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Effects of bio-based residue amendments on greenhouse gas emission from agricultural soil are stronger than effects of soil type with different microbial community composition.

机译:生物基残留物改良剂对农业土壤温室气体排放的影响要强于不同微生物群落组成的土壤类型的影响。

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摘要

With the projected rise in the global human population, agriculture intensification and land-use conversion to arable fields is anticipated to meet the food and bio-energy demand to sustain a growing population. Moving towards a circular economy, agricultural intensification results in the increased re-investment of bio-based residues in agricultural soils, with consequences for microbially-mediated greenhouse gas (GHG) emission, as well as other aspects of soil functioning. To date, systematic studies to address the impact of bio-based residue amendment on the GHG balance, including the soil microorganisms, and nutrient transformation in agricultural soils are scarce. Here, we assess the Global Warming Potential (GWP) of in-situ GHG (i.e. CO2, CH4, and N2O) fluxes after application of six bio-based residues with broad C:N ratios (5-521) in two agricultural soils (sandy loam and clay; representative of vast production areas in north-western Europe). We relate the GHG emission to the decomposability of the residues in a litter bag assay, and determined the effects of residue input on crop (common wheat) growth after incubation. The shift in the bacterial community composition and abundance was monitored using IonTorrentTM sequencing and qPCR, respectively by targeting the 16S rRNA gene. The decomposability of the residues, independent of C:N ratio, was proportional to the GWP derived from the GHG emitted. The soils harbored distinct bacterial communities, but responded similarly to the residue amendments, because both soils exhibited the highest mean GWP after addition of the same residues (sewage sludge, aquatic plant material, and compressed beet leaves). Our results question the extent of using the C:N ratio alone to predict residue-induced response in GHG emission. Taken together, we show that although soil properties strongly affect the bacterial community composition, microbially-mediated GHG emission is residue-dependent.
机译:随着全球人口的预计增长,预计农业集约化和土地利用向耕地的转化将满足粮食和生物能源的需求,以维持不断增长的人口。向循环经济迈进,农业集约化导致对农业土壤中生物基残留物的再投资增加,这对微生物介导的温室气体(GHG)排放以及土壤功能的其他方面产生了影响。迄今为止,缺乏针对生物基残留物修正对温室气体平衡(包括土壤微生物)和农业土壤中养分转化的影响的系统研究。在这里,我们在两种农业土壤中施用了六种具有宽C:N比(5-521)的生物基残留物后,评估了原位GHG(即CO2,CH4和N2O)通量的全球变暖潜势(GWP)(沙壤土和粘土;代表了西北欧的广阔产区)。我们将温室气体排放量与垃圾袋试验中残留物的可分解性联系起来,并确定了培养后残留物输入对作物(普通小麦)生长的影响。分别通过靶向16S rRNA基因,使用IonTorrentTM测序和qPCR监测细菌群落组成和丰度的变化。残留物的可分解性与C:N比率无关,与源自所排放温室气体的GWP成正比。土壤含有不同的细菌群落,但对残留物修正的反应相似,因为在添加相同的残留物(污水污泥,水生植物材料和压缩甜菜叶)后,两种土壤均表现出最高的平均GWP。我们的结果质疑仅使用C:N比来预测温室气体排放中残基诱导的响应的程度。两者合计,我们表明,尽管土壤特性强烈影响细菌群落组成,但微生物介导的温室气体排放是残基依赖性的。

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