Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat

Research output: Contribution to journalArticleResearchpeer review

Authors

  • Johannes Besold
  • Ashis Biswas
  • Elke Suess
  • Andreas C. Scheinost
  • André Rossberg
  • Christian Mikutta
  • Ruben Kretzschmar
  • Jon Petter Gustafsson
  • Britta Planer-Friedrich

Research Organisations

External Research Organisations

  • University of Bayreuth
  • Indian Institute of Science Education and Research Bhopal
  • Swiss Federal Institute of Aquatic Science and Technology (Eawag)
  • European Synchrotron Radiation Facility
  • Helmholtz-Zentrum Dresden-Rossendorf (HZDR)
  • ETH Zurich
  • Swedish University of Agricultural Sciences
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Details

Original languageEnglish
Pages (from-to)7317-7326
Number of pages10
JournalEnvironmental Science and Technology
Volume52
Issue number13
Publication statusPublished - 31 May 2018

Abstract

In peatlands, arsenite was reported to be effectively sequestered by sulfhydryl groups of natural organic matter. To which extent porewater arsenite can react with reduced sulfur to form thioarsenates and how this affects arsenic sequestration in peatlands is unknown. Here, we show that, in the naturally arsenic-enriched peatland Gola di Lago, Switzerland, up to 93% of all arsenic species in surface and porewaters were thioarsenates. The dominant species, monothioarsenate, likely formed from arsenite and zerovalent sulfur-containing species. Laboratory incubations with sulfide-reacted, purified model peat showed increasing total arsenic sorption with decreasing pH from 8.5 to 4.5 for both, monothioarsenate and arsenite. However, X-ray absorption spectroscopy revealed no binding of monothioarsenate via sulfhydryl groups. The sorption observed at pH 4.5 was acid-catalyzed dissociation of monothioarsenate, forming arsenite. The lower the pH and the more sulfhydryl sites, the more arsenite sorbed which in turn shifted equilibrium toward further dissociation of monothioarsenate. At pH 8.5, monothioarsenate was stable over 41 days. In conclusion, arsenic can be effectively sequestered by sulfhydryl groups in anoxic, slightly acidic environments where arsenite is the only arsenic species. At neutral to slightly alkaline pH, monothioarsenate can form and its slow transformation into arsenite and low affinity to sulfhydryl groups suggest that this species is mobile in such environments.

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Cite this

Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat. / Besold, Johannes; Biswas, Ashis; Suess, Elke et al.
In: Environmental Science and Technology, Vol. 52, No. 13, 31.05.2018, p. 7317-7326.

Research output: Contribution to journalArticleResearchpeer review

Besold, J, Biswas, A, Suess, E, Scheinost, AC, Rossberg, A, Mikutta, C, Kretzschmar, R, Gustafsson, JP & Planer-Friedrich, B 2018, 'Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat', Environmental Science and Technology, vol. 52, no. 13, pp. 7317-7326. https://doi.org/10.1021/acs.est.8b01542
Besold, J., Biswas, A., Suess, E., Scheinost, A. C., Rossberg, A., Mikutta, C., Kretzschmar, R., Gustafsson, J. P., & Planer-Friedrich, B. (2018). Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat. Environmental Science and Technology, 52(13), 7317-7326. https://doi.org/10.1021/acs.est.8b01542
Besold J, Biswas A, Suess E, Scheinost AC, Rossberg A, Mikutta C et al. Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat. Environmental Science and Technology. 2018 May 31;52(13):7317-7326. doi: 10.1021/acs.est.8b01542
Besold, Johannes ; Biswas, Ashis ; Suess, Elke et al. / Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat. In: Environmental Science and Technology. 2018 ; Vol. 52, No. 13. pp. 7317-7326.
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title = "Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat",
abstract = "In peatlands, arsenite was reported to be effectively sequestered by sulfhydryl groups of natural organic matter. To which extent porewater arsenite can react with reduced sulfur to form thioarsenates and how this affects arsenic sequestration in peatlands is unknown. Here, we show that, in the naturally arsenic-enriched peatland Gola di Lago, Switzerland, up to 93% of all arsenic species in surface and porewaters were thioarsenates. The dominant species, monothioarsenate, likely formed from arsenite and zerovalent sulfur-containing species. Laboratory incubations with sulfide-reacted, purified model peat showed increasing total arsenic sorption with decreasing pH from 8.5 to 4.5 for both, monothioarsenate and arsenite. However, X-ray absorption spectroscopy revealed no binding of monothioarsenate via sulfhydryl groups. The sorption observed at pH 4.5 was acid-catalyzed dissociation of monothioarsenate, forming arsenite. The lower the pH and the more sulfhydryl sites, the more arsenite sorbed which in turn shifted equilibrium toward further dissociation of monothioarsenate. At pH 8.5, monothioarsenate was stable over 41 days. In conclusion, arsenic can be effectively sequestered by sulfhydryl groups in anoxic, slightly acidic environments where arsenite is the only arsenic species. At neutral to slightly alkaline pH, monothioarsenate can form and its slow transformation into arsenite and low affinity to sulfhydryl groups suggest that this species is mobile in such environments.",
author = "Johannes Besold and Ashis Biswas and Elke Suess and Scheinost, {Andreas C.} and Andr{\'e} Rossberg and Christian Mikutta and Ruben Kretzschmar and Gustafsson, {Jon Petter} and Britta Planer-Friedrich",
note = "Funding Information: This work was funded by the German Research Foundation Grant PL 302/20-1. A. Biswas received a Postdoc stipend from the Alexander-von-Humboldt Foundation. We acknowledge the help from R. Siegel and H. Zier for collecting the NMR and FT-IR spectra of the peat. Arsenic K-edge XAS xperiments were performed at the European Synchrotron Radiation Facility (ESRF), Grenoble, France, and the Stanford Synchrotron Radiation Lightsource (SSRL), a Directorate of SLAC National Accelerator Laboratory and an Office of Science User Facility operated for the US Department of Energy, Office of Science, Office of Basic Energy Sciences under Contract No. DE-AC02-76SF00515. In this regard, we would like to thank R. Davis (SSRL) and J. Lezama Pacheco (Soil and Environmental Biogeochemistry group, Stanford University) for their support in using beamline 4-1. ",
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T1 - Monothioarsenate Transformation Kinetics Determining Arsenic Sequestration by Sulfhydryl Groups of Peat

