
Physics II course sequence · Interactive lesson
Planar symmetry and sheets of charge
A charged plane is the one geometry where the field stops caring how far away you stand. Learn where that comes from, how superposing two sheets builds the parallel-plate field, why the field steps by σ/ε₀ at every charged surface, and how close to a real plate you have to stay for any of it to hold.
UPII-03.06 · Lesson 6 of 8 in this unit. Position is not a completion score.Build the model
Distance drops out, and the field steps
The key idea
Planar symmetry is the case where a charge distribution looks identical under every slide parallel to a plane and every reflection in it, which forces the field to lie along the plane's normal with a magnitude that can depend only on the perpendicular distance.
Example. A sheet carrying σ = 2.0 nC m⁻² makes E = σ/(2ε₀) = 113 N C⁻¹ pointing away from it, and that is the reading 0.50 mm away and 50 cm away alike.
The complete physical model and assumptions
An infinite plane of charge carries a symmetry that fixes almost everything before an integral is written: slide it in either in-plane direction, spin it about its normal, or reflect it in its own plane, and nothing about the source changes. The field must be just as indifferent, so it can only point along the normal, its magnitude can depend on nothing but the perpendicular distance, and it must reverse as you cross the sheet. A pillbox straddling the plane then turns Gauss's law into 2EA = σA/ε₀, and the area cancels: E = σ/(2ε₀), the same at 1 mm and at 1 km. The distance vanished because the inverse-square weakening of each patch of charge is exactly offset by the widening ring of charge that stays in play — which is also the warning, since a real plate runs out of ring. What survives in general is not the value but the jump: crossing any surface charge, the normal component of E steps by σ/ε₀, and that boundary condition still holds for curved surfaces, finite plates and conductors long after σ/(2ε₀) has stopped being true.
1What the symmetry of a sheet forbids
Put a uniform surface charge σ on the plane z = 0 and list what leaves the source unchanged: any slide in x, any slide in y, any rotation about the z axis, and a reflection in the plane itself. The field has to inherit every one of them. Translation in the plane means E cannot depend on x or y. Rotation about the normal kills any in-plane component, because such a component would have to point somewhere and no direction in the plane is special. So E = E(z)ẑ. The reflection maps z to −z while leaving σ alone, so the field on one side is the mirror of the field on the other: E(−z) = −E(z). Three sentences of symmetry have cut an unknown vector function of three variables down to one unknown number at each distance, and that is the entire reason Gauss's law is about to work here.
2The pillbox, and why the area cancels
Take a closed cylinder — a pillbox — with its axis along z, flat caps of area A at z = +h and z = −h, and its curved wall cutting through the sheet. On the wall E is parallel to the surface, so E ⋅ dA = 0 there. On each cap E is normal to the surface and constant over it, and the mirror symmetry makes the outward flux equal on the two caps, so ∮E ⋅ dA = 2EA. The charge inside is whatever σ covers: q(enc) = σA. Gauss's law gives 2EA = σA/ε₀, hence E = σ/(2ε₀). Two features deserve attention. A cancels, so the answer cannot depend on the size of the box you imagined — a sign the calculation is honest. And h never entered at all, which is the claim that the field does not weaken with distance. With σ = 2.0 nC m⁻², E = 2.0 × 10⁻⁹ / (2 × 8.854 × 10⁻¹²) = 113 N C⁻¹, and a probe at 5 mm and a probe at 5 m read the same.
3Why the distance dropped out
A field independent of distance looks like a violation of the inverse-square law, and it is not. Stack rings and integrate to get the axial field of a uniformly charged disc of radius R: E = σ/(2ε₀) [1 − z/√(z² + R²)]. Every ring obeys 1/r², but as you retreat the rings that dominate sit further out, and their circumference grows just fast enough to pay for the weakening. Two limits make the trade explicit. Hold z and let R → ∞: the bracket goes to 1 and E → σ/(2ε₀), so the compensation is exact only when the sheet never runs out. Hold R and let z ≫ R instead: 1 − z/√(z² + R²) ≈ R²/(2z²), so E ≈ σR²/(4ε₀z²) = Q/(4πε₀z²) with Q = σπR². Far enough away the disc is a point charge again, exactly as it should be.
