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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Montanari D; Albanese C; Catalano R; Contino A; +8 Authors

    An integrated review of existing geological and geophysical data – partly acquired during oil and gas exploration – combined with new data provided by deep geothermal studies of selected key areas, was used for the 3D modeling and mapping of the top of the geothermal reservoir developed at a regional scale in Sicily (Central Mediterranean). The resulting 1:500,000 scale map covers the area of the whole Sicily (about 25,700 km2) and is devoted to represent the main input for both the thermal modeling and the evaluation of geothermal potential at a regional scale. As the map indicates the distribution at depth of a likely target for geothermal drilling, it can be also used as a rough indicator of expected drilling cost for geothermal projects. Such a map can be seen as a useful planning tool for any geothermal project, and related exploration to be carried out in the Sicily region in the future.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Journal of Mapsarrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article . 2014 . Peer-reviewed
    Data sources: Crossref
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
    License: CC BY
    Data sources: Datacite
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
    License: CC BY
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
    License: CC BY
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    CNR ExploRA
    Article . 2015
    Data sources: CNR ExploRA
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    IRIS Cnr
    Article . 2015
    Data sources: IRIS Cnr
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Journal of Mapsarrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Journal of Maps
      Article . 2014 . Peer-reviewed
      Data sources: Crossref
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Data sources: UnpayWall
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Other literature type . 2015
      License: CC BY
      Data sources: Datacite
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Other literature type . 2015
      License: CC BY
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Other literature type . 2015
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      CNR ExploRA
      Article . 2015
      Data sources: CNR ExploRA
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      IRIS Cnr
      Article . 2015
      Data sources: IRIS Cnr
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Montanari D; Albanese C; Catalano R; Contino A; +8 Authors

    An integrated review of existing geological and geophysical data – partly acquired during oil and gas exploration – combined with new data provided by deep geothermal studies of selected key areas, was used for the 3D modeling and mapping of the top of the geothermal reservoir developed at a regional scale in Sicily (Central Mediterranean). The resulting 1:500,000 scale map covers the area of the whole Sicily (about 25,700 km2) and is devoted to represent the main input for both the thermal modeling and the evaluation of geothermal potential at a regional scale. As the map indicates the distribution at depth of a likely target for geothermal drilling, it can be also used as a rough indicator of expected drilling cost for geothermal projects. Such a map can be seen as a useful planning tool for any geothermal project, and related exploration to be carried out in the Sicily region in the future.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Journal of Mapsarrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article . 2014 . Peer-reviewed
    Data sources: Crossref
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article
    Data sources: UnpayWall
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
    License: CC BY
    Data sources: Datacite
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
    License: CC BY
    Data sources: Datacite
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
    License: CC BY
    Data sources: Datacite
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    CNR ExploRA
    Article . 2015
    Data sources: CNR ExploRA
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    IRIS Cnr
    Article . 2015
    Data sources: IRIS Cnr
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Journal of Mapsarrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Journal of Maps
      Article . 2014 . Peer-reviewed
      Data sources: Crossref
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Journal of Maps
      Article
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Other literature type . 2015
      License: CC BY
      Data sources: Datacite
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Other literature type . 2015
      License: CC BY
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Other literature type . 2015
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      Article . 2015
      Data sources: CNR ExploRA
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      IRIS Cnr
      Article . 2015
      Data sources: IRIS Cnr
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Iorio M.; Carotenuto A.; Corniello A.; Di Fraia S.; +4 Authors

    In this study, the sustainability of low-temperature geothermal field exploitation in a carbonate reservoir near Mondragone (CE), Southern Italy, is analyzed. The Mondragone geothermal field has been extensively studied through the research project VIGOR (Valutazione del potenzIale Geotermico delle RegiOni della convergenza). From seismic, geo-electric, hydro-chemical and groundwater data, obtained through the experimental campaigns carried out, physiochemical features of the aquifers and characteristics of the reservoir have been determined. Within this project, a well-doublet open-loop district heating plant has been designed to feed two public schools in Mondragone town. The sustainability of this geothermal application is analyzed in this study. A new exploration well (about 300 m deep) is considered to obtain further stratigraphic and structural information about the reservoir. Using the derived hydrogeological model of the area, a numerical analysis of geothermal exploitation was carried out to assess the thermal perturbation of the reservoir and the sustainability of its exploitation. The effect of extraction and reinjection of fluids on the reservoir was evaluated for 60 years of the plant activity. The results are fundamental to develop a sustainable geothermal heat plant and represent a real case study for the exploitation of similar carbonate reservoir geothermal resources.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Energiesarrow_drop_down
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Energies
    Article . 2020 . Peer-reviewed
    License: CC BY
    Data sources: Crossref
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Energies
    Article
    License: CC BY
    Data sources: UnpayWall
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Energies
    Article . 2020
    Data sources: DOAJ
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    CNR ExploRA
    Article . 2020
    Data sources: CNR ExploRA
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      Energies
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    Authors: Iorio M.; Carotenuto A.; Corniello A.; Di Fraia S.; +4 Authors

