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川西亚高山人工林碳氮分配格局及其随凋落叶分解的释放规律

刘增文1;段而军1;潘开文2;张丽萍1;杜红霞1   

  1. 1西北农林科技大学资源环境学院, 陕西杨凌 712100; 2中国科学院成都生物研究所, 成都 610041
  • 收稿日期:2008-05-05 修回日期:1900-01-01 出版日期:2009-01-20 发布日期:2009-01-20

C and N allocation patterns in planted forests and their release patterns during leaf litter decomposition in subalpine area of west Sichuan.

LIU Zeng-wen1;DUAN Er-jun1;PAN Kai-wen2;ZHANG Li-ping1; DU Hong-xia1   

  1. 1College of Resources Environment, Northwest A & F University, Yangling 712100, Shaanxi, China; 2Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610041, China
  • Received:2008-05-05 Revised:1900-01-01 Online:2009-01-20 Published:2009-01-20

摘要: 对四川西部亚高山地区连香树、糙皮桦、云南松和云杉4种主要人工林生态系统的生物量、土壤及林木器官C、N含量进行了测定.结果表明:林木体内C的分布与器官年龄的关系不明显,而N和C/N的分布与年龄的关系较为密切.幼嫩器官中的N含量大于老化器官,老化器官中的C/N比值大于幼嫩器官,且针叶林地枯落叶中的C/N比值大于阔叶林地.C、N在土壤表层具有明显的富集作用,在整个人工林生态系统(包括林木、枯落物和土壤0~40 cm)中的积累量分别达 176.75~228.05 t·hm-2和 11.06~16.54 t·hm-2,在土壤-枯落物分室和林木分室中的分配比例为C (1.9~3.3)∶1,N (15.6~41.5)∶1,且针叶林的“C汇”功能大于阔叶林.阔叶林地的凋落叶分解速率一般大于针叶林地,周转期分别为2.2~3.7 a和3.9~4.2a;在凋落叶分解过程中,C在所有林地均呈超速释出态势,周转期为1.9~3.4 a;N在连香树和糙皮桦林地呈超速释出态势,周转期为1.9~3.2 a,在云南松和云杉林地呈慢速释出态势,周转期为6.7~8.5 a.

关键词: 生理指标, 根瘤共生, 外源钙, 盐胁迫, 豌豆

Abstract: With the planted forest ecosystems of Cercidiphyllum japonicum, Betula utilis, Pinus yunnansinsis, and Picea asperata in subalpine area of west Sichua n as test objects, their total biomass and the C and N contents in soils and tre e organs were determined. The results showed that the allocation of C in tree or gans had less correlation with the age of the organs, while that of N and C/N ra tio had closer relationship with the age. The N content in young organs was high er than that in aged ones, whereas the C/N ratio was higher in aged organs than in young organs, and higher in the leaf litters of needle-leaved forests than i n those of broad-leaved forests. There was an obvious enrichment of C and N in the topsoil of test forests. The accumulated amounts of C and N in the whole pla nted forest ecosystem, including tree, litter, and 0〖KG-*2〗-〖KG-*7〗40 cm soil layer, were 17675〖KG-*2〗-〖KG-*7〗22805 t·hm-2 and 1106〖KG-*2 〗-〖KG-*7〗1654 t·hm-2, respectively, and the nutrients allocation rat io between soil-litter and tree was (19〖KG-*2〗-〖KG-*7〗33)∶〖KG-*2〗1 for C an d (156〖KG-*2〗-〖KG-*7〗415)∶〖KG-*2〗1 for N. Needle-leaved forests functioned as a stronger “C-sink” than broad-leaved forests. The decomposition rate of the l eaf litters in needle-leaved forests was larger than that in broad-leaved fore sts, with the turnover rate being 22〖KG-*2〗-〖KG-*7〗37 years and 39〖KG -*2〗-〖KG-*7〗42 years, respectively. During the decomposition of leaf litter, the C in all of the four forests released at super -speed, with the turnover rate being 19〖KG-*2〗-〖KG-*7〗34 years. As for N, it also released at super-speed in C. japonicum and B. utilis forest s, with the turnover rate being 19〖KG-*2〗-〖KG-*7〗32 years, but released a t low speed in P. yunnansinsis and P. asperata forests, with the turnove r rate being 67〖KG-*2〗-〖KG-*7〗85 years.

Key words: pea, physiological index, exogenous calcium, salt stress, symbiotic rhizobium