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TEMPERATURE DEPENDENCE OF NITROGEN MINERALIZATION RATE CONSTANT - A THEORETICAL APPROACH

机译:氮矿化速率常数的温度依赖性-一种理论方法

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Experimental evidence suggests that nitrogen (N) mineralization proceeds differently under fluctuating temperature conditions than it does at constant temperature. Although N mineralization is believed to follow first-order kinetics, and the mineralization rate constant is believed to follow Q(10) temperature dependence, no effort has been made to use this information to predict the effect of fluctuating temperature on N mineralization. In this paper, we present solutions to the first-order N mineralization equation for a rate coefficient with Q(10) temperature dependence. Solutions are presented for a number of simple patterns of temperature fluctuation in time. Example calculations show that the nonlinear temperature dependence of the Q(10) relationship causes mineralization under fluctuating temperature conditions to exceed that occurring at constant temperature. Sensitivity analysis shows that the Q(10) constant and the amplitude of the temperature fluctuation strongly influence the difference in mineralization obtained for the two temperature patterns. These results can be used to improve the design of experiments conducted to study the effect of temperature fluctuations.
机译:实验证据表明,在不断变化的温度条件下,氮(N)的矿化过程与在恒定温度下不同。尽管N矿化被认为遵循一级动力学,并且矿化速率常数被认为遵循Q(10)温度依赖性,但尚未做出任何努力来使用此信息来预测温度波动对N矿化的影响。在本文中,我们提出了与Q(10)温度相关的速率系数的一阶N矿化方程的解。提出了一些简单的温度随时间波动的解决方案。示例计算表明,Q(10)关系的非线性温度依赖性导致在波动的温度条件下的矿化超过在恒温条件下的矿化。敏感性分析表明,Q(10)常数和温度波动幅度强烈影响两种温度模式获得的矿化差异。这些结果可用于改进为研究温度波动的影响而进行的实验的设计。

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