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温度和水分对草甸草原土壤氧化亚氮产生速率的调控
引用本文:杜睿. 温度和水分对草甸草原土壤氧化亚氮产生速率的调控[J]. 应用生态学报, 2006, 17(11): 2170-2174
作者姓名:杜睿
作者单位:中国科学院大气物理研究所,北京,100029
基金项目:国家自然科学基金;中国科学院科研基金
摘    要:通过试验室模拟试验,研究了调控草甸草原黑钙土N2O产生速率的因素.结果表明,土壤水分对草甸草原土壤N2O产生速率有重要影响(F=6.149,P<0.01).但相关性分析表明,草甸草原土壤含水量与N2O的产生速率间线性相关不显著.就土壤N2O的产生速率而言,温度的影响远低于土壤水分的影响(F=2.275,P=0.106).土壤水分和温度对不同生长阶段的草甸草原土壤N2O产生速率的调控作用主要表现为阶段性的多阶多项式关系:y=ax3+bx2+cx+d,其中a、b、c、d是常数.

关 键 词:N2O产生速率  土壤水分  温度  多阶多项式
文章编号:1001-9332(2006)11-2170-05
收稿时间:2005-09-06
修稿时间:2006-03-28

Effects of soil moisture and temperature on N2O production rate of meadow grassland soil
DU Rui. Effects of soil moisture and temperature on N2O production rate of meadow grassland soil[J]. The journal of applied ecology, 2006, 17(11): 2170-2174
Authors:DU Rui
Affiliation:Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
Abstract:With incubation test, this paper studied the effects of soil moisture and temperature on the N_2O production rate of meadow grassland chernozem in Inner Mongolia. The results showed that soil moisture had a significant effect on the N_2O production rate, with a non-linear relationship between them. Soil temperature had less effect than soil moisture. Their effects on the test soil N_2O production rate at different growth stages could be described as a multi-order polynomial relationship y=ax~3+bx~2+cx+d, where a, b, c and d were the constants.
Keywords:N2O production rate   Soil moisture   Temperature   Multi-order polynomial relationship.
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