Analysis reveals osmotic pressure impacts absorption in myofibrillar protein, suggesting effects of salt concentration on viscosity.
BACKGROUND The classic diffusion equation and that for osmotic pressure use ion solution, but cannot be applied in a complex food system. The diffusion coefficient ( D e ) is a physical quantity that describes the rate at which a substance diffuses in another medium and is commonly used in diffusion equations. Osmotic pressure ( π ) refers to the pressure generated when solute molecules in a solution diffuse through a semipermeable membrane toward the solvent side. Myofibrillar protein (MP), a main component in salted meat, was investigated in this study. RESULTS The results showed that, D e values in ion solution were always higher (4.00–5.69 × 10 −10 m 2 s −1 ) than those in MP (1.33–1.81 × 10 −11 m 2 s −1 ), but the declining rate was slower at a salt concentration of 40–80 g kg −1 and quicker at 80–160 g kg −1 . π MP (2.84 MPa ) was higher than π ion (2.68 MPa ) only at low contents of salt. When the salt concentration exceeded 40 g kg −1 , π MP was lower than π ion ; π MP increased from 2.84 to 10.08 MPa and π ion increased from 2.68 to 10.40 MPa . CONCLUSION Under low contents of salt, solubility increased and α ‐helix decreased, resulting in partial unfolding of the protein and enhanced binding to and absorption of water. This made the viscosity decrease, thus reducing the declining rate of D e and decreasing π MP . At high contents of salt, aggregation increased viscosity, and thus increased the declining rate of D e and π MP . This would provide a theoretical foundation for the amendment of the classic equations of D e and π MP .
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Wang et al. (2025) studied this question.
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