Bibliographies thématiques / Mt. Amiata

Littérature scientifique sur le sujet « Mt. Amiata »

Auteur : Grafiati

Publié le 10 mars 2023

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Articles de revues sur le sujet "Mt. Amiata"

Ferrara, R., B. Mazzolai, H. Edner, S. Svanberg et E. Wallinder. « Atmospheric mercury sources in the Mt. Amiata area, Italy ». Science of The Total Environment 213, n^o 1-3 (juin 1998) : 13–23. http://dx.doi.org/10.1016/s0048-9697(98)00067-9.

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Volpi, Gianni, Adele Manzella et Adolfo Fiordelisi. « Investigation of geothermal structures by magnetotellurics (MT) : an example from the Mt. Amiata area, Italy ». Geothermics 32, n^o 2 (avril 2003) : 131–45. http://dx.doi.org/10.1016/s0375-6505(03)00016-6.

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Pierotti, L., F. Gherardi, G. Facca, L. Piccardi et G. Moratti. « Detecting CO 2 anomalies in a spring on Mt. Amiata volcano (Italy) ». Physics and Chemistry of the Earth, Parts A/B/C 98 (avril 2017) : 161–72. http://dx.doi.org/10.1016/j.pce.2017.01.008.

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Lattanzi, Pierfranco, Valentina Rimondi, Laura Chiarantini, Antonella Colica, Marco Benvenuti, Pilario Costagliola et Giovanni Ruggieri. « Mercury Dispersion through Streams Draining The Mt. Amiata District, Southern Tuscany, Italy ». Procedia Earth and Planetary Science 17 (2017) : 468–71. http://dx.doi.org/10.1016/j.proeps.2016.12.118.

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Battaglia, S., F. Gherardi, G. Gianelli, L. Leoni et F. Origlia. « Clay mineral reactions in an active geothermal area (Mt. Amiata, southern Tuscany, Italy) ». Clay Minerals 42, n^o 3 (septembre 2007) : 353–72. http://dx.doi.org/10.1180/claymin.2007.042.3.08.

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AbstractThis study characterizes the effects of fluid migration into a predominantly shale cover which seals the active geothermal system of Mt. Amiata (Tuscany, Italy). During Alpine orogenesis the shale unit was affected by regional metamorphism at the limit of the diagenesis-anchizone. Subsequently, the phyllosilicate clay minerals of the shales underwent significant alteration at diagenetic temperatures (175±25ºC as determined by the geochemical model) by the pervasive circulation of fluids activated by the geothermal field. The overall mineralogical assemblages indicate that the main transformations consisted mostly of destabilization of illite and formation of kaolinite together with large amounts of I-S mixed layers, with higher smectite content and decreased Reichweite I-S ordering (from R3 to R1) with respect to the original, unaltered phases. Application of computer modelling indicates that the circulation of CO2-rich geothermal fluids into the shale unit was responsible for the observed phyllosilicate clay mineral transformations.

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Loppi, Stefano, et Juri Nascimbene. « Lichen bioindication of air quality in the Mt. Amiata geothermal area (Tuscany, Italy) ». Geothermics 27, n^o 3 (juin 1998) : 295–304. http://dx.doi.org/10.1016/s0375-6505(98)00003-0.

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Sbrana, Alessandro, Paolo Fulignati, Paola Marianelli et Valentina Ciani. « Withdrawal notice to "Mt Amiata hydrothermal system (Italy) : 3D geological and geothermal modeling" ». Italian Journal of Geosciences 134, n^o 3 (octobre 2015) : 579. http://dx.doi.org/10.3301/ijg.2014.50.

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Batini, Fausto, Andrea Brogi, Antonio Lazzarotto, Domenico Liotta et Enrico Pandeli. « Geological features of Larderello-Travale and Mt. Amiata geothermal areas (southern Tuscany, Italy) ». Episodes 26, n^o 3 (1 septembre 2003) : 239–44. http://dx.doi.org/10.18814/epiiugs/2003/v26i3/015.

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Tretiach, Mauro, et Paola Ganis. « Hydrogen Sulphide and Epiphytic Lichen Vegetation : a Case Study on Mt. Amiata (Central Italy) ». Lichenologist 31, n^o 02 (mars 1999) : 163–81. http://dx.doi.org/10.1017/s0024282999000225.

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AbstractA survey aimed at studying the effects of hydrogen sulphide (H2S) on epiphytic lichen vegetation was carried out at Acquapassante (Mt. Amiata, Central Italy). In 1992, lichen vegetation was surveyed using a sampling grid often units, on 18 chestnut trees along a transect from a chimney emitting H2S to c. 200 m in the direction of the prevailing winds. A Lichen Biodiversity Index (LBI) was calculated as the sum of the frequencies of all species present within the grid. The same survey was repeated five years later. Concentration Analysis was applied to describe the data structure, and Procrustes Analysis was used to verify the congruence between the ordinations of 1992 and 1997. The statistically significant linear and non-linear regressions found between environmental variables (distance of relevés from the chimney, bark pH, lichen biomass of selected foliose and fruticose species, total sulphur content ofEvernia prunastri, Hypogymnia physodes, Parmelia sulcataandRamalina fastigiata) and the position of the relevé points on the ordination axes suggest that species distribution along the transect is related to differences in H2S tolerance. However, some crustose species (Lecanora cf. conizaeoides, L. salignaandScolkiosporum umbrinum) should be probably excluded from the computation of the LBI for monitoring purposes, as their optimum is in the immediate vicinity of the H2S source.

