Abstract
Wetlands cover more than 6% of the global ice-free land area, and have been recognized as important sinks for arsenic. Wetland soils and sediments are subject to frequent changes in redox conditions, driven by fluctuations in the water table and shifts in biological activity. Under oxic conditions, natural organic matter promotes arsenic release from metal-(hydr)oxides, thereby enhancing arsenic mobility. Under strongly reducing conditions, however, organic matter triggers the formation of arsenic-sequestering sulphides, leading to a reduction in arsenic mobility. Furthermore, the sorption of arsenic to natural organic matter is increasingly thought to suppress arsenic mobility, but the binding mechanisms have remained elusive. Here we use X-ray absorption spectroscopy to analyse the speciation of solid-phase arsenic in peat samples collected from a naturally arsenic-enriched peatland in Switzerland. We show that natural organic matter can completely sequester arsenic through the formation of covalent bonds between trivalent arsenic and organic sulphur groups, which have an average arsenic–sulphur bond distance of 2.26 Å. We suggest that by binding arsenic in this way, natural organic matter plays an active role in arsenic immobilization in sulphur-enriched, anoxic wetlands.
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Acknowledgements
We thank K. Barmettler for his support in the soil chemistry laboratory, M. Hoffmann, F. Maurer and K. Barmettler for field assistance, as well as S. Hassold and M. Maurer for mapping the vegetation at the field site. We acknowledge the ESRF for provision of synchrotron radiation facilities, and we would like to thank M. Chorro for assistance in using beamline BM29. Portions of this research were carried out at the light source DORIS III at DESY, a member of the Helmholtz Association (HGF). We are grateful to E. Welter for assistance in using beamline C (Hasylab). Portions of this research were also carried out at the 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 by Stanford University. We would like to thank J. Rogers for his support in using beamline 4-1. The authors furthermore acknowledge the support by the Electron Microscopy Center, ETH Zurich (EMEZ, Switzerland), in particular K. Kunze for performing the SEM–EDX analyses. Thanks to A. Massanek (TU Bergakademie Freiberg, Germany) and P. Brack (ETH Zurich) for their assistance in providing mineral reference compounds. We are also indebted to P. Poggiati and M. Sulmoni from the Department of Environment (Ticino, Switzerland) who granted the sampling permission for Gola di Lago. Financial support by the ETH Zurich (research grant 2708-2) is also gratefully acknowledged.
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P.L. and C.M. performed the work in the field and at the synchrotron radiation facilities. P.L. analysed the samples in the laboratory, evaluated the results, and wrote the manuscript as part of her PhD thesis. C.M. conducted the shell-fit and wavelet-transform analyses. C.M. and R.K. initiated and supervised the project. All authors discussed the results and contributed to the manuscript.
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Langner, P., Mikutta, C. & Kretzschmar, R. Arsenic sequestration by organic sulphur in peat. Nature Geosci 5, 66–73 (2012). https://doi.org/10.1038/ngeo1329
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DOI: https://doi.org/10.1038/ngeo1329
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