土壤氮素矿化的生态模型研究

应用生态学报 ›› 1999, Vol. 10 ›› Issue (1): 114-118.

土壤氮素矿化的生态模型研究

穆兴民¹, 樊小林²

1. 中国科学院2水利部水土保持研究所, 杨陵 712100;
2. 西北农业大学, 杨陵 712100

收稿日期:1996-10-28 修回日期:1997-01-29 出版日期:1999-01-25 发布日期:1999-01-25
通讯作者: 穆兴民,男,1961年生,在职博士,副研究员,土地资源环境研究部副主任.在旱作农业及水土保持领域,从事提高水分生产率的水分生态研究和水土保持的水文生态效应研究.
基金资助:
国家“九五”攻关(962004205212)和中国科学院留学支持基金项目.

A review on ecological models of soil N mineralization

Mu Xingmin¹, Fan Xiaolin²

1. Soil and Water Conservation Institute, Academia Sinica and Ministry of Water Resources, Yangling 712100;
2. Northwest Agricultural University, Yangling 712100

Received:1996-10-28 Revised:1997-01-29 Online:1999-01-25 Published:1999-01-25

摘要/Abstract

摘要： 土壤氮素矿化是反映土壤供氮能力的重要因素之一,也是目前国内外土壤生态学研究热点之一。土壤氮素矿化可表示为土壤有机氮的含量、矿化过程中土壤环境因素和矿化持续时间的复合函数;土壤氮素矿化的基本模型有3类,即动力学模型、热力学模型及经验模型;影响矿化过程并可定量表示的土壤环境条件如土壤温度、湿度、pH及有机质形态。

关键词: 土壤有机氮, 矿化, 模型

Abstract: The mineralization of soil organic nitrogen is one of the most important factors reflecting soil nitrogen-supply capability and one of the hot subjects of soil ecology in home and abroad, which could be referred as a function of soil organic content, duration of its mineralization, and soil environmental factors affecting the process of mineralization. There are three basic model types of soil nitrogen mineralization, namely, the kinetic, thermodynamic and empirical types. Soil temperature, moisture, pH and organic N forms are the soil environmental elements which impact the mineralization process and could be quantified.

Key words: Soil organic nitrogen, Mineralization, Model

穆兴民, 樊小林. 土壤氮素矿化的生态模型研究[J]. 应用生态学报, 1999, 10(1): 114-118.

Mu Xingmin, Fan Xiaolin . A review on ecological models of soil N mineralization[J]. Chinese Journal of Applied Ecology, 1999, 10(1): 114-118.

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