Modeling water sorption in okara soy milk

Moisture sorption isotherms of okara soy milk were determined using the gravimetric method in the range 20 - 50°C. The sorption isotherms exhibited hysteresis along all the water activity range (0.1 - 0.9). The amount of sorbed water increased as the temperature was decreased. The GAB and Halsey mod...

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Detalles Bibliográficos
Publicado: 2000
Materias:
GAB
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07373937_v18_n9_p2091_Garcia
http://hdl.handle.net/20.500.12110/paper_07373937_v18_n9_p2091_Garcia
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spelling paper:paper_07373937_v18_n9_p2091_Garcia2023-06-08T15:44:15Z Modeling water sorption in okara soy milk Desorption GAB Halsey model Isosteric heat Isotherms Soy milk Adsorption isotherms Dairy products Mathematical models Moisture Thermal effects Thermogravimetric analysis Water Arrhenius type equations Halsey model Isosteric heat Okara soy milk Water sorption Desorption Desorption emulsion Food processing liquid-solid separation Moisture sorption isotherms of okara soy milk were determined using the gravimetric method in the range 20 - 50°C. The sorption isotherms exhibited hysteresis along all the water activity range (0.1 - 0.9). The amount of sorbed water increased as the temperature was decreased. The GAB and Halsey models gave a good fit for okara isotherms over the range of water activity 0.1 - 0.9. As temperature increased, GAB k-values increased towards unity where the GAB equation reduces to the BET equation. The influence of temperature on the constants of GAB and Halsey models was evaluated through Arrhenius-type equations. The Clausius Clapeyron equation was used to estimate the isosteric heats of sorption. Moisture sorption isotherms of okara soy milk were determined using the gravimetric method in the range 20 - 50 °C. The sorption isotherms exhibited hysteresis along all the water activity range (0.1 - 0.9). The amount of sorbed water increased as the temperature was decreased. The GAB and Halsey models gave a good fit for okara isotherms over the range of water activity 0.1 - 0.9. As temperature increased, GAB k-values increased towards unity where the GAB equation reduces to the BET equation. The influence of temperature on the constants of GAB and Halsey models was evaluated through Arrhenius-type equations. The Clausius Clapeyron equation was used to estimate the isosteric heats of sorption. 2000 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07373937_v18_n9_p2091_Garcia http://hdl.handle.net/20.500.12110/paper_07373937_v18_n9_p2091_Garcia
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Desorption
GAB
Halsey model
Isosteric heat
Isotherms
Soy milk
Adsorption isotherms
Dairy products
Mathematical models
Moisture
Thermal effects
Thermogravimetric analysis
Water
Arrhenius type equations
Halsey model
Isosteric heat
Okara soy milk
Water sorption
Desorption
Desorption
emulsion
Food processing
liquid-solid separation
spellingShingle Desorption
GAB
Halsey model
Isosteric heat
Isotherms
Soy milk
Adsorption isotherms
Dairy products
Mathematical models
Moisture
Thermal effects
Thermogravimetric analysis
Water
Arrhenius type equations
Halsey model
Isosteric heat
Okara soy milk
Water sorption
Desorption
Desorption
emulsion
Food processing
liquid-solid separation
Modeling water sorption in okara soy milk
topic_facet Desorption
GAB
Halsey model
Isosteric heat
Isotherms
Soy milk
Adsorption isotherms
Dairy products
Mathematical models
Moisture
Thermal effects
Thermogravimetric analysis
Water
Arrhenius type equations
Halsey model
Isosteric heat
Okara soy milk
Water sorption
Desorption
Desorption
emulsion
Food processing
liquid-solid separation
description Moisture sorption isotherms of okara soy milk were determined using the gravimetric method in the range 20 - 50°C. The sorption isotherms exhibited hysteresis along all the water activity range (0.1 - 0.9). The amount of sorbed water increased as the temperature was decreased. The GAB and Halsey models gave a good fit for okara isotherms over the range of water activity 0.1 - 0.9. As temperature increased, GAB k-values increased towards unity where the GAB equation reduces to the BET equation. The influence of temperature on the constants of GAB and Halsey models was evaluated through Arrhenius-type equations. The Clausius Clapeyron equation was used to estimate the isosteric heats of sorption. Moisture sorption isotherms of okara soy milk were determined using the gravimetric method in the range 20 - 50 °C. The sorption isotherms exhibited hysteresis along all the water activity range (0.1 - 0.9). The amount of sorbed water increased as the temperature was decreased. The GAB and Halsey models gave a good fit for okara isotherms over the range of water activity 0.1 - 0.9. As temperature increased, GAB k-values increased towards unity where the GAB equation reduces to the BET equation. The influence of temperature on the constants of GAB and Halsey models was evaluated through Arrhenius-type equations. The Clausius Clapeyron equation was used to estimate the isosteric heats of sorption.
title Modeling water sorption in okara soy milk
title_short Modeling water sorption in okara soy milk
title_full Modeling water sorption in okara soy milk
title_fullStr Modeling water sorption in okara soy milk
title_full_unstemmed Modeling water sorption in okara soy milk
title_sort modeling water sorption in okara soy milk
publishDate 2000
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07373937_v18_n9_p2091_Garcia
http://hdl.handle.net/20.500.12110/paper_07373937_v18_n9_p2091_Garcia
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