    In this study, the sustainability of low-temperature geothermal field exploitation in a carbonate reservoir near Mondragone (CE), Southern Italy, is analyzed. The Mondragone geothermal field has been extensively studied through the research project VIGOR (Valutazione del potenzIale Geotermico delle RegiOni della convergenza). From seismic, geo-electric, hydro-chemical and groundwater data, obtained through the experimental campaigns carried out, physiochemical features of the aquifers and characteristics of the reservoir have been determined. Within this project, a well-doublet open-loop district heating plant has been designed to feed two public schools in Mondragone town. The sustainability of this geothermal application is analyzed in this study. A new exploration well (about 300 m deep) is considered to obtain further stratigraphic and structural information about the reservoir. Using the derived hydrogeological model of the area, a numerical analysis of geothermal exploitation was carried out to assess the thermal perturbation of the reservoir and the sustainability of its exploitation. The effect of extraction and reinjection of fluids on the reservoir was evaluated for 60 years of the plant activity. The results are fundamental to develop a sustainable geothermal heat plant and represent a real case study for the exploitation of similar carbonate reservoir geothermal resources.

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    Energies
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    Authors: CAROTENUTO, ALBERTO; DE LUCA, Giuseppina; FABOZZI, SALVATORE; FIGAJ, RAFAL DAMIAN; +3 Authors

    Small and medium size district heating networks have seen some spread over the last two decades, especially in cities which are not supplied by natural gas grids. In this paper, the authors investigate the energetic feasibility of a small district heating network feeding two schools in a city of Southern Italy (Mondragone). In particular, the district heating is powered by a low-temperature geothermal fluid pumped from a well located 2.1 km away from the city center. Geothermal fluid has a temperature of 34 degrees C and a flow rate of 6 l/s. The buildings have been rehabilitated by an energy point of view and are equipped of low-temperature fan-coils in order to ensure their compatibility with the 4th generation district heating system. Energy analysis were conducted through the implementation of transient simulation model in TRNSYS environment. The feasibility of two configurations of the system is compared: the first, with one heat pump installed nearby the geothermal well feeding the grid, and the second one with the heat pumps installed in each building substation. Transient simulations results show that the first configuration is energetically less efficient than the second one due to the high thermal losses (55% of the total consumption) of the district supply pipes.

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    Authors: CAROTENUTO, ALBERTO; DE LUCA, Giuseppina; FABOZZI, SALVATORE; FIGAJ, RAFAL DAMIAN; +3 Authors

    Small and medium size district heating networks have seen some spread over the last two decades, especially in cities which are not supplied by natural gas grids. In this paper, the authors investigate the energetic feasibility of a small district heating network feeding two schools in a city of Southern Italy (Mondragone). In particular, the district heating is powered by a low-temperature geothermal fluid pumped from a well located 2.1 km away from the city center. Geothermal fluid has a temperature of 34 degrees C and a flow rate of 6 l/s. The buildings have been rehabilitated by an energy point of view and are equipped of low-temperature fan-coils in order to ensure their compatibility with the 4th generation district heating system. Energy analysis were conducted through the implementation of transient simulation model in TRNSYS environment. The feasibility of two configurations of the system is compared: the first, with one heat pump installed nearby the geothermal well feeding the grid, and the second one with the heat pumps installed in each building substation. Transient simulations results show that the first configuration is energetically less efficient than the second one due to the high thermal losses (55% of the total consumption) of the district supply pipes.

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    International Journal of Heat and Technology
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      CNR ExploRA
      Article . 2016
      Data sources: CNR ExploRA
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      IRIS Cnr
      Article . 2016
      Data sources: IRIS Cnr
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      International Journal of Heat and Technology
      Article . 2016 . Peer-reviewed
      Data sources: Crossref
      International Journal of Heat and Technology
      Article . 2016 . Peer-reviewed
      Data sources: Crossref
      ZENODO
      Article . 2016
      Data sources: ZENODO
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Nocentini M; Bertini A; Cavinato; G P; +19 Authors

