2.3.8 · D2Modern Physics

Visual walkthrough — Wave function ψ — probability density - ψ - ²

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Step 1 — Start with a wiggle: what does even look like?

WHAT. A particle in quantum mechanics is not a dot at a place. It comes with a curve — read "psi of x" — that has a height at every position along a line.

WHY. We have to draw something before we can talk about probability. The simplest honest picture of is a real, wiggly curve: sometimes above the axis (positive height), sometimes below (negative height).

PICTURE. Look at the magenta curve. The horizontal axis is position (in metres). The vertical axis is the value of at that place — it goes up where and down where .

Figure — Wave function ψ — probability density  - ψ - ²

Right away a problem stares at us: the curve dips below zero. A probability can never be negative — you cannot have a chance of finding a particle somewhere. So itself cannot be the probability. Steps 2–3 fix this.


Step 2 — Kill the sign: square the height

WHAT. Take the height at each point and multiply it by itself: .

WHY. Squaring turns every negative into a positive: and . The valleys of (below the axis) flip up into hills. Now nothing dips below zero — exactly what a probability needs.

PICTURE. The violet curve is . Notice every part now sits on or above the -axis. Where crossed zero, just touches zero and bounces back up.

Figure — Wave function ψ — probability density  - ψ - ²

The term-by-term reading: we multiply the height by itself, so a sign times the same sign is always . This is why squaring is the natural sign-killer — no other simple operation flips negatives up without also mangling positives.


Step 3 — But real curves aren't the whole story: enter the arrow

WHAT. In general is a complex number at each point: it carries two pieces, written . Think of it not as a height but as a little arrow in a plane.

WHY. Real curves can't store everything a quantum particle needs (momentum lives in the "twist" of ). A complex value is a 2D arrow: it has a length and a direction. We need both.

PICTURE. The arrow has a horizontal part (the real part) and a vertical part (the imaginary part). Its length is what we'll care about; its tilt is the "phase."

Figure — Wave function ψ — probability density  - ψ - ²

Now watch the trap: if (a straight-up arrow, ), then . Squaring a complex number can give a negative! So plain is broken for complex arrows. We need a squaring that gives the arrow's length, and length is never negative.


Step 4 — The honest square: conjugate then multiply,

WHAT. Make a mirror copy of the arrow called (say "psi-star"): flip its vertical part, . Then multiply the mirror by the original: .

WHY. This particular product throws away the tilt and keeps only the length-squared — which is real and . It is the "square" that behaves.

PICTURE. The magenta arrow is ; the orange arrow is its mirror (reflected across the horizontal axis). Their product collapses to the length-squared shown as the shaded square.

Figure — Wave function ψ — probability density  - ψ - ²

Let us multiply it out, term by term — every piece labelled:

  • The cross terms and are equal and opposite — they cancel, deleting all the tilt.
  • becomes because .
  • What survives, , is exactly the arrow's length squared (Pythagoras on the little triangle) — real and never negative.

Step 5 — From "length-squared" to "chance in a slice"

WHAT. is a density — a probability per unit length, not a probability. To get an actual chance, multiply by the width of a thin slice: .

WHY. A tall spike that is infinitely thin holds no chance (zero width). Probability lives in area, not height. So we always attach a width .

PICTURE. The violet curve is . A single thin orange strip at position has height and width ; its area is the chance of finding the particle in that slice.

Figure — Wave function ψ — probability density  - ψ - ²

  • — how tall the density is at (units: per metre).
  • — how wide the slice is (units: metres).
  • Their product is a pure number between 0 and 1 — a genuine probability.

Step 6 — Add every slice: the region probability (an integral)

WHAT. To get the chance the particle lies between and , add the areas of all the thin strips from to . That running sum of infinitely thin strips is the integral .

WHY. One strip is one slice. The particle could be in any slice of the region, and these are separate possibilities, so their chances add. An integral is exactly "add up infinitely many infinitely thin pieces."

PICTURE. The shaded orange band is the total area under between and — that whole area is the probability .

Figure — Wave function ψ — probability density  - ψ - ²

  • — the tool that sums strips from to . We chose an integral (not a plain ) because the strips are infinitely thin and infinitely many.
  • The result is the shaded area — one number, the probability for that region.

Step 7 — The particle is somewhere: normalization

WHAT. Stretch the region to cover all space, from to . The total area under must equal exactly .

WHY. The particle certainly exists somewhere on the line. "Certain" means probability . So the whole area under the density is pinned to 1 — no more, no less.

PICTURE. The entire region under is shaded; its total area is labelled . The curve must fall to zero at both far ends, or the area would blow up.

Figure — Wave function ψ — probability density  - ψ - ²

  • — sum over every slice in the universe.
  • — total certainty: the particle is found with probability 1 somewhere.

Degenerate/edge cases you must know:

  • If the total is (but finite): the shape is fine, only the scale is wrong. Rescale . Since scales as the square, dividing by divides the whole area by , landing it on 1. (Divide by and you'd over-shrink to — the classic slip.)
  • If the total is infinite: is not normalizable — it doesn't fall to zero at infinity. Not a valid single-particle state.
  • If is multiplied by a phase (a spin of every arrow by the same angle ): the length of each arrow is unchanged, so and the whole area are unchanged. Global phase is invisible — see Step 8.

Step 8 — The vanishing phase: why leaves no trace

WHAT. Suppose , where is a "spinning" arrow of fixed length 1 that only rotates as changes. Its mirror is .

WHY. Momentum information hides in this spin. But probability only cares about arrow length. When we form , the mirror spin meets the spin and they cancel to 1.

PICTURE. Left: the arrow (magenta) and its mirror (orange) rotate in opposite directions. Right: multiplied together, they always point straight to — the spin is gone.

Figure — Wave function ψ — probability density  - ψ - ²

  • — opposite spins undo each other.
  • The oscillating phase disappears from the probability density. Two wave functions differing only by such a phase are physically identical. ✓

The one-picture summary

Everything above is one pipeline: wiggle → square the length → attach width → sum the strips → pin the total to 1.

Figure — Wave function ψ — probability density  - ψ - ²
Recall Feynman retelling — say it like a story

Picture a ghost's fog spread along a hallway. The recipe for the fog is — but the recipe is sneaky: it dips below zero and even carries little spinning arrows. You can't sell a "negative fog." So you take each arrow and multiply it by its own mirror image; the spin cancels and you're left with the arrow's plain length-squared, — the honest thickness of the fog, never negative. That thickness is per metre, so to get a real chance you slice the hallway into thin strips: chance in a strip = thickness width. Add up the strips across a stretch of hallway and you get the chance the ghost shows up there. Add up every strip in the whole hallway and — because the ghost is definitely somewhere — you must get exactly one whole ghost. If your recipe adds to instead of 1, shrink the recipe by (not !), because thickness grows as the square of the recipe. That's the entire story: square it to be fair, sum it to be there.

Recall Check yourself
  • Why can't itself be the probability? ::: It can be negative or complex; probabilities can't.
  • What does compute geometrically? ::: The squared length of the -arrow, .
  • Why multiply density by ? ::: Probability is area (height × width), not height alone.
  • Why is the total integral fixed at 1? ::: The particle is certainly somewhere.
  • Rescale factor if total is ? ::: Divide by .
  • Why does vanish from ? ::: Its mirror multiplies it to .

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