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Responses of soil methanogens, methanotrophs, and methane fluxes to land-use conversion and fertilization in a hilly red soil region of southern China

机译:南方丘陵红土区土壤甲烷,甲蛋白和甲烷通量对土地利用转化和施肥的反应

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Changes in land-uses and fertilization are important factors regulating methane (CH4) emissions from paddy soils. However, the responses of soil CH4 emissions to these factors and the underlying mechanisms remain unclear. The objective of this study was to explore the effects of land-use conversion from paddies to orchards and fertilization on soil CH4 fluxes, and the abundance and community compositions of methanogens and methanotrophs. Soil CH4 fluxes were quantified by static chamber and gas chromatography technology. Abundance and community structures of methanogens and methanotrophs (based on mcrA and pmoA genes, respectively) were determined by quantitative real-time PCR (qPCR), and terminal restriction fragment length polymorphism (TRFLP), cloning and sequence analysis, respectively. Results showed that land-use conversion from paddies to orchards dramatically decreased soil CH4 fluxes, whereas fertilization did not distinctly affect soil CH4 fluxes. Furthermore, abundance of methanogens and methanotrophs were decreased after converting paddies to orchards. Fertilization decreased the abundance of these microorganisms, but the values were not statistically significant. Moreover, land-use conversion had fatal effects on some members of the methanogenic archaea (Methanoregula and Methanosaeta), increased type II methanotrophs (Methylocystis and Methylosinus), and decreased type I methanotrophs (Methylobacter and Methylococcus). However, fertilization could only significantly affect type I methanotrophs in the orchard plots. In addition, CH4 fluxes from paddy soils were positively correlated with soil dissolved organic carbon contents and methanogens abundance, whereas CH4 fluxes in orchard plots were negatively related to methanotroph abundance. Therefore, our results suggested that land-use conversion from paddies to orchards could change the abundance and community compositions of methanogens and methanotrophs, and ultimately alter the soil CH4 fluxes. Overall, our study shed insight on the underlying mechanisms of how land-use conversion from paddies to orchards decreased CH4 emissions.
机译:土地使用和施肥的变化是调节水稻土甲烷(CH4)排放的重要因素。然而,土壤CH4排放对这些因素的反应和潜在机制仍然尚不清楚。本研究的目的是探讨土地使用转化从粉饼到果园和施肥对土壤CH4助熔剂的影响,以及甲烷酮和甲蛋白的丰富和群落组成。通过静态室和气相色谱技术量化土壤CH 4助熔剂。通过定量实时PCR(QPCR)和末端限制性片段长度多态性(TRFLP),克隆和序列分析,测定丰度和甲蛋白(分别基于MCRA和PMCOA基因)的丰富和群体结构(分别基于MCRA和PMOA基因),克隆和序列分析。结果表明,从粉饼到果园的土地使用转化显着降低了土壤CH4势态,而受精则不明显影响土壤CH4助焊剂。此外,将粉末转化为果园后,降低了丰富的甲烷和甲蛋白。施肥减少了这些微生物的丰富,但这些值没有统计学意义。此外,土地使用转化对甲状腺原古(甲基甲瘤和甲蛋白酶)的一些成员进行了致命作用,增加II型甲蛋白萎缩(甲基核和甲基骨肉),并减少I型甲胰酶(甲基杆菌和甲基球菌)。然而,施肥仅可能显着影响果园图中的I型甲蛋白。另外,从稻田土壤CH4通量呈正与土壤溶解的有机碳含量关联和产甲烷菌丰度,而在CH4果园阴谋甲烷营养丰度负相关通量。因此,我们的结果表明,从粉果上的土地使用转化可以改变甲烷酮和甲蛋白的丰富和群落组成,并最终改变土壤CH4通量。总体而言,我们的研究揭示了对稻田与果园的土地使用转换如何对果园的潜在机制的认识下降了CH4排放。

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