4Superposing sheets: the parallel-plate field
Sheets superpose like anything else: add the vectors. Put σ₁ on a sheet at the left and σ₂ on one at the right, and take x to the right. Each sheet contributes magnitude |σ|/(2ε₀) everywhere, directed away from itself when σ is positive. Left of both, the two contributions point left, giving (σ₁ + σ₂)/(2ε₀) leftward. Between them the left sheet pushes right and the right sheet pushes left, so they subtract: the x component is (σ₁ − σ₂)/(2ε₀). Right of both they add again. Set σ₁ = +σ and σ₂ = −σ and the arithmetic collapses to the capacitor: zero outside, σ/ε₀ in the gap, uniform. With σ = 35 nC m⁻² that is 35 × 10⁻⁹ / (8.854 × 10⁻¹²) = 4.0 × 10³ N C⁻¹, and the gap width never appears. Set σ₁ = σ₂ = +σ instead and the picture inverts: zero between the sheets, σ/ε₀ outside.
5A slab ramps where a sheet jumps
Give the charge a thickness. A slab of uniform ρ filling |z| ≤ d has the same planar symmetry, so E = E(z)ẑ with E(−z) = −E(z), and a pillbox of cap area A reaching from −z to +z inside the slab encloses ρ(2zA). Gauss's law gives 2E(z)A = 2ρzA/ε₀, so E(z) = ρz/ε₀: the field climbs linearly from zero at the mid-plane. Push the caps outside and the enclosed charge stops growing at ρ(2dA), so E = ρd/ε₀ everywhere beyond, which is σ/(2ε₀) for the equivalent sheet σ = 2ρd. With ρ = 3.2 μC m⁻³ and d = 3.0 mm that outside field is 1.08 × 10³ N C⁻¹, matching the inside value at the face — a volume charge has no surface density there, so nothing jumps. Now shrink d towards zero holding σ = 2ρd fixed. The ramp steepens and narrows until it is a step, and the step is σ/ε₀. That is the general boundary condition: crossing any surface charge the normal component of E jumps by σ/ε₀, while the tangential component passes through unchanged.
6How close to a real plate you have to stay
The infinite sheet is a model, and a demanding one. On the axis of a disc of radius R the exact field is σ/(2ε₀) [1 − z/√(z² + R²)], so the fractional shortfall is z/√(z² + R²), which is close to z/R whenever z ≪ R. Landing within 1% of σ/(2ε₀) therefore means staying inside z ≈ 0.01R; at z = 0.1R you are already 10% low. For a plate 12 cm across, R = 6 cm and 1% means under a millimetre — not a few centimetres. The same condition in different costume governs the parallel-plate capacitor: the uniform σ/ε₀ field holds while the gap is small compared with the plate dimensions, and the fringing field at the rim is exactly what the model discards. Off the axis it is worse, because near an edge the field is neither uniform nor perpendicular. Planar symmetry is exact only for an infinite plane; for anything real it is a statement about being close.
Key equations
Read the units, assumptions and limits before substituting.
Field of an infinite charged sheet
E = σ/(2ε₀), away from the sheet for σ > 0
No distance appears, so the field is the same everywhere on either side — there is nothing for it to fall off with.
σ in C m⁻², ε₀ = 8.854 × 10⁻¹² C² N⁻¹ m⁻², E in N C⁻¹The pillbox that delivers it
2EA = σA/ε₀
A cancels, which is why the answer cannot depend on how large a box you chose to draw.
A is one flat cap's area in m²; the curved wall carries no flux because E lies in itTwo sheets, equal and opposite
E = σ/ε₀ in the gap, from the + sheet to the −
One line of superposition gives the whole parallel-plate field, and the gap width never enters.
σ is the magnitude on each sheet in C m⁻²; outside the pair the two contributions cancelJump in the normal field at a surface charge
E₂⊥ − E₁⊥ = σ/ε₀
Electrostatics allows no other discontinuity, and this one survives on curved and finite surfaces.
both components taken along the same normal n̂, which points from side 1 into side 2Uniform slab, field inside
E(z) = ρz/ε₀ for |z| ≤ d
Spread the charge through a thickness and the step becomes a ramp, continuous at each face.
