A gradient theory of grade two based on axiomatic conception of a nonlocal
continuum theory for materials of grade n is presentated. The total stress
tensor of rank two in the equation of linear momentum contains two higher s
tress tensors of rank two and three. In the case of isotropic materials bot
h the tensor of rank two and three are tenser-valued functions of the secon
d order strain rate tensor and its first gradient so that the equation of m
otion is of order four. The necessary boundary conditions for real boundari
es are generated by using so-called porosity tensors. This theory is applie
d to two experiments. To a velocity profile of a turbulent COUETTE flow of
water and a POISEUILLE now of a blood like suspension. On the basis of thes
e experimental data the material and porosity coefficients are identified b
y numerical algorithms like evolution strategies.