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受污染河岸土壤中纳米晶辰砂的晶格缺陷表明生物源硫化物在硫化汞相形成过程中发挥了作用。

Crystal lattice defects in nanocrystalline metacinnabar in contaminated streambank soils suggest a role for biogenic sulfides in the formation of mercury sulfide phases.

作者信息

Koenigsmark Faye, Chiu Michelle, Rivera Nelson, Johs Alexander, Eskelsen Jeremy, Leonard Donovan, Robertson Boakai K, Szynkiewicz Anna, Derolph Christopher, Zhao Linduo, Gu Baohua, Hsu-Kim Heileen, Pierce Eric M

机构信息

Civil and Environmental Engineering, Duke University, Durham, NC 27708, USA.

Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA.

出版信息

Environ Sci Process Impacts. 2023 Mar 22;25(3):445-460. doi: 10.1039/d1em00549a.

Abstract

At mercury (Hg)-contaminated sites, streambank erosion can act as a main mobilizer of Hg into nearby waterbodies. Once deposited into the waters, mercury from these soils can be transformed to MeHg by microorganisms. It is therefore important to understand the solid-phase speciation of Hg in streambanks as differences in Hg speciation will have implications for Hg transport and bioavailability. In this study, we characterized Hg solid phases in Hg-contaminated soils (100-1100 mg per kg Hg) collected from the incised bank of the East Fork Poplar Creek (EFPC) in Oak Ridge, TN (USA). The analysis of the soil samples by scanning electron microscopy-energy dispersive spectroscopy indicated numerous microenvironments where Hg and sulfur (S) are co-located. According to bulk soil analyses by extended X-ray absorption fine structure spectroscopy (EXAFS), the near-neighbor Hg molecular coordination in the soils closely resembled freshly precipitated Hg sulfide (metacinnabar, HgS); however, EXAFS fits indicated the Hg in the HgS structure was undercoordinated with respect to crystalline metacinnabar. This undercoordination of Hg-S observed by spectroscopy is consistent with transmission electron microspy images showing the presence of nanocrystallites with structural defects (twinning, stacking faults, dislocations) in individual HgS-bearing particles. Although the soils were collected from exposed parts of the stream bank (, open to the atmosphere), the presence of reduced forms of S and sulfate-reducing microbes suggests that biogenic sulfides promote the formation of HgS nanoparticles in these soils. Altogether, these data demonstrate the predominance of nanoparticulate HgS with crystal lattice defects in the bank soils of an industrially impacted stream. Efforts to predict the mobilization and bioavailability of Hg associated with nano-HgS forms should consider the impact of nanocrystalline lattice defects on particle surface reactivity, including Hg dissolution rates and bioavailability on Hg fate and transformations.

摘要

在汞(Hg)污染场地,河岸侵蚀可成为汞进入附近水体的主要迁移因素。这些土壤中的汞一旦沉积到水体中,就会被微生物转化为甲基汞。因此,了解河岸中汞的固相形态很重要,因为汞形态的差异会对汞的迁移和生物有效性产生影响。在本研究中,我们对从美国田纳西州橡树岭东叉白杨溪(EFPC)深切河岸采集的汞污染土壤(汞含量为100 - 1100毫克/千克)中的汞固相进行了表征。通过扫描电子显微镜 - 能量色散光谱对土壤样品进行分析,结果表明存在许多汞和硫(S)共定位的微环境。根据扩展X射线吸收精细结构光谱(EXAFS)对整体土壤的分析,土壤中汞的近邻分子配位与新沉淀的硫化汞(黑辰砂,HgS)非常相似;然而,EXAFS拟合表明HgS结构中的汞相对于结晶黑辰砂配位不足。光谱观察到的汞 - 硫配位不足与透射电子显微镜图像一致,该图像显示在单个含HgS的颗粒中存在具有结构缺陷(孪晶、堆垛层错、位错)的纳米微晶。尽管这些土壤是从河岸的暴露部分(即暴露于大气)采集的,但还原态硫和硫酸盐还原微生物的存在表明生物源硫化物促进了这些土壤中HgS纳米颗粒的形成。总之,这些数据表明在受工业影响的溪流河岸土壤中,具有晶格缺陷的纳米颗粒HgS占主导地位。预测与纳米HgS形态相关的汞的迁移和生物有效性的研究应考虑纳米晶格缺陷对颗粒表面反应性的影响,包括汞的溶解速率以及汞的归宿和转化的生物有效性。

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