Viscosities of aqueous solutions of sucrose and sodium chloride of interest in osmotic dehydration processes
Introduction
Osmotic dehydration of food (mainly fruits and vegetables) is a convenient method of improving the quality of a product since nutritional, organoleptic and physical aspects are preserved better than when using other dehydration methods (Raoult-Wack, 1994). Also, the economics of the process were positive compared to other dehydration methods (Lazarides, Gekas, & Mavroudis, 1997). During osmotic treatment several flows occur simultaneously: loss of water from the product to the hypertonic solution, solute impregnation from the solution to the product surface and, additionally, loss of other compounds (mainly soluble solids) from the product to the solution. The mass flow rates depend on several factors such as solution concentration (and, associated physical properties such as density and viscosity), temperature, contact time, level of agitation, sample size and geometry, solution to solid volume ratio and operating pressure. Certainly, the viscosity is an important physical property that influences the required agitation power (economic aspect), and the mass transfer rate. When the osmotic media is highly viscous the global mass transport must be studied as transport in two phases (liquid and solid phase). For this reason, the common assumption that the external resistance to mass transfer is negligible is not always valid.
The two most common solutes in these processes are sugars (mainly sucrose) and salts (mainly sodium chloride) used as binary or as ternary solutions. Sodium chloride solutions present lower water activity and higher osmotic pressure than sucrose solutions. Unfortunately, sodium chloride penetrates into the bulk of the solid whereas sucrose, due to the molecular size, doesn't exhibit this behaviour. Aqueous solutions with sucrose and sodium chloride are interesting because they improve the water loss with low solid gain; that means there is an advantage of using both osmotic agents (Bohuon, Collignan, Rios, & Raoult-Wack, 1998; Lerici, Pinnavaia, Dalla Rosa, & Bartolucci, 1985; Sereno, Moreira, & Martı́nez, 2001). The physical properties (density and viscosity) of aqueous solutions of sucrose and sodium chloride at 20 °C are available in handbooks (Lide, 1992; Weast, 1987) and for other temperatures scarce data can be found for sucrose (Misra & Varshni, 1961; Nabetani, Nakajima, Watanabe, Nakao, & Kimura, 1992) and for sodium chloride (Korosi & Fabuss, 1968; Sawamura, Yoshimura, Kutamura, & Taniguchi, 1992). Nevertheless, little data exists on the physical properties of the ternary aqueous solutions with both solutes in the range of interest (Bohuon, Le Maguer, & Raoult-Wack, 1997; Mulcahy & Steel, 1985). In addition, the correlation equations existing in the literature are in the polynomial form involving a great number of parameters (Brush, 1962; Hai-Lang & Shi-Jun, 1996).
The aim of this work is to report the kinematic viscosities and densities data of binary and ternary solutions of sodium chloride and sucrose at various concentrations and temperatures applicable to osmotic processing. A second aim is to propose a single equation to correlate density data and viscosity data with sugar and salt concentrations at various temperatures involving minimum number of parameters.
Section snippets
Materials and methods
Solutions were prepared using degassed distilled water and “commercial sugar” and “common salt” with purities >98% in saccharose and sodium chloride, respectively; both solutes were dried to constant mass at 105 °C. The solutions were prepared by mass using a Mettler AJ 150 balance with a precision of ±0.0001 g and were filtered before use.
Kinematic viscosities were determined in a Schott Geräte AVS 350 automatic Ubbelohde viscosimeter, using the experimental protocol described elsewhere (
Binary solutions
Table 1 shows experimental density values, , of aqueous solutions of a single solute at 25 °C. These values were correlated with molal concentration of the solute, m, using the equation obtained by simplification of bibliographic polynomial equations (Bettin, Emmerich, Spieweck, & Toth, 1998)where ρW is the water density at the same temperature, 997.2 , and the values obtained of the fitting parameters a and b are listed in Table 2 for aqueous solutions with a single
Conclusions
Experimental data of kinematic viscosity and density, no available in the literature, were obtained and correlated with simple equations involving concentration and temperature for a wide range of experimental conditions. The results were successfully fitted and, in this way, the fittings allow to calculate the physical properties of these solutions of interest with a higher precision necessary for the study of osmotic processes. In this way, maximum deviations of ±0.5% using 4 parameters for
Acknowledgements
The authors acknowledge the partial support from the project PX120905PR of the Xunta de Galicia (Spain).
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