Away from the boundary, derivatives of a smoothly varying solution are much smaller than unless the outer solution vanishes. Nonzero boundary data therefore require a rapidly varying layer. If its thickness is , the radial second derivative is of order ; balancing it with gives .
Put and write . The equation becomes
For fixed and boundary data with angular variation independent of , the leading equation is . Matching to the zero outer solution removes the growing exponential, and the boundary value at fixes its coefficient:
This approximation describes the layer; it is not a uniform expansion in polar coordinates at the origin.
Laplace's method localizes an exponential integral near maxima of its real phase. At an isolated smooth interior maximum with and , Taylor expansion and Gaussian integral give
An endpoint maximum with nonzero inward phase slope instead gives an inverse- factor. Degenerate maxima require their first nonzero local phase term; continuous differentiability alone does not guarantee the quadratic formula.
Here . In its two exponentials, the positive exponential dominates at the interior maximum of . Since ,
The negative exponential has no comparable positive maximum and is negligible. Consequently, where ,
In the boundary layer , , so this reduces to , agreeing with the formal result when .
Define . Differentiation and the original equation give , while rearrangement gives . Write .
On the fast scale ,
Fast trajectories are horizontal. Their equilibria lie on the cubic ; the transverse linearization is , so the outer branches attract and the middle branch repels. On a horizontal line, arrows point right when and left when .
The source prints the slow time as . The slow variable needed here is . With this correction,
At leading order and
The reciprocal printed variable would give , rather than the autonomous slow equations used in the stated period formula.
For , the left attracting branch runs from to the fold , where . The horizontal fast jump at this height lands at . The right branch then runs from to the fold , where , followed by a fast jump to . The equilibrium at is on the repelling middle branch. The two slow segments dominate the period:
The jump times are negligible on this scale. Substituting in the first integral also gives the compact value
For , the negative slow segment takes , and the positive one takes . Thus rises slowly from to , jumps to , decreases more slowly to , then jumps back to ; the jumps are nearly vertical in the time trace.
For the fast horizontal field and attracting branches are unchanged. The right slow branch has arrows toward from both directions; the left branch still moves toward and jumps right. The equilibrium is stable, so the large relaxation cycle is replaced by approach to this equilibrium. If , a landing at moves right toward , rather than left. The sketches display the representative case .
Figure 1.
Fast horizontal flow, slow cubic branches, and the asymmetric relaxation cycle
. Details.
For fixed nonzero , expand the denominator geometrically:
The effective expansion parameter is , so the expansion fails when . In the inner variable ,
for fixed . Expanding the leading outer term toward gives at leading order; expanding the leading inner term for large and returning to gives . Thus the two one-term re-expansions match in . The next common contribution is when the corresponding next inner order is retained.
On , the relative denominator error is bounded by , hence
Integration by parts yields
For the last step split the remaining integral at one: , and replacing by one on that interval has a bounded error.
In the inner interval, gives an explicit error estimate:
The terms cancel between regions. Every displayed remainder is whenever and ; for example . Therefore the leading answer is independent of the arbitrary intermediate cutoff:
On the two independent variables, the total derivative is . Multiplication of by gives exactly the stated multiple-scale equation.
At order one, . Integrating twice gives
The periodic reciprocal coefficient has strictly positive mean. Unless , the integral has a nonzero linear drift in , violating the periodic cell ansatz and creating secular growth when . Thus and .
At order ,
Periodicity requires the derivative to have zero cell average. Consequently
At order , the equation is
The second flux inside braces is , independent of . Integrating over one period annihilates the first derivative, by periodicity, and yields . Hence
The effective transport coefficient is the harmonic mean of over the fast period; the source is averaged arithmetically. Smoothness sufficient for these formal differentiations and uniform positivity on the cells are understood.

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