    We present the preliminary results of a ~ 230 m deep borehole (CN1) drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface (Fig. 1). The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits (Fig. 2). The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro (Fig. 2) (Cosentino et al., 2017; Nocentini et al., 2017; Nocentini et al., 2018). The deep lacustrine facies (San Nicandro Fm. - SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp. (Spadi et al., 2016), allowing to ascribe the SNF to a late Piacenzian-Gelasian age (Cosentino et al., 2017). The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments (Fig. 3). The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations (Fig. 3). In detail, the upper part of the well-log (<71.60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 71.60 and 118.80 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 118.80 to 154.70 m, massive to laminated over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. In the first meters od this interval the CaCO3 content drops down, showing minimum values lower than 10%. From 154.70 to 194.8 m the sequence is formed by alternations of clayey-silts and laminated whitish calcareous silts, while down to 223.30 m it is composed by alternations of clays, marls and clayey-gravels, with coarser sediments becoming more and more frequent. Below 223.30 m, fine grain deposits almost disappear, passing to coarse poligenic calcareous breccias with rare clayey-silty layers. Several centimetric thick tephra layers occur in the first 105 meters of the sedimentary core CN1 and outcropping sections of the deep-lake deposits of the San Nicandro Formation (Fig. 3). These tephras share a common lithology of greyish ash made up of moderately vesicular glass shards, clinopyroxene, plagioclase, and minor orthopyroxene. Glasses and whole rock have a calc-alkaline intermediate composition ranging from basaltic-andesite to andesite, with slightly variable major and trace element contents. This composition is similar to the ? 2 Ma old volcanic rocks found in deep boreholes in Campanian Plain, southern Italy (Albini et al., 1980; Barbieri et al., 1979: Di Girolamo et al., 1976) (Fig. 4a). Incompatible trace elements normalised to the primordial mantle display typical subduction-related patterns with troughs at Ta, Nb, and Ti, and peaks at Pb, which are found in both Plio-Quaternary calc-alkaline rocks of the Balkan and Italian regions. However, Sr, Nd, and Pb isotope ratios differ significantly from Balkan calc-alkaline volcanic rocks, whereas they are within the range of the Early Pleistocene Campanian Plain buried volcanism (Fig. 4b). Based on both major-trace element composition, isotope data and the chronological setting of the San Nicandro Formation, the Early Pleistocene calc-alkaline volcanism of the Neapolitan-Campanian area can be thus regarded as the most likely source for San Nicandro tephra. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao IRIS Cnrarrow_drop_down
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Nocentini M; Bertini A; Cavinato; G P; +19 Authors

    We present the preliminary results of a ~ 230 m deep borehole (CN1) drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface (Fig. 1). The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits (Fig. 2). The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro (Fig. 2) (Cosentino et al., 2017; Nocentini et al., 2017; Nocentini et al., 2018). The deep lacustrine facies (San Nicandro Fm. - SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp. (Spadi et al., 2016), allowing to ascribe the SNF to a late Piacenzian-Gelasian age (Cosentino et al., 2017). The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments (Fig. 3). The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations (Fig. 3). In detail, the upper part of the well-log (<71.60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 71.60 and 118.80 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 118.80 to 154.70 m, massive to laminated over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. In the first meters od this interval the CaCO3 content drops down, showing minimum values lower than 10%. From 154.70 to 194.8 m the sequence is formed by alternations of clayey-silts and laminated whitish calcareous silts, while down to 223.30 m it is composed by alternations of clays, marls and clayey-gravels, with coarser sediments becoming more and more frequent. Below 223.30 m, fine grain deposits almost disappear, passing to coarse poligenic calcareous breccias with rare clayey-silty layers. Several centimetric thick tephra layers occur in the first 105 meters of the sedimentary core CN1 and outcropping sections of the deep-lake deposits of the San Nicandro Formation (Fig. 3). These tephras share a common lithology of greyish ash made up of moderately vesicular glass shards, clinopyroxene, plagioclase, and minor orthopyroxene. Glasses and whole rock have a calc-alkaline intermediate composition ranging from basaltic-andesite to andesite, with slightly variable major and trace element contents. This composition is similar to the ? 2 Ma old volcanic rocks found in deep boreholes in Campanian Plain, southern Italy (Albini et al., 1980; Barbieri et al., 1979: Di Girolamo et al., 1976) (Fig. 4a). Incompatible trace elements normalised to the primordial mantle display typical subduction-related patterns with troughs at Ta, Nb, and Ti, and peaks at Pb, which are found in both Plio-Quaternary calc-alkaline rocks of the Balkan and Italian regions. However, Sr, Nd, and Pb isotope ratios differ significantly from Balkan calc-alkaline volcanic rocks, whereas they are within the range of the Early Pleistocene Campanian Plain buried volcanism (Fig. 4b). Based on both major-trace element composition, isotope data and the chronological setting of the San Nicandro Formation, the Early Pleistocene calc-alkaline volcanism of the Neapolitan-Campanian area can be thus regarded as the most likely source for San Nicandro tephra. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao IRIS Cnrarrow_drop_down
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Marco Nocentini; Adele Bertini; Gian Paolo Cavinato; Francesca Cifelli; +16 Authors

