Separate a conducting material from its cavity
Mobile carriers in an ideal conductor rearrange when a field acts on them.
Learning outcome: Compare q = −1, 0 and +1 nC at fixed shell charge. Retain inner/outer inventories and three spatial regions. Then set Q = −q and explain how exterior zero field can coexist with a nonzero cavity field. Sketch a noncentral-source alternative and identify which totals survive without claiming a spherical local field.
Starting recap
Declare conductor boundaries, integrate potential or charging work, and distinguish controlled charge from voltage.
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Try
With q = +1 nC and Q = 0, the inner surface has −1 nC and the outer +1 nC. The metal field is zero, yet the cavity field at r = 0.5 m is 35.9502 N/C. The conductor potential is 4.49378 V, not zero merely because its field is zero.
Open the experimentPredict
A cavity contains a positive point charge inside a neutral conducting shell. Which conclusion follows?
Experiment
Compare q = −1, 0 and +1 nC at fixed shell charge. Retain inner/outer inventories and three spatial regions. Then set Q = −q and explain how exterior zero field can coexist with a nonzero cavity field. Sketch a noncentral-source alternative and identify which totals survive without claiming a spherical local field.
Account for a charged conducting cavity
Worked teaching model · synthetic values · Concentric spherical cavity radius 1 m, conducting shell outer radius 2 m, central source and isolated shell. Electrostatic equilibrium; no external fields. Cavity is not conducting material. Radial field excludes singular origin; one-sided surface values distinguished.
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Charge inventory across the spherical cavity
Radii use one common geometric scale. The inner circle encloses empty cavity space, not metal. Signed totals are also in the numerical ledger. Field branches show separate one-sided surface limits.
Cavity field before inner surface
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.
Cavity field before inner surface: numerical coordinates
| radius (m) | radial field (N/C) |
|---|---|
| 0.25 | 143.801 |
| 0.2625 | 130.432 |
| 0.275 | 118.844 |
| 0.2875 | 108.734 |
| 0.3 | 99.8617 |
| 0.3125 | 92.0325 |
| 0.325 | 85.0892 |
| 0.3375 | 78.9031 |
| 0.35 | 73.3678 |
| 0.3625 | 68.3952 |
| 0.375 | 63.9115 |
| 0.3875 | 59.8547 |
| 0.4 | 56.1722 |
| 0.4125 | 52.8194 |
| 0.425 | 49.7581 |
| 0.4375 | 46.9554 |
| 0.45 | 44.383 |
| 0.4625 | 42.0163 |
| 0.475 | 39.834 |
| 0.4875 | 37.8174 |
| 0.5 | 35.9502 |
| 0.5125 | 34.2179 |
| 0.525 | 32.6079 |
| 0.5375 | 31.1089 |
| 0.55 | 29.7109 |
| 0.5625 | 28.4051 |
| 0.575 | 27.1835 |
| 0.5875 | 26.0391 |
| 0.6 | 24.9654 |
| 0.6125 | 23.9568 |
| 0.625 | 23.0081 |
| 0.6375 | 22.1147 |
| 0.65 | 21.2723 |
| 0.6625 | 20.4772 |
| 0.675 | 19.7258 |
| 0.6875 | 19.015 |
| 0.7 | 18.3419 |
| 0.7125 | 17.704 |
| 0.725 | 17.0988 |
| 0.7375 | 16.5241 |
| 0.75 | 15.9779 |
| 0.7625 | 15.4583 |
| 0.775 | 14.9637 |
| 0.7875 | 14.4924 |
| 0.8 | 14.043 |
| 0.8125 | 13.6143 |
| 0.825 | 13.2049 |
| 0.8375 | 12.8136 |
| 0.85 | 12.4395 |
| 0.8625 | 12.0816 |
| 0.875 | 11.7388 |
| 0.8875 | 11.4105 |
| 0.9 | 11.0957 |
| 0.9125 | 10.7938 |
| 0.925 | 10.5041 |
| 0.9375 | 10.2258 |
| 0.95 | 9.95851 |
| 0.9625 | 9.70152 |
| 0.975 | 9.45436 |
| 0.9875 | 9.21652 |
| 1 | 8.98755 |
Field in conducting material
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.
