Arsenic Mobilization from Thawing Permafrost

IF 2.9 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY ACS Earth and Space Chemistry Pub Date : 2024-03-18 DOI:10.1021/acsearthspacechem.3c00355
Elliott K. Skierszkan*, Valerie A. Schoepfer, Matthew D. Fellwock, John W. Dockrey, Ardalan Hayatifar, Viorica F. Bondici, Joyce M. McBeth and Matthew B. J. Lindsay, 
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Abstract

Thawing permafrost releases labile organic carbon and alters groundwater geochemistry and hydrology with uncertain outcomes for the mobility of hazardous metal(loid)s. Managing water quality in thawing permafrost regions is predicated on a detailed understanding of the speciation and abundance of metal(loid)s in permafrost soils and porewaters produced during thaw, which remains limited at present. This study contributes new knowledge on the sources and fate of arsenic during the thaw of organic-rich permafrost using samples collected from a subarctic permafrost region associated with geogenic arsenic (Dawson Range, Yukon, Canada). Several permafrost cores and active-layer samples from this region were analyzed for their solid-phase and aqueous geochemical characteristics and their arsenic speciation. Porewaters were extracted from permafrost cores after thaw under anaerobic conditions for aqueous geochemical analyses. Bedrock samples from the field site were also analyzed for arsenic speciation and mineralogy. X-ray diffraction and X-ray near-edge spectroscopy (XANES) analyses of weathered bedrock upgradient of soil sampling locations contained arsenic(V) hosted in iron-(oxyhydr)oxides and scorodite. XANES and micro X-ray fluorescence analyses of permafrost soils indicated a mixture of arsenic(III) and arsenic(V), indicating redox recycling of arsenic. Soil-bound arsenic was colocated with iron, likely as arseniferous iron-(oxyhydr)oxides that have been encapsulated by aggrading permafrost over geologic time. However, permafrost thaw produced porewater containing elevated dissolved arsenic (median 40 μg L–1, range 2–96 μg L–1). Thawed permafrost porewater also contained elevated dissolved iron (median 5.5 mg L–1, range 0.5–40 mg L–1) and dissolved organic carbon (median 423 mg L–1, range 72–3240 mg L–1), indicative of reducing conditions. This study highlights that arsenic can be found in reactive forms in permafrost soil, and that its thaw can release arsenic and iron to porewater and produce poor water quality.

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解冻永久冻土中的砷迁移
永久冻土融化会释放可变有机碳,并改变地下水地球化学和水文学,从而对有害金属(loid)的流动性产生不确定的影响。管理解冻永久冻土地区的水质取决于对永久冻土土壤和解冻过程中产生的孔隙水中金属(loid)的种类和丰度的详细了解,而目前这方面的了解仍然有限。本研究利用从与地生砷有关的亚北极永久冻土区(加拿大育空地区道森山脉)采集的样本,为富含有机质的永久冻土融化过程中砷的来源和归宿提供了新的知识。对该地区的一些永久冻土岩心和活动层样本进行了分析,以了解其固相和水体地球化学特征以及砷的种类。在厌氧条件下,从解冻后的永久冻土岩心中提取孔隙水进行水地球化学分析。此外,还对野外地点的基岩样本进行了砷标示和矿物学分析。对土壤取样地点上游的风化基岩进行的 X 射线衍射和 X 射线近缘光谱(XANES)分析显示,铁(氧水)氧化物和蝎尾石中含有砷(V)。对永久冻土进行的 XANES 和微 X 射线荧光分析表明,砷(III)和砷(V)混合在一起,表明砷进行了氧化还原再循环。土壤中的砷与铁结合在一起,很可能是含砷的铁(氧氢)氧化物,随着地质年代的推移,这些氧化物已被逐渐融化的永久冻土所包裹。然而,永久冻土融化产生的孔隙水含有较高的溶解砷(中位数为 40 μg L-1,范围为 2-96 μg L-1)。解冻的永久冻土孔隙水中还含有较高的溶解铁(中位数为 5.5 毫克/升,范围为 0.5-40 毫克/升)和溶解有机碳(中位数为 423 毫克/升,范围为 72-3240 毫克/升),表明存在还原条件。这项研究表明,砷可以以活性形式存在于永久冻土中,而永久冻土的融化会将砷和铁释放到孔隙水中,从而导致水质变差。
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来源期刊
ACS Earth and Space Chemistry
ACS Earth and Space Chemistry Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
5.30
自引率
11.80%
发文量
249
期刊介绍: The scope of ACS Earth and Space Chemistry includes the application of analytical, experimental and theoretical chemistry to investigate research questions relevant to the Earth and Space. The journal encompasses the highly interdisciplinary nature of research in this area, while emphasizing chemistry and chemical research tools as the unifying theme. The journal publishes broadly in the domains of high- and low-temperature geochemistry, atmospheric chemistry, marine chemistry, planetary chemistry, astrochemistry, and analytical geochemistry. ACS Earth and Space Chemistry publishes Articles, Letters, Reviews, and Features to provide flexible formats to readily communicate all aspects of research in these fields.
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