First order shear deformation theory renders quite accurate in-plane stress
es even for rather thick plates. By means of equilibrium conditions derivat
ives of the in-plane stresses can be integrated to determine transverse she
ar and normal stresses. The need to use in-plane derivatives requires at le
ast cubic shape functions. Simplifying assumptions relieve these requiremen
ts leading to the extended 2D method. While under mechanical load this meth
od yields excellent results, poor transverse normal stresses have been obta
ined for plates under a sinusoidal temperature distribution. This paper tra
ces back these deficiencies to lentil-like deformations of each separate la
yer. It is proved that third or fifth order displacement approximations thr
ough the plate thickness avoid these deficiencies. (C) 2001 Elsevier Scienc
e Ltd. All rights reserved.