Antonello Troncone

Prof. Dr. Antonello Troncone

University of Calabria
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Research Focus & Metrics

Academic Career Length

22Years (2005-Present)

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

Representative Publications

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1 October 2005 in Géotechnique
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Journal Article
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ATAntonello Troncone
Antonello Troncone
The results of an analysis concerning a landslide of great dimensions, which occurred at Senise (Southern Italy) on 26 July 1986, are presented. The landslide was of a translational type, and the failure developed within a thin clayey silt layer interbedded by a slightly cemented sand formation. Both these soils experienced a pronounced strain-softening behaviour during laboratory tests. From the analyses performed using the traditional limit equilibrium approach, it has been found that the average operational resistance along the sliding surface was less than that of the peak and greater than the residual resistance deduced from the laboratory tests. As a consequence, it has been postulated that a progressive failure had occurred. Such a failure process can be appropriately studied using methods that are capable of simulating the formation and development of shear zones, where strain is localised. From a computational point of view this presents many difficulties, because the numerical procedures currently used are very often affected by a lack of convergence, and the solution may depend strongly on the mesh adopted. In order to overcome these numerical drawbacks, in the present study use is made of both an elasto-viscoplastic constitutive model and a nonlocal elasto-viscoplastic model implemented in a finite element code. The Mohr–Coulomb plastic law is adopted, and the strain-softening behaviour of the soil is simulated by reducing the strength parameters with the accumulated deviatoric plastic strains. The results of the analysis show that a progressive failure occurred owing to deep excavations carried out at the toe of the slope. In addition, the soil mass involved in the sliding and the location of the failure surface deduced from the numerical simulation are found to be very similar to those observed.

1 July 2010 in Computers and Geotechnics
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Journal Article
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ECE. Conte
E. Conte
Francesco SilvestriFrancesco Silvestri
Francesco Silvestri
ATAntonello Troncone
Antonello Troncone


1 April 2019 in Engineering Geology
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Journal Article
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ECEnrico Conte
Enrico Conte
LPLuigi Pugliese
Luigi Pugliese
ATAntonello Troncone
Antonello Troncone

16 March 2016 in Landslides
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Journal Article
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ECEnrico Conte
Enrico Conte
ADAntonio Donato
Antonio Donato
ATAntonello Troncone
Antonello Troncone

1 November 2006 in Canadian Geotechnical Journal
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Journal Article
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ECEnrico Conte
Enrico Conte
ATAntonello Troncone
Antonello Troncone
This paper presents an analytical solution for the analysis of one-dimensional consolidation of saturated soil layers subjected to general time-dependent loading. A simple calculation procedure that makes use of the Fourier series is proposed for practical applications. Both single loads and cyclic loads can be considered by choosing a suitable period for the Fourier series. A number of comparisons with existing theoretical solutions are shown to assess the accuracy of the proposed procedure. Moreover, the experimental results from oedometer tests performed in the present study and from a well-documented case history concerning a large embankment constructed on compressible soils are analysed using this solution to evaluate the coefficient of consolidation of the soil.Key words: one-dimensional consolidation, time-dependent loading, excess pore-water pressure, theoretical solution, Fourier series.