ρ in C m⁻³, z measured from the mid-plane in m, half-thickness d in mFinite disc, on its axis
E = σ/(2ε₀) [1 − z/√(z² + R²)]
The shortfall is about z/R close in, so the infinite-sheet value is already 1% high at z = 0.01R.
R is the disc radius and z the axial distance, both in m; z = 0 returns σ/(2ε₀)Interactive lab
Predict first. Explore the model. Compare the result.
Explore the model
Try this. Set σ₁ = +10 and σ₂ = −10 nC m⁻² and the two outer plateaus drop onto zero while the middle one settles at σ/ε₀, exactly twice one sheet's σ/(2ε₀) — the parallel-plate field. Then drag the separation and watch every plateau stay put: distance never enters σ/(2ε₀).
Live results
- Eₓ LEFT OF BOTH
- -282 N C⁻¹
- Eₓ IN THE GAP
- 847 N C⁻¹
- Eₓ RIGHT OF BOTH
- 282 N C⁻¹
- STEP AT SHEET 1 σ₁/ε₀
- 1129 N C⁻¹
Results follow this lesson’s model and assumptions. Displayed values are rounded.
Predict → change one variable → check
Plan a change before running it. Every other input stays at the saved baseline.
Saved baseline. Left sheet density σ₁: 10.0 nC m⁻²; Right sheet density σ₂: −5.0 nC m⁻²; Separation of the sheets: 8 cm
This experiment is kept only while this page is open. It does not change saved course progress.
Catch the common trap
The commonest slip is writing E = σ/ε₀ for one isolated sheet. That result is real, but it belongs to a different pillbox. An isolated sheet radiates into both half-spaces, so the box has two flux-carrying caps and Gauss's law reads 2EA = σA/ε₀, giving σ/(2ε₀). At the surface of a conductor the field inside is zero, so one cap carries no flux at all, the law reads EA = σA/ε₀, and the answer is σ/ε₀ — with σ counting only the charge on that one face. The factor of two is bookkeeping about how many caps carry flux, not a property of the charge. The same care settles a second habit: the field between capacitor plates is σ/ε₀ because two sheets each supply σ/(2ε₀) in the same direction, not because one sheet somehow doubles.
Practice & worked examples
3 authored examples. Make an attempt, then reveal the reasoning one step at a time.
EasyExample 1
A large flat acrylic sheet carries a uniform surface charge density σ = −7.5 nC m⁻². Find the field 2.0 mm from the sheet and 25 cm from the sheet, then find the force on an electron released 2.0 mm away.
Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.
0 of 4 steps revealed.
- Treated as an infinite sheet, planar symmetry gives E = |σ|/(2ε₀), and no distance appears in it, so a single calculation covers both points.
- E = 7.5 × 10⁻⁹ / (2 × 8.854 × 10⁻¹²) = 7.5 × 10⁻⁹ / (1.771 × 10⁻¹¹) = 4.235 × 10² N C⁻¹, so 4.2 × 10² N C⁻¹ at 2.0 mm and the identical 4.2 × 10² N C⁻¹ at 25 cm.
- σ is negative, so E points toward the sheet on both sides of it.
- Force on the electron: F = |q|E = 1.602 × 10⁻¹⁹ × 423.5 = 6.8 × 10⁻¹⁷ N. The electron's charge is negative, so the force opposes E — it is pushed away from the negatively charged sheet.
Answer. E = 4.2 × 10² N C⁻¹ at both distances, directed toward the sheet; F = 6.8 × 10⁻¹⁷ N on the electron, directed away from the sheet.
MediumExample 2
A wide slab of charged plastic is 6.0 mm thick and carries a uniform volume charge density ρ = +3.2 μC m⁻³. Measuring z from the mid-plane, find the field at z = 1.0 mm, at the face, and 5.0 cm outside the slab, and say where the field is continuous.
Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.
0 of 5 steps revealed.
- Half-thickness d = 3.0 mm. Planar symmetry gives E = E(z)ẑ with E(−z) = −E(z), so a pillbox of cap area A running from −z to +z carries flux 2E(z)A.
