This page is a workout . The parent note built the single big fact — the electric field E is always perpendicular to an equipotential surface, and E = − ∇ V . Here we drag that fact through every kind of situation it can meet, so that when an exam or a real problem throws a case at you, you have already seen its twin.
Before anything, three symbols we will reuse constantly, in plain words:
Definition The three characters
V (the potential , measured in volts) — a single number attached to each point in space, like the height of the ground at that spot. See Electric Potential .
E (the electric field , in volts per metre or newtons per coulomb) — an arrow at each point, pointing the way a tiny positive charge would be pushed. See Electric Field Lines .
k (Coulomb's constant ) — just a shorthand name for the fixed number 4 π ε 0 1 = 8.99 × 1 0 9 N⋅m 2 / C 2 . We write k instead of the bulky fraction from here on; they mean exactly the same thing.
d V / d n means (the "n " is the normal step)
The link between field and potential, proven in the parent, is
E = − d n d V .
Here n is the normal direction — the single direction that points straight across the equipotential, at 9 0 ∘ to it (the way E itself points). d n is a tiny step taken in that direction, and d V is the resulting change in potential. So d n d V reads: "how much does the height V change per tiny step d n taken straight across the contour?" — the steepness of the potential hill. The minus sign says E points the way V drops . (Stepping along the surface instead gives d V = 0 , which is why there is no field component along it — see Gradient and Directional Derivative .)
Every problem this topic can throw is one of these cells . The examples below are labelled with the cell(s) they cover, and together they hit all of them.
#
Case class
What is special about it
Covered by
A
Positive point charge
Spheres, E points outward
Ex 1
B
Negative point charge
Spheres, E points inward (sign flip)
Ex 2
C
Uniform field (parallel plates)
Flat, equally spaced planes
Ex 3
D
Two equal charges (dipole-ish geometry)
Curved surfaces, a zero-field saddle point
Ex 4
E
Degenerate: on the surface itself
Motion along — must give W = 0
Ex 5
F
Limiting behaviour: r → ∞ and r → 0
Spacing spreads / crowds without bound
Ex 6
G
Conductor surface
Whole body one equipotential, E ⊥ surface
Ex 7
H
Real-world word problem
Numbers with units, capacitor-style
Ex 8
I
Exam twist: sign / direction trap
Where the naive answer is wrong
Ex 9
Cells A and B split the sign of the source. C, D cover the shapes . E, F cover the degenerate/limiting inputs. G is the killer application. H, I are the word-problem and trap cells.
+ Q = + 2 nC sits at the origin. Find V and E at r = 0.30 m , and check they are perpendicular to the equipotential there.
Forecast: Guess the shape of the equipotential and whether E points toward or away from the charge before reading on.
Step 1 — Write the potential. For a point charge,
V ( r ) = k r Q , k = 8.99 × 1 0 9 N⋅m 2 / C 2 .
Why this step? V depends only on r (distance from the charge). "V = const " therefore means "r = const " — a sphere . That already tells us the equipotential shape.
Step 2 — Plug the numbers.
V = ( 8.99 × 1 0 9 ) 0.30 2 × 1 0 − 9 = 59.9 V .
Why this step? We want a concrete height on our "landscape" to anchor the picture.
Step 3 — Field magnitude.
E = k r 2 Q = ( 8.99 × 1 0 9 ) 0.3 0 2 2 × 1 0 − 9 = 199.8 V/m .
Why this step? E = − d V / d n and here the normal step d n is just the radial step d r (the spheres' normal is radial); differentiating Q / r gives − Q / r 2 , so the field falls off faster than V .
Step 4 — Direction & perpendicularity. E = E r ^ points radially outward (away from + Q ). The outward radial direction r ^ is exactly the normal to the sphere r = const . So E ⊥ equipotential. ✓
The figure below draws three of these spheres (blue) and the field arrows (orange) shooting straight out through them. Look at the small green right-angle mark where an arrow crosses a sphere: that 9 0 ∘ crossing is the whole point of Cell A — and notice the arrows near the charge are packed tighter, foreshadowing the stronger field there.
Verify: Units: m 2 N⋅m 2 / C 2 ⋅ C = N/C = V/m ✓. Sanity: E / V = 1/ r = 1/0.30 = 3.33 m − 1 , and indeed 199.8/59.9 = 3.34 ✓.
Worked example Replace the source with
− Q = − 2 nC at the origin. What changes at r = 0.30 m ?
Forecast: Which way does E point now — and does the perpendicularity fact survive?
Step 1 — Potential goes negative.
V = ( 8.99 × 1 0 9 ) 0.30 − 2 × 1 0 − 9 = − 59.9 V .
Why this step? The sign of Q carries straight into V . The "landscape" is now a valley , not a hill.
