添加铵对水稻土甲烷氧化的影响:微生物相互作用的见解

IF 4 2区 农林科学 Q2 SOIL SCIENCE
Huabin Li, Xian Wu, Jinli Hu, Ronglin Su, Niklas J. Lehto, Muhammad Shaaban, Yan Wang, Shan Lin, Ronggui Hu
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引用次数: 0

摘要

稻田是甲烷的主要人为来源,也是减少温室气体向大气排放的关键目标。水稻土中甲烷生成和氧化之间的微妙平衡在很大程度上取决于土壤生态系统中不同微生物群落的丰度和组成以及它们之间的相互作用。铵的添加可以缓解甲烷氧化菌的缺氮,但过量的铵也会抑制其生长。然而,这种开关的阈值浓度目前尚不清楚。在这里,我们报告了一项为期9天的实验室培养实验的结果,该实验旨在研究在精细化的浓度间隔内增加铵浓度对水稻土壤中甲烷氧化的影响。我们测量了甲烷氧化速率,分析了培养土壤中甲烷氧化菌和氨氧化菌的基因丰度和群落组成,以解码这些群落之间的相互作用。我们的结果表明,10 mg nh4 + $$ {\mathrm{NH}}_4^{+} $$ -N d.w.s的铵浓度刺激了甲烷氧化;但浓度超过30 mg nh4 + $$ {\mathrm{NH}}_4^{+} $$ -N kg−1 d.w。S抑制氧化速率。在较低铵浓度下,Ia型甲烷氧化菌对氮的争夺强于氨氧化菌;然而,当氨氧化剂的增殖受到刺激时,这种情况在较高的浓度下发生逆转。我们发现铵对氨氧化细菌(AOB)的刺激程度大于氨氧化古菌(AOA),但与AOA群落相比,AOB群落组成的具体变化要小得多。我们的研究结果强调了氨浓度是水稻土中甲烷氧化菌与氨氧化剂相互作用的关键调节因素,并确定了氨从促进甲烷氧化转变为抑制甲烷氧化的阈值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of Ammonium Addition on Methane Oxidation in a Paddy Soil: Insights Into Microbial Interactions

Rice paddies are a major anthropogenic source of methane and a key target for reducing emissions of the greenhouse gas to the atmosphere. The delicate equilibrium between the production and oxidation of methane in paddy soils is shaped largely by the abundances and compositions of different microbial communities within the soil ecosystem and the interactions between them. Ammonium addition can alleviate nitrogen deficiency for methanotrophs, but ammonium can also inhibit their growth when present in excess. However, the threshold concentration for this switch is not currently known. Here we report the results of a nine-day laboratory incubation experiment that sought to examine the effects of increasing ammonium concentrations on methane oxidation in rice paddy soil at refined concentration intervals. We measured methane oxidation rates and analysed the gene abundances and community compositions of methanotrophs and ammonia oxidizers in the incubated soils to decode interactions between these communities. Our results showed that an ammonium concentration of 10 mg NH 4 + $$ {\mathrm{NH}}_4^{+} $$ -N d.w.s stimulated methane oxidation, but concentrations above 30 mg NH 4 + $$ {\mathrm{NH}}_4^{+} $$ -N kg−1 d.w.s inhibited the oxidation rate. At the lower ammonium concentration, type Ia methanotrophs appeared to outcompete ammonia oxidizers for nitrogen; however, this was reversed at higher concentration where the proliferation of ammonia oxidizers was stimulated. We show how ammonium stimulated the ammonia-oxidizing bacteria (AOB) to a greater extent than ammonia-oxidizing archaea (AOA), but with much smaller changes in the specific AOB community composition, when compared to the AOA communities. Our findings highlight ammonium concentration as a key factor regulating the interaction between methanotrophs and ammonia oxidizers in paddy soils and identify the threshold where ammonium shifts from promoting to inhibiting methane oxidation.

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来源期刊
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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