Let it be clear that it's practically impossible to describe fundamental principles in the form of basic equations. One can (and surely must) try to draw conclusions using a heuristic way of thinking and then compare the solutions of "invented" equations with experimental measurements.
We have seen earlier that it's possible to describe our observations using the sum of probability amplitudes. One can write the following expression for a one-dimensional wave:
φ = A e−iwt+ikx where k = 2π/λ
According to de Broglie we can write the momentum as p: λ =
h/p and energy as E = hν =
hw for a particle. By substituting
expressions for momentum and energy in the first equation and replacing φ by the
probability amplitude y one can obtain the following
expression:
y =
Ae−iE/ht+ip/hx
¶y/∂t = -iE/ |
® | (i |
¶y/∂x = ip/ |
® | ( |
Notice that E and p are on the right sides of both equations. These two quantities can be measured experimentally. On the left side of each
expression there is a clue as to how one could obtain energy or momentum:
differentiating y on x (and multiplying it by
ih) one can obtain Ey;
differentiating y on x (and multiplying it by
h/i) one can
obtain py. These mathematical instructions are also
referred to as operators.
We introduced them at the end of the last chapter but now were able to draw
parallels between physical quantities and operators:
Energy | E | → | i |
Energy operator ≡ H |
Impulse | p | → | momentum operator ≡ p | |
Coordinate | x | → | x | Characterizing operators we use "bold" symbols |
Classical | Operator |
p = (px, py, pz) | p =
|
E = p²/2m + V | H =
− |
Lx = ypz − zpy | Lx =
|
Ly = zpx − xpz | Ly =
|
Lz = xpy − ypx | Lz =
|
Δ is the Laplace operator: Δ = ∂²/∂x² + ∂²/∂y² + ∂²/∂z².
p²/2my + V(x)y = Ey
we can then expand the expression for impulse by using the concept of an operator p²y = p(py) = p·(h/i·∂/∂xy) =
− h² (∂/∂x)(∂/∂x)y =
- h² (∂²/∂x²)y,
and by using the energy operator ih ∂/∂t, we obtain the following
time dependent Schroedinger equation:
[−
|
Next, let's try to expand the Schroedinger equation to three dimensions x, y, z:
p = (px, py, pz) →h/i(∂/∂x, ∂/∂y,
∂/∂z)
p. p
= p2 = (px2 + py2 +
pz2)→ −
h2(∂²/∂x² + ∂²/∂y² + ∂²/∂z²) = −
h2Δ
[−
|
y =
i |
½¾¾¾¯¾¾½ | |
H : | Hamilton operator |
time dependent Schroedinger equation:
H y= i |
If potential (or generally H)
doesn't depend on time and energy E is almost independent of time we can get rid of
time in the following way:
y(x,y,z,t) = yu(x,y,z) e−iE/ |
time independent Schroedinger equation:
Hyu = Eyu |
This ODE gives us values of stationary energy states.
If we know the time independent solution yu we can easily write the solution of the time
dependent equation unless H is not a
function of t and yu describes stationary
time independent energy states E:
y =yue−iE/ |
The normalization condition:
-¥ò+¥|y(x,y,z)|2dx dy dz = 1 |
The expression |y(x,y,z)|2dxdydz gives us the probability P(x,y,z) of locating the
particle in the location (x,y,z) with the range [x,x+dx], [y,y+dy] and [z,z+dz].
P(x,y,z) has unlike y(x,y,z) clear physical meaning of
probability. The probability amplitude describes the considered system completely and
we can obtain all information about the system according to the probability
amplitude.
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