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温度和水分对华中地区菜地土壤氮素矿化的影响

赵长盛 胡承孝 孙学成 黄魏

中国生态农业学报2012,Vol.20Issue(7):861-866,6.
中国生态农业学报2012,Vol.20Issue(7):861-866,6.DOI:10.3724/SP.J.1011.2012.00861

温度和水分对华中地区菜地土壤氮素矿化的影响

Influence of temperature and moisture on nitrogen mineralization in vegetable fields of central China

赵长盛 1胡承孝 1孙学成 1黄魏1

作者信息

  • 1. 华中农业大学资源与环境学院 华中农业大学微量元素研究中心 武汉 430070
  • 折叠

摘要

Abstract

The processes of nitrogen (N) mineralization was determined in order to establish reasonable N application in vegetable fields in central China. The study researched the influence of temperature and water on N mineralization in two typical vegetable soils (yellow-brown and fluvo-aquic soils) in an indoor cultivation experiment. The results indicated that mineralization and am-monification rates in yellow-brown soils increased with increasing temperature. While nitrification rate at 15% and 25% water contents increased with increasing temperature, it decreased with increasing temperature at 35% water content. At 15% water content, mineralization rate of fluvo-aquic soil increased with increasing temperature. At 25% and 35% water contents, however, mineralization rate initially increased and then decreased. Nitrification rate in fluvo-aquic soil increased with increasing temperature at 15% and 35% water content At 25% water content, however, it initially increased then decreased. Ammonification rate generally decreased with increasing temperature. At 25% water content and 35 ℃, mineralization rate in yellow-brown soil was 34.9 mg·kg-1. Also at 25% water content and 25℃, mineralization in the same soil was 63.9 mg·kg-1. Under different temperature conditions, mineralization rate of fluvo-aquic soil was higher than that of yellow-brown soil. While ammonification rate of yellow-brown soil increased with increasing water content, the reverse was true for nitrification rate. The maximum mineralization rate was at 25% water content. Variations in ammonification, nitrification and mineralization rate with water content in fluvo-aquic soil were not so evident. It was noted that the critical moisture content for microbial activity in yellow-brown soil was 25%, and that in fluvo-aquic soil was not evident. The functional relationship of nitrogen mineralization rate with water content and temperature condition in yellow-brown soil was more significant than that in fluvo-aquic soil.

关键词

潮土/黄棕壤/矿化速率/硝化速率/氨化速率/含水量/温度

Key words

Fluvo-aquic soil, Yellow-brown soil, Mineralization rate, Nitrification rate, Ammonification rate, Soil moisture, Temperature

分类

农业科技

引用本文复制引用

赵长盛,胡承孝,孙学成,黄魏..温度和水分对华中地区菜地土壤氮素矿化的影响[J].中国生态农业学报,2012,20(7):861-866,6.

基金项目

农业部“948”项目(2003-z54,2008-Z25)资助 (2003-z54,2008-Z25)

中国生态农业学报

OA北大核心CSCDCSTPCD

2096-6237

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