首页 | 本学科首页   官方微博 | 高级检索  
   检索      


Soil CO2 efflux and soil carbon balance of a tropical rubber plantation
Authors:Duangrat Satakhun  Frédéric Gay  Naruenat Chairungsee  Poonpipope Kasemsap  Pisamai Chantuma  Sornprach Thanisawanyangkura  Philippe Thaler  Daniel Epron
Institution:1. Center of Thai-French Cooperation on Higher Education and Research, Kasetsart University, Bangkok, 10900, Thailand
2. CIRAD, UMR Eco&sols, 34060, Montpellier, France
3. Department of Agriculture, Office of Agricultural Research and Development Region 1, Chiang Mai, 50200, Thailand
4. Department of Horticulture, Faculty of Agriculture, Kasetsart University, Bangkok, 10900, Thailand
5. Chachoengsao Rubber Research Centre, Rubber Research Institute of Thailand, Chachoengsao, 24160, Thailand
6. Department of Botany, Faculty of Science, Kasetsart University, Bangkok, 10900, Thailand
7. Ecologie et Ecophysiologie Forestières, Faculté des Sciences, Université de Lorraine, UMR 1137, 54506, Vandoeuvre-les-Nancy, France
Abstract:Natural rubber is a valuable source of income in many tropical countries and rubber trees are increasingly planted in tropical areas, where they contribute to land-use changes that impact the global carbon cycle. However, little is known about the carbon balance of these plantations. We studied the soil carbon balance of a 15-year-old rubber plantation in Thailand and we specifically explored the seasonal dynamic of soil CO2 efflux (F S) in relation to seasonal changes in soil water content (W S) and soil temperature (T S), assessed the partitioning of F S between autotrophic (R A) and heterotrophic (R H) sources in a root trenching experiment and estimated the contribution of aboveground and belowground carbon inputs to the soil carbon budget. A multiplicative model combining both T S and W S explained 58 % of the seasonal variation of F S. Annual soil CO2 efflux averaged 1.88 kg C m?2 year?1 between May 2009 and April 2011 and R A and R H accounted for respectively 63 and 37 % of F S, after corrections of F S measured on trenched plots for root decomposition and for difference in soil water content. The 4-year average annual aboveground litterfall was 0.53 kg C m?2 year?1 while a conservative estimate of belowground carbon input into the soil was much lower (0.17 kg C m?2 year?1). Our results highlighted that belowground processes (root and rhizomicrobial respiration and the heterotrophic respiration related to belowground carbon input into the soil) have a larger contribution to soil CO2 efflux (72 %) than aboveground litter decomposition.
Keywords:
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号