华北农学报 ›› 2026, Vol. 41 ›› Issue (3): 148-157. doi: 10.7668/hbnxb.20195771

所属专题: 土壤肥料 热点论文

• 资源环境•植物保护 • 上一篇    下一篇

增温和有机肥配施对土壤硝化、反硝化过程及相关酶活性的影响

吴旗, 李建霖, 陈杨, 栾崇圣, 汪小宇, 林雷利, 李笑笑, 车钊, 王晓波, 宋贺, 吴巩   

  1. 安徽农业大学 农学院, 安徽 合肥 230031
  • 收稿日期:2025-01-15 出版日期:2026-06-28
  • 通讯作者:
    吴 巩(1995-),男,安徽安庆人,副教授,博士,主要从事气候智慧型农业研究。
  • 作者简介:
    吴 旗(1996-),男,安徽阜阳人,在读硕士,主要从事作物栽培生理生态研究。
  • 基金资助:
    国家重点研发计划青年科学家项目(2023YFD2302400); 国家自然科学基金青年项目(32301959); 安徽省自然科学基金青年项目(2308085QC88); 安徽省高等学校科学研究自然科学类重点项目(2023AH050989)

Effects of Warming and Organic Fertilization on Soil Nitrification and Denitrification and the Activities of Enzymes Related to Nitrogen Cycling

WU Qi, LI Jianlin, CHEN Yang, LUAN Chongsheng, WANG Xiaoyu, LIN Leili, LI Xiaoxiao, CHE Zhao, WANG Xiaobo, SONG He, WU Gong   

  1. School of Agronomy, Anhui Agricultural University, Hefei 230031, China
  • Received:2025-01-15 Published:2026-06-28

摘要:

为了明确气候变化和有机肥配施对土壤氮素转化的影响,于2023年6-11月在安徽合肥进行大豆田间试验,利用红外辐射增温设备模拟田间增温,设置2个温度水平(T0:环境温度;T1:增温)和2种施肥模式(SF:单施无机肥;OF:有机肥配施),通过分析土壤理化性质、硝化势和氨氧化细菌(AOB)与古菌(AOA)对硝化势的相对贡献率、反硝化能力和N2O/(N2O+N2)产物比以及土壤呼吸,结合相关酶活性的测定研究增温和有机肥配施对硝化和反硝化过程的影响及其驱动因子。结果表明,增温显著降低了土壤含水率(2.3百分点)、有机碳(22.7%)、全磷(23.8%)和铵态氮含量(17.5%),而显著提高了硝态氮含量(52.8%);有机肥配施使土壤含水率、有机碳、全磷和铵态氮分别显著提高了1.2百分点,26.5%,31.3%,17.0%。增温显著提高了土壤呼吸(26.4%)、硝化势(31.7%)、AOB贡献率(16.4百分点)、反硝化能力(49.1%)以及N2O/(N2O+N2)产物比(10.5百分点);而有机肥配施使硝化势、AOA贡献率、反硝化能力以及N2O/(N2O+N2)产物比分别显著降低了39.3%,18.2百分点,24.7%,16.2百分点。增温和有机肥配施均显著提高了土壤脲酶、亚硝酸还原酶及羟胺还原酶活性;同时,相关分析结果表明,硝态氮含量、脲酶、亚硝酸还原酶及羟胺还原酶活性与AOB贡献率和反硝化能力呈显著正相关。综上,增温提高了土壤硝态氮含量以及脲酶、亚硝酸还原酶、羟胺还原酶的活性,进而增加了AOB硝化贡献、反硝化能力和N2O/(N2O+N2)产物比,导致N2O损失增加;而有机肥配施可以提高土壤养分,调节AOA和AOB在硝化过程中的作用,减小AOA贡献率、反硝化能力以及N2O/(N2O+N2)产物比,降低N2O损失,在一定程度上缓解增温的不利影响。

关键词: 增温, 有机肥配施, 土壤养分, 硝化势, 反硝化能力, 酶活性

Abstract:

In order to clarify the effects of climate change and organic fertilization on soil nitrogen cycling,a soybean field experiment was conducted in Hefei, Anhui from June to November 2023. Field warming was simulated using infrared radiation warming equipment, and two temperature levels(T0:Ambient temperature;T1:Warming)and different fertilization managements(SF:Synthetic fertilization;OF:Organic fertilization),and determined the effects of warming and organic fertilization on nitrification and denitrification processes and their drivers by investigating soil physicochemical properties,the relative contributions of ammonia-oxidizing bacteria(AOB)and archaea(AOA)to the nitrification potential,denitrification capacity and N2O/(N2O+N2)ratio,as well as soil respiration in combination with enzyme activity measurements.The results showed that warming significantly decreased soil moisture(2.3 precentage points),organic carbon(22.7%),total phosphorus(23.8%),N${\mathrm{H}}_{4}^{+}$-N(17.5%),while significantly increased NO3--N(52.8%);organic fertilization significantly increased soil moisture,organic carbon,total phosphorus,NH4+-N content by 1.2 percentage points,26.5%,31.3%,17.0%,respectively.Warming increased soil respiration(26.4%),nitrification potential(31.7%),AOB contribution(16.4 percentage points),denitrification capacity(49.1%),N2O/(N2O+N2)ratio(10.5 percentage points).Organic fertilization significantly decreased the nitrification potential, AOA contribution, denitrification capacity, and N2O/(N2O+N2)ratio by 39.3%, 18.2 percentage points, 24.7% and 16.2 percentage points,respectively.Warming and organic fertilization significantly increased urease (S-UE), nitrite reductase (S-NiR), and hydroxylamine reductase(HR)activities.The correlation analyses showed that NO3--N content,S-UE,S-NiR,and HR activities were significantly positively correlated with AOB contribution rate and denitrification capacity.Therefore,warming increased soil N${\mathrm{O}}_{3}^{-}$-N content and the activities of S-UE,S-NiR and HR,which in turn increased the nitrification contribution of AOB,denitrification capacity and N2O/(N2O+N2)ratio,leading to an increase in the loss of N2O;while organic fertilization could increase the soil nutrients and regulate the role of AOA and AOB in the nitrification process,reduce the contribution of AOA,denitrification capacity and N2O/(N2O+N2)ratio,and thus decrease the N2O loss,consequently,mitigating the adverse effects of warming.

Key words: Warming, Organic fertilization, Soil nutrients, Nitrification potential, Denitrification capacity, Enzyme activity

中图分类号: 

引用本文

吴旗, 李建霖, 陈杨, 栾崇圣, 汪小宇, 林雷利, 李笑笑, 车钊, 王晓波, 宋贺, 吴巩. 增温和有机肥配施对土壤硝化、反硝化过程及相关酶活性的影响[J]. 华北农学报, 2026, 41(3): 148-157. doi: 10.7668/hbnxb.20195771.

WU Qi, LI Jianlin, CHEN Yang, LUAN Chongsheng, WANG Xiaoyu, LIN Leili, LI Xiaoxiao, CHE Zhao, WANG Xiaobo, SONG He, WU Gong. Effects of Warming and Organic Fertilization on Soil Nitrification and Denitrification and the Activities of Enzymes Related to Nitrogen Cycling[J]. Acta Agriculturae Boreali-Sinica, 2026, 41(3): 148-157. doi: 10.7668/hbnxb.20195771.