Estimation of soil respiration using automated chamber systems in an oak (Quercus mongolica) forest at the Nam-San site in Seoul, Korea

摘要

Soil respiration (R_(soil)) is the largest component of ecosystem respiration produced by the autotrophic and heterotrophic respirations. Its variability on multiple time scales strongly depends on environmental variables such as temperature and moisture. To investigate the temporal variations of R_(soil) in a cool-temperate oak (Quercus mongolica) forest at the Nam-San site in Seoul, Korea, continuous measurements of R_(soil) using the automated chamber systems, air and soil temperatures and soil moisture are made for the period from April 2010 to March 2011. The observed data indicate that the R_(soil) shows a remarkable seasonal variation in accordance with temperatures with high in summer and low in winter. The R_(soil) is found to be strongly correlated with soil temperature (T_s) at the 5 cm depth throughout the year. However, the high fluctuation of R_(soil) is found to be related with soil moisture content (M_s) during the forest growing season. The estimated annual Qlo value using the 1.5 m-high air temperature is found to be 2.4 that is comparable with other studies in temperate forest ecosystems. The optimal regression equation of R_(soil) with the T_s at 5 cm depth and the M_s at 15 cm depth is found to be R_(soil) = 124.3 exp (0.097T_s) -55.3 (M_s)~2 +2931.9 (M_s) -38516 for T_s≥0℃ and R_(soil) = 0 for T_s<0℃ with r~2 = 0.97, P<0.01, suggesting the importance of T_s and M_s for R_(soil). The annual total soil respiration estimated by the optimal regression equation is found to be 1264 g C m~(-2) with a maximum of 685 g C m~(-2) in the summer season and a minimum of 33 g C m~(-2) in the winter season. The present study can be implemented for the determination of the carbon balance of a cool-temperate Q. mongolica forest with the provision of photosynthesis.