A study of yolks
stored up to 168 d at −20 °C was conducted
to determine the gelation behavior and mechanism of freeze–thawed
yolk. Methods used were rheology, native and sodium dodecyl sulfate
polyacrylamide gel electrophoresis (native- and SDS-PAGE), differential
scanning calorimetry (DSC), transmission electron microscopy (TEM),
particle size analysis, and proton nuclear magnetic resonance (1H NMR) spectroscopy for matrix mobility. Results indicate
that both constituents of plasma and granules contributed to gelation
of yolk under freezing. PAGE analyses suggest that granular proteins
participated in aggregation during freeze–thaw. Increasing
gel strength and particle size and decreasing water and lipid–water
mobility indicate that lipoproteins or apolipoproteins aggregated.
At storage times ≥84 d, increased protein and lipid mobility,
the detection of smaller particles, and secondarily increased gel
strength suggest the liberation of protein or lipoprotein components
from previously formed aggregates and further aggregation of these
constituents. Disruption of the gelled yolk matrix observed with TEM
supported that ice crystal formation was required for gelation to
occur. A two-stage dynamic gelation model is thus proposed.