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Isotropy
Sunday, May 09, 2004
 
More Ado About Noether

I didn't say exactly how Noether connects e.g. conservation of energy to time-isotropy. Here's John Baez's explanation of Noether's theorem for the Lagrangian (a nice quantity tracking every position and velocity in a physical system): Noether's Theorem in a Nutshell

Baez gives the formula for the conserved quantity in a one-particle system:

C = p dq(s)/ds


where p(t) is the momentum at time t, q(t) the position, and s is the parameter of the symmetry - s measures how much the system was rotated or slid. If the Lagrangian has an s-isotropy, dC/ds = 0.

Let's throw caution to the wind (since we're laymen here) and talk about a Lagrangian that is invariant under changes of scale. Take s > 0 to be any real positive number, the scaling factor - this acts as our "symmetry parameter". For instance, if s = 2, we're doubling the size of the universe. The new position is s times the old position:

q(s,t) = sq(t)

What's C?
C = p dq(s)/ds


= p d(sq)/ds


= p q ds/ds


= p q


Well, that was easier than I hoped - and interesting. The conserved quantity in our scale-invariant system is the product of position and momentum. I wonder what that means....

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