Topic 4 of 7
Adding probability amplitudes
Coherent contributions combine as probability amplitudes. Add them first, then square the result to find density. Adding the separate densities omits interference.
A wavefunction describes one particle's state. In a double-slit arrangement, the coherent alternatives contribute to the amplitude at a detector position. They are not two independently detected fractions of the electron.
For locally real amplitude contributions a and b:
= a2 + b2 + 2ab
The 2ab term depends on the relative signs. The same separate squares can therefore produce different combined densities. For general amplitudes the rule is the modulus squared of their sum.
Worked local cancellation
A zero amplitude at one point
At one detector position, suppose the already weighted contributions are +0.300 and -0.300 mm-1/2:
|a + b|2 = 0 mm-1
Adding their separate squares would give 0.180 mm-1 and miss the cancellation. These are local contributions, not separately normalised complete states. Zero density at an ideal point does not establish zero probability throughout a finite detector bin.
Optional check At one detector position, two coherent, already weighted real amplitude contributions are +0.300 and -0.300 mm^(-1/2). What is the resulting probability density there?
Normalise a complete combined state
For a separate 4.00 nm interval, let L = 4.00 nm and define two normalised profiles, zero outside that interval:
v = √(2/L) sin(2πx/L)
Each squared profile has area 1. The product uv has equal positive and negative areas, which cancel over the whole interval. Consequently the total squared area of u + v, or of u - v, is 2. Dividing the amplitude by √2 normalises either combined state:
ψ- = (u - v)/√2
The factor works because of these particular normalised components and their cancelling product area. It is not an automatic coefficient for every pair of overlapping wavefunctions.
Start with two signed component amplitudes
The component profiles u and v each have squared area 1 and are orthogonal over this interval. Their relative signs matter when amplitudes are combined.
Combine amplitudes and normalize the state
The factor 1/sqrt(2) normalizes these particular orthogonal equal-weight combinations. Changing the relative sign changes the spatial density. A mixed-energy superposition generally evolves; this is one instant.
Square the combined amplitude to obtain density
Both full densities have area 1. Their relative sign information came from amplitude addition before squaring. A negative amplitude is not a negative probability.
At x = 1.00 nm, the plus-state density is about 0.728553 nm-1, while the minus-state density is about 0.0214466 nm-1. At 3.00 nm they swap. In particular, ψ+ there is -0.146447 nm-1/2, whose square is positive. At the midpoint both densities are 0.250 nm-1.
These are state profiles at a specified instant. A superposition of different energy states generally has a density that changes with time; it is not a stationary particle tracing the plotted curve.
Connect interference and standing shapes
Coherent alternative paths produce interference because their amplitudes combine. In a confined region, combining appropriate oppositely travelling amplitude components can produce standing spatial shapes that meet the boundaries. Both use amplitude superposition, but neither is obtained by adding probability densities.
The infinite-well model makes the boundary restriction explicit. Its standing wavefunction does not require a particle to have a definite classical leftward or rightward trajectory.