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Spatial variation in soil pH controls off-season N2O emission in an agricultural soil

机译:土壤pH值的空间变化控制了农业土壤中的淡季N2O排放

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Experiments with soils have provided ample evidence that soil pH controls the N2O/(N2O + N-2) ratio of denitrification, which increases with decreasing pH, most probably because low pH interferes with the expression of N2O reductase in denitrifying bacteria. In contrast, the N2O/NO3- product ratio of nitrification appears to be unaffected by soil pH within the range relevant for agricultural soils (pH 5.5-7.0). We hypothesized that local pH variations in cultivated soil may control in situ N2O emissions during periods of active denitrification. To test this hypothesis, we identified three plots with slightly different soil pH (5.4-5.9) within an agricultural field under spring ploughed cereal cropping, and placed four frames within each plot for measuring N2O emissions throughout autumn and spring. Soil samples were taken from each frame after the experiment to characterize the kinetics of NO, N2O and N-2 production by anoxic incubation. The data were used to calculate an N2O index, I-N2O, which is an inverse measure of the capacity of the denitrifying community to effectively express N2O reductase under anoxia and hence a proxy for the soil's propensity to emit N2O under denitrifying conditions. N2O emissions were greatest during spring thaw, intermediate in autumn and low in late spring. Emissions during autumn and spring thaw were inversely related to soil pH, supporting the hypothesis that soil pH influences N2O emissions when denitrification is the main source of N2O. During these periods, emissions were positively correlated with I-N2O, further substantiating the idea that soil pH affects denitrification product ratios in situ. Total organic carbon and nitrate content were negatively correlated with soil pH, thus co-varying with N2O emissions. However, the relationship of N2O emission to TOC and nitrate appeared weaker than to pH. Off-season emissions dominate N2O budgets in many regions. If the pH relationship holds at greater scales, careful soil pH management by precision liming could be a viable tool to reduce N2O emissions. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在土壤上进行的实验提供了充分的证据,表明土壤的pH值控制着反硝化的N2O /(N2O + N-2)比率,该比率随pH的降低而增加,这很可能是因为低pH值会干扰反硝化细菌中N2O还原酶的表达。相反,硝态氮的N2O / NO3-产物比率似乎不受农业土壤(pH 5.5-7.0)相关范围内的土壤pH的影响。我们假设在主动反硝化期间,耕地土壤的局部pH值变化可能会控制原位N2O排放。为了检验该假设,我们在春季耕作的谷物种植中,确定了农田内土壤pH值(5.4-5.9)略有不同的三个样地,并在每个样地中放置了四个框架,以测量整个秋季和春季的N2O排放量。实验后从每个框架中取土壤样品,以表征通过缺氧孵育产生的NO,N2O和N-2的动力学。数据用于计算N2O指数I-N2O,这是反硝化群落在缺氧条件下有效表达N2O还原酶能力的反向度量,因此可以替代土壤在反硝化条件下排放N2O的倾向。 N2O排放在春季解冻期间最大,秋季为中间,春季末较低。秋季和春季解冻过程中的排放与土壤pH值呈反相关,支持以下假设:当反硝化作用是N2O的主要来源时,土壤pH值会影响N2O排放。在这些时期,排放与I-N2O正相关,进一步证实了土壤pH值会影响原位反硝化产物比率的想法。总有机碳和硝酸盐含量与土壤pH呈负相关,因此与N2O排放成正比。但是,N2O排放与TOC和硝酸盐的关系似乎弱于与pH的关系。在许多地区,淡季排放量主导着N2O预算。如果pH关系在更大范围内保持不变,则通过精密撒石灰仔细管理土壤pH值可能是减少N2O排放的可行工具。 (C)2016 Elsevier Ltd.保留所有权利。

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