Izoterme vlaženja sezamovog brašna pri različitim temperaturama

Moisture equilibrium data (adsorption and desorption) of sesame flour were determined using the static gravimetric method of saturated salt solutions at three temperatures, 10, 25 and 40 °C. The range of water activities for each temperature was between 0.11 and 0.85. Equilibrium moisture content decreased with the increase in storage temperature at any given water activity. The experimental data were fitted by five mathematical models (modified Oswin, modified Halsey, modified Chung-Pfost, modified Henderson and Guggenheim-Anderson-de Boer (GAB)). The GAB model was found to be the most suitable for describing the sorption data. The monolayer moisture content was estimated using the Brunauer-Emmett-Teller equation.Ravnoteža vlage (adsorpcije i desorpcije) u sezamovom brašnu određena je gravimetrijom zasićenih otopina soli na temperaturama od 10, 25 i 40 ºC. Aktivitet vode iznosio je 0,11-0,85 pri svim temperaturama. Ravnotežni udjel vlage smanjio se s povećanjem temperature skladištenja bez obzira na vrijednost aktiviteta vode. Podaci dobiveni istraživanjem uskladeni su uz pomoć pet matematičkih modela (modificirani Oswinov, Halseyev, Ching-Pfostov, Hendersonov i Gugenheim-Anderson-de-Boerov (GAB) model). GAB model bio je najprikladniji za opisivanje vrijednosti sorpcije. Udjel vlage u jednom sloju određen je Brunauer-Emmett-Tellerovom jednadžbom

Moisture Sorption Isotherms of Sesame Flour at Several Temperatures

Moisture equilibrium data (adsorption and desorption) of sesame flour were determined using the static gravimetric method of saturated salt solutions at three temperatures, 10, 25 and 40 °C. The range of water activities for each temperature was between 0.11 and 0.85. Equilibrium moisture content decreased with the increase in storage temperature at any given water activity. The experimental data were fitted by five mathematical models (modified Oswin, modified Halsey, modified Chung-Pfost, modified Henderson and Guggenheim-Anderson-de Boer (GAB)). The GAB model was found to be the most suitable for describing the sorption data. The monolayer moisture content was estimated using the Brunauer-Emmett-Teller equation

Izoterme vlaženja sezamovog brašna pri različitim temperaturama

Moisture equilibrium data (adsorption and desorption) of sesame flour were determined using the static gravimetric method of saturated salt solutions at three temperatures, 10, 25 and 40 °C. The range of water activities for each temperature was between 0.11 and 0.85. Equilibrium moisture content decreased with the increase in storage temperature at any given water activity. The experimental data were fitted by five mathematical models (modified Oswin, modified Halsey, modified Chung-Pfost, modified Henderson and Guggenheim-Anderson-de Boer (GAB)). The GAB model was found to be the most suitable for describing the sorption data. The monolayer moisture content was estimated using the Brunauer-Emmett-Teller equation.Ravnoteža vlage (adsorpcije i desorpcije) u sezamovom brašnu određena je gravimetrijom zasićenih otopina soli na temperaturama od 10, 25 i 40 ºC. Aktivitet vode iznosio je 0,11-0,85 pri svim temperaturama. Ravnotežni udjel vlage smanjio se s povećanjem temperature skladištenja bez obzira na vrijednost aktiviteta vode. Podaci dobiveni istraživanjem uskladeni su uz pomoć pet matematičkih modela (modificirani Oswinov, Halseyev, Ching-Pfostov, Hendersonov i Gugenheim-Anderson-de-Boerov (GAB) model). GAB model bio je najprikladniji za opisivanje vrijednosti sorpcije. Udjel vlage u jednom sloju određen je Brunauer-Emmett-Tellerovom jednadžbom