Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/7071| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Perriello Zampelli, S.; Dipartimento di Scienze della Terra, Universita` di Napoli Federico II, Naples, Italy | en |
| dc.contributor.authorall | Bellucci Sessa, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | Cavallaro, M. | en |
| dc.date.accessioned | 2011-07-15T11:00:50Z | en |
| dc.date.available | 2011-07-15T11:00:50Z | en |
| dc.date.issued | 2012 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/7071 | en |
| dc.description.abstract | A significant part of Campania is extensively covered by volcaniclastic soils, deriving from the alteration of airfall-sedimented formations of layered ashes and pumices that were ejected by Campi Flegrei and Mt. Somma–Vesuvius during explosive eruptions. Where such soils cover steep slopes cut in carbonate bedrock, landforms depend essentially on the morpho-evolution of such slopes prior to the deposition of the volcaniclastic soils, because these are generally present only as thin veneers, up to a few meters of total thickness. Historical records and local literature testify that, in this part of Campania, landslides that originate on carbonate slopes covered by such soils and terminate at their foot or at gully outlets are frequent, following critical rainfall events. Such landslides can be classified as complex, occurring initially as debris slides, but rapidly evolving into debris avalanches and/or debris flows. The localization of the initial sliding areas (i.e. ‘‘sources’’) on the slopes depends on both the spatial distribution of characters of the soil cover and the spatial distribution of the triggering rainfall events. It therefore appears reasonable to separate the two aspects of the problem and focus on the former one, in order to attempt an assessment of soil sliding susceptibility in the event of landslide-triggering rainfall. In this paper, some results of the application of a method aimed at such an assessment are presented. The method, called SLIDE (from SLiding Initiation areas DEtection), is based on the concept that, for a spatially homogeneous soil cover and a spatially homogeneous landslide-triggering rainfall sequence, different values of threshold slope gradient for limit equilibrium conditions exist, depending on morphological characters of the soil cover, such as its continuity and planform curvature. The method is based on the assessment of (1) soil cover presence, (2) discontinuities within soil cover, (3) slope gradients and curvature, by means of good resolution DEMs. It has been applied to sample carbonate slopes of Campania, where landslides originated either repeatedly or recently. Results are encouraging, and a soil sliding susceptibility map of a large area, based on a simplified version of method, is also presented. | en |
| dc.language.iso | English | en |
| dc.publisher.name | Springer | en |
| dc.relation.ispartof | Natural Hazards | en |
| dc.relation.ispartofseries | 1/61(2012) | en |
| dc.subject | Debris-slide susceptibility | en |
| dc.subject | Volcaniclastic soil cover | en |
| dc.subject | Soil cover discontinuities | en |
| dc.subject | Planform curvature | en |
| dc.title | Application of a GIS-aided method for the assessment of volcaniclastic soil sliding susceptibility to sample areas of Campania (Southern Italy) | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 155-168 | en |
| dc.subject.INGV | 05. General::05.08. Risk::05.08.02. Hydrogeological risk | en |
| dc.identifier.doi | 10.1007/s11069-011-9807-7 | en |
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National Academy Press, Washington DC, pp 129–176 Sorbino G, Sica C, Cascini L (2010) Susceptibility analysis of shallow landslides source areas using physically based models. Nat Hazards 53:313–332 Zevenbergen LW, Thorne CR (1987) Quantitative analysis of land surface topography. Earth Surf Process Landforms 12:47–56 | en |
| dc.description.obiettivoSpecifico | 5.5. TTC - Sistema Informativo Territoriale | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | reserved | en |
| dc.contributor.author | Perriello Zampelli, S. | en |
| dc.contributor.author | Bellucci Sessa, E. | en |
| dc.contributor.author | Cavallaro, M. | en |
| dc.contributor.department | Dipartimento di Scienze della Terra, Universita` di Napoli Federico II, Naples, Italy | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Dipartimento di Scienze della Terra, Universita` di Napoli Federico II, Naples, Italy | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.orcid | 0000-0003-2521-6476 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 05. General | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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| Perriello_et_alii.pdf | 1.16 MB | Adobe PDF |
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