NDLI: Belowground carbon balance and carbon accumulation rate in the successional series of monsoon evergreen broad-leaved forest

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Science in China Series D: Earth Sciences : Volume 49, Issue 1, January 2006

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Belowground carbon balance and carbon accumulation rate in the successional series of monsoon evergreen broad-leaved forest

Content Provider	Springer Nature Link
Author	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
Copyright Year	2006
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.
Starting Page	311
Ending Page	321
Page Count	11
File Format	PDF
ISSN	10069313
Journal	Science in China Series D: Earth Sciences
Volume Number	49
Issue Number	3
e-ISSN	18622801
Language	English
Publisher	Science in China Press
Publisher Date	2006-01-01
Publisher Place	Beijing
Access Restriction	Subscribed
Subject Keyword	monsoon evergreen broad-leaved forest successional series of restoration belowground carbon pool accumulation rate Geosciences
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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