首页> 美国卫生研究院文献>Microbial Biotechnology >Arbuscular mycorrhizal fungi in a wetland constructed for benzene- methyl tert-butyl ether- and ammonia-contaminated groundwater bioremediation
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Arbuscular mycorrhizal fungi in a wetland constructed for benzene- methyl tert-butyl ether- and ammonia-contaminated groundwater bioremediation

机译:在湿地中用于苯甲基叔丁基醚和氨污染的地下水生物修复的丛枝菌根真菌

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摘要

Arbuscular mycorrhizal fungi (AMF), which are present in most natural environments, have demonstrated capacity to promote biodegradation of organic pollutants in the greenhouse. However, it is not certain whether AMF can spontaneously establish in phytoremediation systems constructed to decontaminate groundwater, because of the unusual conditions during the construction and operation of such systems. To assess this possibility, root samples from a wetland constructed for the phytoremediation of groundwater contaminated with benzene, methyl tert-butyl ether and ammonia were analysed. Substantial AMF colonization was observed in plant roots sampled close to the inlet of a basin filled with fine gravel and planted with Phragmites australis. In addition, analysis of a fragment of the nuclear large ribosomal subunit, amplified by nested PCR, revealed the presence of AMF molecular operational taxonomic units closely related to Funneliformis mosseae and Rhizophagus irregularis in the samples. These findings demonstrate the capacity of generalist AMF strains to establish spontaneously, rapidly and extensively in groundwater bioremediation technical installations.
机译:大多数自然环境中均存在丛枝菌根真菌(AMF),具有促进温室中有机污染物生物降解的能力。然而,由于在这样的系统的构造和运行过程中存在异常情况,因此尚不确定AMF是否可以自发地建立在用于净化地下水的植物修复系统中。为了评估这种可能性,分析了湿地的根部样品,该湿地是为对苯,甲基叔丁基醚和氨污染的地下水进行植物修复而分析的。在充满细砾石的水池入口附近取样并种植了芦苇的植物根部,观察到大量的AMF菌落。此外,对通过巢式PCR扩增的核大核糖体亚基片段的分析显示,样品中存在与桃耳沙门氏菌和不规则根瘤菌密切相关的AMF分子操作分类单位。这些发现表明,普通AMF菌株能够在地下水生物修复技术设施中自发,迅速和广泛地建立。

著录项

  • 期刊名称 Microbial Biotechnology
  • 作者

    Thomas Fester;

  • 作者单位
  • 年(卷),期 2013(6),1
  • 年度 2013
  • 页码 80–84
  • 总页数 5
  • 原文格式 PDF
  • 正文语种
  • 中图分类 微生物学;
  • 关键词

  • 入库时间 2022-08-21 11:04:35

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