Kumar Naresh, Noël Vincent, Besold Johannes, Planer-Friedrich Britta, Boye Kristin, Fendorf Scott, Brown Gordon E
Department of Geological Sciences, School of Earth, Energy & Environmental Sciences, Stanford University, Stanford, California 94305-2115, United States.
Center for Environmental Implications of NanoTechnology (CEINT), Duke University, Durham, North Carolina 27708, United States.
ACS Earth Space Chem. 2022 Jul 21;6(7):1666-1673. doi: 10.1021/acsearthspacechem.1c00373. Epub 2022 Jul 6.
Knowledge of how arsenic (As) partitions among various phases in Fe-rich sulfidic environments is critical for understanding the fate and mobility of As in such environments. We studied the reaction of arsenite and arsenate sorbed on ferrihydrite nanoparticle surfaces with dissolved sulfide at varying S/Fe ratios (0.1-2.0) to understand the fate and transformation mechanism of As during sulfidation of ferrihydrite. By using aqueous As speciation analysis by IC-ICP-MS and solid-phase As speciation analysis by synchrotron-based X-ray absorption spectroscopy (XAS), we were able to discern the mechanism and pathways of As partitioning and thio-arsenic species formation. Our results provide a mechanistic understanding of the fate and transformation of arsenic during the codiagenesis of As, Fe, and S in reducing environments. Our aqueous-phase As speciation data, combined with solid-phase speciation data, indicate that sulfidation of As-sorbed ferrihydrite nanoparticles results in their transformation to trithioarsenate and arsenite, independent of the initial arsenic species used. The nature and extent of transformation and the thioarsenate species formed were controlled by S/Fe ratios in our experiments. However, arsenate was reduced to arsenite before transformation to trithioarsenate.
了解砷(As)在富铁硫化环境中各相之间的分配情况,对于理解砷在此类环境中的归宿和迁移性至关重要。我们研究了吸附在针铁矿纳米颗粒表面的亚砷酸盐和砷酸盐与不同S/Fe比(0.1 - 2.0)的溶解硫化物之间的反应,以了解针铁矿硫化过程中砷的归宿和转化机制。通过采用离子色谱 - 电感耦合等离子体质谱法(IC - ICP - MS)进行水相砷形态分析以及基于同步辐射的X射线吸收光谱法(XAS)进行固相砷形态分析,我们能够识别砷的分配机制和途径以及硫代砷物种的形成。我们的结果为还原环境中砷、铁和硫共沉积过程中砷的归宿和转化提供了机理认识。我们的水相砷形态数据与固相形态数据相结合表明,吸附砷的针铁矿纳米颗粒的硫化作用导致它们转化为三硫代砷酸盐和亚砷酸盐,这与所使用的初始砷物种无关。在我们的实验中,转化的性质和程度以及形成的硫代砷酸盐物种受S/Fe比控制。然而,砷酸盐在转化为三硫代砷酸盐之前先被还原为亚砷酸盐。