The slow thermal decomposition of olive bagasse at temperatures ranging fro
m 25 to 900 degrees C, with particular stress on the moisture evaporation p
henomena, is analyzed making use of thermogravimetry, derivative thermograv
imetry and differential scanning calorimetry. The results obtained demonstr
ate that Thermal Analysis techniques contribute for the characterization of
internal moisture transfer processes. "Drying curves" obtained from Therma
l Analysis experiments were compared with thin-layer drying curves of olive
bagasse at relatively high temperatures. The existence of a critical moist
ure content, which distinguishes two types of water liaisons, was demonstra
ted, and its value quantified at 17-18%.