Pattern of carbon allocation across three different stages of stand development of a Chinese pine (Pinus tabulaeformis) forest

被引:49
作者
Cao, Jixin [1 ,2 ]
Wang, Xiaoping [3 ,4 ]
Tian, Yun [1 ]
Wen, Zhiyong [5 ]
Zha, Tianshan [1 ,4 ]
机构
[1] Beijing Forestry Univ, Coll Soil & Water Conservat, Minist Educ, Key Lab Soil & Water Conservat & Desertificat Com, Beijing 100083, Peoples R China
[2] Chinese Acad Forestry, Res Inst Forest Ecol Environm & Protect, Key Lab Forest Ecol & Environm, State Forestry Adm China, Beijing 100091, Peoples R China
[3] Beijing Forestry & Pk Dept Int Cooperat, Beijing Forestry Carbon Adm, Beijing 100013, Peoples R China
[4] Chinese Inst Green Carbon, Beijing 100083, Peoples R China
[5] Huairou Dist Gardening & Greening Bur, Beijing 101400, Peoples R China
关键词
Carbon allocation; Biomass; Differently aged stands; Chinese pine; Coniferous forest; SOIL ORGANIC-CARBON; AGE-SEQUENCE; TREE BIOMASS; STORAGE; POOLS; CHRONOSEQUENCE; PLANTATIONS; STOCKS; SEQUESTRATION; ACCUMULATION;
D O I
10.1007/s11284-012-0965-1
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The pattern of carbon (C) allocation across different stages of stand development of Chinese pine (Pinus tabulaeformis) forests is poorly documented. In order to understand the effects of stand age on the C pool of the Chinese pine forest ecosystem, we have examined the above- and belowground C pools in three differently aged stands of Chinese pine in the northern mountains of Beijing, China, by plot-level inventories and destructive sampling. Our results suggest that tree branch and foliage biomass should be estimated by age-specific equations. Reasonably accurate estimates of tree stem, tree root, aboveground, and total tree biomass in a Chinese pine forest at different development stages were obtained using age-independent allometric equations from tree diameter only. The ratio of belowground to aboveground tree biomass was relatively constant with stand aging, remaining around 21 %. The contribution of aboveground tree biomass C increased from 21 % of the total ecosystem C in a 25-year-old stand to 44 % in a 65-year-old stand, subsequently falling to 41 % in a 105-year-old stand, while the contribution of mineral soil C decreased from 64 % of the total ecosystem C in 25-year-old stand to 38 % in a 65-year-old stand, subsequently increasing to 41 % in a 105-year-old stand. The C stock of the total ecosystem and its aboveground tree, tree root, forest floor, and mineral soil components continuously increased with stand ageing, whereas the C stock of the understory showed a declining trend and contributed little to the total site C pool.
引用
收藏
页码:883 / 892
页数:10
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