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林业科学 ›› 2008, Vol. 44 ›› Issue (10): 20-24.doi: 10.11707/j.1001-7488.20081004

• 论文 • 上一篇    下一篇

长沙樟树人工林生长季土壤呼吸特征

王光军 田大伦 朱凡 闫文德 郑威 李树战   

  1. (中南林业科技大学生态教研室 长沙410004)
  • 收稿日期:2007-08-10 修回日期:1900-01-01 出版日期:2008-10-25 发布日期:2008-10-25

Growth Reason Soil Respiration Characters of Cinnamomum camphoraPlantation in Changsha

Wang Guangjun,Tian Dalun,Zhu Fan,Yan Wende,Zheng Wei,Li Shuzhan   

  1. (Research Section of Ecology, Central South University of Forestry & Tech nology Changsha 410004)
  • Received:2007-08-10 Revised:1900-01-01 Online:2008-10-25 Published:2008-10-25

摘要:

用LI COR 6400 09测定并研究湖南长沙樟树人工林生长季节土壤呼吸速率的日变化及季节变化规律,分析土壤呼吸与土壤水热因子的关系。结果表明:樟树林生长季土壤呼吸速率日变化呈单峰曲线,与5 cm 深处土壤温度日变化相一致,2者呈显著指数相关,P=0.003; 樟树林土壤呼吸速率季节变化显著,呈不规则曲线波动,平均呼吸速率为4.0 μmol CO2·m-2s-1,与5 cm深处土壤温度之间呈显著指数相关,拟合方程为y=0.324 2e0.106 4x,R2=0.903,P=0.001, 与5 cm土壤湿度呈显著二次曲线相关,模拟方程为y=-0.026 1w2+1.869w-28.406,R2=0.436,P=0.05,土壤温度和湿度可以分别解释土壤呼吸变化的90.3%和43.6%; 由拟合的指数方程计算出樟树林生长季节的Q10值为2.9,4—6、7—8和9—10月Q 10值分别为3.08,1.59和2.72,呈现Q10 值随土壤温度升高而下降的趋势;土壤呼吸速率同时受土壤湿度的影响,当土壤湿度小于35.8%时,土壤呼吸与土壤湿度呈正相关,但当土壤含水量超过35.8%这个阈值,土壤湿度就成了土壤呼吸的抑制因子。

关键词: 城市森林, 樟树, 土壤呼吸, 土壤温度, 土壤湿度, 长沙

Abstract:

The diurnal and seasonal dynamics of soil respiration in the Cinnamomum camphoraforest ecosystem of a subtropical area were measured at Huitong ecological station for Chinese Fir plantations (Changsha station) in Hunan, China. CO2 effluxes rate was monitored using an infrared gas exchange analyzer (LI COR640009) from Aprip to October 2006, and the controlling factors, such as soil temperature and moisture were also recorded in the C. camphora forest. The results showed that the diurnal fluctuation of soil respiration accorded with that of the soil temperature at 5 cm depth, appearing single peak. The soil respiration exhibited an irregular fluctuated curve during the expenmental period with a mean rate of 4.0 μmol·m-2s-1. A significant exponertial corelation was found between soil respiration rate and soil temperature at 5 cm depth. However, significant relationships were not found between the soil respiration and the soil moisture at 5 cm depth. Soil temperature and moisture were able to be used to explain changes in soil respiration by 90.3% and 43.6% in the C. camphoraforest. The relationship between soil respiration rate (y) and the variable of soil temperature (t) and soil moisture (w) at 5 cm soil depth could be described by the following exponential equation:y=0.324 2e0.106 4x, R2=0.903, P=0.001, and by quadratic equation: y=-0.026 1w2+1.869w-28.406, R2=0.436, P=0.05, respectively. Q10 value of the soil respiration was 29 during the growing season of C. camphora. The Q10 values were 3.08, 1.59 and 2.72, respectively in April to June, July to August. and September to October. Q10 value descended with soil temperature raised. When soil humidity less than 35.8%, the soil respiration rate was positively correlated to soil humidity, however, the highest soil respiration rate was under the condition of soil humidity more than 35.8%.

Key words: urban forest, Cinnamomum camphora, soil respiration, soil temperature, soil water, Changsha