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首页> 外文期刊>Oxidation Communications >DYNAMIC HEAT OF ADSORPTION OF WATER VAPOUR ON ZEOLITIC TUFF AND ZEOLITE 4A BY FLOW MICROCALORIMETRY
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DYNAMIC HEAT OF ADSORPTION OF WATER VAPOUR ON ZEOLITIC TUFF AND ZEOLITE 4A BY FLOW MICROCALORIMETRY

机译:流动微量热法测定沸石絮和4A沸石对水蒸气的动态吸附热。

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摘要

In this study a practical method for measurement of heat of adsorption of water vapour on adsorbents was developed to evaluate the feasibility of substitution of a zeolitic tuff with zeolite 4A in air drying and heat pumps.The change of heat of adsorption with inlet humidity of the air passing through the calorimeter was investigated.Samples were characterised by X-ray diffraction and thermal gravimetric analysis techniques.Specific heats of the zeolitic tuff and zeolite 4A were measured as 1.01 and 1.42 J/g K, respectively.Adsorption isotherms fitted to the Langmuir model with regression coefficient 0.93 and 0.94 with monolayer capacities, X_m 9.68% and 26.35% H_2O for the zeolitic tuff and zeolite 4A, respectively.The energy storage intensity was measured in the range 48-97 J/g and 464-201 J/g for the tuff and zeolite 4A, respectively.Heat of adsorption of zeolite decreased with surface coverage and it was in the range 1750-2835 and 1104-2640 J/g H_2O for the zeolitic tuff and zeolite 4A, respectively.
机译:在这项研究中,开发了一种实用的方法来测量水蒸气在吸附剂上的吸附热,以评估在空气干燥和热泵中用4A沸石代替沸石凝灰岩的可行性。用X射线衍射和热重分析技术对样品进行了表征,测得沸石凝灰岩和4A沸石的比热分别为1.01和1.42 J / g K,Langmuir上的吸附等温线具有单层容量的回归系数0.93和0.94的模型,沸石凝灰岩和4A沸石的X_m分别为9.68%和26.35%H_2O。储能强度的测量范围为48-97 J / g和464-201 J / g凝灰岩和沸石4A的吸附热随表面覆盖率的降低而降低,沸石凝灰岩和沸石的吸附热在1750-2835和1104-2640 J / g H_2O范围内。 e分别为4A。

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