Farmland Irrigation Research Institute, Chinese Academy of Agricultural Sciences /Key Laboratory of Crop Water Requirement and Regulation, Ministry of Agriculture and Rural Affairs, Xinxiang 453002, Henan, China.
Graduate School of Chinese Academy of Agricultural Sciences, Beijing 100081, China.
Ying Yong Sheng Tai Xue Bao. 2021 Nov 15;32(11):3961-3968. doi: 10.13287/j.1001-9332.202111.024.
Excessive nitrogen application would deteriorate soil structure and increase greenhouse gas emission. We set up six treatments, i.e., N, N, N, N, Nand N(nitrogen application rates of 0, 120, 180, 240, 300 and 360 kg·hm, all straws returned into the field in situ) in the nitrogen fertilizer experimental site to investigate the effects of different nitrogen application rates on soil NO emission, soil water-filled porosity (WFPS), soil temperature, nitrate and ammonium contents, composition and stability of water stable aggregates in winter wheat filed in 2018-2020. The results showed that there was a significant positive correlation between soil NO emission and nitrogen application rate. There was no correlation between WFPS and nitrogen application rate. Soil temperature in the 0-10 cm layer decreased significantly with the increases of nitrogen application rates. There was a significant positive correlation between nitrate and ammonium contents and nitrogen application rate. With the increases of nitrogen application rates, the content of water stable aggregates with diameter >2 mm decreased, while that of water-stable aggregates with diameter <0.5 mm increased. The particle size of soil water-stable aggregates also decreased gradually. There was a significant negative correlation between nitrogen application rate with mean weight diameter (MWD) and geometric mean diameter, while no correlation with fractal dimension. The fitting equation between MWD and NO emission flux was y=3928.3e (R=0.55, P<0.001), indicating that NO emission increased markedly as MWD decreasing. The increases in nitrogen application rate reduced soil temperature in the 0-10 cm layer, increased nitrate and ammonium contents, decreased the average particle size of soil water stable aggregates, and the stability of soil aggregates, and increased soil NO emission.
过量施氮会恶化土壤结构并增加温室气体排放。我们在氮肥试验区设置了 6 个处理,即 N、N、N、N、N 和 N(施氮量分别为 0、120、180、240、300 和 360 kg·hm,所有秸秆原位还田),以研究不同施氮量对冬小麦田土壤 NO 排放、土壤水充孔隙度(WFPS)、土壤温度、硝酸盐和铵态氮含量、水稳性团聚体组成和稳定性的影响。结果表明,土壤 NO 排放与施氮量呈显著正相关。WFPS 与施氮量无相关性。0-10 cm 土层土壤温度随施氮量的增加而显著降低。硝酸盐和铵态氮含量与施氮量呈显著正相关。随着施氮量的增加,直径 >2 mm 的水稳性团聚体含量减少,而直径 <0.5 mm 的水稳性团聚体含量增加。土壤水稳性团聚体的粒径也逐渐减小。施氮量与平均质量直径(MWD)和几何平均直径呈显著负相关,与分形维数无相关性。MWD 与 NO 排放通量的拟合方程为 y=3928.3e(R=0.55,P<0.001),表明随着 MWD 的降低,NO 排放显著增加。施氮量的增加降低了 0-10 cm 土层的土壤温度,增加了硝酸盐和铵态氮含量,降低了土壤水稳性团聚体的平均粒径和团聚体的稳定性,增加了土壤 NO 排放。