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Belowground carbon balance and carbon accumulation rate in the successional series of monsoon evergreen broad-leaved forest
基金项目:中国科学院知识创新工程项目;中国科学院资助项目
摘    要:The belowground part of terrestrial ecosystem is a huge carbon pool. It is believed that of the total 2500Gt carbon stored in global terrestrial ecosystem, soil carbon storage within the 1 m surface layer ac- counts for 2000Gt, which is 4-fold of vegetation car- bon storage1,2]. Compared with the carbon in the vegetation, carbon in the deep soil layers is much more stable, and it will stay in soil profile permanentlyunless geological vicissitude occurs. Essentially, forest restoration is the…

收稿时间:6 December 2004
修稿时间:3 May 2005

Belowground carbon balance and carbon accumulation rate in the successional series of monsoon evergreen broad-leaved forest
Authors:ZHOU Guoyi  ZHOU Cunyu  LIU Shuguang  TANG Xuli  OUYANG Xuejun  ZHANG Deqiang  LIU Shizhong  LIU Juxiu  YAN Junhua  ZHOU Chuanyan  LUO Yan  GUAN Lili  LIU Yan
Institution:1. Dinghushan Forest Ecosystem Research Station, Chinese Academy of Sciences, Guangzhou 510650, China
2. SAIC, EROS Data Center, U.S. Geological Survey, Sioux Falls, SD 57198, USA
Abstract:The balance, accumulation rate and temporal dynamics of belowground carbon in the successional series of monsoon evergreen broadleaved forest are obtained in this paper, based on long-term observations to the soil organic matter, input and standing biomass of litter and coarse woody debris, and dissolved organic carbon carried in the hydrological process of subtropical climax forest ecosystem—monsoon evergreen broad-leaved forest, and its two successional forests of natural restoration—coniferous and broad-leaved mixed forest and Pinus massoniana forest, as well as data of root biomass obtained once every five years and respiration measurement of soil, litter and coarse woody debris respiration for 1 year. The major results include: the belowground carbon pools of monsoon evergreen broad-leaved forest, coniferous and broad-leaved mixed forest, and Pinus massoniana forest are 23191 ± 2538 g · m−2, 16889 ± 1936 g · m−2 and 12680 ± 1854 g · m−2, respectively, in 2002. Mean annual carbon accumulation rates of the three forest types during the 24a from 1978 to 2002 are 383 ± 97 g · m−2 · a−1, 193 ± 85 g · m−2 · a−1 and 213 ± 86 g · m−2 · a−1, respectively. The belowground carbon pools in the three forest types keep increasing during the observation period, suggesting that belowground carbon pools are carbon sinks to the atmosphere. There are seasonal variations, namely, they are strong carbon sources from April to June, weak carbon sources from July to September; while they are strong carbon sinks from October to November, weak carbon sinks from December to March.
Keywords:monsoon evergreen broad-leaved forest  successional series of restoration  belowground  carbon pool  accumulation rate  
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