A new salting procedure was tested in Manchego type cheeses in order t
o shorten this processing step by decreasing the initial salt gradient
in the cheese. This procedure was based on a fast mass transfer mecha
nism (the hydrodynamic mechanism) which acts when pressure differences
are applied to porous products immersed in a liquid phase. The effect
ive porosity of the studied cheese of cheese in was 0.049 as establish
ed by the hydrodynamic mechanism. This value represents the introducti
on of 1.03 g NaCl 100 g(-1) the cheese pores, when a 19% (w/w) brine w
as used, at 37 mbar (absolute) of vacuum pressure. This quantity agree
d with the salt content in this experiment. The duration of the new sa
lting process step was 2 h. The hydrodynamic mechanism is based on the
supposition that salt ions penetrate the internal part of the cheese
through pores. Water loss during ripening was controlled by the extern
al drying rate for the cheese. Vacuum-impregnated cheeses always had a
higher water content as a consequence of lower drying rates during th
e brine immersion period. Nevertheless, the differences in water conte
nt neither affected the change in pH nor the ripening process during t
he maturation of the cheese. (C) 1997 Elsevier Science Ltd.