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Kinetic and thermodynamic effects of moisture content and temperature on the ammonia volatilization of soil fertilized with urea

机译:水分和温度对尿素施肥土壤氨挥发的动力学和热力学影响

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The traditional qualitative analysis of the individual factors on the kinetic and thermodynamic parameters cannot sufficiently reveal the mechanism underlying ammonia volatilization in soil. This study aimed to determine the effects of temperature, moisture content, and their interaction on the kinetic and thermodynamic parameters, which revealed the key control mechanism underlying ammonia volatilization, modified the traditional Arrhenius model, and established a quantitative prediction model of cumulative NH3-N loss (CNL). Laboratory culture experiments were conducted under different temperatures (T) (15°C, 20°C, 25°C and 35°C) and moisture contents (θ) (60%, 80%, and 100% field capacities). Soil ammonia volatilization was also measured every 2 d. Results showed that the effects of individual factors and their interaction on the values of reaction rate (KN), Activation free energy (ΔG), and activation entropy (ΔS) followed the descending order of T>θ>T×θ, whereas those of activation enthalpy (ΔH) and activation degree (lgN) followed the descending order of θ>T>T×θ. The interaction showed significant effect on KN value and insignificant effect on all the thermodynamic parameters. The effects of water and temperature were mainly observed during the preparatory stage and the most critical transition state stage of the chemical reaction, respectively. Given that ΔH > 0, ΔG > 0, and ΔS > 0, ammonia volatilization is found to be an endothermic reaction controlled by enthalpy. The new KN(T)-2 model with the determination coefficient (R2) of 0.999 was more accurate than the traditional Arrhenius model with the R2 of 0.936. The new NH3(T, θ) model with the mean absolute percentage error (MAPE) of 4.17% was more accurate than the traditional NH3(T) model with the MAPE of 7.11%. These results supplemented the control mechanism underlying ammonia volatilization in soil fertilized with urea and improved the prediction accuracy of CNL. Keywords: soil ammonia volatilization, kinetic parameters, thermodynamic parameters, soil moisture content, urea fertilizer, Arrhenius model, NH3(T, θ) model DOI: 10.25165/j.ijabe.20171006.3232 Citation: Lei T, Guo X H, Ma J J, Sun X H, Feng Y, Wang H Y. Kinetic and thermodynamic effects of moisture content and temperature on the ammonia volatilization of soil fertilized with urea. Int J Agric & Biol Eng, 2017; 10(6): 134–143.
机译:传统的动力学和热力学参数个体定性分析不能充分揭示土壤中氨挥发的机理。这项研究旨在确定温度,水分含量及其相互作用对动力学和热力学参数的影响,从而揭示了氨挥发的关键​​控制机制,修改了传统的Arrhenius模型,并建立了累积NH3-N的定量预测模型。损失(CNL)。在不同温度(T)(15°C,20°C,25°C和35°C)和水分含量(θ)(60%,80%和100%田间持水量)下进行实验室培养实验。每2天也测量一次土壤氨气挥发。结果表明,各个因素及其相互作用对反应速率(KN),活化能(ΔG)和活化熵(ΔS)值的影响遵循T>θ> T×θ的降序排列,而活化焓(ΔH)和活化度(lgN)遵循θ> T> T×θ的降序。相互作用对KN值显示显着影响,而对所有热力学参数影响不显着。水和温度的影响主要分别在化学反应的准备阶段和最关键的过渡态阶段观察到。给定ΔH> 0,ΔG> 0和ΔS> 0,则发现氨挥发是受焓控制的吸热反应。测定系数(R2)为0.999的新KN(T)-2模型比R2为0.936的传统Arrhenius模型更准确。平均绝对百分比误差(MAPE)为4.17%的新NH3(T,θ)模型比MAPE为7.11%的传统NH3(T)模型更准确。这些结果补充了尿素施肥土壤中氨挥发的控制机理,并提高了CNL的预测准确性。关键词:土壤氨气挥发,动力学参数,热力学参数,土壤含水量,尿素肥料,Arrhenius模型,NH3(T,θ)模型DOI:10.25165 / j.ijabe.20171006.3232引用:雷婷,郭晓红,马继杰XH,冯Y,王慧英。水分含量和温度对尿素施肥土壤氨挥发的动力学和热力学影响。国际农业与生物工程杂志,2017; 10(6):134–143。

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