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Structural characterization of arsenic compounds in volcanic ashes and loessic sediments

机译:火山岩中砷化合物的结构表征和黄土沉积物

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X-ray Absorption Fine Structure spectroscopy (XAFS) was used to determine the oxidation state of Arsenic (As) and its local chemical coordination in recent and ancient volcanic ashes and Chacopampean loess sediments. XANES analysis allowed to discriminate the oxidation states of arsenic in the studied samples: As~(5+) is dominant in loess sediments while in volcanic ashes As~(-1) and As~(3+) were identified. The proposed EXAFS models fit well with the experimental data, suggesting that in loess sediments, As~(5+) could be in the form of arsenate ions adsorbed onto ferric oxyhydroxides. In recent volcanic ashes, the identified As~(-1) species is likely associated with arsenopyrite or arsenical pyrite. Besides, As~(3+) is likely related to As atoms present as impurities within the glass structure, in the form of oxy-hydroxide complexes. In ancient volcanic ashes As~(3+) is the dominant oxidation state but As~(5+) was also identified.
机译:X射线吸收细结构光谱(XAFS)用于确定砷(AS)的氧化状态及其近期的火山岩灰和基波缺陷黄土沉积物的局部化学协调。 XANES分析允许区分研究中砷的氧化状态:如〜(5+)在黄土沉积物中占主导地位,同时鉴定〜(3+),〜(3+)。所提出的EXAFS模型与实验数据相适合,表明在黄土沉积物中,如〜(5+)可以是吸附在铁羟基氧化铁上的砷酸盐离子的形式。在最近的火山灰中,鉴定为〜(-1)种可能与阿塞枯石或砷黄铁矿有关。此外,如〜(3+)可能与氧化氧化物复合物的形式有关作为玻璃结构内的杂质的原子。在古老的火山灰烬中,如〜(3+)是主要的氧化态,但也发现了〜(5+)。

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