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Slope sliding as secondary process in subsidence areas of chloride-karst

Glissements, procédés secondaires dans les régions de chloride-karst

  • Theme 1 Systematic Reconnaissance Mapping and Registration of Slope Movements. Estimation of Risks Dueto Landslides. Influence of Geological and Climatic Conditions on Slope Instability Methods and Economic Importance of the Registration of Slope Movements
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Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur Aims and scope Submit manuscript

Summary

Damage to terrain and buildings which occurs on the flanks of subsidences cannot always be explained by the conception of a sinking trough model. Such damage shows features related to slope sliding. An exact proof of the process on the basis of soil mechanics will be given in subsequent papers.

Résumé

Sur les flancs de vallons d’affaissement, apparaissent en partie des accidents de terrain et de constructions, qui ne peuvent pas être expliqués sur la base de model d’auge d’affaissement. Ils montrent des apparitions de convergence sur les mouvements de pentes. Une démonstration exacte sur la base de la mécanique du sol doit être mise en évidence par les prochains travaux.

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References

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Bergakademie Freiberg, Sektion Geotechnik und Bergbau, 92 Freiberg

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Reuter, F., Molek, H. & Bochmann, G. Slope sliding as secondary process in subsidence areas of chloride-karst. Bulletin of the International Association of Engineering Geology 16, 62–64 (1977). https://doi.org/10.1007/BF02591448

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  • DOI: https://doi.org/10.1007/BF02591448

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