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Impact of bacterial and fungal processes on 14C-hexadecane mineralisation in weathered hydrocarbon contaminated soil

机译:细菌和真菌过程对风化烃污染土壤中14 C-十六烷矿化的影响

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摘要

In this study, the impact of bacterial and fungal processes on 14C-hexadecane mineralisation was investigated in weathered hydrocarbon contaminated soil. The extent of 14C-hexadecane mineralisation varied depending on the bioremediation strategy employed. Under enhanced natural attenuation conditions, 14C-hexadecane mineralisation after 98 days was 8.5 ± 3.7% compared to < 1.2% without nitrogen and phosphorus additions. 14C-hexadecane mineralisation was further enhanced through Tween 80 amendments (28.9 ±2.4%) which also promoted the growth of a Phanerochaete chyrsosporium fungal mat Although fungal growth in weath ered hydrocarbon contaminated soil could be promoted through supplementing additional carbon sources (Tween 80, sawdust, compost, pea straw), fungal 14C-hexadecane mineralisation was negligible when sodi um azide was added to soil microcosms to inhibit bacterial activity. In contrast, when fungal activity was inhibited through nystatin additions, 14C-hexadecane mineralisation ranged from 6.5 ±0.2 to 35.8 ±3.8% after 98 days depending on the supplied amendment. Bacteria inhibition with sodium azide resulted in a reduction in bacterial diversity (33-37%) compared to microcosms supplemented with nystatin or microcosms without inhibitory supplements. However, alfcfl bacterial groups were undetected in sodium azide supplemented microcosms, highlighting the important role of this bacterial group in 14C-hexadecane mineralisation.
机译:在这项研究中,在风化的碳氢化合物污染的土壤中研究了细菌和真菌过程对14C-十六烷矿化的影响。 14C-十六烷矿化的程度取决于所采用的生物修复策略。在增强的自然衰减条件下,98天后14 C-十六烷的矿化度为8.5±3.7%,而未添加氮和磷的矿物质的<1.2%。通过吐温80修正剂(28.9±2.4%)进一步增强了14C-十六烷的矿化作用,该修正剂还促进了Phanerochaete chyrsosporium真菌垫的生长,尽管通过补充其他碳源(吐温80,锯末,堆肥,豌豆秸秆),将叠氮化钠添加到土壤微观世界以抑制细菌活性时,真菌14C-十六烷的矿化作用可忽略不计。相反,当通过制霉菌素抑制真菌活性时,根据所提供的修正,14天的十六烷矿化在98天后的范围为6.5±0.2至35.8±3.8%。与添加制霉菌素的缩微膜或不添加抑制增补剂的微膜相比,叠氮化钠对细菌的抑制导致细菌多样性的降低(33-37%)。然而,在叠氮化钠补充的微观世界中未检测到alfcf1细菌群,突显了该细菌群在14C-十六烷矿化中的重要作用。

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  • 来源
    《Science of the total environment》 |2012年第1期|p.585-591|共7页
  • 作者单位

    School of Biological Sciences. Hinders University, Adelaide, South Australia, 5001, Australia;

    School of Biological Sciences. Hinders University, Adelaide, South Australia, 5001, Australia;

    Centre for Environmental Risk Assessment and Remediation (CERAR), University of South Australia, Mawson Lakes Campus, Adelaide, South Australia, 5095, Australia,Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC CARE), Mawson Lakes, Adelaide, South Australia, 5095, Australia;

    Centre for Environmental Risk Assessment and Remediation (CERAR), University of South Australia, Mawson Lakes Campus, Adelaide, South Australia, 5095, Australia,Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC CARE), Mawson Lakes, Adelaide, South Australia, 5095, Australia;

    Centre for Environmental Risk Assessment and Remediation (CERAR), University of South Australia, Mawson Lakes Campus, Adelaide, South Australia, 5095, Australia,Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC CARE), Mawson Lakes, Adelaide, South Australia, 5095, Australia;

    Centre for Environmental Risk Assessment and Remediation (CERAR), University of South Australia, Mawson Lakes Campus, Adelaide, South Australia, 5095, Australia,Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC CARE), Mawson Lakes, Adelaide, South Australia, 5095, Australia;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    alkb; DGGE; hexadecane; mineralisation;

    机译:alkb;DGGE;十六烷矿化;

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