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生态学杂志 ›› 2003, Vol. ›› Issue (4): 97-101.

• 技术与方法 • 上一篇    下一篇

划分土壤类型的一种新方法——以功能生态学理论为基础(英文)

尹光彩1, A S Kerzhentcef2, V V Bugrovskiy3, 周国逸1, 温达志1   

  1. 1. 俄罗斯科学院基础生物研究所, 普希诺, 莫斯科, 142290;
    2. 俄罗斯科学院乌布苏诺国际生物圈研究中心, 克孜勒, 图瓦, 667000;
    3. 中国科学院华南植物研究所, 广州, 510650
  • 收稿日期:2002-04-28 修回日期:2002-11-02 出版日期:2003-04-10

A new method to distinguish soil types based on functional ecology

YIN Guangcai1, A S Kerzhentcef2, V V Bugrovskiy3, ZHOU Guoyi1, WEN Dazhi 1   

  1. 1. South China Institute of Botany, Chinese Academy of Sciences, Guangzhou, 510650, China;
    2. The Institute of Basic Biology for Fundamental Problems, Pushchino, Russian Cademy of Sciences, Moscow Region 142290, Russia;
    3. Uvs Noor International Biological Center for Biosphere Research, Russian Academy of Sciences, Kyzyl, Tuva 667000, Russia
  • Received:2002-04-28 Revised:2002-11-02 Online:2003-04-10

摘要: 借助功能生态学的理论,提出了运用土壤的特征物质(CM)和特征时间(CT)区分土壤类型的新方法。通过数学模拟,分别计算了灰色森林土和黑钙土的特征物质和特征时间 :当灰色森林土和黑钙土的年凋落物量分别为 5.5t·hm-2 和 11.2t·hm-2 时,它们的CM和CT分别为 133t·hm-2 、80年和 820t·hm-2 、650年。CM和CT的值随着输入土壤的物质量和土壤中分解速度的变化而变化,而且受外界环境因素(包括自然因素和人为因素)的影响。CT随土壤深度的增加而增大

关键词: 径流小区, 迁移参数, 空间变异

Abstract: Based on the theory of functional ecology, a new method for distinguishing soil types according to its characteristic mass(CM)and characteristic time(CT)was presented. By mathematical modeling, the CM and CT of Soddy-podzodsand Cherro zem was calculated as the orders of 133 t穐m-2 and 80 years with an annual litter-fall mass about 5.5 t穐m-2 for Soddy podzods, and 820 t穐m-2, 650 years with an annual litter-fall mass 11.2 t穐m-2 for the Cherro zem. Further more, the CM and CT varied with the change of mass input and decomposed velocity in the soil, which are influenced by the external factors(light, temperature, moisture etc.)and anthropologic factors. We also found that the lower the horizon was, the longer the CT would be.

Key words: Runoff plot, Transport parameters, Spatial variability

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