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应用生态学报 ›› 2002, Vol. ›› Issue (11): 1495-1498.

• 研究论文 • 上一篇    下一篇

有机胶结形成土壤团聚体的机理及理论模型

史奕, 陈欣, 沈善敏   

  1. 中国科学院沈阳应用生态研究所陆地生态过程重点实验室, 沈阳, 110016
  • 收稿日期:2001-05-08 修回日期:2002-01-11
  • 通讯作者: 史奕,女,1961年生,在职博士,副研究员,主要从事土壤特征有机物质及对全球变化的响应研究,发表论文20余篇.E-mail:Shiyi@iae.ac.cn
  • 基金资助:
    国家重点基础研究发展规划资助项目(G1999011804).

SHI Yi, CHEN Xin, SHEN Shanmin   

  1. Key Laboratory of Terrestrial Ecological Process, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016
  • Received:2001-05-08 Revised:2002-01-11

摘要: 土壤团聚体是土壤结构的基本单位,其组成和稳定性直接影响土壤肥力和农作物的生长.对于有机质含量高的黑土,有机胶结物质是形成土壤团聚体的主要因素.在综合有机胶结剂和土壤团聚体的研究的基础上,阐述了有机胶结物质的特性,土壤生物和植物根系在土壤团聚体形成中的作用,土壤团聚体形成的机理及理论模型.

关键词: 有机胶结物质, 土壤团聚体, 理论模型, 磷酸双酯酶, 土壤磷, 微生物生物量磷, 酸性磷酸单酯酶

Abstract: Soil aggregate is the basic unit of soil structure, and its formation and stabilization has direct effect on soil fertility and crop growth.For black soil with high content of organic matter,organic cementing substance is an important factor in forming soil aggregates.Based on the recent researches on organic cementing agents,this paper was focused on the nature of organic cementing substances,the effect of soil organisms and plant roots in forming soil aggregates,and the theoretical models and stable mechanisms of soil aggregate formation.

Key words: acid phosphomonoesterase, microbial biomass phosphorus, soil phosphorus, phosphodiesterase

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