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Net Methylation of Mercury in Estuarine Sediment Microcosms Amended with Dissolved, Nanoparticulate, and Microparticulate Mercuric Sulfides

机译:在河口沉积物缩影中的汞净甲基化被溶解的,纳米微粒和微粒硫化汞修正

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The production of methylmercury (MeHg) by anaerobic microorganisms depends in part on the speciation and bioavailability of inorganic mercury to these organisms. Our previous work with pure cultures of methylating bacteria has demonstrated that the methylation potential of mercury decreased during the aging of mercuric sulfides (from dissolved to nanoparticulate and microcrystalline HgS). The objective of this study was to understand the relationship between mercury sulfide speciation and methylation potential in experiments that more closely simulate the complexity of sediment settings. The study involved sediment slurry microcosms that represented a spectrum of salinities in an estuary and were each amended with different forms of mercuric sulfides: dissolved Hg and sulfide, nanoparticulate HgS (3-4 nm in diameter), and microparticulate HgS (>500 nm). The results indicated that net MeHg production was influenced by both the activity of sulfate-reducing microorganisms (roughly represented by the rate of sulfate loss) and the bioavailability of mercury. In the presence of abundant sulfate and carbon sources (supporting relatively high microbial activity), net MeHg production in the slurries amended with dissolved Hg was greater than in slurries amended with nano-HgS, similar to previous experiments with pure bacterial cultures. In microcosms with minimal microbial activity (indicated by low rates of sulfate loss), the addition of either dissolved Hg or nano-HgS resulted in similar amounts of net MeHg production. For all slurries receiving micro-HgS, MeHg production did not exceed abiotic controls. In slurries amended with dissolved and nano-HgS, mercury was mainly partitioned to bulk-scale mineral particles and colloids, indicating that Hg bioavailability was not simply related to dissolved Hg concentration or speciation. Overall, the results suggest that models for mercury methylation potential in the environment will need to balance the relative contributions of mercury speciation and activity of methylating microorganisms.
机译:厌氧微生物产生甲基汞(MeHg)部分取决于无机汞对这些生物的形态和生物利用度。我们先前对甲基化细菌的纯培养物的研究表明,汞的甲基化潜力在硫化汞的老化过程中(从溶解的HgS到纳米颗粒和微晶的HgS)下降。这项研究的目的是在更紧密模拟沉积物设置复杂性的实验中了解硫化汞形态与甲基化电位之间的关系。该研究涉及代表河口盐度谱的沉积物泥浆微观世界,每个微观世界都被不同形式的硫化汞修正:溶解的汞和硫化物,纳米颗粒的HgS(直径3-4 nm)和微粒的HgS(> 500 nm)。 。结果表明,MeHg的净产量受硫酸盐还原微生物的活性(大致由硫酸盐损失的速率表示)和汞的生物利用度的影响。在存在丰富的硫酸盐和碳源(支持相对较高的微生物活性)的情况下,与以前用纯细菌培养进行的实验相似,用溶解的Hg修正的浆液的净MeHg产量要大于用nano-HgS修正的浆液的净MeHg产量。在具有最小微生物活性的微观世界中(硫酸盐损失率低表明),添加溶解的汞或纳米汞可导致产生类似量的净甲基汞。对于所有接受微量HgS的浆料,MeHg产量均未超过非生物对照。在用溶解的汞和纳米硫化氢修正的浆料中,汞主要分配给大块的矿物颗粒和胶体,表明汞的生物利用度不仅与溶解的汞浓度或形态有关。总体而言,结果表明,环境中汞甲基化潜力的模型将需要平衡汞形态的相对贡献和甲基化微生物的活性。

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  • 来源
    《Environmental Science & Technology》 |2014年第16期|9133-9141|共9页
  • 作者单位

    Duke University, Department of Civil and Environmental Engineering, 121 Hudson Hall, Durham, North Carolina 27708 United States,Woods Hole Oceanographic Institution, Department of Marine Chemistry and Geochemistry, 266 Woods Hole Road, Woods Hole, Massachusetts 02543 United States;

    Duke University, Department of Civil and Environmental Engineering, 121 Hudson Hall, Durham, North Carolina 27708 United States;

    Virginia Polytechnic Institute and State University, Department of Geosciences, Blacksburg, Virginia 24061 United States,Temple University, Department of Earth and Environmental Science, Philadelphia, Pennsylvania 19122 United States;

    Duke University, Department of Civil and Environmental Engineering, 121 Hudson Hall, Durham, North Carolina 27708 United States;

    Duke University, Department of Civil and Environmental Engineering, 121 Hudson Hall, Durham, North Carolina 27708 United States;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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