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温度对厌氧条件下不同pH水稻土氮素矿化的影响

曹竞雄 韦梦 陈孟次 包秀玲 裘琼芬

中国生态农业学报Issue(10):1182-1189,8.
中国生态农业学报Issue(10):1182-1189,8.DOI:10.13930/j.cnki.cjea.140249

温度对厌氧条件下不同pH水稻土氮素矿化的影响

Effects of temperature on soil nitrogen mineralization in different pH paddy soils under anaerobic condition

曹竞雄 1韦梦 1陈孟次 1包秀玲 1裘琼芬1

作者信息

  • 1. 宁波大学海洋学院 宁波 315211
  • 折叠

摘要

Abstract

Nitrogen mineralization has been one of the most important links of nitrogen cycle in soil ecosystems. Temperature and pH are important environmental factors influencing nitrogen mineralization. In this study, two paddy soils with different pH values were used to anaerobically incubate at four different temperatures-15 ℃, 25 ℃, 37 ℃ and 50 ℃. Using the first order reaction kinetics equation in combination with the effective accumulated temperature equation, mineralization parameters such as soil nitrogen mineralization potential (N0), mineralization rate (k), mineralization degree (ka) and potential/total nitrogen mineralization rate (N0/Tot.N) were analyzed in order to determine the impact of temperature on soil nitrogen mineralization under anaerobic condition. The results showed that soil nitrogen mineralization potential (N0) of two paddy soils increased with increasing temperature. The changes in k and ka depended on temperature degrees of soils with different nitrogen mineralization potentials. At 15-37 ℃, soil k and ka increased with increasing temperature. However, the differences between every two soils were not significant at the same temperature. Then within 37-50 ℃, the changes in soil k and ka grew significantly (P<0.01) different with increasing temperatures in different soils. It suggested that at high temperatures, the effect of temperature on the mineralization of different paddy soils changed greatly. N0/Tot. N increased with increasing temperatures, suggesting that the quality of organic nitrogen improved at higher temperatures. Correlation analysis showed a positive correlation between temperature and mineralization parameters within the range of 15-37 ℃. Within the range of 37-50 ℃, the correlation decreased and some even became negative. The pH values did not fluctuate or change with the mineralization parameters. This implied that under anaerobic condition, the&nbsp;response of nitrogen mineralization of soils with different pH was similar to temperature within low to medium temperatures, but was significantly different at high temperatures.

关键词

氮矿化/一级动力方程式/有效积温式/厌氧条件/土壤pH

Key words

Nitrogen mineralization/First order reaction kinetics equation/Effective accumulated temperature equation/Anaerobic condition/Soil pH

分类

农业科技

引用本文复制引用

曹竞雄,韦梦,陈孟次,包秀玲,裘琼芬..温度对厌氧条件下不同pH水稻土氮素矿化的影响[J].中国生态农业学报,2014,(10):1182-1189,8.

基金项目

国家自然科学基金项目(41101234)资助 (41101234)

中国生态农业学报

OA北大核心CSCDCSTPCD

2096-6237

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