WEAK GELS OF FAT CRYSTALS IN OILS AT LOW-TEMPERATURES AND THEIR FRACTAL NATURE

The formation of fat crystal gels in soybean oil has been studied by sedimentation in a low concentration region at 10-25 degrees C. At 10 degrees C, weak gels were formed with 1% crystals, and no gels formed at concentrations of 2-5%. At temperatures of 15-25 degrees C, no gels were formed at concentrations of 1-5%, and samples sedimented. Stronger gels of fat crystals were formed with similar to 10% fat crystals at all temperatures examined. Formation of weak gels is a consequence of the fractal nature of fat crystal aggregates and sediments. At low temperature, the interaction is weak. The fractal dimension is then high, and the flee size is large for low crystal concentrations. These large flocs form a three-dimensional network that act as a weak gel and withstand gravitational force. When the temperature is increased, the fat crystal interaction becomes stronger, fractal dimension decreases, and flee size decreases. Smaller flocs have a higher density, pack more easily, and sediment. Similar effects are observed when the concentration of fat crystals is increased at low temperature due to a decrease in flee size.