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The effect of organic acids on the behaviour and biodegradation of C-14-phenanthrene in contaminated soil

机译:有机酸对污染土壤中C-14菲的行为和生物降解的影响

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The interaction between root exudates and soil microbes has been hypothesised as the primary mechanism for the biodegradation of organic pollutants in the rhizosphere. However, the mechanisms governing this loss process are not completely understood. This study aimed to investigate the effect of two important compounds within root exudates (citric and malic acid) on C-14-phenanthrene desorption and bioaccessibility in soil. Overall results showed that the presence of both citric and malic acid (>100 mmol l(-1)) enhanced the desorption of C-14-phenanthrene; this appeared to be concentration dependant. Increases in extractability were not reflected in a higher bioaccessibility. Despite enhancing the desorption of C-14-phenanthrene in soil, there is no direct evidence indicating that citric or malic acid have the ability to promote the biodegradation of C-14-phenanthrene from soil. Results from this study provide a novel understanding of the role that substrates, typically found within the rhizosphere due to root exudation, play in the bioaccessibility and biodegradation of hydrocarbons in contaminated soil.
机译:根渗出物和土壤微生物之间的相互作用已被假设为根际有机污染物生物降解的主要机制。但是,管辖该损失过程的机制并不完全明白。本研究旨在探讨两种重要化合物在根渗出物(柠檬酸和苹果酸)中对土壤中的C-14菲解吸和生物可接受性的影响。总体结果表明,柠檬酸和苹果酸(> 100mmol L(-1))的存在增强了C-14菲的解吸;这似乎是浓度依赖。提取性的增加并未以更高的生物可接为性反映。尽管增强了土壤中C-14-菲的解吸,但没有直接证据表明柠檬酸或苹果酸有能力促进来自土壤的C-14菲生物降解。本研究的结果提供了一种新颖的对基质的作用,通常在根际在根际发现的作用,在污染土壤中的生物可接为和生物降解中发挥作用。

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