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The adsorption heat of methane on coal: Comparison of theoretical and calorimetric heat and model of heat flow by microcalorimeter

机译:甲烷在煤上的吸附热:理论量热和热量热的比较以及微热量计的热流模型

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摘要

Various methods have been proposed to determine the heat of adsorption indirectly from adsorption isotherms or directly through calorimeter, whereas authors rarely compared different models for calculating isosteric heat of methane adsorption on coal and seldom studied adsorption thermodynamics related to calorimetric heat flux. In this work, for better probing thermodynamics of adsorption of methane on coal, seeking a reliable model to describe adsorption heat, and predicting the adsorption heat at given temperatures and pressures from heat flow, isothermal adsorption experiments of methane on anthracite at temperatures of 298 K, 308 K and 318 K were conducted, with both calorimetric and volumetric method. The calorimetric results indicate that isosteric heat decreases with the increase of adsorption capacity and temperature. Then the calorimetric heat was compared with the isosteric heat using four adsorption models, in the fitness sequence of D-A Toth C-C Virial. To be noted that the heat flux measured calorimetrically increases to the crest rapidly, then gradually decreases to the initial state. This tendency is proposed to be described by the exponential function with the fitting parameters estimated by empirical formulas proposed. The predicted heat flows were thus acquired, agreeing well with the experimental data except for the low coverage or pressure stage. Furthermore, it is revealed that the temperature evolution of adsorption can also be expressed by an exponential-like polynomial solution, induced from the proposed thermal flux prediction model based on the Tian's equation.
机译:已经提出了多种方法来间接地通过吸附等温线或直接通过量热法确定吸附热,而作者很少比较用于计算甲烷在煤上的甲烷等排热的不同模型,并且很少研究与量热通量有关的吸附热力学。在这项工作中,为了更好地探测甲烷在煤上的吸附热力学,寻求一个可靠的模型来描述吸附热,并在给定温度和压力下根据热流预测吸附热,在298 K温度下无烟煤上甲烷的等温吸附实验分别用量热法和体积法进行了308 K和318 K的测定。量热结果表明,随着吸附容量和温度的升高,等排热降低。然后使用四种吸附模型将比色热与等容热进行比较,其适应度顺序为D-A> Toth> C-C> Virial。要注意的是,量热法测得的热通量迅速增加到波峰,然后逐渐减少到初始状态。建议用指数函数描述这种趋势,并用建议的经验公式估算拟合参数。因此获得了预测的热流,除了覆盖率低或压力低以外,与实验数据非常吻合。此外,揭示了吸附的温度演化也可以由拟议的基于田氏方程的热通量预测模型导出的指数式多项式解来表示。

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