Perturbation method to get approximate solutions to singular perturbation problems of differential equations, often when the small parameter is multiplying the highest derivative. Then the problem is of lower order, and will in general not be able to satisfy all the boundary conditions of the original problem
If y is the solution to then one possible behaviour in such cases is that:
In fluid dynamics these regions are known as boundary layers, in solid mechanics they are known as edge layers, in electrodymanics they are known as skin layers, etc.
For this reason the subject of matched asymptotic expansions is sometimes called boundary-layer theory.
Boundary layers can also appear in other circumstances, for instance when the perturbation converts a linear DE into a nonlinear one. See the example in question 2 here (in that case, the linear problem has a solution with a singularity at , but the nonlinearity makes . See solution in black oxford notebook.
Trick for finding scaling in boundary layer: in the boundary layer is often significant (though not always!). We must increase (where ) until this term balances the largest of the others in the equation.
Most elementary.
You simply require
where and refer to boundary layer, and middle (outer) solutions and variables.
Van Dyke's matching 'rule' usually works (more powerful than Prandtl's) and is much more convenient than the Intermediate variable matching below. The rule is
oooooooooooooooooooooooooooooooo
I.e. in outer expansion, in the outer variables expand to terms; then switch to inner variables and reexpand to terms.The result is the same as first expanding the inner expansion in the inner variables to terms, then switching to outer variables and reexpanding to terms.. Hmm, but these expansions are expressed in different variables. I guess, as a last implicit step, I should convert to the same variables to compare. What's the justification of this rule?
When using this matching rule you must treat log as because of the size of logarithmic terms.
Most advanced and powerful of the methods. More tedious to apply too.
Expansions for two "contiguous" regions should actually have an overlap or transition region where both expansions are valid.
For example, suppose there is a boundary layer for for , but the expansion we find is actually valid for , i.e., the expansion breaks when becomes or larger. Suppose also, that the middle, or outer region is defined for , but the expansion is valid for , for . Then in any region with , for , both expansions are valid, and therefore should match due to the uniqueness of Asymptotic approximations.
Note some terms jump order: a term in the examples in the notes comes from the inner expansion of the first-outer term, but it also comes from the outer expansion of the second-inner term. "First-outer" refers to first order in the expansion in outer region. The terms "inner and outer expansion" here refer to the expansion in terms of rescaled variables, but these terms are most often used for the van-Dyke rule where the "outer expansion" refers to the expansion of some term in terms of the outer variable, and similarly for the "inner expansion". The nomenclature he uses, is a bit confusing though.
A composite expansion is an expansion that is valid across the whole domain. It built as , where are the solutions in the boundary layers, are the outer solutions, outside boundary layers, and are overlaps, removed to avoid double counting. The term removes the contribution from the inner expansion, when looking at the outer region(s); or the contribution from the outer expansion, when looking at the inner region(s). In practice, this can be done by substracting a term of the form at the right order.
It is not unique, because it is not in standard Poincare form
Boundary layers
Think of the problem, and that to have the possibility of a non-trivial boundary layer we need some solution in the inner region which decays as we move towards the outer. In the problem considered in the notes, for example, the non-constant solution in the right-hand "boundary layer" grew exponentially as we moved to the outer, so there could never be a boundary layer at .
Transition or interior layers
Regions of fast change, not in the boundary, but in the interior of the domain. Finding the position of an interior layer can sometimes be hard.
Non-linear boundary layers
Boundary layer at infinity
Revise these
Example: van der Pol oscillator
Revise this example pages 36-41