Peng Yi, Li Hui-Tong, Zhang Shao-Wei, Yang Ting, Wang Xiao-Fei, Zhou Chun-Ju, Wang Lin-Quan
College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China.
College of Life Sciences, Northwest A&F University, Yangling 712100, China.
Huan Jing Ke Xue. 2022 Mar 8;43(3):1668-1677. doi: 10.13227/j.hjkx.202105100.
In order to explore the characteristics of NO emissions from winter wheat fields in the Loess Plateau under different farming methods and nitrogen levels, the dynamic changes in NO emissions from rain-fed winter wheat fields were quantified using static box-gas chromatography. Winter wheat 'Xiaoyan22' was used as the material, and a two-factor split area design was adopted. The conventional tillage (CT), straw incorporated into soil (SM), and flat film mulching (FM) were assigned as the main plot, and three nitrogen fertilizer rates (no nitrogen fertilization, 20% nitrogen reduction (144 kg·hm), and conventional nitrogen application (180 kg·hm)) were assigned as a split plot. Taking CT as a control, the effects of FM and SM on soil NO emissions under different nitrogen rates were assessed. Furthermore, the correlation between relevant environmental factors and NO emission flux were analyzed, and N emissions were estimated using empirical formulas. The results showed the following:the NO emissions from the soil of each nitrogen treatment occurred within 20 days, and NO emission flux peaked within two weeks post-fertilization. The average NO flux, the total NO emissions, and the global warming potential of NO were 1.92-22.75 μg·(m·h), 0.10-0.46 kg·hm, and 26.72-122.15 kg·hm, respectively. The NO emission coefficient of fertilizer nitrogen was 0.05%-0.28%. The total N emissions ranged from 0.70-1.82 kg·hm. The N fertilization and film mulching significantly increased the NO emission flux (<0.05) and the cumulative NO emissions (<0.05); however, SM marginally reduced the total NO emissions. The NO emission coefficient and global warming potential of fertilizer nitrogen under FM were significantly higher than those under CT and SM (<0.05). The NO emissions without nitrogen treatment were only significantly positively correlated with soil water-filled pore spaces (WFPS) (<0.05); the NO emissions in the N fertilization condition were significantly positively correlated with WFPS, (NO-N), (NH-N), and 0-5 cm soil layer temperature (<0.05). Overall, under the condition of no fertilization, water was the main factor to control the nitrogen transformation and soil NO emission; nevertheless, under the N fertilization condition, both nitrification and denitrification contributed to the NO emissions in the rain-fed winter wheat fields. Film mulching practice and nitrogen application markedly increased the NO emissions, fertilizer nitrogen emission coefficient, and global warming potential in the rain-fed winter wheat fields. Nonetheless, straw incorporated into the soil resulted in a marginal reduction in NO emissions.
为探究黄土高原不同耕作方式和施氮水平下冬小麦田一氧化氮(NO)排放特征,采用静态箱-气相色谱法对雨养冬小麦田NO排放动态变化进行了量化。以冬小麦品种‘小偃22’为材料,采用二因素裂区设计。主区设置常规耕作(CT)、秸秆还田(SM)和平膜覆盖(FM),副区设置3个施氮量水平(不施氮肥、减氮20%(144 kg·hm)和常规施氮(180 kg·hm))。以CT为对照,评估FM和SM在不同施氮量下对土壤NO排放的影响。此外,分析了相关环境因子与NO排放通量的相关性,并采用经验公式估算了氮素排放量。结果表明:各施氮处理土壤NO排放在20天内完成,施肥后两周内NO排放通量达到峰值。NO平均通量、NO排放总量以及NO的全球增温潜势分别为1.92~22.75 μg·(m·h)、0.10~0.46 kg·hm和26.72~122.15 kg·hm。肥料氮的NO排放系数为0.05%~0.28%。总氮排放量为0.70~1.82 kg·hm。施氮和覆膜显著增加了NO排放通量(<0.05)和NO累积排放量(<0.05);然而,秸秆还田使NO排放总量略有降低。FM处理下肥料氮的NO排放系数和全球增温潜势显著高于CT和SM处理(<0.05)。不施氮处理的NO排放仅与土壤充水孔隙率(WFPS)呈显著正相关(<0.05);施氮条件下的NO排放与WFPS、(NO-N)、(NH-N)以及0~5 cm土层温度呈显著正相关(<0.05)。总体而言,在不施肥条件下,水分是控制氮素转化和土壤NO排放的主要因素;然而,在施氮条件下,硝化作用和反硝化作用均对雨养冬小麦田的NO排放有贡献。覆膜措施和施氮显著增加了雨养冬小麦田的NO排放量、肥料氮排放系数和全球增温潜势。尽管如此,秸秆还田使NO排放量略有降低。