Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Rimondi V.[2"'
Autor:
Zucchi M.[1], Brogi A.[1], Liotta D.[1, Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A. [3]
Publikováno v:
Geothermics 70 (2017): 125–145. doi:10.1016/j.geothermics.2017.05.007
info:cnr-pdr/source/autori:Zucchi M.[1], Brogi A.[1], Liotta D.[1,3], Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A. [3]/titolo:Permeability and hydraulic conductivity of faulted micaschist in the eastern Elba Island exhumed geothermal system (Tyrrhenian sea, Italy): insights from Cala Stagnone/doi:10.1016%2Fj.geothermics.2017.05.007/rivista:Geothermics/anno:2017/pagina_da:125/pagina_a:145/intervallo_pagine:125–145/volume:70
info:cnr-pdr/source/autori:Zucchi M.[1], Brogi A.[1], Liotta D.[1,3], Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A. [3]/titolo:Permeability and hydraulic conductivity of faulted micaschist in the eastern Elba Island exhumed geothermal system (Tyrrhenian sea, Italy): insights from Cala Stagnone/doi:10.1016%2Fj.geothermics.2017.05.007/rivista:Geothermics/anno:2017/pagina_da:125/pagina_a:145/intervallo_pagine:125–145/volume:70
Estimating values of permeability (k), efficient porosity (P) and hydraulic conductivity (K) by analysing field outcrops as analogue of geothermal reservoirs, is a timely theme useful for predictions during geothermal exploration programs. In this pa
Publikováno v:
Applied geochemistry 117 (2020): 1–9. doi:10.1016/j.apgeochem.2020.104600
info:cnr-pdr/source/autori:Pribil M.J.[1], Rimondi V.[2,3], Costagliola P.[2,3], Lattanzi P.[3], Rutherford D.L.[1]/titolo:Assessing mercury distribution using isotopic fractionation of mercury processes and sources adjacent and downstream of a legacy mine district in Tuscany, Italy/doi:10.1016%2Fj.apgeochem.2020.104600/rivista:Applied geochemistry/anno:2020/pagina_da:1/pagina_a:9/intervallo_pagine:1–9/volume:117
info:cnr-pdr/source/autori:Pribil M.J.[1], Rimondi V.[2,3], Costagliola P.[2,3], Lattanzi P.[3], Rutherford D.L.[1]/titolo:Assessing mercury distribution using isotopic fractionation of mercury processes and sources adjacent and downstream of a legacy mine district in Tuscany, Italy/doi:10.1016%2Fj.apgeochem.2020.104600/rivista:Applied geochemistry/anno:2020/pagina_da:1/pagina_a:9/intervallo_pagine:1–9/volume:117
Mercury (Hg) concentrations and isotopic compositions in a range of sample types collected from the legacy Abbadia San Salvatore Mine (ASSM) area were used to evaluate the distribution of Hg in the region. The district generated more than 100,000 met
Autor:
Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2, Brogi A.[4], Liotta D. [4, Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6
Publikováno v:
Sedimentary Geology 364 (2018): 180–203. doi:10.1016/j.sedgeo.2017.12.012
info:cnr-pdr/source/autori:Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2,3], Brogi A.[4], Liotta D. [4,5], Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6,8]/titolo:Calcite veining and feeding conduits in a hydrothermal system: Insights from a natural section across the Pleistocene Golemezli travertine depositional system (western Anatolia, Turkey)/doi:10.1016%2Fj.sedgeo.2017.12.012/rivista:Sedimentary Geology/anno:2018/pagina_da:180/pagina_a:203/intervallo_pagine:180–203/volume:364
Università degli studi di Firenze-IRIS
info:cnr-pdr/source/autori:Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2,3], Brogi A.[4], Liotta D. [4,5], Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6,8]/titolo:Calcite veining and feeding conduits in a hydrothermal system: Insights from a natural section across the Pleistocene Golemezli travertine depositional system (western Anatolia, Turkey)/doi:10.1016%2Fj.sedgeo.2017.12.012/rivista:Sedimentary Geology/anno:2018/pagina_da:180/pagina_a:203/intervallo_pagine:180–203/volume:364
Università degli studi di Firenze-IRIS
Linking the architecture of structural conduits with the hydrothermal fluids migrating from the reservoir up to the surface is a key-factor in geothermal research. A contribution to this achievement derives from the study of spring-related travertine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::696f546238756cc039b7bdc357071368
https://hdl.handle.net/11499/10859
https://hdl.handle.net/11499/10859
Autor:
Zucchi M.[1], Brogi A.[1], Liotta D.[1, Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A.[3]
Publikováno v:
Geothermics 70 (2017): 125–145. doi:10.1016/j.geothermics.2017.05.007
info:cnr-pdr/source/autori:Zucchi M.[1], Brogi A.[1], Liotta D.[1,3], Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A.[3]/titolo:Keywords: Geothermal reservoir Analogue Exhumed geothermal system Micaschist Elba island/doi:10.1016%2Fj.geothermics.2017.05.007/rivista:Geothermics/anno:2017/pagina_da:125/pagina_a:145/intervallo_pagine:125–145/volume:70
info:cnr-pdr/source/autori:Zucchi M.[1], Brogi A.[1], Liotta D.[1,3], Rimondi V.[2], Ruggieri G.[2], Montegrossi G.[2], Caggianelli A.[1], Dini A.[3]/titolo:Keywords: Geothermal reservoir Analogue Exhumed geothermal system Micaschist Elba island/doi:10.1016%2Fj.geothermics.2017.05.007/rivista:Geothermics/anno:2017/pagina_da:125/pagina_a:145/intervallo_pagine:125–145/volume:70
Estimating values of permeability (k), efficient porosity (P) and hydraulic conductivity (K) by analysing field outcrops as analogue of geothermal reservoirs, is a timely theme useful for predictions during geothermal exploration programs. In this pa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::f86c2d4505ad2914455a87d169e49448
https://publications.cnr.it/doc/461100
https://publications.cnr.it/doc/461100
Publikováno v:
Applied geochemistry 87 (2017): 176–187. doi:10.1016/j.apgeochem.2017.10.024
info:cnr-pdr/source/autori:Morelli G.[1,2], Rimondi V.[2], Benvenuti M.[3], Medas D.[4], Costagliola P.[3], Gasparon M.[1]/titolo:Experimental simulation of arsenic desorption from Quaternary aquifer sediments following sea water intrusion/doi:10.1016%2Fj.apgeochem.2017.10.024/rivista:Applied geochemistry/anno:2017/pagina_da:176/pagina_a:187/intervallo_pagine:176–187/volume:87
info:cnr-pdr/source/autori:Morelli G.[1,2], Rimondi V.[2], Benvenuti M.[3], Medas D.[4], Costagliola P.[3], Gasparon M.[1]/titolo:Experimental simulation of arsenic desorption from Quaternary aquifer sediments following sea water intrusion/doi:10.1016%2Fj.apgeochem.2017.10.024/rivista:Applied geochemistry/anno:2017/pagina_da:176/pagina_a:187/intervallo_pagine:176–187/volume:87
Alluvial sediments from the coastal area in southern Tuscany (Italy) characterized by a significant As anomaly (As >500 mg/kg) are subjected to seawater intrusion due to groundwater exploitation. Sequential extractions and kinetic experiments were ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b7488f6026435c150cec7aea7b73c215