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首页> 外文期刊>Atmospheric environment >Fertiliser Induced Nitrous Oxide Emissions During Energy Crop Cultivation On Loamy Sand Soils
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Fertiliser Induced Nitrous Oxide Emissions During Energy Crop Cultivation On Loamy Sand Soils

机译:砂质壤土能量作物耕作过程中肥料诱导的一氧化二氮排放

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Nitrous oxide (N_2O) fluxes from a loamy sand soil have been collected at an experimental field since 1999. To study the nitrogen (N) fertiliser induced emissions, annual crops and perennial plants received three different levels of N fertilisation: 0, 75, and 150 kg N ha~(-1). N_2O was measured by gas chromatography and closed chamber technique. Water content of the soil was determined gravimetrically and the soil content of mineral N by ion chromatography. The N_2O fluxes were below 30 μg N_2O m~2 h~(-1) during the winter season and varied from 10 to more than 1000 μgN_2O m~(-2) h~(-1) in the course of the vegetation season. N_2O emissions after N fertilisation were assigned to fertiliser induced emissions. High N_2O emissions at the end of the vegetation period are the result of increased mineralisation of soil organic matter. N_2O emissions from freeze-thaw cycles gave only a small contribution to the total annual N_2O emission budget from all blocks studied. Since the mean soil moisture content is very low (10%) and the water-filled pore space (WFPS) correlates negatively with N_2O emissions, nitrification is considered the main source for N_2O emissions. Evaluation of the data regarding dependence on fertilisation level indicates that N_2O fluxes are positively correlated to soil NO_3-N content. The N_2O fluxes from annual crop plots are higher than those from plots with perennial plants (grass, willow, poplar). The mean N_2O-N emission factor for fertiliser induced emissions from tilled soil is 1.0% in contrast to that of non-tilled soil with 0.7%. The mean fertiliser induced N_2O-N emissions, averaged over all crops and the total period of nine years, are in the range of 0.8 ± 0.2% of the N fertiliser applied.
机译:自1999年以来,已经在一个实验田地上收集了一块壤土壤土中的一氧化二氮(N_2O)通量。为了研究氮(N)肥料引起的排放,一年生作物和多年生植物分别接受了三种不同的氮肥水平:0、75和150千克N ha〜(-1)。通过气相色谱和密闭室技术测量N_2O。用重量分析法测定土壤的水分含量,并通过离子色谱法测定矿质氮的土壤含量。在冬季,N_2O通量低于30μgN_2O m〜2 h〜(-1),而在植被季节则从10μgN_2Om〜(-2)h〜(-1)变化。施氮后的N_2O排放被归因于肥料引起的排放。植被期结束时N_2O的高排放是土壤有机质矿化增加的结果。冻融循环产生的N_2O排放量仅对所研究所有区块的年度N_2O排放总预算贡献很小。由于土壤平均含水量非常低(10%),且充满水的孔隙空间(WFPS)与N_2O排放负相关,因此硝化被认为是N_2O排放的主要来源。对有关施肥水平依赖性数据的评估表明,N_2O通量与土壤NO_3-N含量呈正相关。一年生作物田的N_2O通量高于多年生植物(草,柳树,杨树)的N_2O通量。耕作土壤中肥料诱导排放的平均N_2O-N排放因子为1.0%,而非耕作土壤的平均N_2O-N排放因子为0.7%。在所有作物上和九年的总期间内,平均肥料诱导的N_2O-N排放量平均为所施氮肥的0.8±0.2%。

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