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Featured researches published by P. Messina.


Near Surface Geophysics | 2007

Geophysical investigations at the Himera archaeological site, northern Sicily

Patrizia Capizzi; Pietro Cosentino; Gianluca Fiandaca; R. Martorana; P. Messina; S. Vassallo

In this paper we present a geophysical survey that was carried out as a research activity during field trips to the Himera archaeological site, where relics of a large Greek settlement are still buried, effected by a joint group of archaeologists and geophysicists during an educational project. Two-dimensional (2D) resistivity and ground-penetrating radar (GPR) surveys were performed to locate buried archaeological structures at this archaeological site. The results of the GPR surveys show some anomalies characterized by semi-hyperbolic shapes. In some restricted areas of the town, two grids of parallel GPR profiles were acquired while time- and depth-slices were calculated to identify the extension of the buried structures. In fact, the shapes of many anomalies recognized in the slices seem to describe the distribution of the relics (i.e. walls, roads, etc.). A 2D electrical resistivity profile showed clear anomalies, which were connected with wall-like relics. This was also obtained by using on-site calibration on partially uncovered structures, while the low background resistivity values were interpreted as representing river deposits having different moisture characteristics. Recommendations were also given to the archaeological site-excavators, following which some of the results were confirmed by subsequent archaeological excavations.


Near Surface Geophysics | 2012

Geophysical and geotechnical investigations to support the restoration project of the Roman ‘Villa del Casale’, Piazza Armerina, Sicily, Italy

R. Capizzi; R. Martorana; P. Messina; Pietro Cosentino

A multidisciplinary geophysical and geotechnical study, including some non-invasive geophysical applications, was carried out during the restoration of the ‘Villa del Casale’, a Roman villa discovered near Piazza Armerina (Sicily, Italy) in 1929, famous for its Roman floor mosaics. The project aims were to characterize the geology of the subsoil and provide information for solving the main building structural problems including the subsidence of some parts of the floor and the detachment of the tesserae (i.e., the tiles) of the mosaics. Another goal was the detailed study of the underground structures of the Corridor of the Great Hunt, a part of the villa strongly affected by subsidence and detachment of mosaics. The acquisition of geotechnical and geophysical surveys, including core drillings, time-domain electromagnetic (TDEM) soundings, downhole seismic logs and a seismic refraction profile, allowed the reconstruction of the geometry of geological formations below the villa to be ascertained, especially with regard to the top of the bedrock. The results suggest the presence of a buried riverbed that has been identified as the main cause of the villa floor subsidence. The study of the Corridor of the Great Hunt involved full 3D electrical resistivity tomography (ERT) and 3D ground-penetrating radar (GPR) data acquisition using 100 MHz, 400 MHz and 1600 MHz antennas, as well as the above mentioned refraction seismic profile. Data acquisition required the use of special non-invasive sensors to avoid any damage to the mosaics. The integrated inversion of all the data and the comparison between the resulting 3D resistivity model and 400 MHz GPR depth-slices allowed the identification of many shallow anomalies to be identified, including some pipes for water drainage and a reinforced concrete basement placed under the floor during a previous restoration intervention. 100 MHz GPR profiles validated the results of the seismic refraction profile model. Finally, 1600 MHz GPR depth-slices, in the most subsided zone, allowed the location of air bubbles under the mosaic to be identified. This work shows that the integrated use of different geophysical techniques for archaeological purposes, especially if constrained by direct explorations, greatly reduced the intrinsic uncertainties of each method. Moreover, customizing standard geophysical equipment to avoid any damage is essential when working on protected cultural heritage.


