Articles | Volume 22, issue 7
https://doi.org/10.5194/nhess-22-2219-2022
https://doi.org/10.5194/nhess-22-2219-2022
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, Thomas Zieher, Jan Schmieder, Thom Bogaard, Martin Rutzinger, and Christoph Spötl

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Cited articles

Binet, S., Jomard, H., Lebourg, T., Guglielmi, Y., Tric, E., Bertrand, C., and Mudry, J.: Experimental analysis of groundwater flow through a landslide slip surface using natural and artificial water chemical tracers, Hydrol. Process., 21, 3463–3472, https://doi.org/10.1002/hyp.6579, 2007. a, b
Blasch, K. W. and Bryson, J. R.: Distinguishing Sources of Ground Water Recharge by Using δ2H and δ18O, Groundwater, 45, 294–308, https://doi.org/10.1111/j.1745-6584.2006.00289.x, 2007. a, b
Bogaard, T., Guglielmi, Y., Marc, V., Emblanch, C., Bertrand, C., and Mudry, J.: Hydrogeochemistry in landslide research: a review, Bulletin de la Société Géologique de France, 178, 113–126, https://doi.org/10.2113/gssgfbull.178.2.113, 2007. a
Bogaard, T. A. and Greco, R.: Landslide hydrology: from hydrology to pore pressure, WIREs Water, 3, 439–459, https://doi.org/10.1002/wat2.1126, 2016. a
Bonzanigo, L., Eberhardt, E., and Loew, S.: Long-term investigation of a deep-seated creeping landslide in crystalline rock. Part I. Geological and hydromechanical factors controlling the Campo Vallemaggia landslide, Can. Geotech. J., 44, 1157–1180, https://doi.org/10.1139/T07-043, 2007. a
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The activity of slow-moving deep-seated landslides is commonly governed by pore pressure...
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