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Time-dependent shifts in populations and activity of bacterial and archaeal ammonia oxidizers in response to liming in acidic soils

机译:在酸性污垢中抗摩尔病的群体和细菌和古代氧化剂的群体和活性的时间依赖性转变

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During the past decades, extensive nitrogen fertilization and acid deposition have greatly contributed to soil acidification in agroecosystems. Liming, the addition of calcium-and magnesium-rich material to soil, is an effective management strategy used to improve fertility and productivity of agricultural soils degraded by acidification. Nitrification plays a central role in nitrogen (N) availability in agroecosystems and contributes to soil acidification. However, little is known regarding the effects of liming on this process and microbial populations that drive it. Here, we investigated population dynamics and activity of ammonia oxidizers in response to a 2-year liming field trial in acidic soils received long-term fertilization with chemical N fertilizers and short-term lime amendment in microcosm incubations. Our results showed that activity, abundance and population structure of both ammonia-oxidizing archaea (AOA) and bacteria (AOB) were sensitive to liming in fertilized acidic soils. AOB abundance and potential nitrification rates increased in field plots subjected to liming, whereas the opposite was observed for AOA. In microcosm incubations, AOA abundance increased progressively over 60 days, namely under low CaO levels, whereas AOB abundance was greatly stimulated only during the first week under high CaO levels. 13CO2-SIP-DNA experiments further supported that AOA were the most active ammonia oxidizers in fertilized field soils. However, in N-fertilized soils freshly amended with CaO, only autotrophic growth of AOB was observed after seven days, but not after 30 days when growth of AOA was observed. Taken together, our results indicated that both AOA and AOB play a role in nitrification following liming in fertilized acidic soils, likely through selection of better adapted clades of organisms. Although AOA were likely the main drivers of nitrification in these soils in the long-term, liming stimulated AOB activity in the short-term. (C) 2017 Elsevier Ltd. All rights reserved.
机译:在过去几十年中,广泛的氮肥和酸沉积极大地导致农业体系中的土壤酸化。雷岭,加入富含钙和富含镁的土壤,是一种有效的管理策略,用于提高农业土壤的生育率和生产力通过酸化降解。硝化在农业体系中的氮气(n)可用性中起着核心作用,并有助于土壤酸化。然而,关于默沃的这种过程和微生物群体的影响很少。在这里,我们研究了氨氧化剂的人口动态和活性,以应对酸性土壤中的2年初步田间试验,接受化学氮肥的长期施肥和微观培养中的短期石灰修正案。我们的研究结果表明,氨氧化古(AOA)和细菌(AOB)的活性,丰度和人口结构对受精酸性土壤中的跛行敏感。在经过黎明的场地图中增加了丰度和潜在的硝化率,而AOA则观察到相反。在微观孵育中,AOA丰度逐渐增加60天,即低CAO水平,而AOB丰富仅在高CAO水平下的第一周中大大刺激。 13CO2-SIP-DNA实验进一步支持AOA是受精场土壤中最活跃的氨氧化剂。然而,在N型施肥的土壤中随着CAO新修正,七天后只观察到AOB的自养生长,但观察到AOA的生长后30天后。我们的结果表明,AOA和AOB都在施用受精酸性土壤中的硝化后发挥作用,可能通过选择更好地适应的生物。尽管AOA可能在长期的这些土壤中硝化的主要驱动因素,但在短期内估计刺激的AOB活性。 (c)2017 Elsevier Ltd.保留所有权利。

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