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Dioxins in Primaiy Kaolin and Secondaiy Kaolinitic Clays

机译:Primaiy高岭土和Secondaiy高岭土中的二恶英

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摘要

Since 1996 dioxins have been repeatedly detected worldwide in Tertiary ball clays used as anticaking agent in the production of animal feed and a variety of other applications. The dioxins of these natural clays are very unlikely of anthropogenic source, but no model of dioxin enrichment has been established. A hypothetical model is presented which explains the highly variable dioxin loadings of the Tertiary kaolinitic clays by natural addition during clay-sedimentation. To prove this hypothesis. Tertiary primary nonsedimentary kaolin and sedimentary kaolinitic clays were collected at three profiles in Europe and analyzed for mineralogy, chemistry, organic carbon, and polychlorinated dibenzo-p-dioxins/-furans (PCDD/F). Primary kaolin, kaolinitic, and lignitic clays contained almost no PCDFs. PCDD concentration differed markedly between primary kaolin (3-91 pg/g) and secondary kaolinitic clay (711-45935 pg/g), respectively, lignitic clays (13513-1191120 pg/g). The dioxin loading of secondary kaolinitic and lignitic clays is approximately 10 to a few thousand times higher than in the primary kaolin or recent environmental settings. The dioxin concentrations decrease from octachlo-rodibenzo-p-dioxin to the tetrachlorodibenzo-p-dioxins and exhibit the "natural formation pattern". No correlation between PCDD/F concentration and bulk composition of clays was found. These findings support the hypothesis of the enrichment of dioxin in clays during sedimentation.
机译:自1996年以来,全球范围内在三级球状粘土中反复检测出二恶英,用作生产动物饲料和其他各种用途的抗结块剂。这些天然粘土中的二恶英极不可能是人为来源,但尚未建立二恶英富集模型。提出了一个假想模型,该模型解释了在粘土沉降过程中自然添加对第三高岭土的二恶英含量变化很大。为了证明这个假设。在欧洲,从三个剖面收集了第三级非沉积性高岭土和沉积高岭土,并对其矿物学,化学,有机碳和多氯二苯并-对二恶英/呋喃(PCDD / F)进行了分析。主要的高岭土,高岭土和木质粘土几乎不含PCDF。初级高岭土(3-91 pg / g)和次级高岭土(711-45935 pg / g)和木质粘土(13513-1191120 pg / g)之间的PCDD浓度显着不同。次生高岭土和木质粘土的二恶英含量比主要高岭土或最近的环境高约10至数千倍。二恶英的浓度从八氯-罗二苯并-对-二恶英减少到四氯二苯并-对-二恶英,并表现出“天然形成模式”。没有发现PCDD / F浓度与粘土体积组成之间的相关性。这些发现支持了沉积过程中二恶英在粘土中富集的假说。

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  • 来源
    《Environmental Science & Technology》 |2011年第2期|p.461-467|共7页
  • 作者单位

    Federal Institute for Geosciences and Natural Resources (BGR), Stilleweg 2, D-30655 Hannover, Germany;

    rnFederal Institute for Geosciences and Natural Resources (BGR), Stilleweg 2, D-30655 Hannover, Germany;

    rnFederal Institute for Geosciences and Natural Resources (BGR), Stilleweg 2, D-30655 Hannover, Germany,Technical University of Berlin (TUB)-lnstitute of Applied Geosciences, Ackerstrafle 76, D-13355 Berlin, Germany;

    rnFederal Institute for Geosciences and Natural Resources (BGR), Stilleweg 2, D-30655 Hannover, Germany,State Authority of Mining, Energy and Geology (LBBG), Stilleweg 2, D-30655 Hannover, Germany;

    rnTechnical University of Berlin (TUB)-lnstitute of Applied Geosciences, Ackerstrafle 76, D-13355 Berlin, Germany;

  • 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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  • 入库时间 2022-08-17 14:03:27

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