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生态学杂志 ›› 2005, Vol. ›› Issue (12): 1380-1383.

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长白山高山冻原生态系统的碳储量

魏晶, 邓红兵, 吴钢   

  1. 中国科学院生态环境研究中心系统生态重点实验室, 北京, 100085
  • 收稿日期:2004-10-16 修回日期:2005-05-19 出版日期:2005-12-10
  • 基金资助:
    国家自然科学基金项目(40173033)和中国科学院知识创新工程重要方向项目(KZCX3-SW-423).

Carbon storage of alpine tundra ecosystem in Changbai Mountains

WEI Jing, DENG Hongbing, WU Gang   

  1. Key Laboratory of Systems Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
  • Received:2004-10-16 Revised:2005-05-19 Online:2005-12-10

摘要: 对长白山高山冻原生态系统碳在植被-凋落物-土壤中的分布进行了研究。结果表明,在长白山高山冻原植被亚系统中,碳储量分布规律是典型高山冻原(TT)>石质高山冻原(ST)>草甸高山冻原(MT)>沼泽高山冻原(WT)>石海高山冻原(RT),长白山高山冻原的植被碳储量为3.3457×104t。而生物量分布规律是WT>TT>MT>ST>RT。在长白山高山冻原凋落物亚系统中,平均凋落物量是0.991 kg·hm-2.年·-1;凋落物碳储量为1.5043×104t,碳储量分布规律是TT>ST>MT>RT>WT。长白山高山冻原土壤(0~20 cm)亚系统中,有机碳储量为3.162×105t;每年约有1.4105×104t碳通过土壤呼吸释放到大气圈,长白山高山冻原植被-土壤系统现已成为3.6471×105t碳储库。

关键词: 降解菌, 甲基对硫磷, 农药残留, 降解率

Abstract: Carbon cycling in the alpine tundra of Changbai Mountains plays a unique role in the climate change of this region.In 2003,a field study was conducted to investigate the carbon distribution and storage in the plant,litter and soil of alpine tundra ecosystems at the elevations from 1950 to 2650 m.Four sampling plots were set up along the elevation transect,with an interval of 100 m.The plot size was 0.2?0.2 m,and all the plants in the plot were harvested.Soil bulk density was determined by the cutting-ring method at the depths of 5 cm and 15 cm.The results showed that the carbon storage of vegetation communities was typical alpine tundra(TT) > stony alpine tundra(ST) > meadow alpine tundra(MT) > swamp alpine tundra(WT) > rock sea alpine tundra(RT).The biomass of litter was 0.991 kg穐m-2穣r-1 in average,which was decreased in order of TT>ST>MT>RT>WT.The net storage of organic carbon was 3.6471?105 t in the plant-soil system of Changbai Mountains,and the carbon storage of vegetation,litter and soil pool was(3.3457?104t),(1.5053?104 t) and(3.1620?105 t),respectively.Plant stored(1.7251?104t) carbon each year,and(1.5043?104 t) of them entered into soil through litter-fall.The annual soil respiration rate was(1.4105?104 t)穣r-1.After vegetation succession stabilized,the average carbon storage was 3146 t穣r-1.The alpine tundra of Changbai Mountains was the sink of CO2.

Key words: Degrading bacterium, Methyl parathion, Pesticide residue, Degrading rate

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