AU - Besold, Johannes

AU - Biswas, Ashis

AU - Suess, Elke

AU - Scheinost, Andreas C.

AU - Rossberg, André

AU - Mikutta, Christian

AU - Kretzschmar, Ruben

AU - Gustafsson, Jon Petter

AU - Planer-Friedrich, Britta

N1 - Funding Information: This work was funded by the German Research Foundation Grant PL 302/20-1. A. Biswas received a Postdoc stipend from the Alexander-von-Humboldt Foundation. We acknowledge the help from R. Siegel and H. Zier for collecting the NMR and FT-IR spectra of the peat. Arsenic K-edge XAS xperiments were performed at the European Synchrotron Radiation Facility (ESRF), Grenoble, France, and the Stanford Synchrotron Radiation Lightsource (SSRL), a Directorate of SLAC National Accelerator Laboratory and an Office of Science User Facility operated for the US Department of Energy, Office of Science, Office of Basic Energy Sciences under Contract No. DE-AC02-76SF00515. In this regard, we would like to thank R. Davis (SSRL) and J. Lezama Pacheco (Soil and Environmental Biogeochemistry group, Stanford University) for their support in using beamline 4-1.

PY - 2018/5/31

Y1 - 2018/5/31

N2 - In peatlands, arsenite was reported to be effectively sequestered by sulfhydryl groups of natural organic matter. To which extent porewater arsenite can react with reduced sulfur to form thioarsenates and how this affects arsenic sequestration in peatlands is unknown. Here, we show that, in the naturally arsenic-enriched peatland Gola di Lago, Switzerland, up to 93% of all arsenic species in surface and porewaters were thioarsenates. The dominant species, monothioarsenate, likely formed from arsenite and zerovalent sulfur-containing species. Laboratory incubations with sulfide-reacted, purified model peat showed increasing total arsenic sorption with decreasing pH from 8.5 to 4.5 for both, monothioarsenate and arsenite. However, X-ray absorption spectroscopy revealed no binding of monothioarsenate via sulfhydryl groups. The sorption observed at pH 4.5 was acid-catalyzed dissociation of monothioarsenate, forming arsenite. The lower the pH and the more sulfhydryl sites, the more arsenite sorbed which in turn shifted equilibrium toward further dissociation of monothioarsenate. At pH 8.5, monothioarsenate was stable over 41 days. In conclusion, arsenic can be effectively sequestered by sulfhydryl groups in anoxic, slightly acidic environments where arsenite is the only arsenic species. At neutral to slightly alkaline pH, monothioarsenate can form and its slow transformation into arsenite and low affinity to sulfhydryl groups suggest that this species is mobile in such environments.

AB - In peatlands, arsenite was reported to be effectively sequestered by sulfhydryl groups of natural organic matter. To which extent porewater arsenite can react with reduced sulfur to form thioarsenates and how this affects arsenic sequestration in peatlands is unknown. Here, we show that, in the naturally arsenic-enriched peatland Gola di Lago, Switzerland, up to 93% of all arsenic species in surface and porewaters were thioarsenates. The dominant species, monothioarsenate, likely formed from arsenite and zerovalent sulfur-containing species. Laboratory incubations with sulfide-reacted, purified model peat showed increasing total arsenic sorption with decreasing pH from 8.5 to 4.5 for both, monothioarsenate and arsenite. However, X-ray absorption spectroscopy revealed no binding of monothioarsenate via sulfhydryl groups. The sorption observed at pH 4.5 was acid-catalyzed dissociation of monothioarsenate, forming arsenite. The lower the pH and the more sulfhydryl sites, the more arsenite sorbed which in turn shifted equilibrium toward further dissociation of monothioarsenate. At pH 8.5, monothioarsenate was stable over 41 days. In conclusion, arsenic can be effectively sequestered by sulfhydryl groups in anoxic, slightly acidic environments where arsenite is the only arsenic species. At neutral to slightly alkaline pH, monothioarsenate can form and its slow transformation into arsenite and low affinity to sulfhydryl groups suggest that this species is mobile in such environments.

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