Department of Soil and Environmental Sciences, National Chung Hsing University, 250 Kuo Kuang Rd., Taichung 40227, Taiwan, ROC.
Department of Soil and Environmental Sciences, National Chung Hsing University, 250 Kuo Kuang Rd., Taichung 40227, Taiwan, ROC; Department of Environmental Science and Engineering, Tunghai University, Taichung 40704, Taiwan, ROC.
J Hazard Mater. 2015 Oct 15;296:230-238. doi: 10.1016/j.jhazmat.2015.03.044. Epub 2015 Mar 24.
Sequential extraction has been widely used to classify metal species in soils and sediments; however, the lack of selectivity in extraction reagents may lead to the misinterpretation of metal speciation. In this study, we used X-ray absorption near edge structure (XANES) spectroscopy to classify Cr species based on its molecular form. These results complement the conventional Cr fractionation derived from the Tessier extraction method. The linear combination fitting (LCF) for the Cr-XANES spectra indicated that the Cr species in the soils could generally be described as Cr(III) sorbed on ferrihydrite (Cr-FH), Cr(III) complexed with humic acid (Cr-HA), and precipitated Cr. While the sum of the adsorbed Cr(III) and Cr(III)/Fe coprecipitates showed a nearly 1:1 relationship with reducible Cr, the total of Cr precipitates and organic Cr also followed the same trend with oxidizable Cr. This result indicated that there might be a underestimation in the reducible fraction as pure Cr(III) precipitates associated with surfaces of Fe minerals would not be extracted in the reducible process. Instead, such pure Cr(III) precipitates were dissolved during the oxidizable process, resulting in a overestimation in the fractionation of organic-related Cr.
连续提取已广泛用于分类土壤和沉积物中的金属物种;然而,提取试剂缺乏选择性可能导致金属形态的错误解释。在本研究中,我们使用 X 射线吸收近边结构(XANES)光谱根据其分子形式对 Cr 物种进行分类。这些结果补充了源自 Tessier 提取方法的传统 Cr 分级。Cr-XANES 光谱的线性组合拟合(LCF)表明,土壤中的 Cr 物种通常可以描述为吸附在铁氢氧化物上的 Cr(III)(Cr-FH)、与腐殖酸络合的 Cr(III)(Cr-HA)和沉淀的 Cr。虽然吸附的 Cr(III)和 Cr(III)/Fe 共沉淀之和与可还原 Cr 呈近 1:1 关系,但总沉淀 Cr 和有机 Cr 也与可氧化 Cr 呈相同趋势。这一结果表明,可还原部分可能存在低估,因为与 Fe 矿物表面相关的纯 Cr(III)沉淀不会在可还原过程中被提取。相反,这种纯 Cr(III)沉淀在可氧化过程中溶解,导致与有机相关的 Cr 分级的高估。