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首页> 外文期刊>Soil Science and Plant Nutrition >N2O and CH4 fluxes from a volcanic grassland soil in Nasu, Japan: Comparison between manure plus fertilizer plot and fertilizer-only plot
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N2O and CH4 fluxes from a volcanic grassland soil in Nasu, Japan: Comparison between manure plus fertilizer plot and fertilizer-only plot

机译:日本那须的火山草地土壤中的N2O和CH4通量:肥料加肥区和仅肥料区的比较

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We examined the effects of manure + fertilizer application and fertilizer-only application on nitrous oxide (N2O) and methane (CH4) fluxes from a volcanic grassland soil in Nasu, Japan. In the manure + fertilizer applied plot (manure plot), the sum of N mineralized from the manure and N applied as ammonium sulfate was adjusted to 210 kg N ha(-1) year(-1). In the fertilizer-only applied plot (fertilizer plot), 210 kg N ha(-1) year(-1) was applied as ammonium sulfate. The manure was applied to the manure plot in November and the fertilizer was applied to both plots in March, May, July and September. From November 2004 to November 2006, we regularly measured N2O and CH4 fluxes using closed chambers. Annual N2O emissions from the manure and fertilizer plots ranged from 7.0 to 11.0 and from 4.7 to 9.1 kg N ha(-1), respectively. Annual N2O emissions were greater from the manure plot than from the fertilizer plot (P < 0.05). This difference could be attributed to NO emissions following manure application. N2O fluxes were correlated with soil temperature (R = 0.70, P < 0.001), NH4+ concentration in the soil (R = 0.67, P < 0.001), soil pH (R = -0.46, P < 0.001) and NO3- concentration in the soil (R = 0.40, P < 0.001). When included in the multiple regression model (R = 0.72, P < 0.001), however, the following variables were significant: NH4+ concentration in the soil (beta = 0.52, P < 0.001), soil temperature (beta = 0.36, P < 0.001) and soil moisture content (beta = 0.26, P < 0.001). Annual CH4 emissions from the manure and fertilizer plots ranged from -0.74 to -0.16 and from -0.84 to -0.52 kg C ha(-1), respectively. No significant difference was observed in annual CH4 emissions between the plots. During the third grass-growing period from July to September, however, cumulative CH4 emissions were greater from the manure plot than from the fertilizer plot (P < 0.05). CH4 fluxes were correlated with NH4+ concentration in the soil (R = 0.21, P < 0.05) and soil moisture content (R = 0.20, P < 0.05). When included in the multiple regression model (R = 0.29, P 0.05), both NH4+ concentration in the soil (beta= 0.20, P < 0.05) and soil moisture content (P = 0.20, P < 0.05) were significant.
机译:我们研究了在日本那须的火山草地土壤中,肥料+肥料和仅肥料的施用对一氧化二氮(N2O)和甲烷(CH4)通量的影响。在肥料+肥料施用区(肥料区)中,将肥料中矿化的N和作为硫酸铵施用的N的总和调整为210 kg N ha(-1)year(-1)。在仅施用肥料的地块(肥料地块)中,施用210千克N ha(-1)年(-1)作为硫酸铵。在11月,将肥料施用到粪肥区,在3月,5月,7月和9月,将肥料施用到两个肥区。从2004年11月到2006年11月,我们使用密闭室定期测量N2O和CH4的通量。粪肥和化肥田的年N2O排放量分别为7.0至11.0和4.7至9.1 kg N ha(-1)。粪肥田的年N2O排放量大于肥料田的N2O排放(P <0.05)。这种差异可以归因于施用肥料后没有排放。 N2O通量与土壤温度(R = 0.70,P <0.001),土壤中NH4 +浓度(R = 0.67,P <0.001),土壤pH(R = -0.46,P <0.001)和NO3​​-浓度相关。土壤(R = 0.40,P <0.001)。当包含在多元回归模型中(R = 0.72,P <0.001)时,以下变量是显着的:土壤中的NH4 +浓度(beta = 0.52,P <0.001),土壤温度(beta = 0.36,P <0.001) )和土壤水分含量(β= 0.26,P <0.001)。粪肥和化肥田的年CH4排放量分别为-0.74至-0.16和-0.84至-0.52 kg C ha(-1)。在各样地之间,每年的CH4排放量没有观察到显着差异。然而,在7月至9月的第三个草场种植期间,粪肥田的累积CH4排放量大于肥料田的累积CH4排放(P <0.05)。 CH4通量与土壤中的NH4 +浓度(R = 0.21,P <0.05)和土壤水分含量(R = 0.20,P <0.05)相关。当包含在多元回归模型中(R = 0.29,P 0.05)时,土壤中的NH 4+浓度(β= 0.20,P <0.05)和土壤水分含量(P = 0.20,P <0.05)均显着。

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