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  • SDSN - Greece
  • 2022-2022
  • Publications
  • MX

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    Authors: Solheim, Anders; Kalsnes, Bjørn; Strout, James Michael; Piciullo, Luca; +3 Authors

    Cross-sectorial and cross-disciplinary collaboration, as well as public-private partnerships are necessary to handle the complexity of climate adaptation. The Research Council of Norway has established the Centres for Research-based Innovation (CRI) in which research- and education organizations, public entities and private enterprises join forces in 8-year long collaborations. CRI-Klima 2050 focuses on climate adaptation of buildings and infrastructure and runs several pilot projects to innovate new solutions for building resilience, stormwater- and landslide risk management. Several of the major infrastructure owners in Norway are partners in the centre. Norway is increasingly affected by precipitation triggered landslides. Klima 2050 pilot projects on landslide risk reduction include a web-based toolbox for prioritizing and choosing optimal mitigation measures, including Nature-Based Solutions, improved early warning systems and mitigation measures for slope instability, and improved local warning for hazardous weather systems, all developed in close collaboration between centre partners from different sectors and disciplines. The results of these projects can all be upscaled and are transferable to other infrastructure elements.

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    Frontiers in Earth Science
    Article . 2022
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    Frontiers in Earth Science
    Article . 2022 . Peer-reviewed
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    NTNU Open
    Article . 2022
    Data sources: NTNU Open
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      Frontiers in Earth Science
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      NTNU Open
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    Authors: Favio Cruz-Hernández; Luis A Gallardo; Marco Calò; Raúl R Castro; +1 Authors

    SUMMARYIn the last 15 yr, the use of surface waves retrieved from the cross-correlation of ambient seismic noise has significantly increased its applications to determine or monitor changes in the elastic properties of the Earth's interior. We designed a methodology for laterally constrained surface wave inversion based on a two-stage technique to estimate the 3-D distribution of the S-wave velocity (Vs). The first stage inverts traveltimes to estimate group or phase velocity dispersion maps and their inverse covariance matrix for different periods. The inverse covariance matrix is constructed explicitly using the ray tracing information. The inverse covariance matrix adds the lateral sensitivity of the maps to the structure, whereas the period-dependency provides sensitivity to the structure at depth. The second stage applies a nonlinear conjugate gradient scheme to estimate the 3-D distribution of S-wave velocity using the ensemble of velocity dispersion maps and their estimated inverse covariance matrix. We validate the methodology using a synthetic model. The results show an improved estimation of subsurface S-wave velocity structures compared to conventional point-wise inversion.

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    Geophysical Journal International
    Article . 2022 . Peer-reviewed
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      Geophysical Journal International
      Article . 2022 . Peer-reviewed
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    Authors: Favio Cruz-Hernández; Luis A Gallardo; Marco Calò; Raúl R Castro; +1 Authors

    SUMMARYWe apply a new technique for a laterally constrained surface wave inversion (LCSWI) to estimate the 3-D sedimentary structure of the Cerro Prieto Basin, Baja California, Mexico. The basin contains the Cerro Prieto geothermal field, which is considered one of the most productive in the world. The data used consist of group velocity measurements of Rayleigh waves extracted from cross-correlations of ambient noise registered at 12 stations distributed in an 18 × 12 km area. We estimated an S-wave velocity model that clearly shows three relatively homogeneous geoseismic units that correlate with the stratigraphic column reported in previous studies. The deepest geoseismic unit is the most heterogeneous and shows low-velocity zones likely associated with fluids. The resulting velocity model shows similarity with the conceptual geological model of the geothermal field reported in the literature and recent geophysical studies that suggest the potential existence of another deeper reservoir west of the current exploitation area.

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    Geophysical Journal International
    Article . 2022 . Peer-reviewed
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      Geophysical Journal International
      Article . 2022 . Peer-reviewed
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    Authors: Granados-Chavarría, I.; Calò, M.; Figueroa-Soto, Á.; Jousset, P.;

    Since the nineteen-eighties, the depth, number, position and shape of the heat sources feeding the super-hot geothermal system of the Los Humeros caldera (Mexico) is under debate. With the aim of providing a seismic constraint of this region, we present a high resolution three-dimensional anisotropic shear wave velocity model. We used the continuous records of ambient seismic noise at 45 seismic stations deployed for more than one year. From the data, we obtained a set of about 1444 phase and 1534 group velocity dispersion curves, for Love and Rayleigh waves, respectively. By using the dispersion data, we obtained three dimensional models for shear wave velocities and radial anisotropy down to 17 km of depth. These models allowed to image three low velocity bodies at different depths: 1) a deep storage of potential molten material rising from the depth and stopping at ~11 km of depth, 2) a second storage region from 3 to 8 km of depth, related with the Los Humeros caldera collapse, and that feeds the 3) shallow low-velocity bodies between 1.3 and 2.2 km, representing the expression of the geothermal reservoir currently exploited. All these low velocity bodies are interconnected and represent part of the remnant magmatic plumbing system beneath the Los Humeros caldera. These seismic images provide insights to the deep upward pathways of fluids feeding the geothermal reservoir from the heat source(s) and its relationship with the structures controlling the hydrothermal system. Previous article in issue

