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不同肥料对稻田根际土壤甲烷排放和产甲烷菌群落结构的影响。

Effects of different fertilizers on methane emissions and methanogenic community structures in paddy rhizosphere soil.

机构信息

School of Agriculture and Biology, Shanghai Jiao Tong University, 800 Dongchuan Road, Shanghai 200240, China.

Irrigation Technology Extension Station of Qingpu, 2 Yuan Road, Shanghai 201707, China.

出版信息

Sci Total Environ. 2018 Jun 15;627:770-781. doi: 10.1016/j.scitotenv.2018.01.233. Epub 2018 Feb 2.

Abstract

Paddy soil accounts for 10% of global atmospheric methane (CH) emissions. Many types of fertilizers may enhance CH emissions, especially organic fertilizer. The aim of this study was to explore the effects of different fertilizers on CH and methanogen patterns in paddy soil. This experiment involved four treatments: chemical fertilizer (CT), organic fertilizer (OT), mixed with chemical and organic fertilizer (MT), and no fertilizer (ctrl). The three fertilization treatments were applied with total nitrogen at the same rate of 300 kg N ha. Paddy CH, soil physicochemical variables and methanogen communities were quantitatively analyzed. Rhizosphere soil mcrA and pmoA gene copy numbers were determined by qPCR. Methanogenic 16S rRNA genes were identified by MiSeq sequencing. The results indicated CH emissions were significantly higher in OT (145.31 kg ha) than MT (84.62 kg ha), CT (77.88 kg ha) or ctrl (32.19 kg ha). Soil organic acids were also increased by organic fertilization. CH effluxes were significantly and negatively related to mcrA and pmoA gene copy numbers, and positively related to mcrA/pmoA. Above all, hydrogenotrophic Methanocella and acetoclastic Methanosaeta were the predominant methanogenic communities; these communities were strictly associated with soil potassium, oxalate, acetate, and succinate. Application of organic fertilizer promoted the dominant acetoclastic methanogens, but suppressed the dominant hydrogenotrophic methanogens. The transformation in methanogenic community structure and enhanced availability of C substrates may explain the increased CH production in OT compared to other treatments. Compared to OT, MT may partially mitigate CH emissions while guaranteeing a high rice yield. On this basis, we recommend the local fertilization pattern should change from 300 N kg ha of organic manure to the same level of mixed fertilization. Moreover, we suggest multiple combinations of mixed fertilization merit more investigation in the future.

摘要

稻田土壤占全球大气甲烷(CH)排放量的 10%。许多类型的肥料都可能增强 CH 排放,尤其是有机肥。本研究旨在探索不同肥料对稻田 CH 和产甲烷菌模式的影响。该实验涉及四种处理:化肥(CT)、有机肥(OT)、化肥和有机肥混合(MT)和不施肥(ctrl)。三种施肥处理的总氮施用量相同,为 300kg N ha。定量分析了稻田 CH、土壤理化性质和产甲烷菌群落。通过 qPCR 测定根际土壤 mcrA 和 pmoA 基因拷贝数。通过 MiSeq 测序鉴定产甲烷 16S rRNA 基因。结果表明,OT(145.31kg ha)的 CH 排放量明显高于 MT(84.62kg ha)、CT(77.88kg ha)或 ctrl(32.19kg ha)。有机施肥还增加了土壤有机酸。CH 通量与 mcrA 和 pmoA 基因拷贝数呈显著负相关,与 mcrA/pmoA 呈显著正相关。最重要的是,氢营养型 Methanocella 和乙酸营养型 Methanosaeta 是主要的产甲烷菌群落;这些群落与土壤钾、草酸盐、乙酸盐和琥珀酸盐密切相关。有机肥的施用促进了优势乙酸营养型产甲烷菌,但抑制了优势氢营养型产甲烷菌。产甲烷菌群落结构的转变和 C 底物可用性的增强可能解释了 OT 与其他处理相比 CH 产量增加的原因。与 OT 相比,MT 可能在保证水稻高产的同时部分减少 CH 排放。在此基础上,我们建议当地施肥模式应从 300kg N ha 有机肥改为相同水平的混合施肥。此外,我们建议未来应进一步研究多种混合施肥的组合。

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