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Naslov:Mercury in the unconfined aquifer of the Isonzo/Soča River alluvial plain downstream from the Idrija mining area
Avtorji:ID Cerovac, Andrea (Avtor)
ID Covelli, Stefano (Avtor)
ID Emili, Andrea (Avtor)
ID Pavoni, Elena (Avtor)
ID Petranich, Elisa (Avtor)
ID Gregorič, Asta (Avtor)
ID Urbanc, Janko (Avtor)
ID Zavagno, Enrico (Avtor)
ID Zini, Luca (Avtor)
Datoteke:URL URL - Predstavitvena datoteka, za dostop obiščite http://dx.doi.org/10.1016/j.chemosphere.2017.12.105
 
Jezik:Angleški jezik
Tipologija:1.01 - Izvirni znanstveni članek
Organizacija:Logo GeoZS - Geološki zavod Slovenije
Povzetek:This work aims at evaluating mercury (Hg) occurrence, spatial distribution and speciation in groundwater of the Isonzo/Soča River upper alluvial plain downstream from the Idrija Hg mine (Western Slovenia). Several wells and piezometers were sampled both in static and dynamic mode. On the basis of hydrochemistry and isotopic composition, the main sources of groundwater were established. Hg concentrations in the Slovenian sector, supplied by local rainfall, are comparable to values measured close to the Isonzo River. Possible further Hg local sources have been suggested. Stability field analysis for the aqueous Hg species revealed that in the presence of chloride Hg solubility may be increased by the formation of chlorocomplexes. Mercury that rarely enters reduced surrounding conditions can be bound to sulphur to form polysulphide species depending on the pH of water. Since Hg-contaminated alluvial sediments of the Isonzo River may act as a secondary Hg source in groundwater, a borehole was dug down to the water table. Mercury content and speciation revealed that cinnabar (HgS) is the prevalent form followed by the matrix-bound Hg (Hgbound). Variations of the physico-chemical boundary conditions, as well as the raising/lowering of the water table, may be locally responsible for the slight variability of Hg concentrations in the aquifer.
Ključne besede:aquifers, groundwater, mercury
Status publikacije:Objavljeno
Verzija publikacije:Objavljena publikacija
Založnik:Elsevier
Leto izida:2018
Št. strani:str. 749-761
Številčenje:Vol. 195
PID:20.500.12556/DiRROS-13323 Novo okno
ISSN:0045-6535
UDK:556.3
DOI:10.1016/j.chemosphere.2017.12.105 Novo okno
COBISS.SI-ID:4978683 Novo okno
Datum objave v DiRROS:22.06.2022
Število ogledov:543
Število prenosov:281
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