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A Method for Redox Mapping by Confocal Micro-X-ray Fluorescence Imaging: Using Chromium Species in a Biochar Particle as an Example

机译:共聚焦微X射线荧光成像的氧化还原映射方法:在生物炭颗粒中使用铬物种作为示例

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摘要

Redox mapping of solid-phase particles has been used for speciation mapping of near-surface materials or within grains through the use of thin-sections without depth information. Here, a procedure is presented for data collection and processing of depth-dependent redox mapping within solid particles using confocal micro-X-ray fluorescence imaging (CMXRFI). The procedure was applied to a biochar particle that was reacted with Cr(VI)-spiked water. The total Cr distribution was first obtained at an above-edge energy of the K-edge, and showed that Cr was primarily distributed near the surface of the particle. Redox mapping was conducted at 33 representative energies and linear combination fitting (LCF) was performed for the 33 data points from each pixel. The results indicate Cr(III) is the primary species with fractions ranging from 0.6 to 1 and that this fraction is greater in the interior pixels of the particle than at the surface; in contrast, the Cr(VI) fraction is greater at the surface than for interior pixels. The results likely indicate Cr(VI) was first adsorbed and diffused into the biochar, and then reduced to Cr(III). With more Cr(VI) adsorption and the exceedance of the reduction potential of the biochar, remaining Cr(VI) was accumulated on the surface. The redox mapping method was validated by micro-XANES (X-ray absorption near-edge structure) and XPS (X-ray photoelectron spectroscopy) results. This demonstration indicates the developed method combined with CMXRFI can be used to delineate the distribution of different oxidation states of an element within an intact particle or layer.
机译:通过在没有深度信息的情况下使用薄截面,固相颗粒的氧化还原映射已经用于近表面材料或谷物内的晶粒。这里,呈现用于使用共聚焦微X射线荧光成像(CMXRFI)的固体颗粒内的数据收集和处理深度依赖的氧化还原映射的过程。将该程序应用于生物炭颗粒,与Cr(vi) - 镁水反应。首先在k边缘的上方能量下获得总Cr分布,并显示Cr主要分布在颗粒表面附近。在33个代表能量下进行氧化还原映射,并且对来自每个像素的33个数据点进行线性组合配合(LCF)。结果表明Cr(III)是具有0.6至1的级分的主要物种,并且该级分在颗粒的内部像素中大于表面;相反,表面在表面略大于内部像素。结果可能表明Cr(VI)首先被吸附并扩散到生物炭中,然后减少至Cr(III)。具有更多Cr(vi)吸附和远离生物炭的减少电位,剩余的Cr(vi)积聚在表面上。通过微XANES(X射线吸收近边缘结构)和XPS(X射线光电子能谱)验证氧化还原映射方法。该示范表明,与CMXRFI结合的开发方法可用于描绘完整颗粒或层内元素的不同氧化状态的分布。

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  • 来源
    《Analytical chemistry》 |2019年第8期|共8页
  • 作者单位

    China Univ Geosci Sch Environm Studies 388 Lumo Rd Wuhan 430074 Hubei Peoples R China;

    Univ Waterloo Dept Earth &

    Environm Sci 200 Univ Ave W Waterloo ON N2L 3G1 Canada;

    Univ Waterloo Dept Earth &

    Environm Sci 200 Univ Ave W Waterloo ON N2L 3G1 Canada;

    Argonne Natl Lab Adv Photon Source CLS APS Sect 20 9700 S Cass Ave Argonne IL 60439 USA;

    Stantec Consulting Ltd 100-300 Hagey Blvd Waterloo ON N2L 0A4 Canada;

    Univ Waterloo Dept Earth &

    Environm Sci 200 Univ Ave W Waterloo ON N2L 3G1 Canada;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 分析化学;
  • 关键词

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