“…So far there has not been any general method that truly exploits the multiscaled nature of the problem. Most numerical work in this area are either based on empirical closure or upscaling methods (see [3,8,9,12,20]), or restricted to rather special flow fields (velocity fields). The difficulty is mainly due to the fact that the effective behavior of the tracer field u e at large scales is rather complicated and may depend on past history.…”