  We present the first study of the dynamic scaling or multiscaling of
passive-scalar and passive-vector turbulence. For the Kraichnan version of
passive-scalar and passive-vector turbulence we show analytically, in both
Eulerian and quasi-Lagrangian frameworks, that simple dynamic scaling is
obtained but with different dynamic exponents. By developing the multifractal
model we show that dynamic multiscaling occurs in passive-scalar turbulence
only if the advecting velocity field is itself multifractal. We substantiate
our results by detailed numerical simulations in shell models of passive-scalar
advection.
