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生态学杂志 ›› 2021, Vol. 40 ›› Issue (4): 1029-1037.doi: 10.13292/j.1000-4890.202104.019

• 研究报告 • 上一篇    下一篇

氮沉降对北亚热带麻栎林土壤呼吸及其温湿度敏感性的影响

余景松1,付若仙1,俞元春2,李春涛     

  1. (1安徽农业大学林学与园林学院, 合肥 230036; 2南京林业大学生物与环境学院, 南京 210037)
  • 出版日期:2021-04-10 发布日期:2021-04-12

Effects of nitrogen deposition on soil respiration and its sensitivity to temperature and humidity in a Quercus acutissima forest in northern subtropics.

YU Jing-song1, FU Ruo-xian1, YU Yuan-chun2, LI Chun-tao1, TAO Xiao1*#br#   

  1. (1College of Forestry and Landscape Architecture, Anhui Agricultural University, Hefei 230036, China; 2College of Biology and Environment, Nanjing Forestry University, Nanjing 210037, China).
  • Online:2021-04-10 Published:2021-04-12

摘要: 近年来,含氮化合物排放量迅速增加,并随着人口增长及城市化程度的提高而持续增加,这些氮元素以沉降的形式降落到森林生态系统中,对森林土壤碳通量产生深远影响,使氮沉降成为影响森林土壤呼吸的一个重要因素。本研究以安徽省万佛山麻栎天然林为对象,通过模拟氮沉降试验,采用LI-8100土壤呼吸仪测定土壤呼吸速率及土壤温湿度,探讨短期氮添加对森林生态系统土壤呼吸及其温湿度敏感性的影响。结果表明:N0(对照)、N1(低氮)、N2(高氮)3种处理下土壤呼吸及其各组分均有明显季节变化特征,N1和N2处理均轻微提高了麻栎天然林土壤总呼吸及各组分呼吸速率,但差异均不显著(P>0.05),N1、N2处理年平均土壤总呼吸速率分别为2.17和2.13 μmol·m-2·s-1,较N0处理分别提高了6.90%和4.93%;麻栎林土壤呼吸与土壤温度呈显著的指数关系(P<0.001),N0、N1、N2处理下土壤总呼吸Q10分别为2.04、1.99和2.10,低氮(N1)在一定程度上提高了自养呼吸Q10,而降低了异养呼吸Q10;高氮(N2)提高了土壤呼吸各组分Q10;土壤含水率与土壤呼吸呈显著相关关系(P<0.05),但其相关性小于土壤温度与土壤呼吸,土壤呼吸与土壤温度和土壤含水率的复合模型优于单因子模型。研究结果为预测土壤呼吸及其组分在氮沉降增加下的变化提供了新的思路。

关键词: 麻栎天然林, 土壤呼吸, 土壤温度, 土壤含水率, Q10, 氮沉降

Abstract: In recent years, emissions of nitrogenous compounds have increased rapidly, which would continue with population growth and urbanization. Such nitrogen falls into forest ecosystems in the form of deposition, with profound impacts on forest soil carbon fluxes. Nitrogen deposition becomes an important factor affecting forest soil respiration. In this study, a nitrogen deposition simulation experiment was carried out in a Quercus acutissima natural forest in Wanfo Mountain, Anhui Province to explore the shortterm impacts of nitrogen addition on soil respiration and components and their sensitivity to temperature and humidity. The soil respiration rate, soil temperature and moisture were measured by LI-8100. Soil respiration and its components had obvious seasonal variations under all the treatments of N0 (control), N1 (low N) and N2 (high N). Both N1 and N2 treatments slightly increased total soil respiration and its components, but without statistical significance (P<0.05). The average annual total soil respiration rates of N0, N1, and N2 treatments were 2.03, 2.17 and 2.13 μmol·m-2·s-1, with 6.90% and 4.93% higher in N1 and N2 treatments than in N0 treatment, respectively. There was a significant exponential relationship between soil respiration and soil temperature (P<0.001). The Q10 values of the total soil respiration under N0, N1 and N2 treatments were 2.04, 1.99 and 2.10, respectively. N1 treatment increased the Q10 of the autotrophic respiration but decreased the Q10 of the heterotrophic respiration. N2 treatment increased the Q10 of each component of soil respiration. There was a significant correlation between soil moisture and soil respiration (P<0.05), with the R2 value of its correlation being smaller than that between soil temperature and soil respiration. The composite model of soil respiration with soil temperature and soil moisture performed better than the singlefactor models. Our findings provide a new way to predict the changes of soil respiration and its components under the increasing nitrogen deposition scenarios.

Key words: Quercus acutissima natural forest, soil respiration, soil temperature, soil moisture content, Q10, N deposition.