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长白山原始阔叶红松林不同演替阶段地下生物量与碳、氮贮量的比较

杨丽韫1,2 罗天祥3 吴松涛2   

  1. 1中国科学院地理科学与资源研究所,北京100101;2北京科技大学冶金与生态工程学院,北京100083;3中国科学院青藏高原研究所,北京100085
  • 收稿日期:2004-05-21 修回日期:2004-11-14 出版日期:2005-07-18

Root biomass and underground C and N storage of primitive Korean pine and broad-leaved climax forest in Changbai Mountains at its different succession stages

YANG Liyun1,2,LUO Tianxiang3,WU Songtao2   

  1. 1Institute of Geographical Sciences and Natural Resources Research,Chines
    e Academy of Sciences,Beijing 100101,China;2School of Metallurgical and Ecological Engineering,Beijing University of Science and Technology,Beijing 100083,China;3Institute of Qinghai-Tibet Al
    tiplano Research,Chinese Academy of Sciences,Beijing 100085,China

  • Received:2004-05-21 Revised:2004-11-14 Online:2005-07-18

摘要: 以我国东北长白山自然保护区内同一海拔水平的原始阔叶红松林及其次生林——白桦山杨成熟林和幼林为对象,对不同演替阶段林地地下生物量与碳、氮贮量进行了研究.结果表明,随着演替的进行,白桦山杨幼林、成熟林和阔叶红松林根系生物量分别为2.437、2.742和4.114 kg·m-2,根系碳贮量分别为1.113、1.323和2.023 kg·m-2,土壤碳贮量分别为11.911、11.943和12.587 kg·m-2,林地地下碳贮量分别为13.024、13.266和14.610 kg·m-2.3块林地中根系氮贮量分别为0.035、0.032和0.039 kg·m-2,土壤氮贮量分别为1.207、1.222和0.915 kg·m-2,林地地下氮贮量分别为1.243、1.254和0.955 kg·m-2.在长白山地区次生林演替和恢复过程中林地地下部分是潜在的碳汇,而土壤氮贮量则没有明显的变化规律.

关键词: 溶解性有机质, 提取方法, 来源, 组成, 生物有效性, 环境意义

Abstract: With more than 200 years old primitive Korean pine and broad?leaved climax forest and its two 20 and 80 years old secondary Populus davidiana and Betula platyphylla forests in Changbai Mountains as test objects,this paper studied their root biomass and underground C and N storage.The results showed that the root biomass of 20 years old,80 years old,and climax forests was 2.437,2.742 and 4.114 kg·m-2,respectively. with forest succession,the root C storage was 1.113,1.323 and 2.023 kg·m-2,soil C storage was 11.911,11.943 and 12.587 kg·m-2,and underground C storage was 13.024,13.266 and 14.610 kg·m-2,respectively,while the root N storage was 0.035,0.032 and 0.038 kg·m-2,soil N storage was 1.207,1.222 and 0.915 kg·m-2,and underground N storage was 1.243,1.254 and 0.955 kg·m-2, respectively, which indicated that along with forest succession,forest underground became a potential “carbon sink",whereas underground N storage did not change obviously.

Key words: Dissolved organic matter, Extraction method, Origin, Composition, Bioavailability, Environmental significance