International Journal of Geophysics | 2011

From Geophysics to Microgeophysics for Engineering and Cultural Heritage

Pietro Cosentino; Patrizia Capizzi; R. Martorana; P. Messina; Salvatore Schiavone

The methodologies of microgeophysics have been derived from the geophysical ones, for the sake of solving specific diagnostic and/or monitoring problems regarding civil engineering and cultural heritage studies. Generally, the investigations are carried out using different 2D and 3D tomographic approaches as well as different energy sources: sonic and ultrasonic waves, electromagnetic (inductive and impulsive) sources, electric potential fields, and infrared emission. Many efforts have been made to modify instruments and procedures in order to improve the resolution of the surveys as well as to significantly reduce the time of the measurements without any loss of information. This last point has been achieved by using multichannel systems. Finally, some applications are presented, and the results seem to be very promising and promote this new branch of geophysics. Therefore, these methodologies can be used even more to diagnose, monitor, and safeguard not only engineering buildings and/or large structures, but also ancient monuments and cultural artifacts, such as pottery, statues, and so forth.


Archive | 2007

Study And Monitoring Of Salt Water Intrusion In The Coastal Area Between Mazara Del Vallo And Marsala (South-Western Sicily)

Pietro Cosentino; Patrizia Capizzi; Gianluca Fiandaca; R. Martorana; P. Messina; S. Pellerito

In this chapter the study of a coastal aquifer located in South-Western Sicily (between the towns of Marsala and Mazara del Vallo) is presented, carried out using geochemical, hydro-geological and geophysical techniques. The aquifer has been over-exploited to the point of being subject to intense and worrisome salt-water intrusion.A preliminary chemical and physical characterization of the waters was carried out; this included measuring their conductivity and their chloride content. This allowed to detect the marine intrusion wedge in the coastal aquifer. A series of electromagnetic soundings, suitably calibrated by well logs, were effected in the whole area and allowed to create a 3D interpretative model of the resistivity distribution in the aquifer, thereby enabling to recognize the main intrusion directions and the pattern of the aquifer bed. Furthermore an integrated geophysical 2D section was carried out along a line roughly perpendicular to the coast, in one of the zones that is particularly involved in the intrusion phenomenon. Field measures included ERT, IP, TDEM and seismic soundings, all of which were aimed at reconstructing a highly detailed geophysical section. The seismic soundings clearly show the lateral variation between the fresh and salt water, such as the overburden and the clayey bed of the aquifer. The final target of this research is to propose an optimized management-model of underground resources. The lessons drawn from the use of different techniques for defining geophysical profiles suggest an integrated methodology to identify in detail the sea intrusion zone in aquifers. Therefore, the methodology used can be suitably extended and exported for studing and monitoring many similar Mediterranean coastal areas


Near Surface 2009 - 15th EAGE European Meeting of Environmental and Engineering Geophysics | 2009

3D ERT for the Study of an Ancient Wall Covered by Precious Mosaics

Gianluca Fiandaca; R. Martorana; P. Messina; Pietro Cosentino

The DC electrical tomography (ERT) is still a method scarcely diffused for the study of masonry of recent and ancient buildings, in spite of the very high resolution power of this methodology. The major limitation on ERT applicability on precious surfaces (like masonries or floors with fresco or mosaic covering) depends on the method of current injection: usually it is necessary to drive electrodes (small nails) into small perforations on the surfaces, to obtain sufficiently high current values (to produce good signal to noise ratio). An interesting application of the MYG array (that reduces significantly, compared to other classical arrays, the number of electrodes utilized for current injection) has been carried out on a wall of the fountain room of the Zisa Palace (Palermo, XII century A.D.), covered by a mosaic wall suffering important detachment of tesserae due to internal moisture. The results seem to suggest that ERT investigation with the MYG array has important applicative potentiality in study of precious walls or floors in artistic buildings, because of the low-invasivity and high resolution power as well as velocity of acquisition.


