Since the potential is a constant we can define it to be zero. The natural coordinate system to use is polar coordinates which greatly simplifies the Schrödinger Equation:
(-hbar2/2I) ∂2/∂φ2ψ = Eψ
This is identical to the very first problem we solved, expect we have traded translational properties (x, m) with rotational analogs (φ, I), a standard practice seen even in classical physics. This leads to, after normalizing, the following equation:
ψ(φ) = 1/√2π eimφ
Further, after constructing the appropriate operator, we see that we have a new quantized property arises naturally in angular momentum, called Lz because the vector lies perpendicular to the plane of rotation.
Rotation in 3d is very similar but we need to use spherical coordinates...
4 comments:
For the radial part of the wavefunction, we are given two different equations. On the equation sheet from the quiz, we have the Laguerre equation as a function of rho. However, on the handouts in class and notes, it is a function of rho/n. Which is it?
The handouts are correct. Thanks for pointing that out.
When drawing the probability diagram for a particle in a 2D box, (where nx = 2 , ny = 3), do you include the (+) and (-) in the boxes? How would you depict the nodes?
When you're referring to probability, the value can never be negative; thus it can only be zero or positive. For this reason, we often don't even bother writing the +'s and indicate the nodes with a line (just as in the wavefunction plots).
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