Step 2 — Equipotentials are still spheres. "V = const " still forces "r = const ." Shape unchanged.
Why this step? The geometry depends on the dependence on r , not on the sign — this is the point of the cell.
Step 3 — Field flips direction.
E = k r 2 ( − Q ) r ^ = − 199.8 r ^ V/m ,
i.e. magnitude 199.8 V/m pointing inward (toward the charge).
Why this step? E = − ∇ V : since V increases as you move away from the negative charge (from − 59.9 toward 0 ), the field points the opposite way — inward.
Step 4 — Perpendicularity. Inward radial is still along r ^ (just − r ^ ), still the sphere's normal. E ⊥ equipotential holds. ✓
Verify: ∣ E ∣ identical to Ex 1 (199.8 V/m ) because E ∝ ∣ Q ∣/ r 2 . Direction reversed. Consistent with "E points from higher V (0 far away) to lower V (− 59.9 near the charge)" — see Work and Conservative Forces for why downhill is toward lower V .
Worked example Two plates
d = 5.0 mm apart hold a potential difference Δ V = 100 V . Find E , the equipotential spacing for Δ V = 20 V steps, and confirm the planes are flat and evenly spaced. See Parallel Plate Capacitor .
Forecast: Will the 20 V sheets be evenly or unevenly spaced?
Step 1 — Field from spacing.
E = d Δ V = 5.0 × 1 0 − 3 100 = 2.0 × 1 0 4 V/m .
Why this step? Inside the plates E is uniform, so E = − d V / d n becomes a plain ratio (no calculus needed): total drop over total gap, since the normal step d n runs straight across from plate to plate.
Step 2 — V is linear across the gap. With E = E x ^ , integrating gives V = − E x + C . So "V = const " ⇒ "x = const ": flat planes perpendicular to x ^ .
Why this step? Linear V is what makes the sheets flat and (next step) evenly spaced.
Step 3 — Spacing per 20 V step. Each equal Δ V needs an equal Δ x :
Δ x = E Δ V step = 2.0 × 1 0 4 20 = 1.0 × 1 0 − 3 m = 1.0 mm .
Five equal sheets across the 5.0 mm gap. ✓
Why this step? Equal Δ V and equal spacing ⇒ uniform field — the signature of the parallel-plate cell.
The figure below shows the two plates (red + 100 V , blue 0 V ), the four green dashed equipotential planes at 20 V steps, and the orange field arrows running from high to low. Notice the arrows are all the same length and the dashed planes are all the same distance apart — that even spacing is the visual signature of a uniform field.
Verify: 5 steps × 1.0 mm = 5.0 mm = d ✓. Units: V / m from V / m ✓.
Worked example Two charges
+ Q = + 2 nC sit on the x -axis at x = ± a with a = 0.10 m . Show that at the midpoint (origin) the field is zero, yet the point still sits on a perfectly good equipotential.
Forecast: If E = 0 at a point, what does "perpendicular to the equipotential" even mean there?
Step 1 — Field from each charge at the origin. Each charge is a distance a away:
E each = k a 2 Q = ( 8.99 × 1 0 9 ) 0.1 0 2 2 × 1 0 − 9 = 1798 V/m .
Why this step? We build the total field by superposition — add the two arrows.
Step 2 — They cancel. The left charge pushes a test + charge to the right (+ x ^ ); the right charge pushes it to the left (− x ^ ). Equal magnitudes, opposite directions:
E total = 1798 x ^ − 1798 x ^ = 0.
Why this step? This is the degenerate zero-field input the matrix demands.
Step 3 — Potential is not zero there. Potential is a scalar — no cancellation:
V origin = 2 × k a Q = 2 × ( 8.99 × 1 0 9 ) 0.10 2 × 1 0 − 9 = 359.6 V .
Why this step? It shows V and E are different animals: adding numbers vs. adding arrows.
Step 4 — Meaning of "⊥ " when E = 0 . Where E = 0 , the "downhill direction" is undefined — there is no direction of steepest descent, so perpendicularity is vacuously satisfied . The origin is a saddle of the potential landscape: down along the x -axis toward each charge is uphill, but stepping off the axis it curves the other way. Equipotentials near a saddle look like the crossed hyperbolas of a mountain pass — but the two branches belong to the same V value, so this is not two different equipotentials crossing (that is still forbidden).
Verify: E total = 0 exactly by symmetry ✓. V origin = 2 × 179.8 = 359.6 V ✓ (twice the single-charge value at 0.10 m ).
+ Q = + 2 nC at the origin (Ex 1). A charge q = + 5 nC is dragged from point A = ( 0.30 , 0 ) m to point B = ( 0 , 0.30 ) m along the circular arc r = 0.30 m . Find the work done by the electric force.
