An important characteristic of many soil models is a volume change during p
lastic flow. In computations, this plastic volume change is expressed via a
kinematic constraint on the possible deformations. Due to this constraint
the plane-strain three-noded triangular element exhibits locking when plast
ic deformations occur, under dilatant, contractant and isochoric conditions
. It is demonstrated that using the method of enhanced assumed strains by S
imol this locking cannot be remedied. Far six-noded wedges and four-noded a
nd five-noded pyramids the same conclusion is obtained.