Published in

Landslide Science and Practice, p. 445-449

DOI: 10.1007/978-3-642-31445-2_58

Links

Tools

Export citation

Search in Google Scholar

Use of the seismic dilatometer (SDMT) in landslide research and practice

Proceedings article published in 2011 by Sara Amoroso ORCID, Ferdinando Totani, Gianfranco Totani
This paper is available in a repository.
This paper is available in a repository.

Full text: Download

Green circle
Preprint: archiving allowed
Green circle
Postprint: archiving allowed
Red circle
Published version: archiving forbidden
Data provided by SHERPA/RoMEO

Abstract

This paper shows the use of the seismic dilatometer (SDMT) testing (Marchetti J Geotech Eng Division, 106:299-321, 1980; Marchetti et al. Proceedings of 2nd international flat dilatometer conference, Washington, DC, pp 7-48, 2001, In Situ tests by Seismic Dilatometer (SDMT), pp 109-138, 2008) in landslide diagnosis and monitoring. The quick KD-DMT method, developed by Totani et al. (1997) for detecting active or old slip surfaces, was recently applied in a research programme on stability conditions of natural slopes shaped in colluvial cover formations in Abruzzo region (Chieti, Teramo). The paper illustrates the capability of SDMT to identify remoulded zones, symptom of instability, and slip surfaces in the investigated slopes. Moreover, the paper presents the possibility to use the DMT blade as a piezometer, to monitor rapidly the variation of the ground water level in relation to weather trend.