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    Journal of Volcanology and Geothermal Research
    Other literature type . Article . 2022 . Peer-reviewed
    License: Elsevier TDM
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      Journal of Volcanology and Geothermal Research
      Other literature type . Article . 2022 . Peer-reviewed
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    Authors: Weydt, L.; Lucci, F.; Lacinska, A.; Scheuvens, D.; +6 Authors

    Hydrothermal alteration is a common process in active geothermal systems and can significantly change the physiochemical properties of rocks. To improve reservoir assessment and modeling of high-temperature geothermal resources linked to active volcanic settings, a detailed understanding of the reservoir is needed. The Los Humeros Volcanic Complex, hosting the third largest exploited geothermal field in Mexico, represents a natural laboratory to investigate the impact of hydrothermal processes on the rock properties through andesitic reservoir cores and outcropping analogs. Complementary petrographic and chemical analyses were used to characterize the intensities and facies of hydrothermal alteration. The alteration varies from argillic and propylitic facies characterized by no significant changes of the REE budget indicating an inert behavior to silicic facies and skarn instead showing highly variable REE contents. Unaltered outcrop samples predominantly feature low matrix permeabilities (<10(-17) m(2)) as well as low to intermediate matrix porosities (<5-15%), thermal conductivities (0.89-1.49 W m(-1) K-1), thermal diffusivities (similar to 0.83 10(-6) m(2) s(-1)), and sonic wave velocities (V-P: similar to 2800-4100 m s(-1), V-S: similar to 1600-2400 m s(-1)). Average magnetic susceptibility and specific heat capacity range between 2.4-7.0 10(-3) SI and 752-772 J kg(-1) K-1, respectively. In contrast, the hydrothermally altered reservoir samples show enhanced porosities (similar to 7-23%), permeabilities (10(-17)-10(-14) m(2)), and thermal properties (> 1.67 W m(-1) K-1; > 0.91 10(-6) m(2) s(-1)), but a significant loss of magnetic susceptibility (10(-3)-10(-6) SI). In particular, this latter characteristic appears to be a suitable indicator during geophysical survey for the identification of hydrothermalized domains and possible pathways for fluids. The lack of clear trends between alteration facies, alteration intensity, and chemical indices in the studied samples is interpreted as the response to multiple and/or repeated hydrothermal events. Finally, the proposed integrated field-based approach shows the capability to unravel the complexity of geothermal reservoir rocks in active volcanic settings.

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    Geothermal Energy
    Article . 2022
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      Geothermal Energy
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    Authors: Solheim, Anders; Kalsnes, Bjørn; Strout, James Michael; Piciullo, Luca; +3 Authors

    Cross-sectorial and cross-disciplinary collaboration, as well as public-private partnerships are necessary to handle the complexity of climate adaptation. The Research Council of Norway has established the Centres for Research-based Innovation (CRI) in which research- and education organizations, public entities and private enterprises join forces in 8-year long collaborations. CRI-Klima 2050 focuses on climate adaptation of buildings and infrastructure and runs several pilot projects to innovate new solutions for building resilience, stormwater- and landslide risk management. Several of the major infrastructure owners in Norway are partners in the centre. Norway is increasingly affected by precipitation triggered landslides. Klima 2050 pilot projects on landslide risk reduction include a web-based toolbox for prioritizing and choosing optimal mitigation measures, including Nature-Based Solutions, improved early warning systems and mitigation measures for slope instability, and improved local warning for hazardous weather systems, all developed in close collaboration between centre partners from different sectors and disciplines. The results of these projects can all be upscaled and are transferable to other infrastructure elements.

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    Frontiers in Earth Science
    Article . 2022
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    Frontiers in Earth Science
    Article . 2022 . Peer-reviewed
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      Frontiers in Earth Science
      Article . 2022 . Peer-reviewed
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    Authors: Favio Cruz-Hernández; Luis A Gallardo; Marco Calò; Raúl R Castro; +1 Authors

    SUMMARYIn the last 15 yr, the use of surface waves retrieved from the cross-correlation of ambient seismic noise has significantly increased its applications to determine or monitor changes in the elastic properties of the Earth's interior. We designed a methodology for laterally constrained surface wave inversion based on a two-stage technique to estimate the 3-D distribution of the S-wave velocity (Vs). The first stage inverts traveltimes to estimate group or phase velocity dispersion maps and their inverse covariance matrix for different periods. The inverse covariance matrix is constructed explicitly using the ray tracing information. The inverse covariance matrix adds the lateral sensitivity of the maps to the structure, whereas the period-dependency provides sensitivity to the structure at depth. The second stage applies a nonlinear conjugate gradient scheme to estimate the 3-D distribution of S-wave velocity using the ensemble of velocity dispersion maps and their estimated inverse covariance matrix. We validate the methodology using a synthetic model. The results show an improved estimation of subsurface S-wave velocity structures compared to conventional point-wise inversion.

