Biogeochemical cycling of silver in acidic, weathering environments

Jeremiah Shuster, Frank Reith, Matthew Richar Izawa, Roberta L. Flemming, Neil R. Banerjee, Gordon Southam

Research output: Contribution to journalArticle

10 Citations (Scopus)

Abstract

Under acidic, weathering conditions, silver (Ag) is considered to be highly mobile and can be dispersed within near-surface environments. In this study, a range of regolith materials were sampled from three abandoned open pit mines located in the Iberian Pyrite Belt, Spain. Samples were analyzed for Ag mineralogy, content, and distribution using micro-analytical techniques and high-resolution electron microscopy. While Ag concentrations were variable within these materials, elevated Ag concentrations occurred in gossans. The detection of Ag within younger regolith materials, i.e., terrace iron formations and mine soils, indicated that Ag cycling was a continuous process. Microbial microfossils were observed within crevices of gossan and their presence highlights the preservation of mineralized cells and the potential for biogeochemical processes contributing to metal mobility in the rock record. An acidophilic, iron-oxidizing microbial consortium was enriched from terrace iron formations. When the microbial consortium was exposed to dissolved Ag, more than 90% of Ag precipitated out of solution as argentojarosite. In terms of biogeochemical Ag cycling, this demonstrates that Ag re-precipitation processes may occur rapidly in comparison to Ag dissolution processes. The kinetics of Ag mobility was estimated for each type of regolith material. Gossans represented 0.6–146.7 years of biogeochemical Ag cycling while terrace iron formation and mine soils represented 1.9–42.7 years and 0.7–1.6 years of Ag biogeochemical cycling, respectively. Biogeochemical processes were interpreted from the chemical and structural characterization of regolith material and demonstrated that Ag can be highly dispersed throughout an acidic, weathering environment.

Original languageEnglish
Article number218
JournalMinerals
Volume7
Issue number11
DOIs
Publication statusPublished - Nov 1 2017

Fingerprint

Weathering
silver
regolith
gossan
Silver
weathering
Iron
terrace
iron
Soils
open pit mine
abandoned mine
Mineralogy
High resolution electron microscopy
Pyrites
microfossil
electron microscopy
analytical method
pyrite
Dissolution

Keywords

  • Argentojarosite
  • Gossan
  • Iron-oxidizing bacteria/archaea
  • Silver biogeochemical cycling
  • Terrace iron formations

ASJC Scopus subject areas

  • Geotechnical Engineering and Engineering Geology
  • Geology

Cite this

Shuster, J., Reith, F., Richar Izawa, M., Flemming, R. L., Banerjee, N. R., & Southam, G. (2017). Biogeochemical cycling of silver in acidic, weathering environments. Minerals, 7(11), [218]. https://doi.org/10.3390/min7110218

Biogeochemical cycling of silver in acidic, weathering environments. / Shuster, Jeremiah; Reith, Frank; Richar Izawa, Matthew; Flemming, Roberta L.; Banerjee, Neil R.; Southam, Gordon.

In: Minerals, Vol. 7, No. 11, 218, 01.11.2017.

Research output: Contribution to journalArticle

Shuster, J, Reith, F, Richar Izawa, M, Flemming, RL, Banerjee, NR & Southam, G 2017, 'Biogeochemical cycling of silver in acidic, weathering environments', Minerals, vol. 7, no. 11, 218. https://doi.org/10.3390/min7110218
Shuster J, Reith F, Richar Izawa M, Flemming RL, Banerjee NR, Southam G. Biogeochemical cycling of silver in acidic, weathering environments. Minerals. 2017 Nov 1;7(11). 218. https://doi.org/10.3390/min7110218
Shuster, Jeremiah ; Reith, Frank ; Richar Izawa, Matthew ; Flemming, Roberta L. ; Banerjee, Neil R. ; Southam, Gordon. / Biogeochemical cycling of silver in acidic, weathering environments. In: Minerals. 2017 ; Vol. 7, No. 11.
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