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Evaluation of variation in background nitrous oxide emissions: A new global synthesis integrating the impacts of climate, soil, and management conditions
Global Change Biology ( IF 10.8 ) Pub Date : 2021-09-02 , DOI: 10.1111/gcb.15860
Yulong Yin 1 , Zihan Wang 1 , Xingshuai Tian 1 , Yingcheng Wang 1 , Jiahui Cong 1 , Zhenling Cui 1
Affiliation  

Robust global simulation of soil background N2O emissions (BNEs) is a challenge due to the lack of a comprehensive system for quantification of the variations in their magnitude and location. We mapped global BNEs based on 1353 field observations from globally distributed sites and high-resolution climate and soil data. We then calculated global and national total BNE budgets and compared them to the IPCC-estimated values. The average BNE was 1.10, 0.92, and 0.84 kg N ha−1 year−1 with variations from 0.18 to 3.47 (5th–95th percentile, hereafter), 0.20 to 3.44, and −1.16 to 3.70 kg N ha−1 year−1 for cropland, forestland, and grassland, respectively. Soil pH, soil N mineralization, atmospheric N deposition, soil volumetric water content, and soil temperature were the principle significant drivers of BNEs. The total BNEs of three land use types was lower than IPCC-estimated total BNEs by 0.83 Tg (1012 g) N year−1, ranging from −47% to 94% across countries. The estimated BNE with cropland values were slightly higher than the IPCC estimates by 0.11 Tg N year−1, and forestland and grassland lower than the IPCC estimates by 0.4 and 0.54 Tg N year−1, respectively. Our study underlined the necessity for detailed estimation of the spatial distribution of BNEs to improve the estimates of global N2O emissions and enable the establishment of more realistic and effective mitigation measures.

中文翻译:

评估背景一氧化二氮排放的变化:综合气候、土壤和管理条件影响的新全球综合

由于缺乏用于量化其幅度和位置变化的综合系统,因此对土壤背景 N 2 O 排放 (BNE) 进行稳健的全球模拟是一项挑战。我们根据来自全球分布站点的 1353 次实地观测以及高分辨率气候和土壤数据绘制了全球 BNE。然后我们计算了全球和国家的 BNE 总预算,并将它们与 IPCC 的估计值进行了比较。平均 BNE 为 1.10、0.92 和 0.84 kg N ha -1 年-1,变化范围为 0.18 至 3.47(第 5-95 个百分位数,下文)、0.20 至 3.44 和 -1.16 至 3.70 kg N ha -1 年-1分别为农田、林地和草地。土壤 pH 值、土壤氮矿化、大气氮沉降、土壤体积含水量和土壤温度是 BNE 的主要驱动因素。三种土地利用类型的总 BNE 比 IPCC 估计的总 BNE 低 0.83 Tg (10 12  g) N 年-1,各国范围从 -47% 到 94%。估计的农田 BNE 值比 IPCC 估计值略高 0.11 Tg N year -1,林地和草地值分别比 IPCC 估计值低 0.4 和 0.54 Tg N year -1。我们的研究强调了详细估计 BNE 空间分布的必要性,以改进对全球 N 2的估计O 排放,并能够制定更现实和有效的缓解措施。
更新日期:2021-09-02
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