氰酸盐
化学
分解
动力学
动能
尿素
降水
化学分解过程
无机化学
热分解
水解
大气温度范围
离子
水溶液中的金属离子
金属
化学分解
热力学
高分子化学
有机化学
物理
量子力学
气象学
作者
Bora Mavış,Müfit Akinç
标识
DOI:10.1111/j.1551-2916.2005.00758.x
摘要
The literature on kinetics of the urea decomposition reaction was reviewed for the 333–373 K range of temperature. Possible reactions in the pH range of 5–9 were identified. Kinetic simulations indicated significant accumulation of the cyanate intermediate in the pH‐time–temperature range that was studied. The effects of Ni 2+ hydrolysis and complexation with the urea decomposition products were incorporated into the simulations. The kinetic simulation of the rate of Ni 2+ removal from the solutions was compared against the experimental data. The experimental results indicated an agglomerative growth mechanism for the precipitation process. Chemical analyses showed that the composition of the precipitate varies with digestion time, in agreement with the predictions of the kinetic simulation.
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