Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Capecchiacci F. [1"'
Autor:
Venturi S.[1, Tassi F.[1, Cabassi J.[2], Randazzo A.[1, Lazzaroni M.[1, Capecchiacci F.[1, 2, Vietina B.[4], Vaselli O.[1
Publikováno v:
Applied Sciences; Volume 11; Issue 24; Pages: 12156
Applied Sciences, Vol 11, Iss 12156, p 12156 (2021)
Applied sciences 11 (2021): 1–26. doi:10.3390/app112412156
info:cnr-pdr/source/autori:Venturi S.[1,2], Tassi F.[1,2], Cabassi J.[2], Randazzo A.[1,2], Lazzaroni M.[1,2], Capecchiacci F.[1,2,3], Vietina B.[4], Vaselli O.[1,2]/titolo:Exploring Methane Emission Drivers in Wetlands: The Cases of Massaciuccoli and Porta Lakes (Northern Tuscany, Italy)/doi:10.3390%2Fapp112412156/rivista:Applied sciences/anno:2021/pagina_da:1/pagina_a:26/intervallo_pagine:1–26/volume:11
Applied Sciences, Vol 11, Iss 12156, p 12156 (2021)
Applied sciences 11 (2021): 1–26. doi:10.3390/app112412156
info:cnr-pdr/source/autori:Venturi S.[1,2], Tassi F.[1,2], Cabassi J.[2], Randazzo A.[1,2], Lazzaroni M.[1,2], Capecchiacci F.[1,2,3], Vietina B.[4], Vaselli O.[1,2]/titolo:Exploring Methane Emission Drivers in Wetlands: The Cases of Massaciuccoli and Porta Lakes (Northern Tuscany, Italy)/doi:10.3390%2Fapp112412156/rivista:Applied sciences/anno:2021/pagina_da:1/pagina_a:26/intervallo_pagine:1–26/volume:11
Wetlands are hotspots of CH4 emissions to the atmosphere, mainly sustained by microbial decomposition of organic matter in anoxic sediments. Several knowledge gaps exist on how environmental drivers shape CH4 emissions from these ecosystems, posing c
Publikováno v:
Chemosphere 297 (2022). doi:10.1016/j.chemosphere.2022.134166
info:cnr-pdr/source/autori:Biagi R.[1], Tassi F.[1,2], Caliro S.[3], Capecchiacci F.[1,3], Venturi S.[2]/titolo:Impact on air quality of carbon and sulfur volatile compounds emitted from hydrothermal discharges: The case study of Pisciarelli (Campi Flegrei, South Italy)/doi:10.1016%2Fj.chemosphere.2022.134166/rivista:Chemosphere/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:297
info:cnr-pdr/source/autori:Biagi R.[1], Tassi F.[1,2], Caliro S.[3], Capecchiacci F.[1,3], Venturi S.[2]/titolo:Impact on air quality of carbon and sulfur volatile compounds emitted from hydrothermal discharges: The case study of Pisciarelli (Campi Flegrei, South Italy)/doi:10.1016%2Fj.chemosphere.2022.134166/rivista:Chemosphere/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:297
Volcanoes are currently to be regarded as natural sources of air pollutants. Climatic and environmental forcing of large volcanic eruptions are well known, although gases emitted through passive degassing during periods of quiescence or hydrothermal
Autor:
Cabassi J.[1, Capecchiacci F.[1, Magi F.[1, Vaselli O.[1, Tassi F.[1, Montalvo F.[4], Esquivel I.[4], Grassa F.[5], Caprai A. [6]
Publikováno v:
Journal of volcanology and geothermal research 378 (2019): 1–15. doi:10.1016/j.jvolgeores.2019.04.009
info:cnr-pdr/source/autori:Cabassi J.[1,2], Capecchiacci F.[1,2], Magi F.[1,3], Vaselli O.[1,2], Tassi F.[1,2], Montalvo F.[4], Esquivel I.[4], Grassa F.[5], Caprai A. [6]/titolo:Water and dissolved gas geochemistry at Coatepeque, Ilopango and Chanmico volcanic lakes (El Salvador, Central America)/doi:10.1016%2Fj.jvolgeores.2019.04.009/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:378
info:cnr-pdr/source/autori:Cabassi J.[1,2], Capecchiacci F.[1,2], Magi F.[1,3], Vaselli O.[1,2], Tassi F.[1,2], Montalvo F.[4], Esquivel I.[4], Grassa F.[5], Caprai A. [6]/titolo:Water and dissolved gas geochemistry at Coatepeque, Ilopango and Chanmico volcanic lakes (El Salvador, Central America)/doi:10.1016%2Fj.jvolgeores.2019.04.009/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:378
