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[中国亚热带次生林土壤呼吸中异养和自养成分的研究]

[Investigation of heterotrophic and autotrophic components of soil respiration in a secondary forest in subtropical China].

作者信息

Shen Xiao-Shuai, Chen Shu-Tao, Hu Zheng-Hua, Shi Yan-Shu, Zhang Yong

机构信息

Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Nanjing University of Information Science and Technology, Nanjing 210044, China.

出版信息

Huan Jing Ke Xue. 2011 Nov;32(11):3181-7.

Abstract

Trenched plots were set up in 2010 in a secondary forest in subtropical China, in order to investigate the seasonal variations of soil respiration (R(s)) and heterotrophic respiration (R(h)). Autotrophic respiration (R(a)) was estimated to be the difference between R(s) and R(h). Soil temperature and moisture were simultaneously measured during respiration measurements. Results indicated that R(s) and R(h) showed the similar seasonal variations. Seasonal mean rates for R(s), R(h) and R(a) were 3.42, 2.36 and 1.06 micromol x (m2 x s)(-1), respectively. Regression analysis indicated that R(h) increased with the increase of R(s); an natural logistic equation could be employed to explained the relationship between R(h) (y) and R(s) (x). Approximately 90.5% (R2 = 0.905) variations in R(h) could be explained by the equation. Apparent exponential relationships of R(h) and R(a) with soil temperature existed, but differed from each other and from the relationship for R(s). The exponential equations explained about 78.4%, 76.4% and 65.6% variations in R(s), R(h) and R(a), respectively, with the P values less than 0.01. The Q10 values for R(s), R(h) and R(a) were 1.97, 1.76 and 3.31, respectively. It was indicated that, seasonally, R(h) and R(a) represented 69% and 31% of R(s). R(a) showed significantly higher temperature sensitivity than R(h).

摘要

2010年,在中国亚热带的一片次生林中设置了带状样地,以研究土壤呼吸(R(s))和异养呼吸(R(h))的季节变化。自养呼吸(R(a))通过R(s)与R(h)的差值估算得出。在进行呼吸测量的同时,同步测量了土壤温度和湿度。结果表明,R(s)和R(h)呈现出相似的季节变化。R(s)、R(h)和R(a)的季节平均速率分别为3.42、2.36和1.06微摩尔·(平方米·秒)⁻¹。回归分析表明,R(h)随R(s)的增加而增加;可用自然逻辑方程解释R(h)(y)与R(s)(x)之间的关系。该方程可解释R(h)中约90.5%(R² = 0.905)的变化。R(h)和R(a)与土壤温度存在明显的指数关系,但彼此不同,且与R(s)的关系也不同。这些指数方程分别解释了R(s)、R(h)和R(a)中约78.4%、76.4%和65.6%的变化,P值均小于0.01。R(s)、R(h)和R(a)的Q10值分别为1.97、1.76和3.31。结果表明,从季节上看,R(h)和R(a)分别占R(s)的69%和31%。R(a)的温度敏感性显著高于R(h)。

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