiphysics for Coupled Dual-permeability Hydrological and Slope Stability Modeling W. Shao et al. 10.1016/j.proeps.2014.06.018
38. Four‐dimensional imaging of moisture dynamics during landslide reactivation S. Uhlemann et al. 10.1002/2016JF003983
39. Role of Landslides and Lithology in Within-Year Variability of Stream Runoff in Small Forested Catchments in the Outer (Flysh) Carpathians in Poland J. Siwek 10.3390/w17020190
40. Investigation and prediction of water infiltration process in cracked soils based on a full-scale model test Y. Luo et al. 10.1016/j.geoderma.2021.115111
41. Quantifying the morphology of flow patterns in landslide-affected and unaffected soils C. Bogner et al. 10.1016/j.jhydrol.2014.01.063
42. Physically-based landslide prediction over a large region: Scaling low-resolution hydrological model results for high-resolution slope stability assessment S. Wang et al. 10.1016/j.envsoft.2019.104607
43. Precursors of instability in a natural slope due to rainfall: a full-scale experiment A. Askarinejad et al. 10.1007/s10346-018-0994-0
44. Reconstruction of landslide model from ERT, geotechnical, and field data, Nargeschal landslide, Iran S. Rezaei et al. 10.1007/s10064-018-1352-0
45. Corrections of surface fissure effect on apparent resistivity measurements J. Gance et al. 10.1093/gji/ggu453
46. Image-based mapping of surface fissures for the investigation of landslide dynamics A. Stumpf et al. 10.1016/j.geomorph.2012.12.010