长期秸秆还田对麦玉种植体系NO排放的影响

Effect of Long-term Stalk Incorporation on NO Emissions from a Winter Wheat-Maize Cropping System

  • 摘要: 农田是大气污染物一氧化氮(NO)的重要人为源,亟需量化和控制其排放量。连续2年(2022年10月 ~ 2024年10月)观测长期定位施肥(始于1990年)冬小麦-玉米种植体系NO通量,目的是定量分析NO排放量对长期秸秆还田的响应及其主要影响因素。设置不施肥对照(CK)、施化肥(NPK)和施化肥加玉米秸秆(NPKS)处理。CK全年不施肥,NPK和NPKS施等量尿素,冬小麦季和玉米季施氮量分别为165和188 kg·hm-2;NPKS在玉米收获时保留全部秸秆(含氮量约40 kg·hm-2)。结果表明,CK处理NO通量低,NPK和NPKS处理NO通量高峰均出现在施肥后。NO通量与土壤温度和充水孔隙度的边界线分别符合逻辑斯蒂克和高斯模型,与铵态氮和硝态氮浓度的边界线均符合线性模型。CK、NPK和NPKS处理NO年排放量分别为0.18 ~ 0.19、0.31 ~ 0.81和0.65 ~ 1.10 kg·hm-2。与NPK相比,NPKS年排放量偏高37% ~ 113%(P<0.05)。在两个冬小麦季,NPKS排放量分别偏低60%和偏高28%(P>0.05);在两个玉米季,NPKS排放量偏高60% ~ 231%(P<0.05)。NPKS处理NO排放量的增加主要发生在玉米季,这可能与其土壤有机质含量偏高约20%有关。在玉米季,土壤有机质对NO通量的促进作用在温暖潮湿的环境中被放大;在冬小麦季,受低温胁迫及秸秆还田的影响,土壤有机质的作用可能被削弱或掩盖。总之,在长期玉米秸秆还田条件下,麦玉种植体系NO年排放量显著增加,气体减排需重点关注玉米季。

     

    Abstract: Agroecosystems are a significant source of nitric oxide (NO) which serves as an air pollutant. There is an urgent need to quantify and control NO emissions from agroecosystems. The NO fluxes were measured in a long-term (since 1990) fertilized winter wheat-maize cropping system for two years (from October 2022 to October 2024). The aims were to quantify the responses of NO emissions to stalk incorporation and to identify the major regulatory factors. The field trials included an unfertilized control (CK), full chemical fertilizers (NPK), and a combination of chemical fertilizers and maize stalk (NPKS). The CK treatment was not fertilized throughout the year. The NPK and NPKS treatments received the same amount of urea, with nitrogen application rates of 165 and 188 kg·hm⁻² in the winter wheat and maize seasons, respectively. Only for NPKS, all stalks (with a nitrogen application rate averaging 40 kg·hm⁻²) were retained at the time of maize harvest. The results showed that the NO fluxes were low in CK, while always peaked following fertilizations in NPK and NPKS. The boundary lines of NO fluxes followed a logistic and a Gaussian model against soil temperature and water-filled pore space, respectively, and linear models against ammonium and nitrate concentrations. The CK, NPK, and NPKS treatments released annual NO emissions of 0.18 ~ 0.19, 0.31~ 0.81, and 0.65 ~ 1.10 kg·hm⁻², respectively. Annual NO emissions of NPKS were 37% ~ 113% higher than those of NPK (P < 0.05). In the two winter wheat seasons, cumulative NO emissions of NPKS were either 60% lower or 28% higher relative to those of NPK (P > 0.05); in the two maize seasons, cumulative NO emissions of NPKS were 60% ~ 231% higher (P < 0.05). The enhanced NO emissions mostly occurred in maize seasons, which were attributed to the 20% higher soil organic matter content of NPKS relative to that of NPK. In maize seasons, the promoting effect of soil organic matter on NO fluxes may be amplified in a warm and humidity environment; while in winter wheat seasons, the effect of soil organic matter may be weakened or overrode by low temperature and stalk incorporation. With long-term stalk incorporation, annual NO emissions from the winter wheat-maize cropping system were significantly enhanced, and mitigation efforts need focus in maize season.

     

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