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Impact of Reed Canary Grass Cultivation and Mineral Fertilisation on the Microbial Abundance and Genetic Potential for Methane Production in Residual Peat of an Abandoned Peat Extraction Area

机译:芦苇金丝雀草种植和矿物施肥对废弃泥炭开采区剩余泥炭中微生物丰度和甲烷生成遗传潜力的影响

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摘要

This study examined physiochemical conditions and prokaryotic community structure (the bacterial and archaeal 16S rRNA genes and mcrA gene abundances and proportions), and evaluated the effect of reed canary grass cultivation and mineral fertilisation on these factors, in the 60 cm thick residual peat layer of experimental plots located on an abandoned peat extraction area. The archaeal proportion was 0.67–39.56% in the prokaryotic community and the methanogens proportion was 0.01–1.77% in the archaeal community. When bacterial abundance was higher in the top 20 cm of peat, the archaea were more abundant in the 20–60 cm layer and methanogens in the 40–60 cm layer of the residual peat. The bacterial abundance was significantly increased, but archaeal abundance was not affected by cultivation. The fertiliser application had a slight effect on peat properties and on archaeal and methanogen abundances in the deeper layer of cultivated peat. The CH4 emission was positively related to mcrA abundance in the 20–60 cm of the bare peat, while in case of reed canary grass cultivation these two parameters were not correlated. Reed canary grass cultivation mitigated CH4 emission, although methanogen abundance remained approximately the same or even increased in different layers of residual peat under cultivated sites over time. This study supports the outlook of using abandoned peat extraction areas to produce reed canary grass for energy purposes as an advisable land-use practice from the perspective of atmospheric impact in peatland-rich Northern Europe.
机译:这项研究检查了理化条件和原核生物群落结构(细菌和古细菌16S rRNA基因和mcrA基因的丰度和比例),并评估了芦苇金丝雀草种植和矿物施肥对这些因素的影响,其位于60 cm厚的剩余泥炭层中位于废弃泥炭提取区的实验区。在原核群落中,古细菌的比例为0.67–39.56%,而在古细菌群落中,产甲烷菌的比例为0.01–1.77%。当泥炭的前20 cm处细菌丰度更高时,古细菌在剩余泥炭的20–60 cm层中更丰富,而产甲烷菌则在剩余泥炭的40–60 cm层中。细菌的丰度显着增加,但古细菌的丰度不受栽培的影响。施肥对泥炭的深层耕层的泥炭特性以及古细菌和产甲烷菌的丰度影响不大。在20-60 cm的裸泥炭中,CH4的排放与mcrA的含量呈正相关,而在芦苇金丝雀草栽培的情况下,这两个参数并不相关。芦苇金丝雀草种植减少了CH4的排放,尽管随着时间的推移,甲烷残留量在不同的剩余泥炭层中保持大致相同甚至增加。从对泥炭地丰富的北欧地区的大气影响角度来看,这项研究支持使用废弃的泥炭采伐区生产芦苇金丝雀草作为能源用途的建议,这是一种可取的土地利用方法。

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