首页> 外文期刊>Environmental Science & Technology >Nature of the Interlayer Environment in an Organoclay Optimized for the Sequestration of Dibenzo-p-dioxin
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Nature of the Interlayer Environment in an Organoclay Optimized for the Sequestration of Dibenzo-p-dioxin

机译:隔离二苯并-p-二恶英优化的有机粘土中的中间层环境的性质。

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摘要

A Na-smectite clay (Na-SWy-2) was exchanged with various amounts of dimethyldioctadecylammonium bromide (DODA-Br) up to twice the cation exchange capacity (CEC). The organoclay (DODA-SWy-2) with DODA-Br added at 2 × CEC exhibited a maximum 4.2 nm d-spacing and a 31.496 carbon content, which demonstrates DODA~+ intercalation. DODA- SWy-2 was evaluated as an archetype of commercial products used to sequester hydrophobic contaminants, and the nature of the primarily C18 alkylhydrocarbon-chain interlayer environment was emhasized. Shirts in ν(CH) and CH_2 rocking band positions in DODA-SWy-2-complex FTIR-spectra indicate that DODA C18 chains were more ordered as DODA surface coverage was increased. Differential scanning calorimetry analysis indicated a DODA- SWy-2 gel-to-liquid transition temperature much lower than the melting point of crystalline DODA-Br and similar to that of aqueous DODA-Br vesicles. This suggests that the transition was governed by C18 alkyl tail-tail interactions in the clay interlamellar region. Dibenzo-p-dioxin (DD) sorption from water by DODA- SWy-2 was compared to DD sorption by the geosorbents granular activated carbon (GAC), K- exchanged saponite, and a muck soil. The linear K_1 sorption coefficients (log K_1) from a linear fit of the sorption isotherms were 4.37 for DODA-SWy-2, 5.55 for GAC, 3.19 for muck soil, and 2.46 for K-saponite. The DD-organic- matter-normalized sorption coefficient (K_(om)) was ~2.4 times the octanol-water partition coefficient (K_(ow)). This indicates that DD has a higher affinity for the nonpolar interlayer DODA organic phase than for octanol. In contrast, the K_(om) for muck soil DD sorption was ~10 times less than K_(ow), which reflects the higher polarity of amorphous soil organic matter relative to octanol. Enhanced DD uptake by the DODA-derived lipophilic phase in the organoclay is attributed to the low polarity, "open" C18 alkyl structure due to the physical dimensions of "v-shaped" DODA~+ molecular, and low density of the interlamellar phase (~0.50 g/ cm3) density of intercalated DODA~+.
机译:将钠蒙脱土(Na-SWy-2)与各种数量的二甲基二十八烷基溴化铵(DODA-Br)交换,交换量达到阳离子交换容量(CEC)的两倍。在2×CEC下添加DODA-Br的有机粘土(DODA-SWy-2)的最大d间距为4.2 nm,碳含量为31.496,表明DODA〜+嵌入。 DODA-SWy-2被评估为用于螯合疏水性污染物的商业产品的原型,并且强调了主要是C18烷基烃链中间层环境的性质。 DODA-SWy-2-复合FTIR光谱中位于v(CH)和CH_2摇摆带位置的衬衫表明,随着DODA表面覆盖率的增加,DODA C18链的排列更加有序。差示扫描量热分析表明DODA-SWy-2凝胶-液体的转变温度远低于结晶的DODA-Br的熔点,并且与含水的DODA-Br囊泡的熔点相似。这表明过渡是由粘土层间区域中的C18烷基尾尾相互作用控制的。将DODA-SWy-2从水中的二苯并对二恶英(DD)吸附与地质吸附剂颗粒活性炭(GAC),K交换的皂石和泥土的DD吸附进行了比较。来自吸附等温线的线性拟合的线性K_1吸附系数(log K_1)对于DODA-SWy-2为4.37,对于GAC为5.55,对于渣土为3.19,对于钾皂石为2.46。 DD-有机物归一化吸附系数(K_(om))约为辛醇-水分配系数(K_(ow))的2.4倍。这表明DD对非极性夹层DODA有机相的亲和力高于对辛醇的亲和力。相比之下,渣土DD吸附的K_(om)比K_(ow)小约10倍,这反映了非晶态土壤有机物相对于辛醇的极性更高。有机粘土中DODA衍生的亲脂相提高的DD吸收归因于低极性,“开放”的C18烷基结构,这归因于“ v形” DODA〜+分子的物理尺寸以及层间相的低密度( 〜0.50 g / cm3)的插层DODA〜+密度。

著录项

  • 来源
    《Environmental Science & Technology》 |2012年第17期|p.9584-9591|共8页
  • 作者单位

    Crop, Soil and Environmental Sdences, Purdue University, 915 W. State Street, West Lafayette, Indiana 47907-2054, United States;

    Crop, Soil and Environmental Sdences, Purdue University, 915 W. State Street, West Lafayette, Indiana 47907-2054, United States;

    Office of Research and Development, U.S. Environmental Protection Agency, 26 W. Martin Luther King Drive, Cincinnati, Ohio 45268, United States;

    Tetra Tech Inc., 250 West Court Street, Suite 200W, Cincinnati, Ohio 45202, United States;

    Department of Crop and Soil Sciences, 532 Plant and Soil Sciences Building, Michigan State University East Lansing, Michigan 48824-1325, 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);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-17 14:02:52

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