Short communication: Little change takes place in Camembert-type cheese water activities throughout ripening in terms of relative humidity and salt

Abstract

Water activity (aw) affects the growth and activity of ripening microorganisms. Moreover, it is generally accepted that aw depends on relative humidity (RH) and salt content; these 3 variables were usually measured on a given day in a cheese without the microorganism layer and without accounting for a distinction between the rind, the underrind, and the core. However, aw dynamics have never been thoroughly studied throughout cheese ripening. Experimental Camembert cheeses were ripened under controlled and aseptic conditions (temperature, gaseous atmosphere, and RH) for 14d. In this study, only RH was varied. Samples were taken from the cheese (microorganism layer)-air interface, the rind, and the core. The aw of the cheese-air interface did not change over ripening when RH varied between 91 and 92% or between 97 and 98%. However, on d 5, we observed a small but significant increase in aw, which coincided with the beginning of growth of Penicillium camemberti mycelia. After d 3, no significant differences were found between the aw of the cheese-air interface, the rind, and the core. From d 0 to 3, cheese rind aw increased from 0.94 to 0.97, which was probably due to the diffusion of salt from the rind to the core: NaCl content in the rind decreased from 3.7to 1.6% and NaCl content in the core increased from 0.0 to 1.6%. Nevertheless, aw did not significantly vary in the core, raising questions about the real effect of salt on aw. © 2013 American Dairy Science Association.