Biomass and carbon dynamics of a tropical mountain rain forest in China

被引：34
|
作者：
Chen DeXiang [1 ]
Li YiDe [1 ]
Liu HePing [2 ]
Xu Han [1 ]
Xiao WenFa [3 ]
Luo TuShou [1 ]
Zhou Zhang [4 ]
Lin MingXian [1 ]
机构：
[1] Chinese Acad Forestry, Res Inst Trop Forestry, Guangzhou 510520, Guangdong, Peoples R China
[2] Jackson State Univ, Dept Phys Atmospher Sci & Geosci, Jackson, MS 39217 USA
[3] Chinese Acad Forestry, Res Inst Forest Ecol Environm & Protect, Beijing 100091, Peoples R China
[4] Peking Univ, Dept Ecol, Coll Urban & Environm Sci, Beijing 100872, Peoples R China
来源：
SCIENCE CHINA-LIFE SCIENCES | 2010年 / 53卷 / 07期
基金：
中国国家自然科学基金;
关键词：
Jianfengling; tropical mountain rain forest; biomass; carbon storage; environmental determinants; CLIMATE-CHANGE; LAND-USE; FLORISTIC COMPOSITION; ABOVEGROUND BIOMASS; SPECIES RICHNESS; NITROGEN STOCKS; NUTRIENT POOLS; AMAZON FOREST; SOIL CARBON; PRODUCTIVITY;
D O I：
10.1007/s11427-010-4024-2
中图分类号：
Q [生物科学];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
Biometric inventories for 25 years, from 1983 to 2005, indicated that the Jianfengling tropical mountain rain forest in Hainan, China, was either a source or a modest sink of carbon. Overall, this forest was a small carbon sink with an accumulation rate of (0.56 +/- 0.22) Mg C ha(-1)yr(-1), integrated from the long-term measurement data of two plots (P9201 and P8302). These findings were similar to those for African and American rain forests ((0.62 +/- 0.23) Mg C ha(-1)yr(-1)). The carbon density varied between (201.43 +/- 29.38) Mg C ha(-1) and (229.16 +/- 39.2) Mg C ha(-1), and averaged (214.17 +/- 32.42) Mg C ha(-1) for plot P9201. Plot P8302, however, varied between (223.95 +/- 45.92) Mg C ha(-1) and (254.85 +/- 48.86) Mg C ha(-1), and averaged (243.35 +/- 47.64) Mg C ha(-1). Quadratic relationships were found between the strength of carbon sequestration and heavy rainstorms and dry months. Precipitation and evapotranspiration are two major factors controlling carbon sequestration in the tropical mountain rain forest.
引用
收藏
页码：798 / 810
页数：13
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