Distinguish equal potential from equal field
Use scalar superposition and vector projection as different measurements of a source.
Learning outcome: Compare center and axial records at two radii. Predict which quantities scale as inverse radius and inverse radius squared. Design a two-observation test for ring versus arc without claiming a single scalar value identifies the source.
Starting recap
Keep source normalization, potential reference, signed energy and evidence independence explicit.
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Try
At R = 1 m, z = 1 m and Q = 2 nC, V ≈ 12.7103 V and Ez ≈ 6.35516 N/C. At the center V ≈ 17.9751 V while the ring field is zero. Replacing the ring by an equal-charge semicircle leaves that center potential unchanged but creates a nonzero field.
Open the experimentPredict
Equal charge on a ring and a semicircle of equal radius gives the same center potential. What follows about center field?
Experiment
Compare center and axial records at two radii. Predict which quantities scale as inverse radius and inverse radius squared. Design a two-observation test for ring versus arc without claiming a single scalar value identifies the source.
Compare scalar potential with a vector field
Worked teaching model · synthetic values · Thin uniform ring Q = 2 nC. V(infinity) = 0; axis only. Separate equal-Q arc-center comparisons use the same radius, not the selected axial coordinate. Identical center potential does not imply identical center field.
Reset keeps your prediction, captures and practice history.
Ring-axis potential
Axes rescale independently. Curves join sampled coordinates; a joining segment is not additional measured evidence. Read physical units rather than screen angles or apparent slopes.
Ring-axis potential: numerical coordinates
| z (m) | V (V) |
|---|---|
| -3 | 5.68423 |
| -2.9 | 5.85972 |
| -2.8 | 6.04568 |
| -2.7 | 6.24301 |
| -2.6 | 6.45269 |
| -2.5 | 6.67579 |
| -2.4 | 6.9135 |
| -2.3 | 7.16714 |
| -2.2 | 7.43815 |
| -2.1 | 7.7281 |
| -2 | 8.03871 |
| -1.9 | 8.37184 |
| -1.8 | 8.72948 |
| -1.7 | 9.11374 |
| -1.6 | 9.52679 |
| -1.5 | 9.97079 |
| -1.4 | 10.4478 |
| -1.3 | 10.9596 |
| -1.2 | 11.5074 |
| -1.1 | 12.0914 |
| -1 | 12.7103 |
| -0.9 | 13.3608 |
| -0.8 | 14.0362 |
| -0.7 | 14.7258 |
| -0.6 | 15.4135 |
| -0.5 | 16.0774 |
| -0.4 | 16.6895 |
| -0.3 | 17.217 |
| -0.2 | 17.626 |
| -0.1 | 17.8859 |
| 0 | 17.9751 |
| 0.1 | 17.8859 |
| 0.2 | 17.626 |
| 0.3 | 17.217 |
| 0.4 | 16.6895 |
| 0.5 | 16.0774 |
| 0.6 | 15.4135 |
| 0.7 | 14.7258 |
| 0.8 | 14.0362 |
| 0.9 | 13.3608 |
| 1 | 12.7103 |
| 1.1 | 12.0914 |
| 1.2 | 11.5074 |
| 1.3 | 10.9596 |
| 1.4 | 10.4478 |
| 1.5 | 9.97079 |
| 1.6 | 9.52679 |
| 1.7 | 9.11374 |
| 1.8 | 8.72948 |
| 1.9 | 8.37184 |
| 2 | 8.03871 |
| 2.1 | 7.7281 |
| 2.2 | 7.43815 |
| 2.3 | 7.16714 |
| 2.4 | 6.9135 |
| 2.5 | 6.67579 |
| 2.6 | 6.45269 |
| 2.7 | 6.24301 |
| 2.8 | 6.04568 |
| 2.9 | 5.85972 |
| 3 | 5.68423 |
| Quantity | Value | Unit |
|---|---|---|
| Ring axial potential | 12.7103 | V |
| Ring axial field | 6.35516 | N/C |
| Ring and equal-Q arc center potential | 17.9751 | V |
| Uniform ring center field magnitude | 0 | N/C |
| Semicircle center field magnitude at same Q and radius | 11.4433 | N/C |
| Quarter-arc center field magnitude at same Q and radius | 16.1833 | N/C |
Equal potential at one location can coexist with very different field vectors there.
Every ring element is at the same axial distance, so scalar integration gives kQ/sqrt(R² + z²). Every arc element is distance R from its center, so center V = kQ/R regardless of span at fixed Q. Field uses vector projection and therefore retains angular-distribution information that one potential value loses.
Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.
Equal potential at one location can coexist with very different field vectors there.
Every ring element is at the same axial distance, so scalar integration gives kQ/sqrt(R² + z²). Every arc element is distance R from its center, so center V = kQ/R regardless of span at fixed Q. Field uses vector projection and therefore retains angular-distribution information that one potential value loses.
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