Abstract

Changes in the water activity (aw) of experimental Cheddar cheeses with different compositions were measured over a 270 d ripening period. The ranges of key compositional parameters were typical of those found in commercial Cheddar cheese: moisture (35.6–38.6%), fat (29.9–33.4%), salt (1.4–2.0%), salt-in-moisture (3.8–5.2%), moisture-in-non-fat substances (MNFS, 52.4–56.3%) and pH (5.0–5.7). Linear regression analysis indicated that at ripening times ≤30 d, the aw was inversely correlated with salt-in-moisture, while at 270 d it was positively correlated with levels of moisture and MNFS, but negatively with fat content. The aw decreased significantly (P < 0.001) during ripening, from a mean of ∼0.965 at 1 d to ∼0.956 at 270 d. The preponderant factor responsible for the decrease in aw was the increase in proteolysis, as measured using pH 4.6 soluble N and free amino acids.

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