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应用生态学报 ›› 2003, Vol. ›› Issue (5): 797-802.

• 研究论文 • 上一篇    下一篇

中国陆地土壤有机碳蓄积量估算误差分析

王绍强, 刘纪远, 于贵瑞   

  1. 中国科学院地理科学与资源研究所生态系统研究网络综合中心, 北京 100101
  • 收稿日期:2002-09-14 修回日期:2003-01-06
  • 通讯作者: 王绍强,男,1972年11月生,博士,副研究员,主要从事陆地生态系统碳循环、土地利用/土地覆被变化和遥感应用研究,发表论文10多篇.E-mial:wangsq@lreis.ac.cn.
  • 基金资助:
    中国科学院地理科学与资源研究所知识创新工程主干科学计划专题“中国陆地生态系统土壤有机碳蓄积估算”(CXIOGE010202);中国科学院“百人计划”生态系统管理的基础生态学过程研究项目

Error analysis of estimating terrestrial soil organic carbon storage in China

WANG Shaoqiang, LIU Jiyuan, YU Guirui   

  1. CERN, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2002-09-14 Revised:2003-01-06

摘要: 简要介绍了土壤碳蓄积量的计算方法,包括土壤类型法、植被类型法、生命地带法、相关关系法和模型方法,以及土壤有机碳蓄积量的误差分析方法.根据中国第二次土壤普查2473个典型土种剖面数据,采用土壤类型法和两种碳密度方法计算,估算的中国陆地土壤有机碳蓄积量处于615.19×1014~1211.37×1014g之间,平均碳密度为10.49~10.53kg·m-2(土壤厚度为100cm)或11.52~12.04kg·m-3(土壤平均厚度为88cm),土壤平均碳蓄积量为913.28±298.09×1014g,估算的不确定性在20%~50%之间.其中,土壤碳计算和采样数量的差异是导致土壤碳蓄积量估算不确定性的重要因素.

关键词: 土壤有机碳蓄积量, 碳循环, 土壤碳循环

Abstract: The paper summarizes different estimating methods of soil organic carbon (SOC) storage including methods of soil taxonomy, vegetation types, Holdridge zones, correlative relationship and modeling. The error analysis of SOCcalculation was introduced. Based on second national soil survey 2473 soil profiles, adopting soil taxonomy method and two kinds of SOCdensity, the terrestrial SOC storage in China was estimated. The range of SOC storage in China is between 615.19 and 1211.37×1014 g and the average SOCdensity is between 10.49~10.53 kg·m-2 (for average soil depth of 100cm) or 11.52~12.04 kg·m-3 (for average soil depth of 88cm). Through estimation and error analysis, the average SOC storage is about 913.28±298.09×1014 g and the uncertainty is among 20%~50%. Results showed that the differences of SOC estimation and sampling methods are important factors of SOCestimating uncertainties.

Key words: Soil organic carbon storage, Carbon cycle, Soil carbon cycle

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