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应用生态学报 ›› 2021, Vol. 32 ›› Issue (11): 3961-3968.doi: 10.13287/j.1001-9332.202111.024

• 研究论文 • 上一篇    下一篇

不同施氮量对麦田土壤水稳性团聚体和N2O排放的影响

陈津赛1,2,孙玮皓1,2,王广帅1,Abubakar Sunusi Amin1,2,高阳1*   

  1. 1中国农业科学院农田灌溉研究所/农业农村部作物需水与调控重点实验室, 河南新乡 453002;
    2中国农业科学院研究生院, 北京 100081
  • 出版日期:2021-11-15 发布日期:2022-05-15
  • 通讯作者: *E-mail: gaoyang@caas.cn
  • 作者简介:陈津赛, 男, 1995年生, 硕士研究生。主要从事作物水分生理与高效用水研究。E-mail:82101182107@caas.com
  • 基金资助:
    本文由国家自然科学基金项目(51879267,51679242)、财政部和农业农村部国家现代农业产业技术体系项目(CARS-03)和中央级科研院所基本科研业务费项目(FIRI20210104)资助

Effects of different nitrogen application rates on soil water stable aggregates and N2O emission in winter wheat field

CHEN Jin-sai1,2, SUN Wei-hao1,2, WANG Guang-shuai1, Abubakar Sunusi Amin1,2, GAO Yang1*   

  1. 1Farmland 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;
    2Graduate School of Chinese Academy of Agricultural Sciences, Beijing 100081, China
  • Online:2021-11-15 Published:2022-05-15
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51879267, 51679242), the China Agriculture Research System of Ministry of Finance and Ministry of Agriculture and Rural Areas (CARS-03), and the Basic Fund of Central Institutes (FIRI20210104).

摘要: 过量施氮可破坏农田土壤结构,增加温室气体排放量。为揭示不同施氮量对土壤团聚体和N2O排放的影响,于2018—2020年基于氮肥定位试验,设置秸秆原位还田条件下施氮 0 (N0)、120 (N120)、180 (N180)、240 (N240)、300 (N300)、360 kg·hm-2 (N360) 6个处理,研究不同施氮量对麦田土壤N2O排放、土壤充水孔隙度(WFPS)、土壤温度、硝态氮、铵态氮含量、水稳性团聚体的组成及稳定性的影响。结果表明: 土壤N2O排放量与氮肥用量之间呈显著正相关关系,WFPS与施氮量之间无显著相关关系,0~10 cm土壤温度随氮肥施用量的增加而显著降低,土壤硝态氮、铵态氮含量与氮肥施用量间存在显著正相关关系。随氮肥施用量的增加,直径>2 mm的水稳性团聚体含量降低,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。氮肥施用量与团聚体平均重量直径(MWD)、几何平均直径之间呈显著负相关关系,但与分形维数之间并无显著相关性。MWD (x)与N2O排放通量(y)之间的拟合方程为:y=3928.3e-2.171x (R2=0.55,P<0.001),表明当MWD减小时,N2O排放量将会剧烈升高。可见,麦田施氮量的增加会降低0~10 cm土壤温度,增加土壤硝态氮和铵态氮含量,减小耕层土壤水稳性团聚体的平均粒径,降低团聚体的稳定性,增加N2O的排放量。

关键词: 冬小麦, 施氮, 土壤理化性质, N2O, 水稳性团聚体

Abstract: Excessive nitrogen application would deteriorate soil structure and increase greenhouse gas emission. We set up six treatments, i.e., N0, N120, N180, N240, N300and N360(nitrogen application rates of 0, 120, 180, 240, 300 and 360 kg·hm-2, 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 N2O 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 N2O 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 N2O emission flux was y=3928.3e-2.171x (R2=0.55, P<0.001), indicating that N2O 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 N2O emission.

Key words: winter wheat, nitrogen application, soil physicochemical property, N2O, water stable aggregate.