Coatepeque (on the E slope of Santa Ana Volcano), Ilopango (inside Ilopango Caldera) and Chanmico (associated with San Salvador Volcano) are volcanic lakes in El Salvador, showing a thermocline at a relatively shallow depth (from 30 to 40 m, from 20
Autor:
Tassi F.[1, Cabassi J.[1, Calabrese S.[3], Nisi B.[4], Venturi S.[1, Capecchiacci F.[1, Giannini L.[1], Vaselli O.[1
Publikováno v:
Applied geochemistry 66 (2016): 234–241. doi:10.1016/j.apgeochem.2016.01.002
info:cnr-pdr/source/autori:Tassi F.[1,2], Cabassi J.[1,2], Calabrese S.[3], Nisi B.[4], Venturi S.[1,2], Capecchiacci F.[1,2], Giannini L.[1], Vaselli O.[1,2]/titolo:Diffuse soil gas emissions of gaseous elemental mercury (GEM) from hydrothermal-volcanic systems: An innovative approach by using the static closed-chamber method/doi:10.1016%2Fj.apgeochem.2016.01.002/rivista:Applied geochemistry/anno:2016/pagina_da:234/pagina_a:241/intervallo_pagine:234–241/volume:66
info:cnr-pdr/source/autori:Tassi F.[1,2], Cabassi J.[1,2], Calabrese S.[3], Nisi B.[4], Venturi S.[1,2], Capecchiacci F.[1,2], Giannini L.[1], Vaselli O.[1,2]/titolo:Diffuse soil gas emissions of gaseous elemental mercury (GEM) from hydrothermal-volcanic systems: An innovative approach by using the static closed-chamber method/doi:10.1016%2Fj.apgeochem.2016.01.002/rivista:Applied geochemistry/anno:2016/pagina_da:234/pagina_a:241/intervallo_pagine:234–241/volume:66
This study was aimed to test a new methodological approach to carry out measurements of gaseous elemental mercury (GEM) diffusively emitted from soils in hydrothermal-volcanic environments. This method was based on the use of a static closed-chamber
Autor:
Tassi F.[1, Venturi S.[1], Cabassi J.[1], Vaselli O.[1, Gelli I.[1], Cinti D. [3], Capecchiacci F. [1
Publikováno v:
Organic geochemistry 86 (2015): 81–93. doi:10.1016/j.orggeochem.2015.06.004
info:cnr-pdr/source/autori:Tassi F.[1,2], Venturi S.[1], Cabassi J.[1], Vaselli O.[1,2], Gelli I.[1], Cinti D. [3], Capecchiacci F. [1,2]/titolo:Biodegradation of CO2, CH4 and volatile organic compounds (VOCs) in soil gas from the Vicano-Cimino hydrothermal system (central Italy)/doi:10.1016%2Fj.orggeochem.2015.06.004/rivista:Organic geochemistry/anno:2015/pagina_da:81/pagina_a:93/intervallo_pagine:81–93/volume:86
info:cnr-pdr/source/autori:Tassi F.[1,2], Venturi S.[1], Cabassi J.[1], Vaselli O.[1,2], Gelli I.[1], Cinti D. [3], Capecchiacci F. [1,2]/titolo:Biodegradation of CO2, CH4 and volatile organic compounds (VOCs) in soil gas from the Vicano-Cimino hydrothermal system (central Italy)/doi:10.1016%2Fj.orggeochem.2015.06.004/rivista:Organic geochemistry/anno:2015/pagina_da:81/pagina_a:93/intervallo_pagine:81–93/volume:86
We investigated the effect of microbial activity on the chemistry of hydrothermal fluids related to the Vicano-Cimino system, central Italy. The database included the composition and delta C-13 CO2 and delta C-13 CH4 values for soil gas from an area
Publikováno v:
Applied geochemistry 56 (2015): 37–49. doi:10.1016/j.apgeochem.2015.02.005
info:cnr-pdr/source/autori:Tassi F. [1,2] Venturi S.[1], Cabassi J.[1], Capecchiacci F.[1,2], Nisi B.[3], Vaselli O. [1,2]/titolo:Volatile organic compounds (VOCs) in soil gases from Solfatara crater (Campi Flegrei, southern Italy): Geogenic source(s) vs. biogeochemical processes/doi:10.1016%2Fj.apgeochem.2015.02.005/rivista:Applied geochemistry/anno:2015/pagina_da:37/pagina_a:49/intervallo_pagine:37–49/volume:56
