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Inhibition of methane oxidation by nitrogenous fertilizers in a paddy soil

机译:水稻土中氮肥对甲烷氧化的抑制作用

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摘要

Nitrogenous fertilizers are generally thought to have an important role in regulating methane oxidation. In this study, the effect of ammonium on methane oxidation activity was investigated in a paddy soil using urea at concentrations of 0, 50, 100, 200, and 400 μg N per gram dry weight soil (N/g.d.w.s) and ammonium sulfate at concentrations of 0, 50, and 200 μg N/g.d.w.s. The results of this study demonstrate that urea concentrations of 200 μg N/g.d.w.s. and above significantly inhibit methane oxidation activity, whereas no statistically significant difference was observed in methane oxidation activity among soil microcosms with urea concentrations of less than 200 μg N/g.d.w.s after incubation for 27 days. Similar results were obtained in a sense that methane oxidation activity was inhibited only when the ammonium sulfate concentration was 200 μg N/g.d.w.s in soil microcosms in this study. Phylogenetic analysis of pmoA genes showed that nitrogen fertilization resulted in apparent changes in the community composition of methane-oxidizing bacteria (MOB). Type I MOB displayed an increased abundance in soil microcosms amended with nitrogenous fertilizers, whereas type II MOB dominated the native soil. Furthermore, although no statistically significant relationship was observed between pmoA gene and amoA gene abundances, methane oxidation activity was significantly negatively correlated with nitrification activity in the presence of urea or ammonium sulfate. Our results indicate that the methane oxidation activity in paddy soils might be inhibited when the concentration of ammonium fertilizers is high and that the interactions between ammonia and methane oxidizers need to be further investigated.
机译:通常认为,氮肥在调节甲烷氧化中起重要作用。在这项研究中,研究了铵对稻田土壤中甲烷氧化活性的影响,其中尿素的浓度为每克干重土壤(N / gdws)分别为0、50、100、200和400μgN,浓度为每克干重土壤硫酸铵0、50和200μgN / gdws这项研究的结果表明尿素浓度为200μgN / g.d.w.s。尿素浓度小于200μgN / g.d.w.s的土壤微观温育27天后,在甲烷和土壤中的尿素浓度低于200μgN / g.d.w.s时,其甲烷氧化活性没有统计学上的显着差异。在本研究中,仅当土壤铵态中的硫酸铵浓度为200μgN / g.d.w.s时,甲烷氧化活性才受到抑制,因此获得了类似的结果。对pmoA基因的系统进化分析表明,氮肥导致甲烷氧化细菌(MOB)的群落组成发生明显变化。 I型MOB在用氮肥改良的土壤微观世界中显示出更高的丰度,而II型MOB则以原生土壤为主。此外,尽管在pmoA基因和amoA基因丰度之间未观察到统计学上显着的关系,但是在尿素或硫酸铵存在下,甲烷氧化活性与硝化活性显着负相关。我们的结果表明,当铵肥浓度较高时,稻田土壤中的甲烷氧化活性可能会受到抑制,氨与甲烷氧化剂之间的相互作用需要进一步研究。

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