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Effects of Chemical, Biological, and Physical Aging As Well As Soil Addition on the Sorption of Pyrene to Activated Carbon and Biochar

机译:化学,生物和物理老化以及土壤添加对P对活性炭和生物炭的吸附作用

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摘要

In this study, the suitability of biochar and activated carbon (AC) for contaminated soil remediation is investigated by determining the sorption of pyrene to both materials in the presence and absence of soil and before as well as after aging. Biochar and AC were aged either alone or mixed with soil via exposure to (a) nutrients and microorganisms (biological), (b) 60 and 110 ℃ (chemical), and (c) freeze-thaw cycles (physical). Before and after aging, the pH, elemental composition, cation exchange capacity (CEC), microporous SA, and sorption isotherms of pyrene were quantified. Aging at 110 ℃ altered the physicochemical properties of all materials to the greatest extent (for example, pH increased by up to three units and CEC by up to S0% for biochar). Logarithmic K_(Fr), values ranged from 7.80 to 8.21 (ng kg~(-1)) (ng L~(-1)) ~(nF) for AC and 5.22 to 6.21 (ng kg~(-1))(ng L~(-1))~(-nf) for biochar after the various aging regimes. Grinding biochar to a smaller particle size did not significantly affect the sorption of d_(10) pyrene, implying that sorption processes operate on the subpartjcle scale. Chemical aging decreased the sorption of pyrene to the greatest extent (up to 1.8 log unit for the biochar+soil). The sorption to AC was affected more by the presence of soil than the sorption to biochar was. Our results suggest that AC and biochar have a high sorption capacity for pyrene that is maintained both in the presence of soil and during harsh aging. Both materials could therefore be considered in contaminated land remediation.
机译:在这项研究中,通过确定在存在和不存在土壤的情况下以及老化前后,to对两种材料的吸附能力,研究了生物炭和活性炭(AC)对污染土壤的修复能力。 Biochar和AC可以单独老化,也可以通过与(a)营养成分和微生物(生物),(b)60和110℃(化学)和(c)冻融循环(物理)接触而与土壤混合。老化前后,对the的pH,元素组成,阳离子交换容量(CEC),微孔SA和吸附等温线进行定量。 110℃时效会最大程度地改变所有材料的理化特性(例如,对于生物炭,pH值最多增加3个单位,CEC最多增加S0%)。对数K_(Fr),交流范围为7.80至8.21(ng kg〜(-1))(ng L〜(-1))〜(nF),而数值范围为5.22至6.21(ng kg〜(-1))( ng L〜(-1))〜(-nf)在各种老化方式下的生物炭。将生物炭磨成较小的粒径不会显着影响d_(10)pyr的吸附,这意味着吸附过程在子级范围内进行。化学老化最大程度地降低了the的吸附(生物炭+土壤的吸附量高达1.8 log单位)。土壤对AC的吸附比对生物碳的吸附影响更大。我们的结果表明,AC和生物碳对pyr具有很高的吸附能力,无论在土壤存在还是恶劣的老化过程中都能保持这种吸附能力。因此,两种材料都可以在受污染的土地修复中考虑。

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  • 来源
    《Environmental Science & Technology》 |2011年第24期|p.10445-10453|共9页
  • 作者单位

    Department of Environmental Engineering, Norwegian Geotechnical Institute (NGI), P.O. Box 3930, Ulleval Stadion, N-0806, Oslo, Norway;

    Department of Crop and Soil Sciences, Cornell University, Ithaca, New York 14853, United States;

    Department of Crop and Soil Sciences, Cornell University, Ithaca, New York 14853, United States;

    Department of Geological Sciences, University of Florida, 241 Williamson Hall, P.O. Box 112120, Gainesville, Florida 32611, United States;

    Department of Environmental Engineering, Norwegian Geotechnical Institute (NGI), P.O. Box 3930, Ulleval Stadion, N-0806, Oslo, Norway,Department of Applied Environmental Sciences, Stockholm University, 10691 Stockholm, Sweden,Institute for Plant and Environmental Sciences, University of Life Sciences, 5003 As, Norway;

  • 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 14:03:51

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