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Adnan Khan Lahore University of Management Sciences Peter Kramer Rensselaer Polytechnic Institute
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To study turbulent transport Transport occurs via two mechanisms Advection Diffusion The advective field being turbulent has waves at a continuum of wavelengths We study simplified models with widely separated scales to understand these issues
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We study the simplest case of two scales with periodic fluctuations and a mean flow The case of weak and equal strength mean flows has been well studied For the strong mean flow case standard homogenization theory seems to break down
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We study the transport using Monte Carlo Simulations for tracer trajectories We compare our MC results to numerics obtained by extrapolating homogenization code We develop a non standard homogenization theory to explain our results
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Transport is governed by the following non dimensionalized Advection Diffusion Equation There are different distinguished limits Weak Mean Flow Equal Strength Mean Flow Strong Mean Flow
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For the first two cases we obtain a coarse grained effective equation is the effective diffusivity given by is the solution to the ‘cell problem’ The goal is to try an obtain a similar effective equation for the strong mean flow case
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We use Monte Carlo Simulations for the particle paths to study the problem The equations of motion are given by The enhanced diffusivity is given by
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We use the CS flow as the fluctuation and different mean flows Changing the parameter gives different flow topologies We run Monte Carlo simulation of the tracer trajectories with this flow
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We note that the Monte Carlo Simulations in the Strong Mean Flow case also seem to agree with the homogenization numerics This indicates that homogenization does take place in this case as well Standard derivation of homogenization theory leads to ill posed equations We develop a Non Standard homogenization theory to explain our numerical results
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We consider one distinguished limit where we take We develop a Multiple Scales calculation for the strong mean flow case in this limit We get a hierarchy of equations (as in standard Multiple Scales Expansion) of the form is the advection operator, is a smooth function with mean zero over a cell
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We develop the correct solvability condition for this case We want to see if becomes large on time scales This is equivalent to estimating the following integral The magnitude of this integral will determine the solvability condition
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Analysis of the integral gives the following Hence the magnitude of the integral depends on the ratio of and For low order rational ratio the integral gets in time For higher order rational ratio the integral stays small over time
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We develop the asymptotic expansion in both the cases We have the following multiple scales hierarchy We derive the effective equation for the quantity
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For the low order rational case we get Where the operators are given by
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For the high order rational ratio case we get the following homogenized equation
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