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Tretiach, Mauro, et Paola Ganis. « Hydrogen Sulphide and Epiphytic Lichen Vegetation : a Case Study on Mt. Amiata (Central Italy) ». Lichenologist 31, n^o 2 (mars 1999) : 163–81. http://dx.doi.org/10.1006/lich.1998.0173.

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AbstractA survey aimed at studying the effects of hydrogen sulphide (H2S) on epiphytic lichen vegetation was carried out at Acquapassante (Mt. Amiata, Central Italy). In 1992, lichen vegetation was surveyed using a sampling grid often units, on 18 chestnut trees along a transect from a chimney emitting H2S to c. 200 m in the direction of the prevailing winds. A Lichen Biodiversity Index (LBI) was calculated as the sum of the frequencies of all species present within the grid. The same survey was repeated five years later. Concentration Analysis was applied to describe the data structure, and Procrustes Analysis was used to verify the congruence between the ordinations of 1992 and 1997. The statistically significant linear and non-linear regressions found between environmental variables (distance of relevés from the chimney, bark pH, lichen biomass of selected foliose and fruticose species, total sulphur content of Evernia prunastri, Hypogymnia physodes, Parmelia sulcata and Ramalina fastigiata) and the position of the relevé points on the ordination axes suggest that species distribution along the transect is related to differences in H2S tolerance. However, some crustose species (Lecanora cf. conizaeoides, L. saligna and Scolkiosporum umbrinum) should be probably excluded from the computation of the LBI for monitoring purposes, as their optimum is in the immediate vicinity of the H2S source.

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Thèses sur le sujet "Mt. Amiata"

RIMONDI, VALENTINA. « Distribution of mercury and other trace elements in the Mt. Amiata region (Southern Tuscany, Italy) ». Doctoral thesis, 2013. http://hdl.handle.net/2158/796454.

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This PhD project focuses on the Hg mining district of Mt. Amiata, and to the environmental consequences deriving from the mining activity occurring in this region up to 1980's. Different aspects of Hg environmental impact are taken into consideration, focussing in particular to the Paglia Riber Basin (PRB), which drains the eastern sector of the Hg district. The main goals of the work are then: i) to establish an updated picture of Hg and methyl-Hg (MMHg) diffusion and distribution in the PBR; ii) to estimate the mass load of Hg transported by this river; iii) to characterize the speciation of Hg − and hence its bioavailability − in different environmental matrices; iv) to define the regional background for Hg.

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CABASSI, JACOPO. « Il mercurio gassoso (Hg0) nella ex-zona mineraria di Abbadia San Salvatore (Mt. Amiata, Siena) ed in aree vulcaniche attive e quiescenti : distribuzione e comportamento in relazione ad altri inquinanti atmosferici ». Doctoral thesis, 2015. http://hdl.handle.net/2158/981792.

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Il lavoro svolto nell'ambito del dottorato è stato indirizzato allo studio e alla comprensione del comportamento geochimico e delle modalità di dispersione di inquinanti in aria, rivolgendosi alla valutazione della qualità dell’aria, con particolare riferimento alla mobilità del mercurio e di altri composti gassosi, quali le specie dello zolfo (e.g. H2S e SO2), ad elevato impatto ambientale.

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Chapitres de livres sur le sujet "Mt. Amiata"

Ferrara, R., B. E. Maserti, B. Mazzolai, F. Francesco, H. Edner, S. Svanberg et E. Wallinder. « Atmospheric Mercury in Abandoned Mine Structures and Restored Mine Buildings at Mt. Amiata, Italy ». Dans Mercury Contaminated Sites, 249–57. Berlin, Heidelberg : Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-662-03754-6_13.

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Minissale, Angelo, Gabriella Magro, Franco Tassi et Carlo Verrucchi. « Origin and circulation patterns of deep and shallow hydrothermal fluids in the Mt. Amiata geothermal region (central Italy) ». Dans Water-Rock Interaction, 523–28. London : Routledge, 2021. http://dx.doi.org/10.1201/9780203734049-129.

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Actes de conférences sur le sujet "Mt. Amiata"

Fornasaro, Silvia, Guia Morelli, Pilario Costagliola, Valentina Rimondi, Pierfranco Lattanzi et Cesare Fagotti. « Mapping the Hg-Impacted Area in the Paglia River Basin (Mt. Amiata Mining District – Italy) ». Dans Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.728.

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