Field in conducting material: numerical coordinates
| radius (m) | radial field (N/C) |
|---|---|
| 1 | 0 |
| 1.01667 | 0 |
| 1.03333 | 0 |
| 1.05 | 0 |
| 1.06667 | 0 |
| 1.08333 | 0 |
| 1.1 | 0 |
| 1.11667 | 0 |
| 1.13333 | 0 |
| 1.15 | 0 |
| 1.16667 | 0 |
| 1.18333 | 0 |
| 1.2 | 0 |
| 1.21667 | 0 |
| 1.23333 | 0 |
| 1.25 | 0 |
| 1.26667 | 0 |
| 1.28333 | 0 |
| 1.3 | 0 |
| 1.31667 | 0 |
| 1.33333 | 0 |
| 1.35 | 0 |
| 1.36667 | 0 |
| 1.38333 | 0 |
| 1.4 | 0 |
| 1.41667 | 0 |
| 1.43333 | 0 |
| 1.45 | 0 |
| 1.46667 | 0 |
| 1.48333 | 0 |
| 1.5 | 0 |
| 1.51667 | 0 |
| 1.53333 | 0 |
| 1.55 | 0 |
| 1.56667 | 0 |
| 1.58333 | 0 |
| 1.6 | 0 |
| 1.61667 | 0 |
| 1.63333 | 0 |
| 1.65 | 0 |
| 1.66667 | 0 |
| 1.68333 | 0 |
| 1.7 | 0 |
| 1.71667 | 0 |
| 1.73333 | 0 |
| 1.75 | 0 |
| 1.76667 | 0 |
| 1.78333 | 0 |
| 1.8 | 0 |
| 1.81667 | 0 |
| 1.83333 | 0 |
| 1.85 | 0 |
| 1.86667 | 0 |
| 1.88333 | 0 |
| 1.9 | 0 |
| 1.91667 | 0 |
| 1.93333 | 0 |
| 1.95 | 0 |
| 1.96667 | 0 |
| 1.98333 | 0 |
| 2 | 0 |
Exterior field after outer surface
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.
Exterior field after outer surface: numerical coordinates
| radius (m) | radial field (N/C) |
|---|---|
| 2 | 2.24689 |
| 2.03333 | 2.17382 |
| 2.06667 | 2.10427 |
| 2.1 | 2.03799 |
| 2.13333 | 1.9748 |
| 2.16667 | 1.91451 |
| 2.2 | 1.85693 |
| 2.23333 | 1.80192 |
| 2.26667 | 1.74931 |
| 2.3 | 1.69897 |
| 2.33333 | 1.65077 |
| 2.36667 | 1.6046 |
| 2.4 | 1.56034 |
| 2.43333 | 1.51788 |
| 2.46667 | 1.47714 |
| 2.5 | 1.43801 |
| 2.53333 | 1.40041 |
| 2.56667 | 1.36428 |
| 2.6 | 1.32952 |
| 2.63333 | 1.29607 |
| 2.66667 | 1.26387 |
| 2.7 | 1.23286 |
| 2.73333 | 1.20297 |
| 2.76667 | 1.17416 |
| 2.8 | 1.14637 |
| 2.83333 | 1.11956 |
| 2.86667 | 1.09367 |
| 2.9 | 1.06867 |
| 2.93333 | 1.04452 |
| 2.96667 | 1.02118 |
| 3 | 0.998617 |
| 3.03333 | 0.97679 |
| 3.06667 | 0.955671 |
| 3.1 | 0.935229 |
| 3.13333 | 0.915436 |
| 3.16667 | 0.896266 |
| 3.2 | 0.877691 |
| 3.23333 | 0.859687 |
| 3.26667 | 0.842232 |
| 3.3 | 0.825303 |
| 3.33333 | 0.80888 |
| 3.36667 | 0.792942 |
| 3.4 | 0.77747 |
| 3.43333 | 0.762447 |
| 3.46667 | 0.747855 |
| 3.5 | 0.733678 |
| 3.53333 | 0.7199 |
| 3.56667 | 0.706507 |
| 3.6 | 0.693484 |
| 3.63333 | 0.680818 |
| 3.66667 | 0.668496 |
| 3.7 | 0.656505 |
| 3.73333 | 0.644834 |
| 3.76667 | 0.633471 |
| 3.8 | 0.622407 |
| 3.83333 | 0.611629 |
| 3.86667 | 0.601129 |
| 3.9 | 0.590898 |
| 3.93333 | 0.580925 |
| 3.96667 | 0.571202 |
| 4 | 0.561722 |
Continuous cavity and material 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.
