Kinetics of Water Sorption on a CaCl2-in-Silica-Gel-Pores Sorbent: The Effects of the Pellet Size and Temperature Научная публикация
Журнал |
Kinetics and Catalysis
ISSN: 0023-1584 , E-ISSN: 1608-3210 |
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Вых. Данные | Год: 2006, Том: 47, Номер: 5, Страницы: 770-775 Страниц : 6 DOI: 10.1134/S002315840605017X | ||||
Ключевые слова | Effective Diffusivity; Kinetic Curf; Water Sorption; Water Vapor Pressure; Sorption Rate | ||||
Авторы |
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Организации |
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Информация о финансировании (4)
1 | Российский фонд фундаментальных исследований | 05-02-16953 |
2 | Российский фонд фундаментальных исследований | 05-03-34762 |
3 | Российский фонд фундаментальных исследований | 03-02-39017 |
4 | Ассоциация «Глобальная энергия» | MG-2005/04/3 |
Реферат:
Kinetics of water vapor sorption on the CaCl2-in-KSK-pores composite (SWS-1L) have been studied at T = 33–69°C and vapor pressures of 8–70 mbar for pellet sizes of 2R pel = 0.355–0.425, 0.71–0.85, and 1.2–1.4 mm. Sorption has been measured under isothermal conditions on a thermobalance by abruptly raising the vapor pressure in the measurement cell by a small value and then maintaining the new pressure. In the initial portion of the kinetic curves, the amount of sorbed water (Δm) increases in proportion to the sorption time (t) to the power 1/2. From the slope of the Δm versus t 1/2 curve, it is possible to derive the sorption rate constant k D = D eff/R 2 pel and the effective diffusivity D eff. The latter is independent of R pel for 2R pel ≥ 0.71 mm. The rate of water sorption on smaller (0.355-to 0.425-mm) pellets grows less rapidly, apparently because of the effect of the heat of sorption. The effective diffusivity is determined by the local slope of the water vapor sorption isotherm for SWS-1L. Applying an appropriate correction enables one to calculate the effective diffusivity for water vapor in the sorbent pores, which appears to be D e = (0.35 ± 0.17) × 10−6 m2/s. This value is approximately 10 times smaller than the Knudsen water diffusion coefficient calculated for a single cylindrical pore with a size equal to the average pore size of the composite. Two possible causes of this discrepancy are discussed, specifically, an increase in the pore tortuosity because of the presence of the salt and the interaction between water and the salt.
Библиографическая ссылка:
Aristov Y.I.
, Glaznev I.S.
, Freni A.
, Restuccia G.
Kinetics of Water Sorption on a CaCl2-in-Silica-Gel-Pores Sorbent: The Effects of the Pellet Size and Temperature
Kinetics and Catalysis. 2006. V.47. N5. P.770-775. DOI: 10.1134/S002315840605017X WOS Scopus РИНЦ
Kinetics of Water Sorption on a CaCl2-in-Silica-Gel-Pores Sorbent: The Effects of the Pellet Size and Temperature
Kinetics and Catalysis. 2006. V.47. N5. P.770-775. DOI: 10.1134/S002315840605017X WOS Scopus РИНЦ
Оригинальная версия:
Аристов Ю.И.
, Глазнев И.С.
, Френи А.
, Рестучча Д.
Кинетика поглощения паров воды сорбентом "CaCl2 в порах силикагеля": влияние размера гранул и температуры
Кинетика и катализ. 2006. Т.47. №5. С.793-798. RSCI РИНЦ
Кинетика поглощения паров воды сорбентом "CaCl2 в порах силикагеля": влияние размера гранул и температуры
Кинетика и катализ. 2006. Т.47. №5. С.793-798. RSCI РИНЦ
Даты:
Поступила в редакцию: | 10 февр. 2005 г. |
Опубликована в печати: | 1 сент. 2006 г. |
Идентификаторы БД:
Web of science | WOS:000241045200017 |
Scopus | 2-s2.0-33749411545 |
РИНЦ | 13517728 |
Chemical Abstracts | 2006:1026909 |
Chemical Abstracts (print) | 145:461069 |
OpenAlex | W2044139295 |