Normalize both pieces of a continuous asymmetric amplitude
Let u=x/L on a finite support 0..L. A real triangular amplitude rises as N u/q for 0≤u≤q and falls as N(1−u)/(1−q) for q≤u≤1, with zero outside. Here q strictly between zero and one is a peak-position fraction, not a probability. The two pieces agree at the peak and vanish at the endpoints.
Learning outcome: Normalize the two pieces separately, verify continuity at the peak and compare two intervals that cross different branches. Move the peak without changing L and explain why N stays fixed while interval probabilities change. State which extra information would turn this into a stationary-state problem.
Starting recap
Review definite integrals, complex amplitudes, probability moments, elementary differential equations and energy-momentum units. State boundary and normalization conditions, and distinguish calibration from unused validation.
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For L=1 nm and q=0.5, N=sqrt(3) nm^−1/2. The probability left of x=L/4 is (1/4)³/(1/2)²=1/16, not one quarter or the density height. For q=0.25, the probability to the left of the peak is 0.25 even though that point is the amplitude maximum.
Open the experimentPredict
Which quantity must integrate to one over physical position?
Experiment
Normalize the two pieces separately, verify continuity at the peak and compare two intervals that cross different branches. Move the peak without changing L and explain why N stays fixed while interval probabilities change. State which extra information would turn this into a stationary-state problem.
Normalize a continuous piecewise amplitude
Worked teaching model · synthetic values · Support0..L with L1 nm. Real amplitude N u/q before peak q and N(1−u)/(1−q) after it, u=x/L; zero outside. Normalize with physical dx. Continuous amplitude has derivative corners and is not asserted to be a stationary state of a smooth finite potential.
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Continuous amplitude is not probability density
Graph axes rescale independently; read units and values, not screen angles. 1: normalized real amplitude (solid). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Continuous amplitude is not probability density
normalized real amplitude
| u = x/L | amplitude times sqrt(L) |
|---|---|
| 0 | 0 |
| 0.01666667 | 0.05773503 |
| 0.03333333 | 0.1154701 |
| 0.05 | 0.1732051 |
| 0.06666667 | 0.2309401 |
| 0.08333333 | 0.2886751 |
| 0.1 | 0.3464102 |
| 0.1166667 | 0.4041452 |
| 0.1333333 | 0.4618802 |
| 0.15 | 0.5196152 |
| 0.1666667 | 0.5773503 |
| 0.1833333 | 0.6350853 |
| 0.2 | 0.6928203 |
| 0.2166667 | 0.7505553 |
| 0.2333333 | 0.8082904 |
| 0.25 | 0.8660254 |
| 0.2666667 | 0.9237604 |
| 0.2833333 | 0.9814955 |
| 0.3 | 1.03923 |
| 0.3166667 | 1.096966 |
| 0.3333333 | 1.154701 |
| 0.35 | 1.212436 |
| 0.3666667 | 1.270171 |
| 0.3833333 | 1.327906 |
| 0.4 | 1.385641 |
| 0.4166667 | 1.443376 |
| 0.4333333 | 1.501111 |
| 0.45 | 1.558846 |
| 0.4666667 | 1.616581 |
| 0.4833333 | 1.674316 |
| 0.5 | 1.732051 |
| 0.5166667 | 1.674316 |
| 0.5333333 | 1.616581 |
| 0.55 | 1.558846 |
| 0.5666667 | 1.501111 |
| 0.5833333 | 1.443376 |
| 0.6 | 1.385641 |
| 0.6166667 | 1.327906 |
| 0.6333333 | 1.270171 |
| 0.65 | 1.212436 |
| 0.6666667 | 1.154701 |
| 0.6833333 | 1.096966 |
| 0.7 | 1.03923 |
| 0.7166667 | 0.9814955 |
| 0.7333333 | 0.9237604 |
| 0.75 | 0.8660254 |
| 0.7666667 | 0.8082904 |
| 0.7833333 | 0.7505553 |