info:cnr-pdr/source/autori:Tassi F. [1,2] Venturi S.[1], Cabassi J.[1], Capecchiacci F.[1,2], Nisi B.[3], Vaselli O. [1,2]/titolo:Volatile organic compounds (VOCs) in soil gases from Solfatara crater (Campi Flegrei, southern Italy): Geogenic source(s) vs. biogeochemical processes/doi:10.1016%2Fj.apgeochem.2015.02.005/rivista:Applied geochemistry/anno:2015/pagina_da:37/pagina_a:49/intervallo_pagine:37–49/volume:56
The chemical composition of volatile organic compounds (VOCs) in soil gases from the Solfatara crater (Campi Flegrei, Italy) was analyzed to investigate the effects of biogeochemical processes on gases discharged from the hydrothermal reservoir and r
Autor:
Tassi F.[1, Fazi S.[3], Rossetti S.[3], Pratesi P.[1], Ceccotti M.[3], Cabassi J.[1, Capecchiacci F.[1], Venturi S.[1, Vaselli O.[1
Publikováno v:
PloS one 13 (2018): 1–26. doi:10.1371/journal.pone.0193914
info:cnr-pdr/source/autori:Tassi F.[1,2], Fazi S.[3], Rossetti S.[3], Pratesi P.[1], Ceccotti M.[3], Cabassi J.[1,2], Capecchiacci F.[1], Venturi S.[1,2], Vaselli O.[1,2]/titolo:The biogeochemical vertical structure renders a meromictic volcanic lake a trap for geogenic CO2 (Lake Averno, Italy)/doi:10.1371%2Fjournal.pone.0193914/rivista:PloS one/anno:2018/pagina_da:1/pagina_a:26/intervallo_pagine:1–26/volume:13
PLoS ONE, Vol 13, Iss 3, p e0193914 (2018)
PLoS ONE
info:cnr-pdr/source/autori:Tassi F.[1,2], Fazi S.[3], Rossetti S.[3], Pratesi P.[1], Ceccotti M.[3], Cabassi J.[1,2], Capecchiacci F.[1], Venturi S.[1,2], Vaselli O.[1,2]/titolo:The biogeochemical vertical structure renders a meromictic volcanic lake a trap for geogenic CO2 (Lake Averno, Italy)/doi:10.1371%2Fjournal.pone.0193914/rivista:PloS one/anno:2018/pagina_da:1/pagina_a:26/intervallo_pagine:1–26/volume:13
PLoS ONE, Vol 13, Iss 3, p e0193914 (2018)
PLoS ONE
Volcanic lakes are characterized by physicochemical favorable conditions for the development of reservoirs of C-bearing greenhouse gases that can be dispersed to air during occasional rollover events. By combining a microbiological and geochemical ap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3dee7984c711f4b5395da51f93638ad2
https://publications.cnr.it/doc/385621
https://publications.cnr.it/doc/385621
Autor:
Vaselli O.[1, Rappuoli D.[3], Nisi B.[4], Bianchi F.[5], Tassi F.[1, Cabassi J.[2], Giannini L.[2], Magi F.[1], Capecchiacci F.[1, Maddii V. [1]
Publikováno v:
Il Vulcano di Monte Amiata, edited by a cura di Claudia Principe, Guido Lavorini e Luigina M. Vezzoli, pp. 283–302, 2017
info:cnr-pdr/source/autori:Vaselli O.[1,2], Rappuoli D.[3], Nisi B.[4], Bianchi F.[5], Tassi F.[1,2], Cabassi J.[2], Giannini L.[2], Magi F.[1], Capecchiacci F.[1,2], Maddii V. [1]/titolo:Geochimica delle acque di Galleria Italia (Abbadia San Salvatore, Siena)/titolo_volume:Il Vulcano di Monte Amiata/curatori_volume:a cura di Claudia Principe, Guido Lavorini e Luigina M. Vezzoli/editore:/anno:2017
info:cnr-pdr/source/autori:Vaselli O.[1,2], Rappuoli D.[3], Nisi B.[4], Bianchi F.[5], Tassi F.[1,2], Cabassi J.[2], Giannini L.[2], Magi F.[1], Capecchiacci F.[1,2], Maddii V. [1]/titolo:Geochimica delle acque di Galleria Italia (Abbadia San Salvatore, Siena)/titolo_volume:Il Vulcano di Monte Amiata/curatori_volume:a cura di Claudia Principe, Guido Lavorini e Luigina M. Vezzoli/editore:/anno:2017
This paper presents and discusses the geochemical and isotopic data obtained on the waters from Galleria Italia (Abbadia San Salvatore) during a discontinuous monitoring carried out from January 2009 to April 2017. The Galleria Italia waters are char
