Set . The phase-plane system is , . The origin is its only equilibrium, and its Jacobian matrix is . Thus
For the stated small positive , the eigenvalues have positive real part and nonzero imaginary part: the origin is an unstable focus.
Use the Poincaré-Lindstedt method. Introduce and . The leading equation gives and , after fixing the arbitrary phase. At order ,
Here . Periodicity requires the two resonant coefficients to vanish. With , this gives
Therefore the leading limit cycle is , with frequency . For example the nonresonant first correction contains ; its homogeneous sine/cosine pieces depend on phase and amplitude conventions. The absence of a first-order frequency shift is a solvability condition, not an assumption.
Use the method of multiple scales with independent fast and slow variables and , and write , . At the next order, . Its resonant terms are
Suppressing secular terms yields
The leading initial data are , up to adding an integer multiple of to the phase. Thus . The amplitude decreases from four towards the stable value one, consistent with the selected limit cycle; the zero-amplitude state is unstable. Order- corrections enforce the exact initial derivative after differentiating the slow amplitude term.
Let on the mixed endpoint domain , in . Integration by parts gives the boundary form
At zero, is free, forcing ; at one, is free, forcing . Therefore the formal adjoint expression and full adjoint endpoint conditions coincide with the original ones:
With the usual second-order operator domain this is a self-adjoint problem. The consequences for its eigenvalues and eigenfunctions follow below.
For , self-adjointness gives . Since an eigenfunction is nonzero, . One may also see reality directly from , whose boundary term vanishes under the mixed conditions.
If , then gives . Thus eigenfunctions belonging to distinct eigenvalues are orthogonal. Normalization can make them orthonormal. Equality of eigenvalues alone would not force arbitrary eigenvectors to be orthogonal, although in this particular scalar separated problem each eigenspace is one-dimensional.
The equation is . If , the linear or hyperbolic branches cannot meet both homogeneous endpoint conditions nontrivially. Otherwise , , and gives . Therefore
The factor makes the eigenfunctions unit normalized. All the eigenvalues are positive, in particular none is zero.
The difference of two solutions would satisfy with , . This would be a zero eigenvalue of the homogeneous problem, but part (b) shows there is none. Hence at most one solution exists. For continuous forcing the standard second-order existence construction also works: the free initial slope is fixed by an equation with coefficient . Thus for the stated regular boundary-value problem the solution is unique even with nonzero endpoint data.
Expand a forcing in the complete orthonormal basis . Since , its inverse multiplies the th coefficient by . Consequently
The negative sign follows from the eigenvalue convention . This kernel satisfies the mixed endpoint conditions in its first argument and .
The integral equation says precisely with the homogeneous mixed endpoint conditions. Since the supplied satisfies those conditions, apply directly:
No integration is required. The absence of a zero eigenvalue established in (b)–(c) also proves uniqueness of this recovered forcing.
Write the integral part as , where and . The kernel is real, so its adjoint transposes the two arguments. Hence
This follows by exchanging the two integrations in the inner product; the exponential factors make the finite-rank operators bounded.
Every eigenvector with eigenvalue different from one lies in , because . The elementary overlaps are , , . Thus
Its characteristic polynomial is , so the finite-multiplicity eigenpairs are
Each eigenspace has dimension one. On , both integrals defining vanish, so . Thus is also an eigenvalue, of infinite multiplicity, and there are no others.
The adjoint also leaves invariant, with and . By adjoint in weighted coordinates, its matrix in the same basis is . Solving the two eigenvector equations gives
The basis is not orthonormal, so one must not simply transpose the previous numerical matrix without accounting for its Gram matrix. Directly transposing the integral kernel avoids that error.
The nonzero kernel of rules out a unique solution for every value of . By the Fredholm alternative, solvability requires orthogonality of the forcing to . Its pairing with is
Thus only is compatible. In that case and a particular solution is . All solutions are
Therefore infinitely many solutions exist for , no solution exists for , and no parameter value gives a unique solution.
Integrate the conservation law over : . The Gaussian data and their finite-time characteristic/entropy evolution have vanishing far-field flux. Taking yields and hence . After a shock forms, its Rankine-Hugoniot condition preserves the same integral mass; the formal multivalued characteristic surface itself must be replaced by the conservative entropy solution.
Expanding the flux gives . Along characteristics, and . Labeling the initial point by gives
Equivalently, time reparametrization for a separable conservation-law flux uses . The projection derivative is . For large enough it becomes negative on an interval of positive , although it tends to one at both far ends. The projection then folds and assigns several density values to one position. This establishes multivaluedness of the formal characteristic continuation, not of the admissible shock solution.
The first fold occurs when . Differentiation gives , so the maximum is at . Therefore
At that point the first singular projection is at , with density .
The two characteristic families are , for left-state labels, and , for right-state labels. The explicit time-dependent flux is , so the shock speed is
Starting at zero gives
The characteristic speeds are behind and zero ahead, with shock speed between them. The left parabolas and right vertical lines terminate at the compressive shock.
Figure 1.
Parabolic characteristics entering a shock whose speed grows linearly in time
. Details.
Try , . The boundary data force and . The time derivative scales as , advection as and the source as . Balancing all three gives and . Substitution then yields
For the pointwise initial trace at any fixed , the far-profile requirement is as on any smooth branch extending that far; a compact-support continuation also meets it. Solving or selecting a shock continuation was not required. The time-dependent source is singular at , so the similarity reduction is stated on .

Articles by others on the same topic (0)

There are currently no matching articles.