EGG - Exploration Geophysics Group

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About EGG

We are a research group in the Department of Geological, Environmental and Marine Sciences, University of Trieste. Our areas of interest lie mainly in the use of geophysical surveying to investigate the nature of the Earth's crust. Much of our research is directly applicable and is actually applied to solve problems in archaeology, hydrocarbon exploration, engineering and environmental investigation.

We have recently participated in the following major field experiments:

-Onshore and offshore NVR and WARR seismic surveys off the Pacific Coast of the Antarctic Peninsula.
-Onshore and offshore NVR and WARR seismic surveys off the Italian Coast [National Research Programme Deep
Crust (CROP) for which our group is scientific responsible and coordinator of the marine leg].
-Offshore NVR seismic surveys in the Ross Sea and Scotia Sea areas (Antarctica).
-Ground Penetrating Radar multi-fold 2-D and 3-D surveys of LNAPL contaminated areas (project supported by the

National Fund for the Protection against Industrial, Chemical and Ecological Hazards)
-Ground Penetrating Radar multi-fold 2-D and 3-D surveys of archaeological sites in Italy (project supported by the

National Cultural Heritage Research Programme).
-Ground Penetrating Radar multi-fold 2-D and 3-D surveys of archaeological sites in Kazakhstan, Peru', Israel (international scientific programmes).
-Integrated Acoustic - Ground Penetrating Radar survey of the Cheko Lake in Russia (international scientific programme).
-Ground Penetrating Radar multi-fold 2-D and 3-D surveys to locate shallow subsurface utilities in hostile soil conditions (Venice and Trieste area, national research programme).

We also actively research the theoretical aspects of seismic and georadar exploration of the crust. Some of our current areas of interest include multiple attenuation, AVO analysis and theoretical models for EM wave propagation, polarization analysis applied to GPR, depth imaging in thrust belt areas.

A wide range of research projects are underway, funded by a variety of sources including; CNR, MURST, the European Union, the Cultural Heritage Ministry.

NEAR SURFACE AND GPR RESEARCH GROUP

Our areas of interest lie mainly in the use of georadar and acoustic techniques to investigate the nature of the Earth's shallow crust. Our current major field experiments and theoretical research activities focus on the study of archaeological and contaminated (LNAPL) sites and on the location of shallow subsurface utilities (pipes, cables) in hostile soil conditions. Further research topics are:
-Fresh water basins high resolution surveys.
-Fracture location in metric size stone blocks from quarries.
-Joint palaeontological-geophysical study of unconformities (e.g. Cretaceous-Tertiary in carbonate platforms).
-Study of the strike-slip deformation of the Northern Victoria Land Antarctica from land GPR and marine seismic data.
-Humanitarian Demining.

We have seismic and GPR instruments and most of the processing and interpretation software we use is developed in house. Our processing centre is equipped with a state-of-the-art network of servers and workstations.

Our research projects:
The following research projects are based on the theoretical and methodological research of our group in the field of multi-fold/multi-offset GPR data processing and interpretation.

1. CULTURAL HERITAGE
a. Italy

The National Cultural Heritage Research Programme and several Archaeological Suprintendencies from all over Italy support our research work on the development and application of multi-fold GPR techniques to study archaeological sites. Since the beginning of our research activity in this field (1993), we have successfully completed more than 30 2-D/3-D multi-fold studies. A large part of them was followed by archaeological excavation which validated the interpretation of the GPR profiles. Figs.1 and 2 show two examples from recent surveys of the Aquileia Archaeological Park in northern Italy.
b. Kazakhstan
We participated in a international archaeological-geophysical expedition to southern Kazakhstan. Two tombs of the Iron Age (Saka period) were discovered and successfully excavated based on the results of the multi-fold GPR profiles (Fig.3).
c. Peru'
The objective of the 1998 expedition to northern Peru' was the study of large pyramids of the Moche culture. A new important discovery was made after the georadar surveys of the Sipan site (Fig.4).
d. Israel

This project aims at the study of two archaeological sites (Khirbet Ain Fattir and Khirbet Jiljil) where documentary evidences indicate the likely location of important necropolises. The first expedition was completed during summer 1999 and the results will be shortly issued.

2. CONTAMINANTS
The project aims at the development and application of Ultra-High-Resolution (UHR) GPR techniques to detect liquid contaminants and monitor their diffusion. The research focusses on field experiments, development of processing tools suited to image discontinuities rapidly varying in time and space, theoretical study of the variations of the reflection coefficients betweeen water and LNAPL saturated soils, simulations and laboratory measurements. Several 4-D GPR multifold experiments have been carried out to date. An example of the results obtained during controlled injection of 100 litres of gasoline is shown in Fig. 5. Joint ultra-shallow seismic experiments with an innovative source were recently completed and the data are currently being processed.

3. UTILITIES

A large project is being carried out with the support of an industrial consortium. The aim is the high resolution mapping of shallow (30 to 80 cm) subsurface utilities buried in clayey soils. After preliminary tests to assess the penetration limits of the high frequency radar waves, necessary to image such shallow targets, an extensive 3-D programme has been carried out. The focus from the processing standpoint is in the development of ad hoc deconvolution algorithms to enhance the vertical resolution in highly dispersive media. Fig.6 shows an example of the results of a blind test with the actual location of the searched for utilities.

4. FRACTURES
The research is supported by the local industry and aims at the study of large volumes of stone scheduled to be cut. The results obtained to date allow high resolution imaging of discontinuities associated to bedding and fracture.

5. WATER BASINS
Several surveys were performed in lakes and rivers of our region to test the sub-bottom imaging potential of GPR and develop processing techniques suited for the high resolution shallow stratigraphy study. The next step on this research topic is the integration of acoustic techniques and GPR to improve resolution and penetration and perform a joint inversion of the elastic and electric parameters of the ground. On the basis of such experiments, we were invited to survey a lake at the Tunguska Meteorite Site (Russia) in the framework of an international expedition to the area. The first results of such expedition have been published in the proceedings of the international conference on Ground Penetrating radar GPR2000 (Australia).

6. ANTARCTICA
A joint seismic-GPR exploration project is being carried out to reconstruct the subglacial topography and the main geomorphological and geological features related to the Meso-Cenozoic evolution of the Northern Victoria Land (Antarctica). Such reconstruction is of interest to correlate the offshore structural features, to study the projections of the regional transform faults of the Southern Ocean, to study the Meso-Cenozoic magmatic activity and the evolution of the East Antarctic ice sheet (Pacific Sector).

7. HUMANITARIAN DEMINING

A research programme has just started which focusses on the development of automated multi-offset, -azimuth and polarization GPR techniques for the identification of AP mines

 

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2005 , Exploration Geophysics Group

Modified: 11 apr 2005

Department of Geological, Environmental and Marine Sciences

 

University of Trieste

 

Hygeia - Hybrid Geophysical technology for the Evaluation of Insidious contaminated Areas