Integrate a radial density before invoking Gauss symmetry
Distinguish insulating volume charge from a conducting surface distribution.
Learning outcome: Compare density powers 0,1,2 at fixed Q and R. Integrate enclosed charge at radii.25,.5,.75 and 1, then derive the interior and exterior fields. Contrast the volume distribution with the same-charge conducting shell. Explain why an exterior measurement alone cannot distinguish these symmetric interior distributions. Independently normalize the written sigma(r) annulus and change its outer radius at fixed coefficient, then at fixed total charge.
Starting recap
Choose source and observer coordinates, integrate normalized charge, and justify symmetry before simplifying field or flux.
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WithQ = 2 nC,R = 1 m andn = 1, rho 0 = Q/pi≈.636620 nC/m³. At radius .5 m, enclosed charge isQ(.5)^4 = .125 nC and Er = kQ(.5)²≈4.49378 N/C. A conducting shell with the same total Q has zero interior field.
Open the experimentPredict
Which charge belongs in Gauss law for an interior spherical observation surface?
Experiment
Compare density powers 0,1,2 at fixed Q and R. Integrate enclosed charge at radii.25,.5,.75 and 1, then derive the interior and exterior fields. Contrast the volume distribution with the same-charge conducting shell. Explain why an exterior measurement alone cannot distinguish these symmetric interior distributions. Independently normalize the written sigma(r) annulus and change its outer radius at fixed coefficient, then at fixed total charge.
Integrate enclosed charge before applying symmetry
Worked teaching model · synthetic values · Insulating sphere R=1 m,totalQ=2 nC,rho=rho0(r/R)^n. Spherical symmetry exact. Exterior field matches a point charge; comparison conducting shell carries same Q on surface. At shell surface use exterior limiting value.
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Piecewise sphere field
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.
Piecewise sphere field: numerical coordinates
| radius (m) | Er (N/C) |
|---|---|
| 0 | 0 |
| 0.05 | 0.0449378 |
| 0.1 | 0.179751 |
| 0.15 | 0.40444 |
| 0.2 | 0.719004 |
| 0.25 | 1.12344 |
| 0.3 | 1.61776 |
| 0.35 | 2.20195 |
| 0.4 | 2.87602 |
| 0.45 | 3.63996 |
| 0.5 | 4.49378 |
| 0.55 | 5.43747 |
| 0.6 | 6.47104 |
| 0.65 | 7.59448 |
| 0.7 | 8.8078 |
| 0.75 | 10.111 |
| 0.8 | 11.5041 |
| 0.85 | 12.987 |
| 0.9 | 14.5598 |
| 0.95 | 16.2225 |
| 1 | 17.9751 |
| 1.05 | 16.3039 |
| 1.1 | 14.8555 |
| 1.15 | 13.5918 |
| 1.2 | 12.4827 |
| 1.25 | 11.5041 |
| 1.3 | 10.6362 |
| 1.35 | 9.86288 |
| 1.4 | 9.17097 |
| 1.45 | 8.5494 |
| 1.5 | 7.98893 |
| 1.55 | 7.48183 |
| 1.6 | 7.02152 |
| 1.65 | 6.60243 |
| 1.7 | 6.21976 |
| 1.75 | 5.86942 |
| 1.8 | 5.54787 |
| 1.85 | 5.25204 |
| 1.9 | 4.97925 |
| 1.95 | 4.72718 |
| 2 | 4.49378 |
| 2.05 | 4.27724 |
| 2.1 | 4.07599 |
| 2.15 | 3.88861 |
| 2.2 | 3.71386 |
| 2.25 | 3.55064 |
| 2.3 | 3.39794 |
| 2.35 | 3.25489 |
| 2.4 | 3.12068 |
| 2.45 | 2.9946 |
| 2.5 | 2.87602 |
| 2.55 | 2.76434 |
| 2.6 | 2.65904 |
| 2.65 | 2.55964 |
| 2.7 | 2.46572 |
| 2.75 | 2.37687 |
| 2.8 | 2.29274 |
| 2.85 | 2.213 |
| 2.9 | 2.13735 |
| 2.95 | 2.06551 |
| 3 | 1.99723 |
| Quantity | Value | Unit |
|---|---|---|
| Boundary volume density | 0.63662 | nC/m³ |
| Enclosed charge | 0.125 | nC |
| Insulating sphere radial field | 4.49378 | N/C |
| Conducting shell radial field | 0 | N/C |
The interior Gaussian surface encloses only part of the volume charge.
Integrate 4pi rho r²dr, normalize the total, then use spherical symmetry to remove E from the surface integral. A shell and a volume distribution have identical exterior fields but distinct interior records.
Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.
The interior Gaussian surface encloses only part of the volume charge.
Integrate 4pi rho r²dr, normalize the total, then use spherical symmetry to remove E from the surface integral. A shell and a volume distribution have identical exterior fields but distinct interior records.
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