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ERICo Velenje, Environmental Research & Industrial Co-operation Institute, Koroška 58, SI-3320 Velenje, Slovenia
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- PublicationRestrictedA case-study of complex gas–water–rock–pollutants interactions in shallow groundwater: Šalek Valley (Slovenia)(2009-03)
; ; ; ; ;Giammanco, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia ;Justin, B.; ERICo Velenje, Environmental Research & Industrial Co-operation Institute, Koroška 58, SI-3320 Velenje, Slovenia ;Speh, N.; ERICo Velenje, Environmental Research & Industrial Co-operation Institute, Koroška 58, SI-3320 Velenje, Slovenia ;Veder, M.; Kardeljev trg 2, SI-3320 Velenje, Slovenia; ; ; The complex geochemical interactions in the groundwater of the industrial area of S ˇ alek Valley (Slovenia) between natural and anthropogenic fluids were studied by means of major (Ca, Mg, Na, K, HCO3 -, Cl- and SO4 2-) and trace elements’ (As , Cd, Cu, Pb, Zn, Hg, Se and V) abundances, geochemical classification and statistical analysis of data. Cation abundances indicate mixing between a dolomitic end-member and an evaporitic or geothermal end-member. Anion abundances indicate mixing between bicarbonate waters and either sulphateenriched waters (suggesting hydrothermalism) or chlorinerich waters. Principal component analysis (PCA) allowed the extraction of seven factors, which describe, respectively: water–rock interaction mainly on dolomitic rocks; redox conditions of water; Cd–Zn enrichment in chlorinerich waters (probably from industrial wastes); hydrothermal conditions in waters close to major faults; Pb and Cu pollution; V and K enrichments, indicating their common organic source; the role of partial pressure of CO2 dissolved in water, which is highest in three wells with bubbling gases. Average underground discharge rates of solutes from the Valley range between 0.09 t/a (V) and 1.8 9 104 t/a (HCO3 -) and indicate how natural fluids can significantly contribute to the levels of elements in the environment, in addition to the amount of elements released by human activities.160 27 - PublicationOpen AccessGeochemical comparison of natural and anthropogenic metal fluxes in extreme environments: Mt. Etna volcano (Italy) and Salek Valley (Slovenia)(2009-10-06)
; ; ; ; ; ; ; ;Calabrese, S.; Università di Palermo, Dipartimento CFTA ;Veder, M.; ERICo Velenje, Environmental Research & Industrial Cooperation Institute, Slovenia ;Giammanco, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia ;Speh, N.; ERICo Velenje, Environmental Research & Industrial Cooperation Institute, Slovenia ;Justin, B.; ERICo Velenje, Environmental Research & Industrial Cooperation Institute, Slovenia ;Parello, F.; Università di Palermo, Dipartimento CFTA ;D'Alessandro, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia; ; ; ; ; ;; ; ; ; ;Sajn, R.; Geological Survey of Slovenia ;Zibret, G.; Geological Survey of Slovenia ;Alijagic, J.; Geological Survey of Slovenia; ; Geochemical comparison between some metals (As, Cd, Cu, Pb, Se, V, Zn) emissions from an active volcano (Mt. Etna) and a highly industrialized area (Salek Valley) showed some interesting similarities: in general, most of the elements emitted into the atmosphere do not return to the Earth's surface and are therefore dispersed into the environment. Exceptions for Salek Valley are Cd, which probably derives in large part from rock leaching, and in part As and Pb, which fall mostly as ash. Also, Etna's emissions are richer in Cd and Cu, whereas industrial emissions at Salek Valley are richer in V and Zn. All other metals have similar fluxes in the two types of emissions.252 182