Near Surface 2008 - 14th EAGE European Meeting of Environmental and Engineering Geophysics | 2008

Integrated Full 3D Geoelectrical and GPR Tomographies in the Ambulatory of the Roman "Villa Del Casale", Piazza Armerina

Pietro Cosentino; Patrizia Capizzi; Gianluca Fiandaca; R. Martorana; P. Messina; I. Razo Amoroz

The “Villa del Casale” is a wonderful Roman Villa excavated in the archaeological site of Piazza Armerina (Sicily) in 1929. Its interest is mainly to be referred to the floor mosaics, among the largest and most beautiful ones of Roman times, of superlative quality. The floor of the Corridor is covered by a wonderful mosaic depicting the hunt and capture of wild animals, so that it is called the “Corridor of the Great Hunting Scene”. The Villa is now under restoration, and during the planning of the restoration a 3D electrical resistivity tomography was performed on the corridor by using an acquisition grid composed by 704 electrodes. Furthermore 25 GPR profiles with 400 MHz antenna were acquired. The 3D ERT survey was carried out by utilizing a new 3D array, named “Maximum Yield Grid” (MYG), that allows a great decrease of the acquisition time and of the invasivity of the ERT investigation in respect of classical arrays. The results show shallow anomalies, that correspond to the canalizations for water drainage and to the concrete basement built below the corridor during a previous restoration intervention, and a diminution of resistivity with depth, related to the aquifer below the Villa.


Current Analytical Chemistry | 2010

Identification of Precious Artefacts: The Sonic Imprint for Small Artefacts

Pietro Cosentino; Patrizia Capizzi; Gianluca Fiandaca; R. Martorana; P. Messina; Isaac Razo Amoroz

Identification of artworks is mainly based on a few characteristics which can be observed using non-invasive tools (sight, touch, simple instruments), the investigated properties being geometry, weight, colours, texture, etc. Nowadays, technology allows reproducing all these characteristics to such an extent that even expert conservators can be deceived: in particular at the present time even the geometry of an artwork can be easily reproduced with the help of laser scanner analysis and with a rapid prototyping machine or a computer numerical control (CNC) milling machine. We propose a new tool, the Sonic Imprint, producing a code capable of identifying a rigid artefact from its vibrational resonance frequencies beyond doubt. In fact the vibration modes of an artefact strongly depend on the spatial distributions of its density and elastic parameters, as well as on its internal defects, definable in terms of abrupt changes of elastic properties in a small portion of the object. Then even small differences of these properties (differences usually present even among “identical” objects produced with industrial methods, at least in terms of defects) give appreciable variations of the Sonic Imprint codes, allowing secure identification of artworks, prevention of clonation and even damage monitoring. Moreover the procedure is really robust, rapid, inexpensive and not invasive. We tested it on a large number of commercial objects with the same shape and dimension and on many artworks in archaeological museums: an example is described. The application of this methodology to small-size artefacts (from small stones, vessels, pottery to medium-large coins) involves some problems in the detection of the Sonic Imprint. The problems, just due to the smaller sizes of this kind of objects, arise from the presence of higher resonance frequencies and larger damping of the induced vibrations. This implies that probes and instrumentation should be replaced to be adapted to the new experimental conditions.


Journal of Earth Science | 2009

Advances in microgeophysics for engineering and cultural heritage

Pietro Cosentino; Patrizia Capizzi; Gianluca Fiandaca; R. Martorana; P. Messina


Journal of the Acoustical Society of America | 2013

Method of detecting a sonic imprint of a three dimensional object and related apparatus

Pietro Cosentino; Gianluca Fiandaca; P. Messina; R. Martorana; Patrizia Capizzi; Isaac Razo Amoroz


Bollettino Di Geofisica Teorica Ed Applicata | 2010

Integrated hydrogeochemical and geophysical surveys for a study of sea-water intrusion

Mariano Valenza; Gianluca Fiandaca; Patrizia Capizzi; Dario Cellura; Pietro Cosentino; R. Martorana; P. Messina; Salvatore Schiavone

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F Loddo

University of Cagliari

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Carlo Piga

University of Cagliari

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