    We present the preliminary results of a~230 m deep borehole drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface. The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits. The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro. The deep lacustrine facies (San Nicandro Fm.-SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp., allowing to ascribe the SNF to a late Piacenzian-Gelasian age. The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments. The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations. In detail, the upper part of the well-log (<60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 60 and 115 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 115 to 150 m, massive over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. From 150 to 190 m the sequence is formed by alternations of clayey-silts and whitish calcareous silts, while down to 220 m it is composed by alternations of clay and clayey-gravels, with coarser sediments becoming more and more frequent. Below 220 m, fine grain deposits almost disappear, passing to coarse calcareous breccias with rare clayey-silty layers. Several tephra layers are present between 25-30 m, 55-75 m, 100-105 m and 165-170 m. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao IRIS Cnrarrow_drop_down
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Marco Nocentini; Adele Bertini; Gian Paolo Cavinato; Francesca Cifelli; +16 Authors

    We present the preliminary results of a~230 m deep borehole drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface. The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits. The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro. The deep lacustrine facies (San Nicandro Fm.-SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp., allowing to ascribe the SNF to a late Piacenzian-Gelasian age. The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments. The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations. In detail, the upper part of the well-log (<60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 60 and 115 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 115 to 150 m, massive over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. From 150 to 190 m the sequence is formed by alternations of clayey-silts and whitish calcareous silts, while down to 220 m it is composed by alternations of clay and clayey-gravels, with coarser sediments becoming more and more frequent. Below 220 m, fine grain deposits almost disappear, passing to coarse calcareous breccias with rare clayey-silty layers. Several tephra layers are present between 25-30 m, 55-75 m, 100-105 m and 165-170 m. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao IRIS Cnrarrow_drop_down
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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    Authors: Antonio Galgaro; Eloisa Di Sipio; Elisa Destro; Sergio Chiesa; +21 Authors

    In the framework of VIGOR Project, a national project coordinated by the Institute of Geosciences and Earth Resources (CNR-IGG) and sponsored by the Ministry of Economic Development (MiSE), dedicated to the evaluation of geothermal potential in the regions of the Convergence Objective in Italy (Puglia, Calabria, Campania and Sicily), is expected to evaluate the ability of the territory to heat exchange with the ground for air conditioning of buildings. To identify the conditions for the development of low enthalpy geothermal systems collected and organized on a regional scale geological and stratigraphic data useful for the preparation of a specific thematic mapping, able to represent in a synergistic and simplified way the physical parameters (geological, lithostratigraphic, hydrogeological, thermodynamic) that most influence the subsoil behavior for thermal exchange. The litho-stratigraphic and hydrogeological database created for every region led to the production of different cartographic thematic maps, such as the thermal conductivity (lithological and stratigraphical), the surface geothermal flux, the average annual temperature of air, the climate zoning, the areas of hydrogeological restrictions. To obtain a single representation of the geo-exchange potential of the region, the different thematic maps described must be combined together by means of an algorithm, defined on the basis of the SINTACS methodology. The purpose is to weigh the contributions of the involved parameters and to produce a preliminary synthesis map able to identify the territorial use of geothermal heat pump systems, based on the geological characteristics and in agreement with the existing regulatory constraints.

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    Authors: Antonio Galgaro; Eloisa Di Sipio; Elisa Destro; Sergio Chiesa; +21 Authors

    In the framework of VIGOR Project, a national project coordinated by the Institute of Geosciences and Earth Resources (CNR-IGG) and sponsored by the Ministry of Economic Development (MiSE), dedicated to the evaluation of geothermal potential in the regions of the Convergence Objective in Italy (Puglia, Calabria, Campania and Sicily), is expected to evaluate the ability of the territory to heat exchange with the ground for air conditioning of buildings. To identify the conditions for the development of low enthalpy geothermal systems collected and organized on a regional scale geological and stratigraphic data useful for the preparation of a specific thematic mapping, able to represent in a synergistic and simplified way the physical parameters (geological, lithostratigraphic, hydrogeological, thermodynamic) that most influence the subsoil behavior for thermal exchange. The litho-stratigraphic and hydrogeological database created for every region led to the production of different cartographic thematic maps, such as the thermal conductivity (lithological and stratigraphical), the surface geothermal flux, the average annual temperature of air, the climate zoning, the areas of hydrogeological restrictions. To obtain a single representation of the geo-exchange potential of the region, the different thematic maps described must be combined together by means of an algorithm, defined on the basis of the SINTACS methodology. The purpose is to weigh the contributions of the involved parameters and to produce a preliminary synthesis map able to identify the territorial use of geothermal heat pump systems, based on the geological characteristics and in agreement with the existing regulatory constraints.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Acque Sotterraneearrow_drop_down
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Montanari D; Albanese C; Catalano R; Contino A; +8 Authors

