The effect of encapsulants on the heat of sorption in vacuum-dried caja powder

Equilibrium moisture data from the powdered pulp of Spondias mombin, L., both with and without additives - 58% maltodextrin (MD) or 58% gum arabic (GA) - were determined at 20, 30, 40 and 50 degrees C, using the static gravimetric method for a water activity range of 0.06 to 0.90. The resulting isot...

Descripción completa

Detalles Bibliográficos
Autores: Silva Oliveira Gomes, Maron Stanley, Polachini, Tiago Carregari [UNESP], Lopes Filho, Jose Francisco [UNESP], Romero, Javier Telis [UNESP]
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2019
País:Brasil
Institución:Universidade Estadual Paulista (UNESP)
Repositorio:Repositório Institucional da UNESP
Idioma:inglés
OAI Identifier:oai:repositorio.unesp.br:11449/196198
Acceso en línea:http://dx.doi.org/10.5935/1806-6690.20190069
http://hdl.handle.net/11449/196198
Access Level:acceso abierto
Palabra clave:Isotherms
Maltodextrin
Gum arabic Water activity
Descripción
Sumario:Equilibrium moisture data from the powdered pulp of Spondias mombin, L., both with and without additives - 58% maltodextrin (MD) or 58% gum arabic (GA) - were determined at 20, 30, 40 and 50 degrees C, using the static gravimetric method for a water activity range of 0.06 to 0.90. The resulting isotherms were sigmoidal and typical Type III, with the Guggenheim-Anderson-de-Boer model (GAB) adjusted to the experimental data for equilibrium moisture vs water activity. The addition of additives was shown to affect the isotherms in such a way that, for the same water activity, samples of CP+GA and CP+MD showed a lower equilibrium moisture content and were not affected by the variations in temperature. The isosteric heat of sorption for the caja powder with additives was greater (less negative) than that of the caja powder with no additives, suggesting that polar sites in the product without the addition of GA or MD are more active. An empirical exponential relationship can describe the dependence of the heat of sorption as a function of the moisture content of the material.