Wheat starch suspensions in water (5% dry matter) were subjected to various
pressures (0.1-600 MPa) and temperatures (-20 to 96 degreesC) for 15 min.
The gelatinization rate was measured after treatment by using microscopic m
easurements of the loss of birefringence of the granules. This method was p
reviously calibrated by differential scanning calorimetry. Curves of isogel
atinization were found to be quite similar to a pressure-temperature (P-T)
diagram of unfolding proteins. Results were first analyzed by considering t
he thermodynamic aspects related to the dT/dP curve shifts. On the basis of
equations already shown for proteins, the P-T gelatinization diagram of wh
eat starch would shaw different kinds of thermal contributions, suggesting
endothermic, athermic, or exothermic melting reactions. Second, as a practi
cal consequence, these previous P-T areas corresponded to specific gelatini
zation conditions as confirmed by hydration evaluation measured by starch s
welling index. Depending on the pressure-temperature conditions, gelatiniza
tion would involve hydration. Lowering the pressure and temperature resulte
d in a complete gelatinization with less hydration in comparison with a the
rmal treatment at atmospheric pressure. A hydration model based on an energ
etic approach was proposed.