20150523

Author : Li, H. J. Yan, J. X. Yue, X. F. Wang, M. B.
Year : 2008
Title : Significance of soil temperature and moisture for soil respiration in a Chinese mountain area
Journal : Agricultural and Forest Meteorology
Comment Temporal variations of soil respiration were dominantly controlled by soil temperature during most days of the year. The calculated Q10 and R10 of each site at the seasonal time scale were negatively correlated with soil temperature and positively correlated with soil moisture. For all data sets, four two-variable equations including linear and non-linear ones could be used to model relationships of soil respiration to both soil temperature and  moisture together, with the R2 ranging from a minimum of 0.58 to a maximum of 0.86 for individual site.

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