    An integrated review of existing geological and geophysical data – partly acquired during oil and gas exploration – combined with new data provided by deep geothermal studies of selected key areas, was used for the 3D modeling and mapping of the top of the geothermal reservoir developed at a regional scale in Sicily (Central Mediterranean). The resulting 1:500,000 scale map covers the area of the whole Sicily (about 25,700 km2) and is devoted to represent the main input for both the thermal modeling and the evaluation of geothermal potential at a regional scale. As the map indicates the distribution at depth of a likely target for geothermal drilling, it can be also used as a rough indicator of expected drilling cost for geothermal projects. Such a map can be seen as a useful planning tool for any geothermal project, and related exploration to be carried out in the Sicily region in the future.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Journal of Mapsarrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article . 2014 . Peer-reviewed
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    CNR ExploRA
    Article . 2015
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    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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    Article . 2015
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    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Journal of Mapsarrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Journal of Maps
      Article . 2014 . Peer-reviewed
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      CNR ExploRA
      Article . 2015
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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      Article . 2015
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Montanari D; Albanese C; Catalano R; Contino A; +8 Authors

    An integrated review of existing geological and geophysical data – partly acquired during oil and gas exploration – combined with new data provided by deep geothermal studies of selected key areas, was used for the 3D modeling and mapping of the top of the geothermal reservoir developed at a regional scale in Sicily (Central Mediterranean). The resulting 1:500,000 scale map covers the area of the whole Sicily (about 25,700 km2) and is devoted to represent the main input for both the thermal modeling and the evaluation of geothermal potential at a regional scale. As the map indicates the distribution at depth of a likely target for geothermal drilling, it can be also used as a rough indicator of expected drilling cost for geothermal projects. Such a map can be seen as a useful planning tool for any geothermal project, and related exploration to be carried out in the Sicily region in the future.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Journal of Mapsarrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article . 2014 . Peer-reviewed
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Maps
    Article
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2015
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    Authors: Iorio M.; Carotenuto A.; Corniello A.; Di Fraia S.; +4 Authors

    In this study, the sustainability of low-temperature geothermal field exploitation in a carbonate reservoir near Mondragone (CE), Southern Italy, is analyzed. The Mondragone geothermal field has been extensively studied through the research project VIGOR (Valutazione del potenzIale Geotermico delle RegiOni della convergenza). From seismic, geo-electric, hydro-chemical and groundwater data, obtained through the experimental campaigns carried out, physiochemical features of the aquifers and characteristics of the reservoir have been determined. Within this project, a well-doublet open-loop district heating plant has been designed to feed two public schools in Mondragone town. The sustainability of this geothermal application is analyzed in this study. A new exploration well (about 300 m deep) is considered to obtain further stratigraphic and structural information about the reservoir. Using the derived hydrogeological model of the area, a numerical analysis of geothermal exploitation was carried out to assess the thermal perturbation of the reservoir and the sustainability of its exploitation. The effect of extraction and reinjection of fluids on the reservoir was evaluated for 60 years of the plant activity. The results are fundamental to develop a sustainable geothermal heat plant and represent a real case study for the exploitation of similar carbonate reservoir geothermal resources.

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    Authors: Iorio M.; Carotenuto A.; Corniello A.; Di Fraia S.; +4 Authors

    In this study, the sustainability of low-temperature geothermal field exploitation in a carbonate reservoir near Mondragone (CE), Southern Italy, is analyzed. The Mondragone geothermal field has been extensively studied through the research project VIGOR (Valutazione del potenzIale Geotermico delle RegiOni della convergenza). From seismic, geo-electric, hydro-chemical and groundwater data, obtained through the experimental campaigns carried out, physiochemical features of the aquifers and characteristics of the reservoir have been determined. Within this project, a well-doublet open-loop district heating plant has been designed to feed two public schools in Mondragone town. The sustainability of this geothermal application is analyzed in this study. A new exploration well (about 300 m deep) is considered to obtain further stratigraphic and structural information about the reservoir. Using the derived hydrogeological model of the area, a numerical analysis of geothermal exploitation was carried out to assess the thermal perturbation of the reservoir and the sustainability of its exploitation. The effect of extraction and reinjection of fluids on the reservoir was evaluated for 60 years of the plant activity. The results are fundamental to develop a sustainable geothermal heat plant and represent a real case study for the exploitation of similar carbonate reservoir geothermal resources.