- Inside, it encloses ρ(2zA), so 2E(z)A = 2ρzA/ε₀ and E(z) = ρz/ε₀. At z = 1.0 mm: E = 3.2 × 10⁻⁶ × 1.0 × 10⁻³ / (8.854 × 10⁻¹²) = 3.6 × 10² N C⁻¹.
- At the face, z = d = 3.0 mm: E = 3.2 × 10⁻⁶ × 3.0 × 10⁻³ / (8.854 × 10⁻¹²) = 1.08 × 10³ N C⁻¹.
- Outside, the caps stop collecting charge: q(enc) = ρ(2dA) however far out they go, so E = ρd/ε₀ = 1.08 × 10³ N C⁻¹ at 5.0 cm as well.
- Cross-check with the equivalent sheet: σ = 2ρd = 1.92 × 10⁻⁸ C m⁻², and σ/(2ε₀) = 1.08 × 10³ N C⁻¹. Inside and outside agree at the face, so the field is continuous there — a volume charge carries no surface density to make it jump.
Answer. E = 3.6 × 10² N C⁻¹ at z = 1.0 mm, and 1.1 × 10³ N C⁻¹ both at the face and at 5.0 cm, every one of them pointing away from the mid-plane. The field ramps linearly inside and is flat outside, with no discontinuity at either face.
HardExample 3
A flat circular plate of radius R = 12 cm carries σ = +45 nC m⁻² spread uniformly, with axial field E = σ/(2ε₀) [1 − z/√(z² + R²)]. Find the infinite-sheet value, compare it with the exact field at z = 2.0 mm and z = 6.0 cm, locate the axial distance where the exact field is 1.0% of the sheet value, and test that point against the point-charge formula.
Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.
0 of 5 steps revealed.
- Sheet value: σ/(2ε₀) = 45 × 10⁻⁹ / (2 × 8.854 × 10⁻¹²) = 2.541 × 10³ N C⁻¹.
- At z = 2.0 mm: z/√(z² + R²) = 0.0020/√(0.0020² + 0.120²) = 0.0020/0.12002 = 0.01666, so E = 2541 × 0.98334 = 2.50 × 10³ N C⁻¹, which is 98.3% of the sheet value.
- At z = 6.0 cm: z/√(z² + R²) = 0.060/√(0.060² + 0.120²) = 0.060/0.13416 = 0.4472, so E = 2541 × 0.5528 = 1.40 × 10³ N C⁻¹, only 55.3%. Half a radius out, the infinite-sheet model is wrong by nearly a factor of two.
- Set the bracket to 0.010, so z/√(z² + R²) = 0.990 and z² = 0.9801(z² + R²). Then 0.0199 z² = 0.9801 R², giving z = 7.02R = 0.842 m, where E = 2541 × 0.010 = 25.4 N C⁻¹.
- Point-charge check: Q = σπR² = 45 × 10⁻⁹ × π × 0.120² = 2.036 × 10⁻⁹ C, so kQ/z² = 8.988 × 10⁹ × 2.036 × 10⁻⁹ / 0.842² = 25.8 N C⁻¹ — 1.5% above the exact value, which is right, since at seven radii the disc is nearly but not quite a point.
Answer. σ/(2ε₀) = 2.54 × 10³ N C⁻¹; the exact field is 2.50 × 10³ N C⁻¹ (98.3%) at 2.0 mm and 1.40 × 10³ N C⁻¹ (55.3%) at 6.0 cm, and reaches 1.0% of the sheet value at z = 0.84 m, where the point-charge estimate 25.8 N C⁻¹ sits just above the exact 25.4 N C⁻¹.
Quick check
Select an answer and explain it before checking.
Review & continue
Planar symmetry is the case where a charge distribution looks identical under every slide parallel to a plane and every reflection in it, which forces the field to lie along the plane's normal with a magnitude that can depend only on the perpendicular distance.
- Explain the relationship without looking at the equation.
- Check a sign, a unit and a model assumption in your working.
- Return to the lab or worked example if a step is still unclear.
Optional supporting lessons
These chapter resources can help with earlier ideas; they are not additional required Physics II completion tasks.