The objectives of this work was to evaluate the effect of variation of water content on the physical properties of wheat grain and to adjust different mathematical models to the obtained experimental values as a function of moisture content. Also two different methodologies for determining bulk density and the real density were analysed. Based on the obtained results it may be concluded that the reduction of the moisture content affects the physical properties of wheat grain promoting the decrease of porosity and increase of both the bulk density and the specific gravity. Also the wheat grain bulk density and specific and real gravity values found through the chemical composition of grain were lower than the experimental data. However, the differences in values found between the two methodologies decreased as the moisture content decreases. The adapted Bala & Woods model fits best the individual wheat grain shrinkage as well as the bulk grain volume shrinkage. The grain shape (sphericity and circularity) did not vary for the moisture content range in this experiment.
density; porosity; mathematical model; shrinkage
