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Nonlinear Mechanics - Physics at Oregon State University

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2.5. ACTION-ANGLE VARIABLES 29<br />

2. We are using an F2 type gener<strong>at</strong>ing function, which is a function of the<br />

old coordin<strong>at</strong>e and new momentum. Hamilton’s characteristic function<br />

can be written as<br />

W = W (q, I). (2.48)<br />

The transform<strong>at</strong>ion equ<strong>at</strong>ions are<br />

Note th<strong>at</strong><br />

so<br />

<br />

dψ =<br />

∂ψ<br />

∂q<br />

ψ = ∂W<br />

∂I<br />

∂ψ<br />

∂q<br />

<br />

∂ ∂W<br />

dq =<br />

∂I ∂q<br />

p = ∂W<br />

∂q<br />

( )<br />

∂ ∂W<br />

=<br />

∂I ∂q<br />

<br />

∂<br />

dq =<br />

∂I<br />

2.5.1 The harmonic oscill<strong>at</strong>or (for the last time)<br />

H = 1<br />

2m (p2 + m 2 ω 2 q 2 )<br />

p = ± √ 2mE − m2ω2q 2<br />

I = 1<br />

<br />

√2mE<br />

− m2ω2q 2 dq<br />

2π<br />

(2.49)<br />

p dq = ∂<br />

(2πI) = 2π.<br />

∂I<br />

The integral is tricky in this form because p changes sign <strong>at</strong> the turning<br />

points. We won’t have to worry about this if we make the substitution<br />

q =<br />

√<br />

2E<br />

sin ψ (2.50)<br />

mω2 This substitution not only makes the integral easy and takes care of the sign<br />

change, it also makes clear the meaning of an integral over a complete cycle,<br />

i.e. ψ goes from 0 to 2π.<br />

I = E<br />

πω<br />

<br />

cos 2 ψ dψ = E/ω<br />

From this point of view the introduction of ψ <strong>at</strong> (50) seems nothing<br />

more th<strong>at</strong> a m<strong>at</strong>hem<strong>at</strong>ical trick. We would have stumbled on it eventually,

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