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首页> 外文期刊>Chemosphere >Effects of biochar and the geophagous earthworm Metaphire guillelmi on fate of ~(14)C-catechol in an agricultural soil
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Effects of biochar and the geophagous earthworm Metaphire guillelmi on fate of ~(14)C-catechol in an agricultural soil

机译:生物炭和食盐earth变种对土壤中〜(14)C-邻苯二酚的命运的影响

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摘要

Both biochar and earthworms can exert influence on behaviors of soil-borne monomeric phenols in soil; however, little was known about the combined effects of biochar and earthworm activities on fate of these chemicals in soil. Using ~(14)C-catechol as a representative, the mineralization, transformation and residue distribution of phenolic humus monomer in soil amended with different amounts of biochar (0%, 0.05%, 0.5%, and 5%) without/with the geophagous earthworm Metaphire guillelmi were investigated. The results showed biochar at amendment rate <0.5% did not affect ~(14)C-catechol mineralization, whereas 5% biochar amendment significantly inhibited the mineralization. Earthworms did not affect the mineralization of ~(14)C-catechol in soil amended with <0.5% biochar, but significantly enhanced the mineralization in 5% biochar amended soil when they were present in soil for 9 d. When earthworms were removed from the soil, the mineralization of ~(14)C-catechol was significantly lower than that of in earthworm-free soil indicating that ~(14)C-catecholic residues were stabilized during their passage through earthworm gut. The assimilation of ~(14)C by earthworms was low (1.2%), and was significantly enhanced by biochar amendment, which was attributed to the release of biochar-associated ~(14)C-catecholic residues during gut passage of earthworm.
机译:生物炭和earth都可以影响土壤中的土壤传播的单体酚的行为。然而,关于生物炭和worm活动对这些化学物质在土壤中的命运的综合影响知之甚少。以〜(14)C-邻苯二酚为代表,在不添加/不添加噬菌剂的情况下,用不同量的生物炭(0%,0.05%,0.5%和5%)修正了土壤中酚类腐殖质单体的矿化,转化和残留分布研究了MetaMetaphire guillelmi。结果表明,生物炭修正率<0.5%不会影响〜(14)C-邻苯二酚的矿化作用,而5%的生物炭修正会显着抑制矿化作用。 did对浓度<0.5%的生物炭改良的土壤中〜(14)C-儿茶酚的矿化没有影响,但是当土壤中存在9 d时,对5%生物炭改性的土壤的矿化作用显着增强。当将from从土壤中移出时,〜(14)C-儿茶酚的矿化度显着低于无soil土壤中的矿化度,这表明〜(14)C-儿茶酚残基在穿过earth肠时得以稳定。 〜对〜(14)C的同化率低(1.2%),并通过生物炭改良得到显着增强,这归因于bio肠道通过过程中与生物炭相关的〜(14)C-儿茶酚残基的释放。

著录项

  • 来源
    《Chemosphere》 |2014年第7期|109-114|共6页
  • 作者单位

    State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China,Changshu Agro-ecological Experimental Station, Chinese Academy of Sciences, Changshu 215555, China;

    State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, 163 Xianlin Avenue, Nanjing 210023, China;

    State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, 163 Xianlin Avenue, Nanjing 210023, China;

    State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, 163 Xianlin Avenue, Nanjing 210023, China;

    State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, 163 Xianlin Avenue, Nanjing 210023, China,Institute for Climate and Global Change Research, Nanjing University, 22 Hankou Road, Nanjing 210093, China;

    State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China,Changshu Agro-ecological Experimental Station, Chinese Academy of Sciences, Changshu 215555, China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Black carbon; Phenolic compounds; Mineralization; Transformation; Accumulation;

    机译:黑炭;酚类化合物;矿化;转型;积累;

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