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The local first-return map of a scalar harmonic oscillator near (1,0) is the reflection x->-x

Example

Let ω>0 and let F:R2→R2, F(x,y)=(y,−ω2x), be the phase-plane field of the scalar harmonic oscillator x′′+ω2x=0, with y=x′, with local flow Φ (The local flow of an autonomous first-order system). Its solutions are

Φ(t,(x,y))=(xcos⁡ωt+yωsin⁡ωt, −ωxsin⁡ωt+ycos⁡ωt),

defined for all real t. Take the section Σ={y=0}, the reference point x0=(1,0) with h(x,y):=y, and t0:=π/ω, so that x1=Φ(t0,x0)=(−1,0). Then h(x0)=h(x1)=0 and

Dh(x0)F(x0)=−ω2≠0,Dh(x1)F(x1)=ω2≠0,

and Φ(s,x0) has second coordinate −ωsin⁡(ωs)≠0 for 0<s<π/ω, so it avoids the closed section on that interval. Thus the first-return clause of A transversal return of a C¹ flow yields a local C¹ Poincaré map, with inverse given by the reversed crossing applies and produces a local C1 Poincaré map near x0. On the section itself the map and its inverse can be computed exactly: for (x,0) with x near 1, the return time is τ(x,0)=π/ω and the return map is

P(x,0)=(−x,0),

the reflection in the origin restricted to the section, with inverse Q(y,0)=(−y,0); this is a C1 diffeomorphism between neighbourhoods of (1,0) and (−1,0) in Σ.

Facts & Assumptions

Given: The frequency ω>0, the field F(x,y)=(y,−ω2x), the section Σ={y=0}, the points x0=(1,0), x1=(−1,0), and the function h(x,y)=y.

[L1]

The derivative formulas (sin⁡)′=cos⁡, (cos⁡)′=−sin⁡ and initial values sin⁡0=0, cos⁡0=1 hold (The derivatives of sine and cosine are cosine and minus sine, Sine and cosine defined by their real power series); vector-valued derivatives are computed componentwise (The derivative and the Riemann integral of a vector-valued function: an intrinsic derivative and a componentwise integral). The linear field F is globally Lipschitz: its Euclidean norm satisfies ∥F(z)−F(w)∥2≤max⁡(1,ω2)∥z−w∥2. Hence each initial datum has a unique maximal solution, and any solution through it is a restriction of that solution (The local flow of an autonomous first-order system).

[L2]

The return-map proposition applies under the two displayed transversality conditions, and its first-return clause applies when the open reference segment avoids the closure of the section and gives a local C1 diffeomorphism with inverse given by the reversed crossing (A transversal return of a C¹ flow yields a local C¹ Poincaré map, with inverse given by the reversed crossing).

[L3]

The zero set of sine is {kπ:k∈Z}, and sine has period 2π (The zero sets of sine and cosine and the least positive common period 2 pi); moreover sin⁡π=0 and cos⁡π=−1 (Quarter-turn values and shifts by pi/2 and pi).

Verification

technique · direct; verify the explicit solution, the crossings and the restriction of the return map to the section
1.1givenL1

Differentiating the two components of the displayed curve with respect to t using (sin⁡)′=cos⁡, (cos⁡)′=−sin⁡ gives (−ωxsin⁡ωt+ycos⁡ωt, −ω2xcos⁡ωt−ωysin⁡ωt), whose first component is the second component of the curve and whose second component is −ω2 times the first; hence the curve solves the phase system z′=F(z) and takes the value (x,y) at t=0. It is defined on all of R, so [L1] makes it the unique maximal solution and gives Ω=R×R2.

2.1step 1.1L1L3algebra

For x≠0 on the section, Φ(t,(x,0))=(xcos⁡ωt,−ωxsin⁡ωt): the second component vanishes exactly when sin⁡ωt=0, i.e. at t=kπ/ω, k∈Z, by [L3]. For x>0 the first positive time at which the orbit meets Σ is t=π/ω, with Φ(π/ω,(x,0))=(−x,0); therefore τ(x,0)=π/ω and P(x,0)=(−x,0) for every x>0 close to 1.

3.1step 1.12.1L2L3

The transversality conditions: with h(x,y)=y we have Dh=(0,1), F(x0)=(0,−ω2) and F(x1)=(0,ω2), so Dh(x0)F(x0)=−ω2≠0 and Dh(x1)F(x1)=ω2≠0. By step 2.1 and [L3] the open reference segment has no hit of the closed section Σ, which verifies the extra exclusion condition of [L2]. Hence [L2] applies at the reference data (t0,x0)=(π/ω,(1,0)), and its conclusion is realized by the explicit map of step 2.1: P maps a neighbourhood of (1,0) in Σ onto a neighbourhood of (−1,0) in Σ, and Q(y,0)=(−y,0) inverts it.

4.1step 3.1L2algebra∎

Finally the map x↦−x is a C1 diffeomorphism of R onto itself, so its restriction to the section is a C1 diffeomorphism between the stated neighbourhoods; this agrees with the general conclusion of the proposition and shows that the local inverse is again given by the reversed crossing, since the same computation with x<0 runs the reference orbit backwards.

Remarks

  • The example is the simplest case in which the local Poincaré map can be written in closed form. The proposition's hypothesis that the section be transversal at both crossings is visible in the computation: at the crossing the velocity is purely vertical, with Dh⋅F=∓ω2≠0.

  • The return map is computed on the section only; the general map τ(x,y) for points off the section is a C1 function near (1,0) by the proposition, but its explicit formula is not needed here. No stability or periodicity of the map is asserted: the reflection is an involution, and every point of the reference orbit is periodic for the flow with period 2π/ω.

  • At (0,0) the displayed flow is stationary. Every positive time is a hitting time of Σ, so there is no least positive hitting time and hence no first-return map there. The asserted local map is near (1,0), with its image near (−1,0).

Depends on

Dependency tree · 2 levels

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