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Abstract
In this work, the moisture adsorption and desorption isotherms were determined with the aim of defining the range of moisture content for storage of sludge powder. Equilibrium moisture content provides the basis for information not only on how much water has been taken out of a system but also on how fast drying is taking place (drying rate). Once the drying process is accomplished, the main concern rests on the storage of the dried final product. Still, the equilibrium moisture content is valuable information in that it has a major effect on the product physical and chemical properties. The present work also addresses the problem of selecting the best fit for equilibrium moisture content of sludge powder out of six well-known correlations for moisture sorption isotherms of solids: Henderson, Henderson-Thompson, Chung-Pfost, Chen-Clayton, Modified Halsey and Oswin. The equilibrium moisture content was determined by the static method (saturated salt solutions), in which the atmosphere surrounding the product is in equilibrium with the product without mechanical movement of the air or the product. Experiments were carried out under isothermal conditions at 20 and 40 °C. By calculating the regression coefficient, the residuals and the bias measure of Box for the equilibrium moisture content, the study showed that the Oswin Model was the most suitable. The range enclosed within the adsorption isotherm at 40°C and the desorption isotherm at 20°C defines the moisture extremes for storage in most tropical areas of the world.