Continuous cavity and material potential: numerical coordinates
| radius (m) | potential (V) |
|---|---|
| 0.25 | 31.4564 |
| 0.3125 | 24.2664 |
| 0.375 | 19.473 |
| 0.4375 | 16.0492 |
| 0.5 | 13.4813 |
| 0.5625 | 11.4841 |
| 0.625 | 9.88631 |
| 0.6875 | 8.57903 |
| 0.75 | 7.48963 |
| 0.8125 | 6.56783 |
| 0.875 | 5.77771 |
| 0.9375 | 5.09295 |
| 1 | 4.49378 |
| 1.0625 | 4.49378 |
| 1.125 | 4.49378 |
| 1.1875 | 4.49378 |
| 1.25 | 4.49378 |
| 1.3125 | 4.49378 |
| 1.375 | 4.49378 |
| 1.4375 | 4.49378 |
| 1.5 | 4.49378 |
| 1.5625 | 4.49378 |
| 1.625 | 4.49378 |
| 1.6875 | 4.49378 |
| 1.75 | 4.49378 |
| 1.8125 | 4.49378 |
| 1.875 | 4.49378 |
| 1.9375 | 4.49378 |
| 2 | 4.49378 |
| 2.0625 | 4.3576 |
| 2.125 | 4.22944 |
| 2.1875 | 4.1086 |
| 2.25 | 3.99447 |
| 2.3125 | 3.88651 |
| 2.375 | 3.78423 |
| 2.4375 | 3.6872 |
| 2.5 | 3.59502 |
| 2.5625 | 3.50734 |
| 2.625 | 3.42383 |
| 2.6875 | 3.34421 |
| 2.75 | 3.2682 |
| 2.8125 | 3.19557 |
| 2.875 | 3.1261 |
| 2.9375 | 3.05959 |
| 3 | 2.99585 |
| 3.0625 | 2.93471 |
| 3.125 | 2.87602 |
| 3.1875 | 2.81962 |
| 3.25 | 2.7654 |
| 3.3125 | 2.71322 |
| 3.375 | 2.66298 |
| 3.4375 | 2.61456 |
| 3.5 | 2.56787 |
| 3.5625 | 2.52282 |
| 3.625 | 2.47932 |
| 3.6875 | 2.4373 |
| 3.75 | 2.39668 |
| 3.8125 | 2.35739 |
| 3.875 | 2.31937 |
| 3.9375 | 2.28255 |
| 4 | 2.24689 |
| Quantity | Value | Unit |
|---|---|---|
| Central source charge | 1 | nC |
| Inner induced surface charge | -1 | nC |
| Outer surface charge | 1 | nC |
| Net conductor charge | 0 | nC |
| Material electric field | 0 | N/C |
| Conductor potential | 4.49378 | V |
| Cavity field at radius 0.5 m | 35.9502 | N/C |
| Exterior field at radius 3 m | 0.998617 | N/C |
Zero field in the metal does not imply zero field in a cavity containing a source.
A Gaussian surface wholly within the metal requires q plus inner-surface charge to vanish. The isolated shell inventory then fixes its outer charge. Separate branch curves include one-sided surface limits; do not connect field discontinuities as a smooth physical curve. Empty closed cavities without internal charges screen static external fields under ideal equilibrium.
Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.
Zero field in the metal does not imply zero field in a cavity containing a source.
A Gaussian surface wholly within the metal requires q plus inner-surface charge to vanish. The isolated shell inventory then fixes its outer charge. Separate branch curves include one-sided surface limits; do not connect field discontinuities as a smooth physical curve. Empty closed cavities without internal charges screen static external fields under ideal equilibrium.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
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