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    Authors: CAROTENUTO, ALBERTO; DE LUCA, Giuseppina; FABOZZI, SALVATORE; FIGAJ, RAFAL DAMIAN; +3 Authors

    Small and medium size district heating networks have seen some spread over the last two decades, especially in cities which are not supplied by natural gas grids. In this paper, the authors investigate the energetic feasibility of a small district heating network feeding two schools in a city of Southern Italy (Mondragone). In particular, the district heating is powered by a low-temperature geothermal fluid pumped from a well located 2.1 km away from the city center. Geothermal fluid has a temperature of 34 degrees C and a flow rate of 6 l/s. The buildings have been rehabilitated by an energy point of view and are equipped of low-temperature fan-coils in order to ensure their compatibility with the 4th generation district heating system. Energy analysis were conducted through the implementation of transient simulation model in TRNSYS environment. The feasibility of two configurations of the system is compared: the first, with one heat pump installed nearby the geothermal well feeding the grid, and the second one with the heat pumps installed in each building substation. Transient simulations results show that the first configuration is energetically less efficient than the second one due to the high thermal losses (55% of the total consumption) of the district supply pipes.

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      International Journal of Heat and Technology
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    Authors: CAROTENUTO, ALBERTO; DE LUCA, Giuseppina; FABOZZI, SALVATORE; FIGAJ, RAFAL DAMIAN; +3 Authors

    Small and medium size district heating networks have seen some spread over the last two decades, especially in cities which are not supplied by natural gas grids. In this paper, the authors investigate the energetic feasibility of a small district heating network feeding two schools in a city of Southern Italy (Mondragone). In particular, the district heating is powered by a low-temperature geothermal fluid pumped from a well located 2.1 km away from the city center. Geothermal fluid has a temperature of 34 degrees C and a flow rate of 6 l/s. The buildings have been rehabilitated by an energy point of view and are equipped of low-temperature fan-coils in order to ensure their compatibility with the 4th generation district heating system. Energy analysis were conducted through the implementation of transient simulation model in TRNSYS environment. The feasibility of two configurations of the system is compared: the first, with one heat pump installed nearby the geothermal well feeding the grid, and the second one with the heat pumps installed in each building substation. Transient simulations results show that the first configuration is energetically less efficient than the second one due to the high thermal losses (55% of the total consumption) of the district supply pipes.

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    International Journal of Heat and Technology
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    Authors: Nocentini M; Bertini A; Cavinato; G P; +19 Authors

    We present the preliminary results of a ~ 230 m deep borehole (CN1) drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface (Fig. 1). The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits (Fig. 2). The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro (Fig. 2) (Cosentino et al., 2017; Nocentini et al., 2017; Nocentini et al., 2018). The deep lacustrine facies (San Nicandro Fm. - SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp. (Spadi et al., 2016), allowing to ascribe the SNF to a late Piacenzian-Gelasian age (Cosentino et al., 2017). The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments (Fig. 3). The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations (Fig. 3). In detail, the upper part of the well-log (<71.60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 71.60 and 118.80 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 118.80 to 154.70 m, massive to laminated over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. In the first meters od this interval the CaCO3 content drops down, showing minimum values lower than 10%. From 154.70 to 194.8 m the sequence is formed by alternations of clayey-silts and laminated whitish calcareous silts, while down to 223.30 m it is composed by alternations of clays, marls and clayey-gravels, with coarser sediments becoming more and more frequent. Below 223.30 m, fine grain deposits almost disappear, passing to coarse poligenic calcareous breccias with rare clayey-silty layers. Several centimetric thick tephra layers occur in the first 105 meters of the sedimentary core CN1 and outcropping sections of the deep-lake deposits of the San Nicandro Formation (Fig. 3). These tephras share a common lithology of greyish ash made up of moderately vesicular glass shards, clinopyroxene, plagioclase, and minor orthopyroxene. Glasses and whole rock have a calc-alkaline intermediate composition ranging from basaltic-andesite to andesite, with slightly variable major and trace element contents. This composition is similar to the ? 2 Ma old volcanic rocks found in deep boreholes in Campanian Plain, southern Italy (Albini et al., 1980; Barbieri et al., 1979: Di Girolamo et al., 1976) (Fig. 4a). Incompatible trace elements normalised to the primordial mantle display typical subduction-related patterns with troughs at Ta, Nb, and Ti, and peaks at Pb, which are found in both Plio-Quaternary calc-alkaline rocks of the Balkan and Italian regions. However, Sr, Nd, and Pb isotope ratios differ significantly from Balkan calc-alkaline volcanic rocks, whereas they are within the range of the Early Pleistocene Campanian Plain buried volcanism (Fig. 4b). Based on both major-trace element composition, isotope data and the chronological setting of the San Nicandro Formation, the Early Pleistocene calc-alkaline volcanism of the Neapolitan-Campanian area can be thus regarded as the most likely source for San Nicandro tephra. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

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    Authors: Nocentini M; Bertini A; Cavinato; G P; +19 Authors

