首页> 外文期刊>The Science of the Total Environment >Use of hardwood and sulfurized-hardwood biochars as amendments to floodplain soil from South River, VA, USA: Impacts of drying-rewetting on Hg removal
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Use of hardwood and sulfurized-hardwood biochars as amendments to floodplain soil from South River, VA, USA: Impacts of drying-rewetting on Hg removal

机译:使用硬木和硫化硬木生物炭作为美国弗吉尼亚州南河泛滥平原土壤的改良剂:干湿再湿对汞去除的影响

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摘要

Periodic flooding and drying conditions in floodplains affect the mobility and bioavailability of Hg in aquatic sediments and surrounding soils. Sulfurized materials have been recently proposed as Hg sorbents due to their high affinity to bind Hg, while sulfurizing organic matter may enhance methylmercury (MeHg) production, offsetting the beneficial aspects of these materials. This study evaluated hardwood biochar (OAK) and sulfurized-hardwood biochar (MOAK) as soil amendments for controlling Hg release in a contaminated floodplain soil under conditions representative of periodic flooding and drying in microcosm experiments in three stages: (1) wet biochar amended-systems with river water in an anoxic environment up to 200 d; (2) dry selected reaction vessels in an oxic environment for 90 d; (3) rewet such vessels with river water in an anoxic environment for 90 d. In Stage 1, greater Hg removal (17-98% for unfiltered total Hg (THg) and 47-99% for 0.45-μm THg) and lower MeHg concentrations (<20 ng L~(-1)) were observed in MOAK-amended systems (10%MOAKs). In Stage 3, release of Hg in 10%MOAKs was eight-fold lower than in soil controls (SedCTRs), while increases in aqueous (up to 21 ng L~(-1)) and solid (up to 88 ng g~(-1)) MeHg concentrations were observed. The increases in MeHg corresponded to elevated aqueous concentrations of Mn, Fe, SO_4~(2-), and HS~- in Stage 3. Results of S K-edge X-ray absorption near edge structure (XANES) analysis suggest oxidation of S in Stage 2 and formation of polysulfur in Stage 3. Results of pyrosequencing analysis indicate sulfate-reducing bacteria (SRB) became abundant in Stage 3 in 10%MOAKs.The shifts in biogeochemical conditions in 10%MOAKs in Stage 3 may increase the bioavailability of Hg to methylating bacteria. The results suggest limited impacts on Hg removal during drying and rewetting, while changes in biogeochemical conditions may affect MeHg production in sulfurized biochar-amended systems.
机译:洪泛区的周期性洪水和干燥条件会影响汞在水生沉积物和周围土壤中的迁移率和生物利用度。硫化材料由于其与汞的高亲和力而最近被提出作为汞吸附剂,而硫化有机物可增强甲基汞(MeHg)的产生,从而抵消了这些材料的有利方面。这项研究评估了硬木生物炭(OAK)和硫化硬木生物炭(MOAK)作为土壤改良剂的用途,以控制污染的洪泛区土壤中汞的释放,在三个阶段的缩微实验中,它们代表周期性的淹水和干燥:(1)湿生物炭在缺氧环境中长达200 d的河水系统; (2)在有氧环境中干燥选定的反应容器90 d; (3)在缺氧的环境中用河水将此类容器再润湿90 d。在第1阶段,在MOAK--中观察到较高的汞去除率(未过滤的总Hg(THg)为17-98%,0.45-μmTHg为47-99%)和较低的MeHg浓度(<20 ng L〜(-1))。修改后的系统(10%MOAK)。在第3阶段,汞在10%MOAK中的释放比土壤对照(SedCTR)低8倍,而水(释放至21 ng L〜(-1))和固体(释放至88 ng g〜( -1))观察到MeHg浓度。 MeHg的增加与阶段3中Mn,Fe,SO_4〜(2-)和HS〜-的水含量升高相对应。S K边缘X射线近边缘结构(XANES)吸收的分析结果表明S的氧化第2阶段的硫酸根和第3阶段的多硫形成。焦磷酸测序分析结果表明,第3阶段10%MOAK中的硫酸盐还原细菌(SRB)变得丰富。第3阶段10%MOAK中生物地球化学条件的变化可能会增加汞使细菌甲基化。结果表明,在干燥和重新润湿过程中,对汞去除的影响有限,而生物地球化学条件的变化可能会影响硫化生物炭改良系统中甲基汞的产量。

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  • 来源
    《The Science of the Total Environment》 |2020年第10期|136018.1-136018.14|共14页
  • 作者

  • 作者单位

    Department of Earth and Environmental Sciences University of Waterloo 200 University Ave. W Waterloo ON N2L 3G1 Canada;

    CLS@APS Sector 20 Advanced Photon Source Argonne National Laboratory 9700 S. Cass Avenue Argonne IL 60439 USA Science Division Canadian Light Source Inc. Saskatoon SK S7N 2V3 Canada;

    CanmetMlNING Natural Resource Canada Ottawa ON K1A 0G1 Canada;

    Formerly E. I. du Pont de Nemours and Company 974 Centre Road Wilmington DE 19805 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Dissimilatory Mn(IV) reduction; Fe(III) and SO_4~(2-) reduction; Methyl mercury production; S disproportionation; Hg HERFD-XAS; S K-edge XANES;

    机译:Mn(IV)异化还原;Fe(III)和SO_4〜(2-)还原;甲基汞生产;S不成比例;汞HERFD-XAS;S K-edge XANES;

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