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应用生态学报 ›› 2010, Vol. 21 ›› Issue (07): 1649-1655.

• 研究报告 • 上一篇    下一篇

模拟氮沉降对华西雨屏区慈竹林土壤呼吸的影响

李仁洪1,2,涂利华1,胡庭兴1**,张 健1,鲁 洋2,刘文婷1,雒守华1,向元彬1
  

  1. 1四川农业大学林学院四川省林业生态工程省级重点实验室, 四川雅安 625014;2四川省林业调查规划院,成都 610081
  • 出版日期:2010-07-20 发布日期:2010-07-20

Effects of simulated nitrogen deposition on soil respiration in a Neosinocalamus affinis plantation in Rainy Area of West China

LI Ren-hong1,2, TU Li-hua1, HU Ting-xing1, ZHANG Jian1, LU Yang2, LIU Wen-ting1, LUO Shou-hua1, XIANG Yuan-bin1
  

  1. 1Sichuan Province Key Laboratory of Forestry Ecological Engineering, College of Forestry, Sichuan Agricultural University, Ya’an 625014, Sichuan, China;2Sichuan Forestry Inventory and Plan Institute, Chengdu 610081,China
  • Online:2010-07-20 Published:2010-07-20

摘要: 2007年12月至2008年11月,在华西雨屏区采用0(对照)、50、150、300 kg·hm-2·a-1施氮处理和红外CO2分析法,研究了模拟N沉降对慈竹林土壤呼吸特征的影响.结果表明:慈竹林土壤呼吸速率年内季节变化呈明显的单峰型曲线,7月末最高,为(3.36±0.20) μmol·m-2·s-1,2月末最低,为(0.33±0.07) μmol·m-2·s-1.土壤呼吸速率与土壤温度之间呈极显著指数相关(P<0.001),10 cm深的土壤温度解释了土壤呼吸速率季节变化的91.6%;而土壤含水量与土壤呼吸之间相关性不显著(R2=0.0758).2008年6—11月根呼吸对土壤总呼吸的贡献率在46%~59%.50、150和300 kg·hm-2·a-1施氮处理的年CO2释放量分别比对照低23.6%、46.7%和50.5%.0、50、150和300 kg·hm-2·a-1施氮处理的土壤呼吸速率Q10值分别为3.72、3.51、2.95和2.71.

关键词: 氮沉降, 土壤呼吸, 慈竹林, 华西雨屏区, 植物, 高温胁迫, 分子机制, 蛋白质组学

Abstract: From December 2007 to November 2008, an in situ experiment was conducted to study the effects of simulated nitrogen deposition on the soil respiration in a Neosinocalamus affinis plantation in Rainy Area of West China. Four treatments were installed, i.e., 0 (CK), 50, 150, and 300 kg N·hm-2·a-1, and soil respiration rate was measured by infrared gas analyzer. In the test plantation, soil respiration rate had a distinct seasonal fluctuation, with the highest (3.36±0.20 μmol·m-2·s-1) by the end of July and the lowest by the end of February (0.33±0.07 μmol·m-2·s-1). There was a significant exponential relationship (P<0.001) between soil respiration rate and soil temperature, and the temperature at 10 cm soil depth explained 91.6% of the seasonal change of soil respiration. However, less relationship was observed between soil respiration rate and soil moisture content (R2=0.0758). From June to November 2008, the contribution of root respiration to total soil respiration ranged from 46% to 59%. The annual release amount of CO2 in treatments 50, 150, and 300 kg·hm-2·a-1 was 23.6%, 46.7%, and 50.5% lower than that in CK (2.17×104 kg ·hm-2), and the Q10 value of soil respiration rate in treatments 0, 50, 150, and 300 kg·hm-2·a-1 was 3.72, 3.51, 2.95, and 2.71, respectively.

Key words: nitrogen deposition, soil respiration, Neosinocalamus affinis, Rainy Area of West China, plant , heat stress, molecular mechanism, proteomics.