    We present the preliminary results of a ~ 230 m deep borehole (CN1) drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface (Fig. 1). The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits (Fig. 2). The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro (Fig. 2) (Cosentino et al., 2017; Nocentini et al., 2017; Nocentini et al., 2018). The deep lacustrine facies (San Nicandro Fm. - SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp. (Spadi et al., 2016), allowing to ascribe the SNF to a late Piacenzian-Gelasian age (Cosentino et al., 2017). The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments (Fig. 3). The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations (Fig. 3). In detail, the upper part of the well-log (<71.60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 71.60 and 118.80 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 118.80 to 154.70 m, massive to laminated over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. In the first meters od this interval the CaCO3 content drops down, showing minimum values lower than 10%. From 154.70 to 194.8 m the sequence is formed by alternations of clayey-silts and laminated whitish calcareous silts, while down to 223.30 m it is composed by alternations of clays, marls and clayey-gravels, with coarser sediments becoming more and more frequent. Below 223.30 m, fine grain deposits almost disappear, passing to coarse poligenic calcareous breccias with rare clayey-silty layers. Several centimetric thick tephra layers occur in the first 105 meters of the sedimentary core CN1 and outcropping sections of the deep-lake deposits of the San Nicandro Formation (Fig. 3). These tephras share a common lithology of greyish ash made up of moderately vesicular glass shards, clinopyroxene, plagioclase, and minor orthopyroxene. Glasses and whole rock have a calc-alkaline intermediate composition ranging from basaltic-andesite to andesite, with slightly variable major and trace element contents. This composition is similar to the ? 2 Ma old volcanic rocks found in deep boreholes in Campanian Plain, southern Italy (Albini et al., 1980; Barbieri et al., 1979: Di Girolamo et al., 1976) (Fig. 4a). Incompatible trace elements normalised to the primordial mantle display typical subduction-related patterns with troughs at Ta, Nb, and Ti, and peaks at Pb, which are found in both Plio-Quaternary calc-alkaline rocks of the Balkan and Italian regions. However, Sr, Nd, and Pb isotope ratios differ significantly from Balkan calc-alkaline volcanic rocks, whereas they are within the range of the Early Pleistocene Campanian Plain buried volcanism (Fig. 4b). Based on both major-trace element composition, isotope data and the chronological setting of the San Nicandro Formation, the Early Pleistocene calc-alkaline volcanism of the Neapolitan-Campanian area can be thus regarded as the most likely source for San Nicandro tephra. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao IRIS Cnrarrow_drop_down
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    Authors: Marco Nocentini; Adele Bertini; Gian Paolo Cavinato; Francesca Cifelli; +16 Authors

    We present the preliminary results of a~230 m deep borehole drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface. The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits. The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro. The deep lacustrine facies (San Nicandro Fm.-SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp., allowing to ascribe the SNF to a late Piacenzian-Gelasian age. The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments. The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations. In detail, the upper part of the well-log (<60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 60 and 115 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 115 to 150 m, massive over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. From 150 to 190 m the sequence is formed by alternations of clayey-silts and whitish calcareous silts, while down to 220 m it is composed by alternations of clay and clayey-gravels, with coarser sediments becoming more and more frequent. Below 220 m, fine grain deposits almost disappear, passing to coarse calcareous breccias with rare clayey-silty layers. Several tephra layers are present between 25-30 m, 55-75 m, 100-105 m and 165-170 m. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao IRIS Cnrarrow_drop_down
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    Authors: Marco Nocentini; Adele Bertini; Gian Paolo Cavinato; Francesca Cifelli; +16 Authors