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    Geophysical Journal International
    Article . 2022 . Peer-reviewed
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      Geophysical Journal International
      Article . 2022 . Peer-reviewed
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    Authors: Favio Cruz-Hernández; Luis A Gallardo; Marco Calò; Raúl R Castro; +1 Authors

    SUMMARYWe apply a new technique for a laterally constrained surface wave inversion (LCSWI) to estimate the 3-D sedimentary structure of the Cerro Prieto Basin, Baja California, Mexico. The basin contains the Cerro Prieto geothermal field, which is considered one of the most productive in the world. The data used consist of group velocity measurements of Rayleigh waves extracted from cross-correlations of ambient noise registered at 12 stations distributed in an 18 × 12 km area. We estimated an S-wave velocity model that clearly shows three relatively homogeneous geoseismic units that correlate with the stratigraphic column reported in previous studies. The deepest geoseismic unit is the most heterogeneous and shows low-velocity zones likely associated with fluids. The resulting velocity model shows similarity with the conceptual geological model of the geothermal field reported in the literature and recent geophysical studies that suggest the potential existence of another deeper reservoir west of the current exploitation area.

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    Geophysical Journal International
    Article . 2022 . Peer-reviewed
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      Geophysical Journal International
      Article . 2022 . Peer-reviewed
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    Authors: Granados-Chavarría, I.; Calò, M.; Figueroa-Soto, Á.; Jousset, P.;

    Since the nineteen-eighties, the depth, number, position and shape of the heat sources feeding the super-hot geothermal system of the Los Humeros caldera (Mexico) is under debate. With the aim of providing a seismic constraint of this region, we present a high resolution three-dimensional anisotropic shear wave velocity model. We used the continuous records of ambient seismic noise at 45 seismic stations deployed for more than one year. From the data, we obtained a set of about 1444 phase and 1534 group velocity dispersion curves, for Love and Rayleigh waves, respectively. By using the dispersion data, we obtained three dimensional models for shear wave velocities and radial anisotropy down to 17 km of depth. These models allowed to image three low velocity bodies at different depths: 1) a deep storage of potential molten material rising from the depth and stopping at ~11 km of depth, 2) a second storage region from 3 to 8 km of depth, related with the Los Humeros caldera collapse, and that feeds the 3) shallow low-velocity bodies between 1.3 and 2.2 km, representing the expression of the geothermal reservoir currently exploited. All these low velocity bodies are interconnected and represent part of the remnant magmatic plumbing system beneath the Los Humeros caldera. These seismic images provide insights to the deep upward pathways of fluids feeding the geothermal reservoir from the heat source(s) and its relationship with the structures controlling the hydrothermal system. Previous article in issue

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    Journal of Volcanology and Geothermal Research
    Other literature type . Article . 2022 . Peer-reviewed
    License: Elsevier TDM
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      Journal of Volcanology and Geothermal Research
      Other literature type . Article . 2022 . Peer-reviewed
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    Authors: Weydt, L.; Lucci, F.; Lacinska, A.; Scheuvens, D.; +6 Authors

    Hydrothermal alteration is a common process in active geothermal systems and can significantly change the physiochemical properties of rocks. To improve reservoir assessment and modeling of high-temperature geothermal resources linked to active volcanic settings, a detailed understanding of the reservoir is needed. The Los Humeros Volcanic Complex, hosting the third largest exploited geothermal field in Mexico, represents a natural laboratory to investigate the impact of hydrothermal processes on the rock properties through andesitic reservoir cores and outcropping analogs. Complementary petrographic and chemical analyses were used to characterize the intensities and facies of hydrothermal alteration. The alteration varies from argillic and propylitic facies characterized by no significant changes of the REE budget indicating an inert behavior to silicic facies and skarn instead showing highly variable REE contents. Unaltered outcrop samples predominantly feature low matrix permeabilities (<10(-17) m(2)) as well as low to intermediate matrix porosities (<5-15%), thermal conductivities (0.89-1.49 W m(-1) K-1), thermal diffusivities (similar to 0.83 10(-6) m(2) s(-1)), and sonic wave velocities (V-P: similar to 2800-4100 m s(-1), V-S: similar to 1600-2400 m s(-1)). Average magnetic susceptibility and specific heat capacity range between 2.4-7.0 10(-3) SI and 752-772 J kg(-1) K-1, respectively. In contrast, the hydrothermally altered reservoir samples show enhanced porosities (similar to 7-23%), permeabilities (10(-17)-10(-14) m(2)), and thermal properties (> 1.67 W m(-1) K-1; > 0.91 10(-6) m(2) s(-1)), but a significant loss of magnetic susceptibility (10(-3)-10(-6) SI). In particular, this latter characteristic appears to be a suitable indicator during geophysical survey for the identification of hydrothermalized domains and possible pathways for fluids. The lack of clear trends between alteration facies, alteration intensity, and chemical indices in the studied samples is interpreted as the response to multiple and/or repeated hydrothermal events. Finally, the proposed integrated field-based approach shows the capability to unravel the complexity of geothermal reservoir rocks in active volcanic settings.

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    Geothermal Energy
    Article . 2022
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      Geothermal Energy
      Article . 2022
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