Zobrazeno 1 - 10
of 43
pro vyhledávání: '"Tassi F.[1]"'
Autor:
Lazzaroni M.[1], Ceccatelli M.[1], Rossato L.[2], Nisi B.[3], Venturi S.[1, Fanti R.[1], Tassi F.[1, Vaselli O.[1
Publikováno v:
Italian Journal of Geosciences (Testo stamp.) 140 (2021): 121–140. doi:10.3301/IJG.2020.23
info:cnr-pdr/source/autori:Lazzaroni M.[1], Ceccatelli M.[1], Rossato L.[2], Nisi B.[3], Venturi S.[1,3], Fanti R.[1], Tassi F.[1,3],Vaselli O.[1,3]/titolo:Boron pollution in the shallow groundwater system from Isola di Castelluccio (central-eastern, Tuscany): Evidences from a geochemical survey and new remediation perspectives from a recently-installed hydraulic barrier and hydrogeological modelling/doi:10.3301%2FIJG.2020.23/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2021/pagina_da:121/pagina_a:140/intervallo_pagine:121–140/volume:140
info:cnr-pdr/source/autori:Lazzaroni M.[1], Ceccatelli M.[1], Rossato L.[2], Nisi B.[3], Venturi S.[1,3], Fanti R.[1], Tassi F.[1,3],Vaselli O.[1,3]/titolo:Boron pollution in the shallow groundwater system from Isola di Castelluccio (central-eastern, Tuscany): Evidences from a geochemical survey and new remediation perspectives from a recently-installed hydraulic barrier and hydrogeological modelling/doi:10.3301%2FIJG.2020.23/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2021/pagina_da:121/pagina_a:140/intervallo_pagine:121–140/volume:140
A severe boron pollution has been recognized in the shallow aquifer of Isola di Castelluccio (central-eastern Tuscany, Italy) since 2009. Previous investigations showed that the high boron concentrations (up to 57 mg L-1) were related to an anthropog
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:
Randazzo A.[1], Asensio-Ramos M.[2], Melián G.V. [2, Venturi S.[1, Padrón E. [2, 3, Hernández P.A.[2, Perez N.M.[2, Tassi F.[1
Publikováno v:
Science of the total environment 726 (2020). doi:10.1016/j.scitotenv.2020.138326
info:cnr-pdr/source/autori:Randazzo A.[1], Asensio-Ramos M.[2], Melián G.V. [2,3], Venturi S.[1,4], Padrón E. [2,3,5], Hernández P.A.[2,3,5], Perez N.M.[2,3,5], Tassi F.[1,4]/titolo:Volatile organic compounds (VOCs) in solid waste landfill cover soil: Chemical and isotopic composition vs. degradation processes/doi:10.1016%2Fj.scitotenv.2020.138326/rivista:Science of the total environment/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:726
info:cnr-pdr/source/autori:Randazzo A.[1], Asensio-Ramos M.[2], Melián G.V. [2,3], Venturi S.[1,4], Padrón E. [2,3,5], Hernández P.A.[2,3,5], Perez N.M.[2,3,5], Tassi F.[1,4]/titolo:Volatile organic compounds (VOCs) in solid waste landfill cover soil: Chemical and isotopic composition vs. degradation processes/doi:10.1016%2Fj.scitotenv.2020.138326/rivista:Science of the total environment/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:726
Landfills for solid waste disposal release to the atmosphere a large variety of volatile organic compounds (VOCs). Bacterial activity in landfill cover soils can play an important role in mitigating VOC emission. In order to evaluate the effects of d
Autor:
Tassi F.[1, Feyzullayev A.A.[3], Bonini M.[2], Sani F.[1, Aliyev C.S.[3], Darrah T.H.[4, Vaselli O.[1, Baghirli R.J.[3]
Publikováno v:
Applied geochemistry 118 (2020): 1–12. doi:10.1016/j.apgeochem.2020.104643
info:cnr-pdr/source/autori:Tassi F.[1,2], Feyzullayev A.A.[3], Bonini M.[2], Sani F.[1,2], Aliyev C.S.[3], Darrah T.H.[4,5], Vaselli O.[1,2], Baghirli R.J.[3]/titolo:Mantle vs. crustal fluid sources in the gas discharges from Lesser Caucasus and Talysh Mountains (Azerbaijan) in relation to the regional geotectonic setting/doi:10.1016%2Fj.apgeochem.2020.104643/rivista:Applied geochemistry/anno:2020/pagina_da:1/pagina_a:12/intervallo_pagine:1–12/volume:118
info:cnr-pdr/source/autori:Tassi F.[1,2], Feyzullayev A.A.[3], Bonini M.[2], Sani F.[1,2], Aliyev C.S.[3], Darrah T.H.[4,5], Vaselli O.[1,2], Baghirli R.J.[3]/titolo:Mantle vs. crustal fluid sources in the gas discharges from Lesser Caucasus and Talysh Mountains (Azerbaijan) in relation to the regional geotectonic setting/doi:10.1016%2Fj.apgeochem.2020.104643/rivista:Applied geochemistry/anno:2020/pagina_da:1/pagina_a:12/intervallo_pagine:1–12/volume:118
Azerbaijan is famous for the impressive phenomenon of mud volcanism that dominates the landscape of the central sector of the country. The gases released are here strongly CH4 enriched. Conversely, the Lesser Caucasus to the NW host numerous thermo-m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d58643e771a2834c07a58bf6f20ba4c0
http://www.cnr.it/prodotto/i/424344
http://www.cnr.it/prodotto/i/424344
Autor:
Cabassi J.[1], Venturi S.[1, Di Bennardo F.[2], Nisi B.[1], Tassi F.[1, Magi F.[2, 3, Ricci A.[5, Picchi G.[2], O. Vaselli O.[1
Publikováno v:
Journal of geochemical exploration 228 (2021): 1–9. doi:10.1016/j.gexplo.2021.106824
info:cnr-pdr/source/autori:Cabassi J.[1], Venturi S.[1,2], Di Bennardo F.[2], Nisi B.[1], Tassi F.[1,2], Magi F.[2,3,4], Ricci A.[5,6], Picchi G.[2], O. Vaselli O.[1,2]/titolo:Flux measurements of gaseous elemental mercury (GEM) from the geothermal area of "Le Biancane" natural park (Monterotondo Marittimo, Grosseto, Italy): Biogeochemical processes controlling GEM emission/doi:10.1016%2Fj.gexplo.2021.106824/rivista:Journal of geochemical exploration/anno:2021/pagina_da:1/pagina_a:9/intervallo_pagine:1–9/volume:228
info:cnr-pdr/source/autori:Cabassi J.[1], Venturi S.[1,2], Di Bennardo F.[2], Nisi B.[1], Tassi F.[1,2], Magi F.[2,3,4], Ricci A.[5,6], Picchi G.[2], O. Vaselli O.[1,2]/titolo:Flux measurements of gaseous elemental mercury (GEM) from the geothermal area of "Le Biancane" natural park (Monterotondo Marittimo, Grosseto, Italy): Biogeochemical processes controlling GEM emission/doi:10.1016%2Fj.gexplo.2021.106824/rivista:Journal of geochemical exploration/anno:2021/pagina_da:1/pagina_a:9/intervallo_pagine:1–9/volume:228
Diffuse soil fluxes of gaseous elemental mercury (GEM) were measured in a hydrothermal area (20,000 m2 ) located inside "Le Biancane" natural park, north of Monterotondo Marittimo village (Larderello-Travale geothermal field, Central Italy), using a
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, 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:
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