Soil respiration in response to year-to-year variations in rainfall in a tropical seasonal forest in northern Thailand
Article first published online: 3 FEB 2012
Copyright © 2012 John Wiley & Sons, Ltd.
Volume 6, Issue 1, pages 134–141, February 2013
How to Cite
Kume, T., Tanaka, N., Yoshifuji, N., Chatchai, T., Igarashi, Y., Suzuki, M. and Hashimoto, S. (2013), Soil respiration in response to year-to-year variations in rainfall in a tropical seasonal forest in northern Thailand. Ecohydrol., 6: 134–141. doi: 10.1002/eco.1253
- Issue published online: 15 FEB 2013
- Article first published online: 3 FEB 2012
- Manuscript Accepted: 12 JAN 2012
- Manuscript Revised: 10 JAN 2012
- Manuscript Received: 24 AUG 2011
- soil CO2 efflux;
- carbon balance;
- tropical deciduous;
- teak plantation
In a tropical deciduous forest in northern Thailand, an area affected by the Asian monsoon, we made soil respiration measurements for 4 years to determine their inter-annual variability. We also made continuous measurements of soil moisture, soil temperature, and soil CO2 concentration. Annual soil respiration rates were estimated using two methods: multiple regression analysis and Fick's first law of diffusion. During the study period, between June 2000 and December 2004, the annual rainfall and the length of the wet period showed considerable year-to-year variation, differing by 1162–1435 mm year−1 falling over 146–189 days, respectively. In response to the inter-annual variability in rainfall, annual soil respiration rates estimated by the two models also showed large inter-annual variations for the 4 years (coefficient of variation = 14–17%). The range in the inter-annual variation for soil respiration was comparable with values for net ecosystem exchange reported in other Southeast Asian tropical forests. Historical rainfall records at this site showed further large inter-annual variations that occurred in times other than in the study period, suggesting that long-term monitoring would be required for a better understanding of the C balance at this site. Copyright © 2012 John Wiley & Sons, Ltd.