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Natural Hazards and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 4 | Copyright

Special issue: Rockfall protection – from hazard identification to mitigation...

Nat. Hazards Earth Syst. Sci., 9, 1119-1131, 2009
https://doi.org/10.5194/nhess-9-1119-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  15 Jul 2009

15 Jul 2009

Towards rockfall forecasting through observing deformations and listening to microseismic emissions

D. Arosio1, L. Longoni2, M. Papini2, M. Scaioni3, L. Zanzi1, and M. Alba2 D. Arosio et al.
  • 1Dipartimento di Ingegneria Strutturale, Politecnico di Milano, Piazza L. da Vinci 32, 20133 Milano, Italy
  • 2Dipartimento di Ingegneria Idraulica, Ambientale, Infrastrutture Viarie, Rilevamento, Politecnico di Milano, Piazza L. da Vinci 32, 20133 Milano, Italy
  • 3Dipartimento di Scienza e Tecnologie dell'Ambiente Costruito, Politecnico di Milano, Via Bonardi 3, 20133 Milano, Italy

Abstract. Reliable forecasting of rockfall is a challenging task, mainly because of the lack of clearly noticeable forerunners as well as due to the geological and geo-mechanical complexity of the rock movements involved. Conventional investigation devices still present some drawbacks, since most measurements are generally carried out at isolated locations as well as on the surface only. Novel remote-sensing monitoring instruments, such as Terrestrial Laser Scanning (TLS) and Ground-Based Interferometric Synthetic Aperture Radars (GB-InSAR), are capable of inspecting an unstable slope with a high spatial and temporal frequency. But they still rely on measurements of the failure surface, from which displacement or velocity are measured. On the contrary, acoustic emission/microseismic monitoring may provide a deeper insight of stress and strain conditions within the sub-surface rock mass. In fact, the capability to detect microseismic events originating within an unstable rock mass is a key element in locating growing cracks and, as a consequence, in understanding the slide kinematics and triggering mechanisms of future collapses. Thus, a monitoring approach based on the combination of classical methodologies, remote sensing techniques and microseismic investigations would be a promising research field. In the present paper we discuss the technologies and we illustrate some experiments conducted in the framework of a project whose final goal is the installation of an integrated monitoring and alerting system on a rockface nearby Lecco (Italy). In particular, we present a review of performances and applications of remote sensing devices and some results concerning a terrestrial laser scanner preliminary campaign. Then, we report findings regarding amplitude, frequency content and rate of signals recorded during an in situ test carried out to evaluate the performance of three different microseismic transducers.

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