    We present the preliminary results of a~230 m deep borehole drilled in the eastern part of the Paganica-San Demetrio-Castelnuovo Basin (PSC) (L'Aquila, central Italy), at the top of the Castelnuovo hill within the Valle Daria paleosurface. The PSC is a NW-SE trending graben bordered by active normal faults and filled by Plio-Quaternary deposits. The oldest ones, largely outcropping in the Valle Daria area, pertain to the San Demetrio-Colle Cantaro Synthem and are composed by several formations, laterally interfingered each other, representing different depositional environments of the Paleolake San Nicandro. The deep lacustrine facies (San Nicandro Fm.-SNF) is formed by laminated to massive whitish calcareous silts, bearing an endemic ostracod assemblage mainly composed by Caspiocypris ssp., allowing to ascribe the SNF to a late Piacenzian-Gelasian age. The outcropping part of the SNF, usually less than 50 m thick, shows a normal magnetic polarity in the basal 10 m, passing upwards to a reverse polarity. In addition, in the upper portion of the SNF, close to Castelnuovo village, three blackish tephra layers are present. Starting from these premises, the Castelnuovo deep borehole (CN1) was realized to investigate, in a palaeoenvironmental and palaeoclimatic perspective, the early sedimentary infilling of the PSC and the evolution of the lacustrine system. The borehole reached a depth of 229.30 m b.g.l., drilling a succession mainly composed by cyclic alternations of fine-grained laminated and massive sediments. The cyclic variations of different parameters among which the CaCO3 content, the granulometry, the sediment colour and the magnetic susceptibility testify that sedimentation was controlled by orbital and climatic oscillations. In detail, the upper part of the well-log (<60 m), partly matching the outcropping succession, is characterized by the typical features of the SNF, consisting of a cyclic alternation of white calcareous silts and light grey clayey-silts couplets, often separated by a thin oxidized silty-sandy layer. In this interval, the CaCO3 content cyclically ranges between 50% and 90%, mostly occurring as lacustrine endogenic calcite. Between 60 and 115 m, clayey levels become more abundant and thicker and organic-rich clay levels appear, whereas minima CaCO3 contents are periodically recorded, around 25%. From 115 to 150 m, massive over-consolidated organic-rich clays are predominant, while calcareous silty levels become occasional and thin. From 150 to 190 m the sequence is formed by alternations of clayey-silts and whitish calcareous silts, while down to 220 m it is composed by alternations of clay and clayey-gravels, with coarser sediments becoming more and more frequent. Below 220 m, fine grain deposits almost disappear, passing to coarse calcareous breccias with rare clayey-silty layers. Several tephra layers are present between 25-30 m, 55-75 m, 100-105 m and 165-170 m. Ongoing analyses, consisting in a multidisciplinary approach that integrates sedimentology, micropaleontology, palynology, tephrochronology, geochemistry and magnetostratigraphy, will constrain the onset and subsequent evolution of the San Nicandro lacustrine system, unraveling the late Pliocene-early Pleistocene climatic variations in the central Mediterranean area and bringing new insights on the post-orogenic evolution of the central Apennines.

    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao IRIS Cnrarrow_drop_down
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    Authors: Antonio Galgaro; Eloisa Di Sipio; Elisa Destro; Sergio Chiesa; +21 Authors

    In the framework of VIGOR Project, a national project coordinated by the Institute of Geosciences and Earth Resources (CNR-IGG) and sponsored by the Ministry of Economic Development (MiSE), dedicated to the evaluation of geothermal potential in the regions of the Convergence Objective in Italy (Puglia, Calabria, Campania and Sicily), is expected to evaluate the ability of the territory to heat exchange with the ground for air conditioning of buildings. To identify the conditions for the development of low enthalpy geothermal systems collected and organized on a regional scale geological and stratigraphic data useful for the preparation of a specific thematic mapping, able to represent in a synergistic and simplified way the physical parameters (geological, lithostratigraphic, hydrogeological, thermodynamic) that most influence the subsoil behavior for thermal exchange. The litho-stratigraphic and hydrogeological database created for every region led to the production of different cartographic thematic maps, such as the thermal conductivity (lithological and stratigraphical), the surface geothermal flux, the average annual temperature of air, the climate zoning, the areas of hydrogeological restrictions. To obtain a single representation of the geo-exchange potential of the region, the different thematic maps described must be combined together by means of an algorithm, defined on the basis of the SINTACS methodology. The purpose is to weigh the contributions of the involved parameters and to produce a preliminary synthesis map able to identify the territorial use of geothermal heat pump systems, based on the geological characteristics and in agreement with the existing regulatory constraints.

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    Authors: Antonio Galgaro; Eloisa Di Sipio; Elisa Destro; Sergio Chiesa; +21 Authors

    In the framework of VIGOR Project, a national project coordinated by the Institute of Geosciences and Earth Resources (CNR-IGG) and sponsored by the Ministry of Economic Development (MiSE), dedicated to the evaluation of geothermal potential in the regions of the Convergence Objective in Italy (Puglia, Calabria, Campania and Sicily), is expected to evaluate the ability of the territory to heat exchange with the ground for air conditioning of buildings. To identify the conditions for the development of low enthalpy geothermal systems collected and organized on a regional scale geological and stratigraphic data useful for the preparation of a specific thematic mapping, able to represent in a synergistic and simplified way the physical parameters (geological, lithostratigraphic, hydrogeological, thermodynamic) that most influence the subsoil behavior for thermal exchange. The litho-stratigraphic and hydrogeological database created for every region led to the production of different cartographic thematic maps, such as the thermal conductivity (lithological and stratigraphical), the surface geothermal flux, the average annual temperature of air, the climate zoning, the areas of hydrogeological restrictions. To obtain a single representation of the geo-exchange potential of the region, the different thematic maps described must be combined together by means of an algorithm, defined on the basis of the SINTACS methodology. The purpose is to weigh the contributions of the involved parameters and to produce a preliminary synthesis map able to identify the territorial use of geothermal heat pump systems, based on the geological characteristics and in agreement with the existing regulatory constraints.

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