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  • Authors: Curbelo Hernández, David; González Dávila, Melchor; González Santana, David; González González, Aridane; +1 Authors

    The seasonal and spatial variability of the CO2 system parameters and air-sea CO2 exchange was studied in the Northeast Atlantic through the Northwest African coastal transitional area between the Canary Islands and the Strait of Gibraltar. High spatio-temporal resolution data were collected by a Surface Ocean Observation Platform (SOOP) aboard a volunteer observing ship (VOS) from February 2019 to February 2020. The variability of the CO2 fugacity in seawater (fCO2,sw) was strongly driven by the seasonal pattern of the sea surface temperature (SST), which increased with latitude and was lower throughout the year in the high-intense coastal upwelling areas. The fCO2,sw increased from winter to summer by 11.84 ± 0.28 μatm ºC-1 in the Canary archipelago and by 11.71 ± 0.25 μatm ºC-1 along the northwest African continental shelf. The thermal to non-thermal effect ratio (T/B) was approximately 2, with minimum values along the African coastline explained by higher biological activity in the upwelled waters. The factors controlling the seasonality of total inorganic carbon (CT) normalized to constant salinity of 36.7 (NCT) were assessed. The effect of net community production on NCT between February and October represented >90% of the reduction of inorganic carbon while air-sea CO2 exchange described <6%. The seasonality of air-sea CO2 fluxes was driven by SST fluctuations. The surface waters of the entire region acted as a strong CO2 sink during the cold months and as a weak CO2 source during the warm months. A net annual CO2 sink behaviour was observed in both the Canary basin (-0.26 ± 0.04 mol C m-2 yr-1) and the northwest African continental shelf (-0.48 ± 0.09 mol C m-2 yr-1). The calculated average CO2 flux for the entire area in the Northeast Atlantic was -2.65 ± 0.44 Tg CO2 yr-1 (-0.72 ± 0.12 Tg C yr-1). 33 1

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    Authors: Romero March, Romualdo;

    Abstract not avalaible

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    Authors: Rahimzadeh Kivi, I.; Vilarrasa, Víctor; Makhnenko, R.;

    Geologic storage of carbon dioxide (CO2), mainly in deep saline aquifers, has emerged as a key solution to reach the Paris Agreement goal of limiting the global temperature increase below 2ºC and effectively mitigate climate change. The injected CO2 is less dense at the storage condictions than the resident brine and tends to flow upward by buoyancy. Therefore, to achieve the primary objective of permanently storing CO2 underground during geological time scales, the host reservoir should be overlain by a low-permeability and high-entry pressure caprock that prevents CO2 escaping from the storage formation. Meanwhile, the caprock sealing capacity is of particular significance and yet to be assessed in more detail. In this presentation, we aim at shedding light on the flow processes governing potential CO2 leakage through shaly caprocks by combining experimental observations and numerical simulations. We present breakthrough experiments on Opalinus Clay, which is a representative caprock for CO2 storage. These experiments reproduce supercritical CO2 intrusion and flow through the caprock sample under representative reservoir conditions. Next, we address numerical simulation of the breakthrough experiments using a twophase flow model in deformable porous media to provide a mechanistic interpretation of experimental observations. Overall, we conclude that CO2 leakage through the caprock is dominated by molecular diffusion rather than by rapid bulk volumetric advection. Peer reviewed

    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/ Recolector de Cienci...arrow_drop_down
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    Authors: Alejandro Ramón-Ballesta;

    Esta guía recopila una serie de actividades prácticas relacionadas con la hidrosfera y la geosfera destinadas a alumnos de la asignatura Didáctica de las Ciencias Experimentales I del Grado en Educación Primaria Bilingüe a realizar durante una salida de campo que incluye una visita guiada a la Cueva de Nerja en Málaga y a la Playa de La Herradura. Universidad de Granada. Departamento de Didáctica de las Ciencias Experimentales

