scholarly journals Distribution of gaseous Hg in the Mercury mining district of Mt. Amiata (Central Italy): A geochemical survey prior the reclamation project

2013 ◽  
Vol 125 ◽  
pp. 179-187 ◽  
Author(s):  
Orlando Vaselli ◽  
Pablo Higueras ◽  
Barbara Nisi ◽  
José María Esbrí ◽  
Jacopo Cabassi ◽  
...  
2021 ◽  
Author(s):  
Marta Lazzaroni ◽  
Marino Zuccolini ◽  
Barbara Nisi ◽  
Jacopo Cabassi ◽  
Daniele Rappuoli ◽  
...  

<p>The Mediterranean area hosts three important mercury mining districts, which are presently abandoned and partially reclaimed: Almadén (Spain), Monte Amiata-Abbadia San Salvatore (Italy) and Idrija (Slovenia). The Galleria Italia (Italy) is the only mining drainage of the former mining area from Abbadia San Salvatore, which feeds the 2.5 km long Fosso della Chiusa. The Galleria Italia waters are circumneutral (pH ≈ 6) and characterized by Ca(Mg)-SO<sub>4</sub> composition; TDS around 1000 mg/L; high concentrations of Fe, Mn and Al (18714.5, 493.3, 486.6 μg/L, respectively) and dissolved CO<sub>2</sub>. The high content of these elements is also present in the stream sediments. In the mining district area of Abbadia San Salvatore, the Galleria Italia-Fosso della Chiusa system is connected to a major riverine network: i.e. the Pagliola, Paglia and Tiber rivers. This work is aimed to (i) characterize the interaction of Hg and As between the water and sediment compartments in the Fosso della Chiusa by including the suspended particulate; (ii) estimate the total Hg and As mass load released by Galleria Italia and iii) evaluate the total load discharged in the riverine network from the circumneutral mine drainage using the Igeo index. In 2020, during four sampling sessions, waters, sediments and suspended particulate were collected all along the Fosso della Chiusa creek. Each sampling station was located maintaining a relatively equidistance from the source to the confluence with the Pagliola river. Specific aliquots at 13 sites were collected to geochemically characterize the creek waters. Also, stream sediments were collected for determining the mineral composition and As, Hg, Sb while at the source and the mouth  2 L of waters were filtered at  <0.45 μm to measure the suspended material and the concentration of three chalcophile elements. A general decrease of the As content was observed along the creek in both waters and sediments, i.e. from 336 to 2 mg/kg and from 12 to 0.3 μg/L, respectively whereas no a clear trend was recognized for Hg, where the higher contents being up to 105 mg/kg and 2.8 μg/L, respectively. It is to mention that the reddish-whitish colour of the waters and sediments (due to the presence of oxy-hydroxide of Fe and, subordinately, Al and Mn) decreasing down to about 1 km from the source, suggesting, as supported by the analytical data, that the presence of the toxic elements in both the solid and aqueous phase. This implies that the environmental impact by the Galleria Italia waters and related sediments is limited spatially at least for As, as also evidenced by the Igeo index applied to sediments for As and Hg, the former showing a general decrease from Class 6 ( “extremely contaminated’’) to 1 (‘’non to moderately contaminated’’). Differently, Hg in each sampling site belongs to Class 6. Nevertheless, the Igeo ranking suggests that As tends to be preferentially partitioned in the liquid phase whilst Hg is mainly enriched in the solid fraction. This contrasting behaviour of As and Hg is also analytically observed when the suspended particulate is considered.</p><p> </p>


2020 ◽  
Vol 201 ◽  
pp. 110833 ◽  
Author(s):  
Samantha Jiménez-Oyola ◽  
María-Jesús García-Martínez ◽  
Marcelo F. Ortega ◽  
David Bolonio ◽  
Clara Rodríguez ◽  
...  

2020 ◽  
Author(s):  
Pierfranco Lattanzi ◽  
Pilario Costagliola ◽  
Mario Paolieri

<p>Mercury contamination of stream sediments in the Paglia and Tiber river catchments (Central Italy) from the abandoned Monte Amiata mining district has long been documented (Rimondi et al., 2019, and references therein). Along the river courses, fluvial sediments have been quarried for decades to obtain sand and gravel for several industrial uses, including construction of road and rail embankments. Although specific information is not available, there is a high chance that some of this material was used for two major Italian transport routes, the A1 Expressway, and the Alta Velocità (=high speed; AV) railroad.</p><p>A preliminary survey was conducted near the city of Orvieto (Umbria region, Central Italy) by taking soil samples in proximity of the embankments of A1 and AV. Both constructions occurred in the 1960s-1970s, when the Monte Amiata mines were still active; specifically, the A1 section Chiusi-Orvieto was completed in 1964, and the AV section Città della Pieve-Roma was completed in 1977. Samples from the embankment of the older railroad Orvieto-Orte (completed in 1874, when mining at Monte Amiata was just beginning) were also taken for comparison.</p><p>Samples near the A1 and AV embankments show Hg contents ranging from 1.4 to 9.2 mg/kg, and 2.7 to 5.8 mg/kg, respectively. All these values exceed the limit (1 mg/kg) established by Italian regulations for public green and civil use soil; some also exceed the limit (5 mg/kg) for industrial soil. By contrast, samples from the old railroad show values of 0.3-0.4 mg/kg, below the law limits.</p><p>The immediate risk to local inhabitants is deemed low; however, these preliminary results indicate a potential contamination of highway and railroad embankments from mine-impacted sediments, and suggest the opportunity of a more systematic study.</p><p>Rimondi V., et al. (2019) – Environmental Pollution 255, 113191</p>


2013 ◽  
Vol 20 (11) ◽  
pp. 7490-7508 ◽  
Author(s):  
A. Ordóñez ◽  
R. Álvarez ◽  
J. Loredo

Clay Minerals ◽  
2001 ◽  
Vol 36 (3) ◽  
pp. 345-354 ◽  
Author(s):  
D. Morata ◽  
P. Higueras ◽  
S. Domínguez-Bella ◽  
J. Parras ◽  
F. Velasco ◽  
...  

AbstractFuchsite and other Cr-rich phyllosilicates, paragenetic with dolomite, are present in some ultramafic enclaves from the ‘frailesca’ rock (a lapilli- to block-size pyroclastic lithic-tuff), in the Almadén mercury mining district, Spain. Analyses (EMPA and TEM) of fuchsite and Cr-chlorite showed a relatively large range in levels of Cr2O3. Petrographic relationships between these phyllosilicates and primary relics of Cr-spinel crystals, as well as their high Cr content, indicate that these Cr-rich minerals originated from primary chromian spinels through an early hydrothermal alteration stage. The hydrothermal fluids accounting for this early alteration would be of relatively high temperature, high aCO2 and aK, and variable aNa/K. In a later alteration stage, fuchsite was partially or totally replaced by illite and Cr-illite, giving rise to an argillitic alteration.


2010 ◽  
Vol 176 (1-3) ◽  
pp. 323-332 ◽  
Author(s):  
Jorge Loredo ◽  
María Dolores Petit-Domínguez ◽  
Almudena Ordóñez ◽  
María Pilar Galán ◽  
Rodolfo Fernández-Martínez ◽  
...  

2011 ◽  
Vol 30 (12) ◽  
pp. 2725-2731 ◽  
Author(s):  
Jianxu Wang ◽  
Xinbin Feng ◽  
Christopher W.N. Anderson ◽  
Wei Zhu ◽  
Runsheng Yin ◽  
...  

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