Comparative Study of Iron and Trace Element Mobilization during Fe-Oxide Bioreduction in Mine Tailings: a case study of Ensenada Chapaco (Chile) and Portman Bay (Spain)

dc.contributor.author
Benaiges-Fernández, Robert
dc.contributor.author
Palau, Jordi
dc.contributor.author
Urmeneta, Jordi
dc.contributor.author
Cama, Jordi
dc.contributor.author
Soler, Josep M.
dc.contributor.author
Dold, Bernhard
dc.date.accessioned
2026-02-28T20:06:37Z
dc.date.available
2026-02-28T20:06:37Z
dc.date.issued
2026-02-26T10:30:11Z
dc.date.issued
2026-02-26T10:30:11Z
dc.date.issued
2025-02
dc.date.issued
2026-02-26T10:30:11Z
dc.identifier
1695-6133
dc.identifier
https://hdl.handle.net/2445/227504
dc.identifier
758435
dc.identifier.uri
https://hdl.handle.net/2445/227504
dc.description.abstract
Bioreduction of Feoxides in mine tailings deposited under marine conditions releases Fe and associated trace elements (e.g. Ti, Ni, Cd, Pb), leading to contamination of the marine environment. Sea-Tailings Disposal (STD) along the northern coast of Chile (Ensenada Chapaco) and along the eastern coast of Spain (Portman Bay) results in an adverse impact on the environment. This paper focuses on bioreduction under marine conditions. To this end, two column experiments were carried out with samples from Portman Bay and Ensenada Chapaco. Lactate (i.e.organic matter source) was supplied during the experiments. The results obtained are compared with those from batch experiments performed under similar conditions.In the column filled with Portman Bay tailings, the high content of magnetite (15wt%) in contact with water gives rise to a large magnetite surface area and abundant Fe(III), which results in a high release of Fe(II) and Trace Elements (TE). Since Fe(II) adsorbs onto the magnetite surface reducing the availability of Fe(III), the magnetite bioreduction and the consequent TE release decrease after 2000h. By contrast, the magnetite bioreduction lasts longer (3000h) in the column with Ensenada Chapaco tailings. This is because a lower magnetite content in the tailings (1wt%) provides a smaller reactive surface area yielding less Fe(III). Consequently, the concentrations of Fe(II) and TE in the output solutions are lower, which slows down the Fe(II) adsorption onto magnetite. This results in a longer magnetite bioreduction. Bioreduction is regulated by the availability of Fe(III) in both columns. It is inferred that the bioreduction rate diminishes as a function of time and increases as a function of soluble Fe(II) concentration. Moreover, the concentrations of TE released from the two bioreduced tailings exceed the elemental concentrations under marine conditions.
dc.format
12 p.
dc.format
application/pdf
dc.language
eng
dc.publisher
(UB). (ICTJA). (IDEA). (UAB). (CSIC)
dc.relation
Reproducció del document publicat a: https://doi.org/10.1344/GeologicaActa2025.23.5
dc.relation
Geologica Acta, 2025, vol. 5, num.23, p. 1-12
dc.relation
https://doi.org/10.1344/GeologicaActa2025.23.5
dc.rights
cc-by-sa (c) Benaiges-Fernández, Robert et al., 2025
dc.rights
http://creativecommons.org/licenses/by-sa/4.0/
dc.rights
info:eu-repo/semantics/openAccess
dc.subject
Òxids metàl·lics
dc.subject
Contaminació
dc.subject
Elements traça
dc.subject
Metallic oxides
dc.subject
Pollution
dc.subject
Trace elements
dc.title
Comparative Study of Iron and Trace Element Mobilization during Fe-Oxide Bioreduction in Mine Tailings: a case study of Ensenada Chapaco (Chile) and Portman Bay (Spain)
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/publishedVersion


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