    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/ Recolector de Cienci...arrow_drop_down
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  • Authors: Curbelo Hernández, David; González Dávila, Melchor; González Santana, David; González González, Aridane; +1 Authors

    The seasonal and spatial variability of the CO2 system parameters and air-sea CO2 exchange was studied in the Northeast Atlantic through the Northwest African coastal transitional area between the Canary Islands and the Strait of Gibraltar. High spatio-temporal resolution data were collected by a Surface Ocean Observation Platform (SOOP) aboard a volunteer observing ship (VOS) from February 2019 to February 2020. The variability of the CO2 fugacity in seawater (fCO2,sw) was strongly driven by the seasonal pattern of the sea surface temperature (SST), which increased with latitude and was lower throughout the year in the high-intense coastal upwelling areas. The fCO2,sw increased from winter to summer by 11.84 ± 0.28 μatm ºC-1 in the Canary archipelago and by 11.71 ± 0.25 μatm ºC-1 along the northwest African continental shelf. The thermal to non-thermal effect ratio (T/B) was approximately 2, with minimum values along the African coastline explained by higher biological activity in the upwelled waters. The factors controlling the seasonality of total inorganic carbon (CT) normalized to constant salinity of 36.7 (NCT) were assessed. The effect of net community production on NCT between February and October represented >90% of the reduction of inorganic carbon while air-sea CO2 exchange described <6%. The seasonality of air-sea CO2 fluxes was driven by SST fluctuations. The surface waters of the entire region acted as a strong CO2 sink during the cold months and as a weak CO2 source during the warm months. A net annual CO2 sink behaviour was observed in both the Canary basin (-0.26 ± 0.04 mol C m-2 yr-1) and the northwest African continental shelf (-0.48 ± 0.09 mol C m-2 yr-1). The calculated average CO2 flux for the entire area in the Northeast Atlantic was -2.65 ± 0.44 Tg CO2 yr-1 (-0.72 ± 0.12 Tg C yr-1). 33 1

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    Authors: Romero March, Romualdo;

    Abstract not avalaible

    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/ Recolector de Cienci...arrow_drop_down
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    Authors: Rahimzadeh Kivi, I.; Vilarrasa, Víctor; Makhnenko, R.;

    Geologic storage of carbon dioxide (CO2), mainly in deep saline aquifers, has emerged as a key solution to reach the Paris Agreement goal of limiting the global temperature increase below 2ºC and effectively mitigate climate change. The injected CO2 is less dense at the storage condictions than the resident brine and tends to flow upward by buoyancy. Therefore, to achieve the primary objective of permanently storing CO2 underground during geological time scales, the host reservoir should be overlain by a low-permeability and high-entry pressure caprock that prevents CO2 escaping from the storage formation. Meanwhile, the caprock sealing capacity is of particular significance and yet to be assessed in more detail. In this presentation, we aim at shedding light on the flow processes governing potential CO2 leakage through shaly caprocks by combining experimental observations and numerical simulations. We present breakthrough experiments on Opalinus Clay, which is a representative caprock for CO2 storage. These experiments reproduce supercritical CO2 intrusion and flow through the caprock sample under representative reservoir conditions. Next, we address numerical simulation of the breakthrough experiments using a twophase flow model in deformable porous media to provide a mechanistic interpretation of experimental observations. Overall, we conclude that CO2 leakage through the caprock is dominated by molecular diffusion rather than by rapid bulk volumetric advection. Peer reviewed

    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/ Recolector de Cienci...arrow_drop_down
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    Authors: Alejandro Ramón-Ballesta;

    Esta guía recopila una serie de actividades prácticas relacionadas con la hidrosfera y la geosfera destinadas a alumnos de la asignatura Didáctica de las Ciencias Experimentales I del Grado en Educación Primaria Bilingüe a realizar durante una salida de campo que incluye una visita guiada a la Cueva de Nerja en Málaga y a la Playa de La Herradura. Universidad de Granada. Departamento de Didáctica de las Ciencias Experimentales

    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/ Recolector de Cienci...arrow_drop_down
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