| 0.8 | 0.6928203 |
| 0.8166667 | 0.6350853 |
| 0.8333333 | 0.5773503 |
| 0.85 | 0.5196152 |
| 0.8666667 | 0.4618802 |
| 0.8833333 | 0.4041452 |
| 0.9 | 0.3464102 |
| 0.9166667 | 0.2886751 |
| 0.9333333 | 0.2309401 |
| 0.95 | 0.1732051 |
| 0.9666667 | 0.1154701 |
| 0.9833333 | 0.05773503 |
| 1 | 0 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
Probability integrates the squared amplitude
Graph axes rescale independently; read units and values, not screen angles. 1: absolute amplitude squared (solid). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Probability integrates the squared amplitude
absolute amplitude squared
| u = x/L | density per unit u |
|---|---|
| 0 | 0 |
| 0.01666667 | 0.003333333 |
| 0.03333333 | 0.01333333 |
| 0.05 | 0.03 |
| 0.06666667 | 0.05333333 |
| 0.08333333 | 0.08333333 |
| 0.1 | 0.12 |
| 0.1166667 | 0.1633333 |
| 0.1333333 | 0.2133333 |
| 0.15 | 0.27 |
| 0.1666667 | 0.3333333 |
| 0.1833333 | 0.4033333 |
| 0.2 | 0.48 |
| 0.2166667 | 0.5633333 |
| 0.2333333 | 0.6533333 |
| 0.25 | 0.75 |
| 0.2666667 | 0.8533333 |
| 0.2833333 | 0.9633333 |
| 0.3 | 1.08 |
| 0.3166667 | 1.203333 |
| 0.3333333 | 1.333333 |
| 0.35 | 1.47 |
| 0.3666667 | 1.613333 |
| 0.3833333 | 1.763333 |
| 0.4 | 1.92 |
| 0.4166667 | 2.083333 |
| 0.4333333 | 2.253333 |
| 0.45 | 2.43 |
| 0.4666667 | 2.613333 |
| 0.4833333 | 2.803333 |
| 0.5 | 3 |
| 0.5166667 | 2.803333 |
| 0.5333333 | 2.613333 |
| 0.55 | 2.43 |
| 0.5666667 | 2.253333 |
| 0.5833333 | 2.083333 |
| 0.6 | 1.92 |
| 0.6166667 | 1.763333 |
| 0.6333333 | 1.613333 |
| 0.65 | 1.47 |
| 0.6666667 | 1.333333 |
| 0.6833333 | 1.203333 |
| 0.7 | 1.08 |
| 0.7166667 | 0.9633333 |
| 0.7333333 | 0.8533333 |
| 0.75 | 0.75 |
| 0.7666667 | 0.6533333 |
| 0.7833333 | 0.5633333 |
| 0.8 | 0.48 |
| 0.8166667 | 0.4033333 |
| 0.8333333 | 0.3333333 |
| 0.85 | 0.27 |
| 0.8666667 | 0.2133333 |
| 0.8833333 | 0.1633333 |
| 0.9 | 0.12 |
| 0.9166667 | 0.08333333 |
| 0.9333333 | 0.05333333 |
| 0.95 | 0.03 |
| 0.9666667 | 0.01333333 |
| 0.9833333 | 0.003333333 |
| 1 | 0 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
| Quantity | Value | Unit |
|---|---|---|
| Normalization constant for length one nanometre | 1.732051 | nm^−1/2 |
| Probability left of chosen upper position | 0.0625 | ratio |
| Probability left of amplitude peak | 0.5 | ratio |
| Probability over full support | 1 | ratio |
Normalization uses the physical integration measure; a density height is not an interval probability.
The two shape-square integrals are q/3 and (1−q)/3, so N² L/3=1. Integrate the square piecewise: P(0<u<w)=w³/q² before the peak and1−(1−w)³/(1−q)² after it. At the peak P=q, not necessarily one half. The continuous triangular state has derivative corners; it is not claimed to solve a stationary smooth-potential Schrödinger equation.
Predict before inspecting the values. Save contrasting records with assumptions and one alternative explanation. This virtual display does not certify practical measurement technique.
Normalization uses the physical integration measure; a density height is not an interval probability.
The two shape-square integrals are q/3 and (1−q)/3, so N² L/3=1. Integrate the square piecewise: P(0<u<w)=w³/q² before the peak and1−(1−w)³/(1−q)² after it. At the peak P=q, not necessarily one half. The continuous triangular state has derivative corners; it is not claimed to solve a stationary smooth-potential Schrödinger equation.
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