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生态学杂志 ›› 2010, Vol. 29 ›› Issue (06): 1047-1053.

• 研究报告 •    下一篇

哀牢山亚热带常绿阔叶林乔木碳储量及固碳增量

张鹏超1,4;张一平1,2,3**;杨国平1,2,3;郑 征1,2,3;刘玉洪1,2,3;谭正洪1,4   

  1. 1中国科学院热带森林生态学重点实验室(西双版纳热带植物园),云南勐仑 666303;2中国科学院哀牢山亚热带森林生态系统研究站,云南景东676209;3云南哀牢山森林生态系统国家野外科学观测研究站,云南景东 676209;4中国科学院研究生院,北京 100049
  • 出版日期:2010-06-10 发布日期:2010-06-10

Carbon storage and sequestration of tree layer in subtropical evergreen broadleaf forests in Ailao Mountain of Yunnan.

ZHANG Peng-chao1,4;ZHANG Yi-ping1,2,3;YANG Guo-ping1,2,3;ZHENG Zheng1,2,3;LIU Yu-hong1,2,3;TAN Zheng-hong1,4   

  1. 1Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Menglun 666303, Yunnan, China;2Ailaoshan Station for Subtropical Forest Ecosystem Studies, Jingdong 676209, Yunnan, China;3National Forest Ecosystem Research Station at Ailaoshan, Jingdong 676209, Yunnan, China;4Graduate University of Chinese Academy of Sciences, Beijing 100049, China
  • Online:2010-06-10 Published:2010-06-10

摘要: 了解哀牢山亚热带常绿阔叶林的乔木碳储量及其固碳增量,利用2005和2008年的植被调查数据,对哀牢山3种主要常绿阔叶林的乔木碳储量及其固碳增量进行了分析。结果表明:原生的中山湿性常绿阔叶林、滇山杨次生林和旱冬瓜次生林的乔木碳储量分别为257.90、222.95和105.39 t C·hm-2;中山湿性常绿阔叶林乔木碳储量主要存储在DBH≥91 cm的乔木中(34.68%);而次生林的乔木碳储量主要分布在径级21 cm≤DBH<41 cm的乔木中(滇山杨林77.29%;旱冬瓜林69.28%)。由此可见,哀牢山地区原生的中山湿性常绿阔叶林乔木层在碳蓄积方面占主导优势。哀牢山亚热带常绿阔叶林的3个森林类型乔木层均具有固碳增量,即使是原生的中山湿性常绿阔叶林,其乔木层年平均固碳增量也达2.47 t C·hm-2·a-1;次生林乔木层的年平均固碳增量约为原生林的2倍,显示了哀牢山亚热带常绿阔叶林乔木层具有较强的碳汇增量。初步估算,哀牢山亚热带常绿阔叶林林区内每年乔木固碳增量为8.52×10.4 t C·a-1

关键词: 三江平原, 泥炭, 营养元素, 分布特征

Abstract: In order to understand the tree layer carbon storage and sequestration in the subtropical evergreen broadleaf forests in Ailao Mountain, an analysis was made on the tree layer carbon storage and sequestration in three dominant forests in the Mountain, based on the field surveys in 2005 and 2008. The tree layer carbon storage in the primary evergreen broadleaf forest, secondary Populus bonatii forest, and secondary Alnus nepalensis forest in the Mountain was 257.90, 222.95, and 105.39 t C·hm-2, respectively. The tree layer carbon storage of the primary evergreen broadleaf forest was mainly contributed by the trees with DBH ≥91 cm (34.68%), while that of the two secondary forests was mainly contributed by the trees with DBH from 21 cm to 41 cm (77.29% for P. bonatii secondary forest, and 69.28% for A. nepalensis secondary forest), suggesting that the tree layer of primary evergreen broadleaf forest played an important role in the carbon storage in Ailao Mountain. The tree layers of the three forests all had the capability of carbon sequestration. The mean annual increment of tree layer carbon sequestration in primary evergreen broadleaf forest was 2.47 t C·hm-2·a-1, and that in the two secondary forests was about two times of the primary evergreen broadleaf forest, suggesting a great potential of carbon sequestration in secondary forests. Based on the above-mentioned results,it was estimated that the mean annual increment of tree layer carbon sequestration within the Ailao Mountain National Nature Reserve was 8.52×10.4 t C·a-1.

Key words: Sanjiang Plain, Peat, Nutrient elements, Distribution character