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首页> 外文期刊>Applied Soil Ecology >Effects of inorganic fertilizer and manure on soil archaeal abundance at two experimental farms during three consecutive rotation-cropping seasons.
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Effects of inorganic fertilizer and manure on soil archaeal abundance at two experimental farms during three consecutive rotation-cropping seasons.

机译:在三个连续轮作季节中,两个实验农场的无机肥料和肥料对土壤古细菌丰度的影响。

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摘要

Soil archaeal population dynamics at two experimental sites of the same clay-loam type in Ottawa and Woodslee, Ontario, were investigated to determine fertilizer and manure effects following their different long-term crop rotation and fertilization schemes. Phylogenetic analysis of cloned soil archaeal 16S rRNA gene libraries of both sites identified them with group 1.1b of Thaumarchaeota. The gene population dynamics subtly varied in the order of 107 copies g-1 soil when monitored by quantitative real-time PCR during three growing seasons (2007-2009). In Ottawa, where plots were amended with dairy-farm manure, soil thaumarchaeal gene abundance was double of the unamended plots. At the Woodslee N-P-K-fertilized plots, it remained at least 30% fewer than that of the unfertilized ones. These cultivated plots showed soil carbon limitation while the fertilized ones were low in soil pH (ca. 5.5). Surface soils from an unfertilized sod plot and an adjacent deciduous forest had higher total carbon content (C:N ratio of 9 and 11, respectively). Their thaumarchaeal gene abundance varied up to 4.8x107 and 7.0x107 copies g-1 soil, respectively. The former value was also attained at the manure-amended plots in Ottawa, where the C:N ratio was just below 10. Where soil pH was above 6.0, there was a weak and positive correlation between soil total C and the estimated gene abundance. Such gene population dynamics consistently demonstrated the stimulating and suppressive effects of dairy-farm manure (Ottawa site) and inorganic fertilizers (Woodslee site), respectively, on soil thaumarchaea. At both sites archaeal amoA and 16S rRNA gene abundance were similarly affected. Archaeal amoA gene abundance also outnumbered bacterial amoA abundance, suggesting that ammonia-oxidizing archaea might be dominant in these soils. Only minor crop effects on gene population dynamics were detected.
机译:在渥太华和安大略省伍德斯里的两个相同的壤土类型实验地点的土壤古细菌种群动态进行了调查,以确定不同长期作物轮作和施肥方案下的肥料和肥料效应。对这两个位点的克隆土壤古细菌16S rRNA基因文库进行系统进化分析,将它们鉴定为Thaumarchaeota 1.1b组。在三个生长季节(2007-2009)通过实时定量PCR监测,基因种群动态以10 7 拷贝g -1 土壤的顺序微妙变化。在渥太华,用奶牛粪便对地块进行了改良,其土壤拟南芥基因丰度是未改良地块的两倍。在Woodslee N-P-K施肥的地块,它比未施肥的地块至少少了30%。这些耕地显示出土壤碳限制,而施肥土壤的pH值低(约5.5)。未施肥的草皮地块和附近的落叶林的表层土壤具有较高的总碳含量(C:N比分别为9和11)。它们的拟南芥基因丰度分别高达4.8x10 7 和7.0x10 7 拷贝g -1 土壤。前值也是在渥太华的肥料改良区获得的,那里的C:N比刚好低于10。当土壤pH值高于6.0时,土壤总C与估计的基因丰度之间存在弱而正的相关性。这样的基因种群动态一致地证明了乳场肥料(渥太华站点)和无机肥料(Woodslee站点)分别对土壤拟南芥有刺激和抑制作用。在这两个站点古细菌amoA和16S rRNA基因丰度受到类似的影响。古细菌amoA基因的丰度也超过了细菌amoA的丰度,这表明氨氧化古细菌可能在这些土壤中占主导地位。仅检测到作物对基因种群动态的微小影响。

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