The mechanism (s) of Ca2+-induced cold gelation of whey protein isolate was
investigated. Kinetic data revealed that the rate constant of aggregation
(20 g/L protein, 3 degrees C) progressively increased as [CaCl2] was raised
from 10 mmol/L to a maximum of 30 mmol/L, and then declined as [CaCl2] was
raised to 120 mmol/L. This could be explained as the combined effect of ch
arge dispersion and Ca2+-bridging caused by increasing [CaCl2]. Young modul
us increased as protein was raised from 60 to 100g/L w/v at each of the cal
cium levels tested (5 to 150 mmol/L). The calculated fractal dimension of t
he gels increased from 2.3 to 2.6 as a function of increasing [CaCl2]. This
was also observed by scanning and transmission electron micrographs. (C) 1
999 Academic Press.