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锡林河流域一个原生草原群落的碳素平衡研究
引用本文:李凌浩,韩兴国,王其兵,白文明,白永飞,闫志丹,陈全胜,张焱,杨晶,李鑫,宋世环. 锡林河流域一个原生草原群落的碳素平衡研究[J]. 植物学报(英文版), 2002, 44(6): 740-742
作者姓名:李凌浩  韩兴国  王其兵  白文明  白永飞  闫志丹  陈全胜  张焱  杨晶  李鑫  宋世环
作者单位:中国科学院植物研究所植被数量生态学开放研究实验室,北京,100093 
基金项目:国家重点基础研究发展计划(973计划),中国科学院知识创新工程项目 
摘    要:野外调查与历史资料相结合,对内蒙古锡林河流域一个永久试验样地内的羊草( Leymus chinensis (Trin.) Tzvel.)草原群落(原生草原群落)的碳素贮量、主要流量和周转速度等进行了估计.结果表明:1)该群落中地上部净初级生产的碳素固定量的多年平均值为79.8 g C*m-2*a-1,根系碳素输入量的多年平均值为311.9 g C*m-2*a-1,碳素输入总量为391.7 g C*m-2*a-1; 2)土壤净呼吸量为346.9 g C*m-2*a-1,动物(昆虫)采食量14.7 g C*m-2*a-1,地上立枯阶段的淋溶与光化学分解损失为3.2 g C*m-2*a-1,碳素输出总量为364.8 g C*m-2*a-1; 3)该群落中碳素输入略大于输出,净积累速率为26.9 g C*m-2*a-1,0-30 cm土壤中的碳素周转速率为6.2%,周转时间为16年.

关 键 词:羊草草原  碳素平衡  土壤呼吸  周转速率  净初级生产

Soil Carbon Balance in a Native Temperate Grassland in the Xilin RiverBasin of Inner Mongolia
Li Ling-hao,HAN Xing-Guo,WANG Qi-Bing,BAI Wen-Ming,BAI Yong-Fei,YAN Zhi-Dan,CHEN Quan-sheng,ZHANG Yan,YANG Jing,LI Xin,SONG Shi-Huan. Soil Carbon Balance in a Native Temperate Grassland in the Xilin RiverBasin of Inner Mongolia[J]. Journal of integrative plant biology, 2002, 44(6): 740-742
Authors:Li Ling-hao  HAN Xing-Guo  WANG Qi-Bing  BAI Wen-Ming  BAI Yong-Fei  YAN Zhi-Dan  CHEN Quan-sheng  ZHANG Yan  YANG Jing  LI Xin  SONG Shi-Huan
Abstract:Based on historical data and field investigation, some major fluxes and reserves of carbon were estimated, and a tentative analysis of the soil carbon balance was made in a native grassland community in the Xilin River basin of Inner Mongolia. Major results were reported as follows: 1) Annual average carbon input from above ground biomass production was 79.8 g C·m-2·a-1, and from root biomass to 30 cm depth averaged 311.9 g C·m-2·a-1. The summed mean annual carbon input of shoot and root materials in the study site was approximately 391.7 g C·m-2·a-1. 2) The annual amount of above ground biomass consumed by insects averaged 14.7 g C·m-2·a-1, and the carbon output by leaching or light chemical oxidation was 3.2 g C·m-2·a-1. The annual evolution rate of CO2 from net soil respiration averaged 346.9 g C·m-2·a-1, and the summed mean annual output was approximately 364.8 g C·m-2·a-1. 3) A mature, steady state system could be assumed for the community for which growth and decay were approximately in balance, with a net carbon accumulation of about 26.9 g C·m-2·a-1. Based on the soil organic carbon density of the field, the turnover rate of soil carbon in 0-30 cm depth was calculated to be 6.2%, with a turnover time of 16 years.
Keywords:Leymus chinensis steppe  carbon balance  soil respiration  turnover rate  net primary productivity (NPP)
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