http://www.cnr.it/ontology/cnr/individuo/prodotto/ID41582
Landslide triggering scenarios in homogeneous geological contexts: The area surrounding Acri (Calabria, Italy) (Articolo in rivista)
- Type
- Label
- Landslide triggering scenarios in homogeneous geological contexts: The area surrounding Acri (Calabria, Italy) (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.geomorph.2006.09.021 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Terranova O.; Antronico L.; Gullà G.; (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Titolo
- Landslide triggering scenarios in homogeneous geological contexts: The area surrounding Acri (Calabria, Italy) (literal)
- Abstract
- The paper describes a methodology to detect landslide triggering scenarios in geological homogeneous areas and for some
specific landslide categories. In these scenarios, the rainfall-landslide relationship as well as the pluviometric load conditions
influencing slope instability have to be investigated.
The methodology is applied to an area located in northern Calabria (Italy) and affected by widespread and different slope
instability phenomena. Outcropped, fractured, and deeply weathered crystalline rock masses, determining geologic homogeneous
conditions, are present. In the same area, suitable and homogeneous climatic features have also been found.
According to the methodology adopted, the hydrologic analysis of rainfall time-series is initially carried out notwithstanding
historical data concerning landslide mobilization, but using simple models to determine critical pluviometric scenarios for the three
landslide categories: shallow, medium-deep, and deep. Landslide-triggering scenarios individualized according to this procedure
are less significant as compared to the landslide mobilization detected in the study area by means of historical research and ascribed
to the three landslide categories according to geomorphologic analysis.
Subsequently, the possible landslide triggering scenarios are outlined by carefully investigating the hydrologic analysis limited
to the periods identified according to the historical data.
In the study area and approximately for all the areas characterized by the outcrop of fractured and deeply weathered crystalline
rocks, significant triggering scenarios can be outlined. In particular, shallow landslide triggers could be activated by rainfall events
with intensities exceeding 90 mm/day and/or with amounts exceeding 160 mm. As for medium-deep and deep landslides,
triggering mechanisms are more complicated; and effective rainfall contribution must be taken into account compared to
groundwater storage. Moreover, a more complex link between deep landslides and precipitation is confirmed.
The results obtained to date highlight the potential of this methodology, which enables us to define and progressively improve
the knowledge framework by means of a work sequence integrating different disciplinary tools and results. (literal)
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