南亚热带杉木生态系统生物量和碳素积累及其空间分布特征

被引:50
作者
康冰 [1 ,2 ]
刘世荣 [2 ]
蔡道雄 [3 ]
卢立华 [3 ]
机构
[1] 西北农林科技大学生命科学学院
[2] 中国林业科学研究院森林生态环境与保护研究所
[3] 中国林业科学研究院热带林业实验中心
关键词
生物量; 碳贮存; 空间分布; 杉木人工林; 极限分布区; 南亚热带;
D O I
暂无
中图分类号
S718.556 [];
学科分类号
摘要
Carbon accumulation and distribution were studied in three plots of a 13 years old Chinese fir (Cunninghamia lanceolata) forest in Daqingshan,Guangxi. The results showed that the average carbon concentration in all organs was in the following order: leaf (510.5)>bark (501.8)>wood (485.1)>root (476.5)>branch(462.1) (g·kg~ -1 ). The carbon concentration of soil (to 60 cm depth) ranged from 11.4 to 21.1 (g·kg~ -1 ),with an average of 16.6 (g·kg~ -1 ). Carbon concentration of surface soil (to 20 cm) was higher than the other layer. The average carbon concentrations (g·kg~ -1 ) in different layers were in the order as: trees (497)> shrub (437.5) >standing litters (437.5)>herb (407.8). The carbon storage of the forest ecosystem was in order of soil layer>vegetation >standing litter. Of total average carbon,23.87% was in vegetation component,74.27% in soil (60 cm depth),and only 1.86% in standing ground litter layer. The tree layer occupied 22.93% of total carbon storage in the ecosystem and 96.07% of carbon storage in the vegetation layer. The carbon storage in different organs was positively related to the biomass of corresponding organs. Trunk accumulated the highest carbon storage,comprising 58.40% of carbon storage in tree layer. Secondly,root made up 20.09% of total tree carbon. The annual net productivity of Chinese fir plantation was 10.10 t·hm~ -2 a~ -1 ,stored carbon up to 4.67 t·hm~ -2 a~ -1 ,equal to 17.13 t·hm~ -2 a~ -1 of CO2. Chinese fir plantation was an important sink of atmospheric CO2. But its capacity of C sequestration decreased gradually in this region.
引用
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页码:147 / 153
页数:7
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