Diego Di Martire

Dr. Diego Di Martire

University of Naples Federico II Department of Earth, Environment and Resources Sciences
+1
orcid

Research Focus & Metrics

Academic Career Length

15Years (2012-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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17 April 2020 in Landslides
Verified
Journal Article
Closed access
PDF file
Mariano Di NapoliMariano Di Napoli
Mariano Di Napoli
FCFrancesco Carotenuto
Francesco Carotenuto
ACAndrea CEVASCO
Andrea CEVASCO
Pierluigi ConfuortoPierluigi Confuorto
Pierluigi Confuorto
Diego Di MartireDiego Di Martire
Diego Di Martire
Domenico CalcaterraDomenico Calcaterra
Domenico Calcaterra

1 May 2014 in Remote Sensing of Environment
Verified
Journal Article
Closed access
Diego Di MartireDiego Di Martire
Diego Di Martire
RIRuben Iglesias
Ruben Iglesias
DMDani Monells
Dani Monells
GCGiuseppe Centolanza
Giuseppe Centolanza
SSStefania Sica
Stefania Sica
DCDomenico Calcaterra
Domenico Calcaterra

1 January 2017 in Remote Sensing of Environment
Verified
Journal Article
Open access
Pierluigi ConfuortoPierluigi Confuorto
Pierluigi Confuorto
Diego Di MartireDiego Di Martire
Diego Di Martire
GCGiuseppe Centolanza
Giuseppe Centolanza
RIRuben Iglesias
Ruben Iglesias
JMJordi J. Mallorqui
Jordi J. Mallorqui
DCDomenico Calcaterra
Domenico Calcaterra
Persistent Scatterers Interferometry (PSI) represents one of the most powerful techniques for Earth's surface deformation processes' monitoring, especially for long-term evolution phenomena. In this work, a dataset of 34 TerraSAR-X StripMap images (October 2013–October 2014) has been processed by two PSI techniques - Coherent Pixel Technique-Temporal Sublook Coherence (CPT-TSC) and Small Baseline Subset (SBAS) - in order to study the evolution of a slow-moving landslide which occurred on February 23, 2012 in the Papanice hamlet (Crotone municipality, southern Italy) and induced by a significant rainfall event (185 mm in three days). The mass movement caused structural damage (buildings' collapse), and destruction of utility lines (gas, water and electricity) and roads. The results showed analogous displacement rates (30–40 mm/yr along the Line of Sight – LOS-of the satellite) with respect to the pre-failure phase (2008–2010) analyzed in previous works. Both approaches allowed detect the landslide-affected area, however the higher density of targets identified by means of CPT-TSC enabled to analyze in detail the slope behavior in order to design possible mitigation interventions. For this aim, a slope stability analysis has been carried out, considering the comparison between groundwater oscillations and time-series of displacement. Hence, the crucial role of the interaction between rainfall and groundwater level has been inferred for the landslide triggering. In conclusion, we showed that the integration of geotechnical and remote sensing approaches can be seen as the best practice to support stakeholders to design remedial works.Peer ReviewedPostprint (author's final draft

13 February 2021 in Water
Verified
Journal Article
Open access
PDF file
Mariano Di NapoliMariano Di Napoli
Mariano Di Napoli
Diego Di MartireDiego Di Martire
Diego Di Martire
GBGiuseppe Bausilio
Giuseppe Bausilio
Domenico CalcaterraDomenico Calcaterra
Domenico Calcaterra
Pierluigi ConfuortoPierluigi Confuorto
Pierluigi Confuorto
ACAndrea CEVASCO
Andrea CEVASCO
Rainfall-induced shallow landslides represent a serious threat in hilly and mountain areas around the world. The mountainous landscape of the Cinque Terre (eastern Liguria, Italy) is increasingly popular for both Italian and foreign tourists, most of which visit this outstanding terraced coastal landscape to enjoy a beach holiday and to practice hiking. However, this area is characterized by a high level of landslide hazard due to intense rainfalls that periodically affect its rugged and steep territory. One of the most severe events occurred on 25 October 2011, causing several fatalities and damage for millions of euros. To adequately address the issues related to shallow landslide risk, it is essential to develop landslide susceptibility models as reliable as possible. Regrettably, most of the current land-use and urban planning approaches only consider the susceptibility to landslide detachment, neglecting transit and runout processes. In this study, the adoption of a combined approach allowed to estimate shallow landslide susceptibility to both detachment and potential runout. At first, landslide triggering susceptibility was assessed using Machine Learning techniques and applying the Ensemble approach. Nine predisposing factors were chosen, while a database of about 300 rainfall-induced shallow landslides was used as input. Then, a Geographical Information System (GIS)-based procedure was applied to estimate the potential landslide runout using the “reach angle” method. Information from such analyses was combined to obtain a susceptibility map describing detachment, transit, and runout. The obtained susceptibility map will be helpful for land planning, as well as for decision makers and stakeholders, to predict areas where rainfall-induced shallow landslides are likely to occur in the future and to identify areas where hazard mitigation measures are needed.

12 April 2012 in Natural Hazards and Earth System Sciences
Verified
Journal Article
Open access
PDF file
Diego Di MartireDiego Di Martire
Diego Di Martire
MRM. De Rosa
M. De Rosa
VPV. Pesce
V. Pesce
MSM. A. Santangelo
M. A. Santangelo
Domenico CalcaterraDomenico Calcaterra
Domenico Calcaterra
Results deriving from a research focused on the interplay between landslides and urban development are presented here, with reference to two densely populated settings located in the Campania region, Italy: the city of Naples and the island of Ischia. Both areas suffer adverse consequences from various types of landslides since at least 2000 yr. Our study evidences that, despite the long history of slope instabilities, the urban evolution, often illegal, disregarded the high landslide propensity of the hillsides; thus, unsafe lands have been occupied, even in recent years, when proper and strict rules have been enacted to downgrade the landslide risk. It is finally argued that future guidelines should not be entirely based upon physical countermeasures against mass movements. On the contrary, national and local authorities should enforce the territorial control, obliging citizens to respect the existing regulations and emphasizing the role of alternative, non-structural solutions.

1 February 2016 in CATENA
Verified
Journal Article
Closed access
Diego Di MartireDiego Di Martire
Diego Di Martire
STSerena Tessitore
Serena Tessitore
DBDomenico Brancato
Domenico Brancato
MCMaria Grazia Ciminelli
Maria Grazia Ciminelli
SCSalvatore Costabile
Salvatore Costabile
DCDomenico Calcaterra
Domenico Calcaterra