2170 - Notes, Syllabus Section IV, lecture 26 (3/15/96)

(Here is the previous lecture )
Last time, I claimed that (roughly speaking) if the potential at the bottom of a well moves up, then the amplitude of the wave function tends to get larger as well. I said that I could show this mathematically, for the case of a simple "step" potential", e.g.:

Here's how the argument goes: Inside each step we will have . This means that

,

with k2<k1 by inspection. Now, to match the wave functions at the boundary between I and II, and also to match the derivative, we need A2>A1, as claimed above.

Proof:

(F+T have a different, but very similar proof)


In general, if you move to an adjacent region where k is smaller, your amplitude gets bigger. As I mentioned last time, adjacent turns out to be critical to this argument, I need to match and for this argument to work. (You can come up with some odd examples where the amplitude is smaller in a region that has small kinetic energy, if that region is physically well separated) Since I should be able to produce any arbitrary potential as a limit of such "stepwise flat" functions, this argument should hold quite generally.

One final issue for this qualitative discussion we're doing: Many potentials, V(x), are symmetric, i.e. V(x) = V(-x).

(There are other, subtler symmetries than this, of course, especially in more than one dimension) If this is the case, we can argue that particles should be just as likely to be on one side as the other. But,

Here, I emphasize we're only looking at time independent wave functions. Otherwise, the particle could "slosh" back and forth with time, breaking the symmetry at some particular times.

Anyway, there are two different classes of solutions:

The odd functions always run through the origin. This symmetry property of is called parity.

If is even, we say the function has even parity.

If is odd, we say it has odd parity.

When doing computer calculations, recognizing symmetry makes life easier! E.g., even wave functions are flat at the origin.

So, you can start at x=0, with some value , and with slope exactly 0, and numerically integrate the Schrodinger equation, and then if your E gives you going to 0 at infinity, you're happy (and done, except for normalizing).

Alternatively, you can start with =0, and pick some value for the slope. But, you needn't ever bother with different from zero along with slope different from zero. This saves a lot of unneeded effort! Physicists are always looking for any kind of symmetry they can, to help ease the work like this! (B.t.w, I study forces (weak forces) in my research which are not symmetric, so I have to worry about "parity violating wave functions"!)

Summary of qualitative wave function sketches.

1) Don't worry too much about the norm - we're interested in the basic shape now. (You can always rescale by an overall constant, as we discussed, to properly normalize at the end)

2) If V is symmetric, better be purely even or odd.

3) The nth level has n-1 nodes, always.

4) As the potential gets higher, (but is still below your energy), your KE drops, so momentum drops, so wavelength gets longer, and amplitude gets bigger. (as long as the potential steps are next to each other)

5) The farther under the potential your energy is outside the well, the faster the wave function must drop towards zero.

(This also affects the behavior of different states of increasing energy)

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