Analysis of Isotope Separation Factor for Adsorption of Tracer-HTO/Bulk-H2O on Cobalt Complex [Co (en) 3] Cl3 Based on Ideal Adsorbed Solution Theory
The isotope separation factor for adsorption of tracer-HTO/bulk-H2Oon tris (ethylenediamine) cobalt complex [Co (en) 3] Cl3is analyzed in accordance with the ideal adsorbed solution theory by using the isotherms for pure-component adsorption ofH2OandD2O.It has been studied that the isotherms are com...
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Published in | RADIOISOTOPES Vol. 47; no. 3; pp. 197 - 205 |
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Main Authors | , , |
Format | Journal Article |
Language | Japanese |
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Japan Radioisotope Association
15.03.1998
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Abstract | The isotope separation factor for adsorption of tracer-HTO/bulk-H2Oon tris (ethylenediamine) cobalt complex [Co (en) 3] Cl3is analyzed in accordance with the ideal adsorbed solution theory by using the isotherms for pure-component adsorption ofH2OandD2O.It has been studied that the isotherms are composite which result from two types of adsorption of water molecules on primary and secondary coordination sites in the complex crystal. The separation factorβshows two of high and low plateaus which respectively correspond to the primary adsorption where the equilibrium pressure exhibits a plateau and the secondary adsorption where the pressure rises up to the saturated vapor pressure. The high plateauβis larger thanα, the relative volatility ofH2OtoHTO.On the other hand, the low plateauβis smaller thanα.In this paper, approximate equations are presented for estimating the plateausβwith respect to temperature. |
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AbstractList | The isotope separation factor for adsorption of tracer-HTO/bulk-H2Oon tris (ethylenediamine) cobalt complex [Co (en) 3] Cl3is analyzed in accordance with the ideal adsorbed solution theory by using the isotherms for pure-component adsorption ofH2OandD2O.It has been studied that the isotherms are composite which result from two types of adsorption of water molecules on primary and secondary coordination sites in the complex crystal. The separation factorβshows two of high and low plateaus which respectively correspond to the primary adsorption where the equilibrium pressure exhibits a plateau and the secondary adsorption where the pressure rises up to the saturated vapor pressure. The high plateauβis larger thanα, the relative volatility ofH2OtoHTO.On the other hand, the low plateauβis smaller thanα.In this paper, approximate equations are presented for estimating the plateausβwith respect to temperature. |
Author | NAONO, Hiromitu KOTOH, Kenji KUDO, Kazuhiko |
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References | 3) Kotoh, K., Enoeda, M., Matsui, T. and Nishikawa, M.: J. Chem. Eng. Jpn., 26, 355-360 (1993) ; J. Chem. Eng. Jpn., 26, 570-572 (1993 1) Kotoh, K., Naono, H., Hakuman, M. and Shiono, T.: Radioisotopes, 47, (2) , 112-119 (1998 5) Van Hook, W. A.: J. Phys. Chem., 72, 1234-1244 (1968 4) Myers, A. L. and Prausnitz, J. M.: AIChE J., 11, 121-127 (1965) ; Ruthven, D. M.: “Principles of Adsorption and Adsorption Processes”, pp. 70-72, Wiley & Sons, New York (1984) ; Yang, R. T.: “Gas Separation by Adsorption Processes”, pp. 64-67, Butterworths, Boston (1987 2) Kotoh, K., and Nishikawa, M.: Memo. Faculty Eng. Kyushu Univ., 53, 121-138 (1993 |
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SubjectTerms | adsorption adsorption isotherm cobalt complex heavy water ideal adsorbed solution theory isotope separation factor plateau pressure tritiated water water |
Title | Analysis of Isotope Separation Factor for Adsorption of Tracer-HTO/Bulk-H2O on Cobalt Complex [Co (en) 3] Cl3 Based on Ideal Adsorbed Solution Theory |
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