author_facet Becker, H. A.
Becker, H. A.
author Becker, H. A.
spellingShingle Becker, H. A.
Canadian Journal of Chemistry
AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
Organic Chemistry
General Chemistry
Catalysis
author_sort becker, h. a.
spelling Becker, H. A. 0008-4042 1480-3291 Canadian Science Publishing Organic Chemistry General Chemistry Catalysis http://dx.doi.org/10.1139/v58-208 <jats:p> It is shown that the moisture desorption isotherm of wheat can be interpreted in harmony with Cassie's theoretical assumptions regarding adsorption on localized sites by the equation[Formula: see text]where N is the number of adsorbed molecules per gram of wheat and S is the number of localized sites. Kf/(1 + Kf) is a Langmuir-type factor for adsorption of the low energy fraction of molecules, and K′f<jats:sup>n</jats:sup> is a factor for adsorption of the normally condensed fraction of molecules. In agreement with theory K′,n,and S are independent of temperature. The dependence of K on temperature gives a value of −6.27 kcal/mole for the partial molal enthalpy of dilution of the low energy fraction of molecules, which is in the order of magnitude of a hydrogen bond. The analysis also illuminates the practice of the drying of wheat. An exact correspondence appears to exist between the calculated values of S and the apparent surface (or equilibrium) moistures observed in studying the diffusion of moisture out of wheat. The theoretical relation[Formula: see text]is therefore given for predicting apparent surface moisture contents in the vacuum drying of wheat, where[Formula: see text] </jats:p> AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT Canadian Journal of Chemistry
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series Canadian Journal of Chemistry
source_id 49
title AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_unstemmed AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_full AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_fullStr AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_full_unstemmed AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_short AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_sort an interpretation of the moisture desorption isotherm of wheat
topic Organic Chemistry
General Chemistry
Catalysis
url http://dx.doi.org/10.1139/v58-208
publishDate 1958
physical 1416-1423
description <jats:p> It is shown that the moisture desorption isotherm of wheat can be interpreted in harmony with Cassie's theoretical assumptions regarding adsorption on localized sites by the equation[Formula: see text]where N is the number of adsorbed molecules per gram of wheat and S is the number of localized sites. Kf/(1 + Kf) is a Langmuir-type factor for adsorption of the low energy fraction of molecules, and K′f<jats:sup>n</jats:sup> is a factor for adsorption of the normally condensed fraction of molecules. In agreement with theory K′,n,and S are independent of temperature. The dependence of K on temperature gives a value of −6.27 kcal/mole for the partial molal enthalpy of dilution of the low energy fraction of molecules, which is in the order of magnitude of a hydrogen bond. The analysis also illuminates the practice of the drying of wheat. An exact correspondence appears to exist between the calculated values of S and the apparent surface (or equilibrium) moistures observed in studying the diffusion of moisture out of wheat. The theoretical relation[Formula: see text]is therefore given for predicting apparent surface moisture contents in the vacuum drying of wheat, where[Formula: see text] </jats:p>
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author Becker, H. A.
author_facet Becker, H. A., Becker, H. A.
author_sort becker, h. a.
container_issue 10
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container_title Canadian Journal of Chemistry
container_volume 36
description <jats:p> It is shown that the moisture desorption isotherm of wheat can be interpreted in harmony with Cassie's theoretical assumptions regarding adsorption on localized sites by the equation[Formula: see text]where N is the number of adsorbed molecules per gram of wheat and S is the number of localized sites. Kf/(1 + Kf) is a Langmuir-type factor for adsorption of the low energy fraction of molecules, and K′f<jats:sup>n</jats:sup> is a factor for adsorption of the normally condensed fraction of molecules. In agreement with theory K′,n,and S are independent of temperature. The dependence of K on temperature gives a value of −6.27 kcal/mole for the partial molal enthalpy of dilution of the low energy fraction of molecules, which is in the order of magnitude of a hydrogen bond. The analysis also illuminates the practice of the drying of wheat. An exact correspondence appears to exist between the calculated values of S and the apparent surface (or equilibrium) moistures observed in studying the diffusion of moisture out of wheat. The theoretical relation[Formula: see text]is therefore given for predicting apparent surface moisture contents in the vacuum drying of wheat, where[Formula: see text] </jats:p>
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spelling Becker, H. A. 0008-4042 1480-3291 Canadian Science Publishing Organic Chemistry General Chemistry Catalysis http://dx.doi.org/10.1139/v58-208 <jats:p> It is shown that the moisture desorption isotherm of wheat can be interpreted in harmony with Cassie's theoretical assumptions regarding adsorption on localized sites by the equation[Formula: see text]where N is the number of adsorbed molecules per gram of wheat and S is the number of localized sites. Kf/(1 + Kf) is a Langmuir-type factor for adsorption of the low energy fraction of molecules, and K′f<jats:sup>n</jats:sup> is a factor for adsorption of the normally condensed fraction of molecules. In agreement with theory K′,n,and S are independent of temperature. The dependence of K on temperature gives a value of −6.27 kcal/mole for the partial molal enthalpy of dilution of the low energy fraction of molecules, which is in the order of magnitude of a hydrogen bond. The analysis also illuminates the practice of the drying of wheat. An exact correspondence appears to exist between the calculated values of S and the apparent surface (or equilibrium) moistures observed in studying the diffusion of moisture out of wheat. The theoretical relation[Formula: see text]is therefore given for predicting apparent surface moisture contents in the vacuum drying of wheat, where[Formula: see text] </jats:p> AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT Canadian Journal of Chemistry
spellingShingle Becker, H. A., Canadian Journal of Chemistry, AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT, Organic Chemistry, General Chemistry, Catalysis
title AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_full AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_fullStr AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_full_unstemmed AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_short AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
title_sort an interpretation of the moisture desorption isotherm of wheat
title_unstemmed AN INTERPRETATION OF THE MOISTURE DESORPTION ISOTHERM OF WHEAT
topic Organic Chemistry, General Chemistry, Catalysis
url http://dx.doi.org/10.1139/v58-208