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Geophysical survey of the offshore microtunnel


            route in Delimara Peninsula (Malta)





            Assessing the seafloor integrity and the possible deteriorations that
            might arise from the bedrock collapse during the nearshore
            microtunnelling, and identifying and avoiding cavities during the work


            Vanessa Barcaglioni, Giuseppe Canna, Giuseppe Vecchio
            Techfem S.p.A.
            Maurizio Ponte, Università della Calabria
            Giuseppe Ferraro, Geofisica Misure s.n.c.







                       his paper reports the main result of the   cavities along the pathway analysed and, thus, to
                       geophysical survey performed in the   distinguish the karst lithologies (limestone and marly
                       Delimara peninsula (Malta) along the   limestone) from the non-karst ones (marls and clays).
                       offshore route of the microtunnel
                       realized for the shore approach of the
            T 22” Melita Transgas Pipeline. The main  Introduction
            goals of the survey were to assess the seafloor integrity   The geophysical investigations aim to support the
            and the possible deteriorations that might arise from   design of a gas pipeline (Melita Transgas Pipeline) in the
            the bedrock collapse during the nearshore   section interested by the microtunnelling technology.
            microtunnelling, and then to identify and avoid cavities   The microtunnel crosses under the Delimara peninsula
            during the work.                         for 600 m and extends under the seabed for other 600
            The preliminary geognostic investigations carried out   m. The purpose of the investigations was reconstructing
            on this segment through several boreholes highlighted   the lithostratigraphic structure of this nearshore section,
            the presence of fractured limestone and possible   up to a depth of 50-60 m from the seabed, also
            cavities. A following tomographic analysis (Electrical   assessing the fracturing conditions and any karst
            Resistivity Tomography) allowed the detailed   processes that affect the lithological formation present.
            reconstruction  of  the  lithostratigraphic  and
            geomechanics characteristic of the entire corridor. The   “The geophysical investigations aim
            geoelectric prospect also allowed to verify and evaluate   to support the design of the Melita
            the risk of intercepting cavities along the corridor during   Transgas Pipeline in the section
            the drilling phase.                         interested by the microtunnelling
            The  installation  of  seven  multielectrode  lines  were   technology
            performed: one of them was longitudinal to the
            microtunnel pathway, two parallel and the rest   The activities are subsequent to  a first  phase of
            transversal to it. Six of them were installed on the   investigations carried out “on the land” (drilling, refraction
            seabed, with the help of divers, to better mitigate the   seismic and geoelectric tomography prospecting). In the
            effects of the marine depth. The post-processing of the   nearshore area, two continuous drilling operations and a
            data, optimized through the precise knowledge of the   morpho-bathymetric survey of the seabed have already
            electrode positions and the resistivity values of the   been carried out, the latter used as a support for the
            seawater, led to the definition of a two-dimensional and   programming and processing activities carried out in this
            a three-dimensional predicting model, able to work up   phase. Just starting from the acquired data, it was
            to 50 m depth from the seabed. Such models link the   possible to evaluate the most suitable geophysical
            values of the resistivity measured and the lithologies of   methodology for the achievement of the expected
            the seabed (known from the stratigraphic logs) to its   objectives. The seabed is featured by a very variable
            stratigraphy, allowing to exclude the presence of   depth between the coast and the outermost part, which

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