“…Fick's laws of diffusion and Fourier's law of conduction as well as its derived equation (e.g. Thin-layer drying equation) account for a significant proportion of the mathematical models employed in clay science (Evans and Keey, 1975;Tomas, et al, 1993;Kanno, et al, 1996;Su 1997;Sander, et al, 1998Sander, et al, , 2001Sander, et al, , 2003Moropoulou, et al, 2004Moropoulou, et al, , 2005Murugesan, et al, 2001;Mihoubi, et al, 2004;Dincer and Sahin, 2004;Akpinar and Dincer, 2005;;Chemkhi, et al, 2004Chemkhi, et al, , 2005. However, many of these models include different moisture transfer parameters that have a wide variation of reported values, depending on the complexity of the product and methods of moisture estimation.…”