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::bfdde0a7f836685e7ff141a09b4c1061
https://publications.cnr.it/doc/382475
https://publications.cnr.it/doc/382475
Autor:
Cabassi J.[1, Tassi F.[1, 2] Venturi S.[1, Calabrese S.[3], Capecchiacci F.[1, D'Alessandro W.[4], Vaselli O. [1
Publikováno v:
Journal of geochemical exploration 175 (2017): 48–58. doi:10.1016/j.gexplo.2016.12.017
info:cnr-pdr/source/autori:Cabassi J.[1,2], Tassi F.[1,2] Venturi S.[1,2], Calabrese S.[3], Capecchiacci F.[1,2], D'Alessandro W.[4], Vaselli O. [1,2]/titolo:A new approach for the measurement of gaseous elemental mercury (GEM) and H2S in air from anthropogenic and natural sources: Examples from Mt. Amiata (Siena, Central Italy) and Solfatara Crater (Campi Flegrei, Southern Italy)/doi:10.1016%2Fj.gexplo.2016.12.017/rivista:Journal of geochemical exploration/anno:2017/pagina_da:48/pagina_a:58/intervallo_pagine:48–58/volume:175
info:cnr-pdr/source/autori:Cabassi J.[1,2], Tassi F.[1,2] Venturi S.[1,2], Calabrese S.[3], Capecchiacci F.[1,2], D'Alessandro W.[4], Vaselli O. [1,2]/titolo:A new approach for the measurement of gaseous elemental mercury (GEM) and H2S in air from anthropogenic and natural sources: Examples from Mt. Amiata (Siena, Central Italy) and Solfatara Crater (Campi Flegrei, Southern Italy)/doi:10.1016%2Fj.gexplo.2016.12.017/rivista:Journal of geochemical exploration/anno:2017/pagina_da:48/pagina_a:58/intervallo_pagine:48–58/volume:175
Real-time measurements of GEM and H2S discharged from natural and anthropogenic sources are a valuable tool to investigate the dispersion dynamics of these contaminants in air. In this study, a new approach to measure GEM and H2S concentrations in ai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b90325919327bc497fdf6ad03ab4f464
http://www.cnr.it/prodotto/i/369347
http://www.cnr.it/prodotto/i/369347
Autor:
Venturi S.[1, Tassi F.[1, Gould I.[3], Shock E.[3, Hartnett H.[3, Lorance E. [5], Bockisch C.[3], Fecteau K.[3], Capecchiacci F.[1], Vaselli O.[1
Publikováno v:
Journal of volcanology and geothermal research 346 (2017): 21–27.
info:cnr-pdr/source/autori:Venturi S.[1,2], Tassi F.[1,2], Gould I.[3], Shock E.[3,4], Hartnett H.[3,4], Lorance E. [5], Bockisch C.[3], Fecteau K.[3], Capecchiacci F.[1], Vaselli O.[1,2]/titolo:Mineral-assisted production of benzene under hydrothermal conditions: Insights from experimental studies on C6 cyclic hydrocarbons/doi:/rivista:Journal of volcanology and geothermal research/anno:2017/pagina_da:21/pagina_a:27/intervallo_pagine:21–27/volume:346
info:cnr-pdr/source/autori:Venturi S.[1,2], Tassi F.[1,2], Gould I.[3], Shock E.[3,4], Hartnett H.[3,4], Lorance E. [5], Bockisch C.[3], Fecteau K.[3], Capecchiacci F.[1], Vaselli O.[1,2]/titolo:Mineral-assisted production of benzene under hydrothermal conditions: Insights from experimental studies on C6 cyclic hydrocarbons/doi:/rivista:Journal of volcanology and geothermal research/anno:2017/pagina_da:21/pagina_a:27/intervallo_pagine:21–27/volume:346
Volatile Organic Compounds (VOCs) are ubiquitously present at low but detectable concentrations in hydrothermal fluids from volcanic and geothermal systems. Although their behavior is strictly controlled by physical and chemical parameters, the mecha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::5b252a07a65f87474c0e6068c2dcc0c9
https://publications.cnr.it/doc/378382
https://publications.cnr.it/doc/378382