Turbulent transport in bulk-phase fluids and transport in porous media
with fractal character involve fluctuations on all space and time sca
les. Consequently one anticipates constitutive theories should be nonl
ocal in character and involve constitutive parameters with arbitrary w
avevector and frequency dependence. We provide here a nonequilibrium s
tatistical mechanical theory of transport which involves both diffusiv
e and convective mixing (dispersion) at all scales. The theory is base
d on a generalization of classical approaches used in molecular hydrod
ynamics and on time-correlation functions defined in terms of nonequil
ibrium expectations. The resulting constitutive laws are nonlocal and
constitutive parameters are wavevector and frequency dependent. All re
sults reduce to their convolution-Fickian, quasi-Fickian, or Fickian c
ounterparts in the appropriate limits.