Abstract
Arsenic (As) is a priority pollutant found in water bodies, sediments and soils; therefore, mineral surfaces are critical for the environmental distribution of this element. The objective of this work was to analyse expandable clay minerals [hectorite (Fe-poor) and nontronite (Fe-rich)] exposed to As [as As(III), the most toxic form of As; 10−4 M sodium arsenite in water, pH0 = 7.2, 25 ± 1 °C] with 1 nm precision using hydride generation–cryotrapping–atomic absorption spectrometry, high-resolution scanning electron microscopy and energy-dispersive spectrometry. In supernatant solutions, As(III) underwent no transformation. The accumulation of As(III) was registered in hectorite (4%) and nontronite (2.7%). The outcome of this work expanded on current knowledge on the interaction between As(III) and expandable clay minerals. The higher content of structural Fe in nontronite vs. hectorite favoured the retention of As(III). Arguably, adsorbed As(III) on nontronite surfaces (1) transformed to arsenical ferrihydrite or (2) bonded with naturally occurring S; both processes facilitated its nonreversible surface bonding. In addition, adsorbed As(III) on nontronite and hectorite surfaces reversibly bonded to surface O.
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References
Bonnisel-Gissinger P, Alnot M, Ehrhardt J-J, Behra P (1998) Surface oxidation of pyrite as a function of pH. Environ Sci Technol 32:2839–2845. https://doi.org/10.1021/es980213c
Bostick BC, Fendorf S (2003) Arsenite sorption on troilite (FeS) and pyrite (FeS2). Geochim Cosmochim Acta 67:909–921. https://doi.org/10.1016/S0016-7037(02)01170-5
Chipera SJ, Bish DL (2001) Baseline studies of the clay minerals society source clays: powder X-ray diffraction analyses. Clays Clay Miner 49:398–409. https://doi.org/10.1346/CCMN.2001.0490507
Cornell R Schwertmann U (2006) The iron oxides: structure, properties, reactions, occurrences and uses, 2nd completely revised and extended edn. Wiley-VCH, Weinheim
Devesa V, Del Razo LM, Adair B, Drobna Z, Waters SB, Hughes MF, Stýblo M, Thomas DJ (2004) Comprehensive analysis of arsenic metabolites by pH-specific hydride generation atomic absorption spectrometry. J Anal At Spectrom 19:1460–1467. https://doi.org/10.1039/B407388F
Fendorf S, Nico PS, Kocar BD, Masue Y, Tufano KJ (2010b) Arsenic chemistry in soils and sediments. Dev Soil Sci 34:357–378. https://doi.org/10.1016/S0166-2481(10)34012-8
Fendorf S, Michael HA, van Geen A (2010) Spatial and temporal variations of groundwater arsenic in South and Southeast Asia. Science 328:1123–1127. https://doi.org/10.1126/science.1172974
Frau F, Rossi A, Ardau C, Biddau R, da Pelo S, Atzei D, Licheri C, Cannas C, Capitani GC (2005) Determination of arsenic speciation in complex environmental samples by combined use of TEM and XPS. Microchim Acta 151:189–201. https://doi.org/10.1007/s00604-005-0399-3
Ghorbanzadeh N, Jung W, Halajnia A, Lakzian A, Kanra AN, Jeon B-H (2015) Removal of arsenate and arsenite from aqueous solution by adsorption on clay minerals. Geosystems Engineering 18:302–311. https://doi.org/10.1080/12269328.2015.1062436
Goldberg S (2002) Competitive adsorption of arsenate and arsenite on oxides and clay minerals. Soil Science Society America Journal 66:413–421. https://doi.org/10.2136/sssaj2002.4130
Hernández-Zavala A, Matoǔsek T, Drobná Z, Paul DS, Walton F, Adair BM, Jiří D, Thomas DJ, Stýblo M (2008) Speciation of arsenic in biological matrices by automated hydride generation-cryotrapping-atomic absorption spectrometry with the multiple microflame quartz tube atomizer (multiatomizer. Spectrochim). J Anal At Spectrom 23:342–351. https://doi.org/10.1039/b706144g
Ilgen AG, Kukkadapu RK, Dunphy DR, Artyushkova K, Cerrato JM, Kruichak JN, Janish MT, Sun CJ, Argo JM, Washington RE (2017) Synthesis and characterization of redox-active ferric nontronite. Chem Geol 470:1–12. https://doi.org/10.1016/j.chemgeo.2017.07.010
Keeling J, Raven M, Gates WP (2000) Geology and characterization of two hydrothermal nontronites from weathered metamorphic rocks at the Uley Graphite Mine, South Australia. Clays Clay Miner 48:537–548. https://doi.org/10.1346/CCMN.2000.0480506
Mermut AR, Cano AF (2001) Baseline studies of the clay minerals society source clays: chemical analysis of major elements. Clays Clay Miner 49:381–386. https://doi.org/10.1346/CCMN.2001.0490504
Moore JN, Ficklin WH, Johns C (1988) Partitioning of arsenic and metals in reducing sulfidic sediments. Environ Sci Technol 22:432–437. https://doi.org/10.1021/es00169a011
Moore DM, Reynolds RC Jr (1989) X-ray diffraction and the identification and analysis of clay minerals, 2nd edn. Oxford University Press, Oxford
Ona-Nguema G, Morin G, Juiliot F, Calas G, Brown GEJ (2005) EXAFS analysis of arsenate adsorption onto two-line ferrihydrite, hematite, goethite, and lepidocrocite. Environ Sci Technol 39:9147–9155. https://doi.org/10.1021/es050889p
Paktunc D, Dutrizac J, Gertsman V (2008) Synthesis and phase transformations involving scorodite, ferric arsenate and arsenical ferrihydrite: Implications for arsenic mobility. Geochim Cosmochim Acta 72:2649–2672. https://doi.org/10.1016/j.gca.2008.03.012
Del Razo LM, Stýblo M, Cullen WR, Thomas DJ (2001) Determination of trivalent methylated arsenicals in biological matrices. Toxicol Appl Pharmacol 174:282–293. https://doi.org/10.1006/taap.2001.9226
Saunders J, Lee M-K, Dhakal P (2018) Bioremediation of arsenic-contaminated groundwater by sequestration of arsenic in biogenic pyrite. Appl Geochem 98:233–243. https://doi.org/10.1016/j.apgeochem.2018.07.007
Smedley P, Kinniburgh D (2002) A review of the source, behavior and distribution of arsenic in natural water. Appl Geochem 17:517–568. https://doi.org/10.1016/S0883-2927(02)00018-5
Sparks DL (2003) Environmental soil chemistry. Academic Press, Cambridge
Środoń J, McCarty DK (2008) Surface area and layer charge of smectite from CEC and EGME/H2O retention measurements. Clays Clay Miner 56:155–174. https://doi.org/10.1346/CCMN.2008.0560203
Sverjensky DA, Fukushi K (2006) A predictive model (ETLM) for As(III) adsorption and surface speciation on oxides consistent with spectroscopic data. Geochim Cosmochim Acta 70:3778–3802. https://doi.org/10.1016/j.gca.2006.05.012
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This research was funded by the National Council of Science and Technology (Consejo Nacional para Ciencia y Tecnología, Mexico, Grant no. 41607).
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Cervini-Silva, J., Palacios, E., Nieto-Camacho, A. et al. One-nanometre-resolution evidence of As(III) anoxic and oxic transformations on the surfaces of expandable clay minerals. Int. J. Environ. Sci. Technol. 20, 31–40 (2023). https://doi.org/10.1007/s13762-022-04030-0
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DOI: https://doi.org/10.1007/s13762-022-04030-0