Forecast: Guess the work before computing. Does the curvy path matter?
Step 1 — Are A and B on the same equipotential? Both are at r = 0.30 m , so both have V = 59.9 V (from Ex 1). Yes — same sphere.
Why this step? The whole point of the equipotential is that "same V " is all that matters.
Step 2 — Apply the work formula.
W A B = q ( V A − V B ) = q ( 59.9 − 59.9 ) = 0 J .
Why this step? The electric force is conservative (Work and Conservative Forces ): work depends only on endpoints, and here the endpoints tie.
Step 3 — Geometric echo. Along the arc, every step d l is tangent to the sphere, and E is radial (normal). Their dot product E ⋅ d l = 0 at every point, so no work accumulates — consistent with Step 2.
Why this step? It connects the algebra (V A = V B ) back to the geometry (perpendicularity) — the two are the same fact.
Verify: W = 5 × 1 0 − 9 × ( 59.9 − 59.9 ) = 0 ✓. Any other path on the same sphere gives 0 too — path length is irrelevant.
+ Q = + 2 nC , draw equipotentials at V = 60 , 30 , 15 V (each half the previous). Find their radii and comment on the spacing as r → ∞ and r → 0 .
Forecast: As you halve the voltage, does the gap between spheres grow, shrink, or stay equal?
Step 1 — Invert V ( r ) to get radii. From V = r k Q (with k Coulomb's constant, so k Q = 17.98 V⋅m ):
r = V k Q .
Why this step? We want the positions of the surfaces to measure their spacing.
Step 2 — Compute.
r 60 = 60 17.98 = 0.300 m , r 30 = 30 17.98 = 0.599 m , r 15 = 15 17.98 = 1.199 m .
Gaps: r 30 − r 60 = 0.299 m , then r 15 − r 30 = 0.599 m — doubling each time .
Why this step? This makes the spreading concrete.
Step 3 — The two limits.
As r → ∞ (V → 0 + ): spheres spread farther and farther apart for equal Δ V → field weakens toward 0 (E ∼ 1/ r 2 ).
As r → 0 (V → ∞ ): spheres crowd infinitely close → field blows up. The point charge is a singular ("infinitely steep") spot.
Why this step? These are the boundary inputs the matrix insists on — the reader now knows what happens at the extremes, not just in the comfortable middle.
Verify: Ratio check — halving V doubles r : r 30 / r 60 = 0.599/0.300 = 2.00 ✓, r 15 / r 30 = 1.199/0.599 = 2.00 ✓.
Worked example A solid metal sphere of radius
R = 0.05 m carries Q = + 2 nC . Find V everywhere inside and the surface value, and explain the field direction just outside. See Conductors in Electrostatic Equilibrium .
Forecast: Is the inside of the metal at a lower, higher, or equal potential compared with its surface?
Step 1 — Inside a conductor E = 0 . Free electrons rearrange until no field remains inside (electrostatic equilibrium).
Why this step? E = 0 is the starting axiom for conductors.
Step 2 — Zero field ⇒ constant V . Since E = − d V / d n = 0 everywhere inside, V cannot change: the entire sphere, surface included, is one equipotential .
V surface = R k Q = 0.05 17.98 = 359.6 V .
Why this step? Outside a charged sphere the field is that of a point charge, so V = k Q / r ; evaluating at r = R gives the constant interior value.
Step 3 — Field just outside is perpendicular. The surface is an equipotential, so E (which is ⊥ every equipotential) must meet the metal at exactly 9 0 ∘ . Any tangential component would shove the surface charges until it cancelled.
Why this step? This is why field lines strike metal at right angles — the whole reason this topic matters in real devices.
Verify: V surface = 17.98/0.05 = 359.6 V ✓. Note it matches Ex 4's origin value coincidentally because both used k Q and a 0.10 /0.05 -type ratio; here r = R = 0.05 .
Worked example An air-gap capacitor in a smoke detector has plates
2.0 mm apart across 9.0 V . (a) What is the field between the plates? (b) A dust particle carrying q = + 1.6 × 1 0 − 19 C is moved fully from the low plate to the high plate — how much work does the external agent do against the field? (c) How far apart are the 3.0 V equipotential sheets?
Forecast: Will the work be positive or negative for an external agent pushing a + charge toward the high plate?
Step 1 — Field (uniform).
E = d V = 2.0 × 1 0 − 3 9.0 = 4500 V/m .
Why this step? Parallel plates ⇒ uniform field ⇒ the simple ratio E = − d V / d n becomes total drop over the gap.
Step 2 — Work by external agent. Moving + q from the low plate (V = 0 ) to the high plate (V = 9.0 V ), the field does W field = q ( V A − V B ) = q ( 0 − 9.0 ) . The agent does the opposite:
W agent = q ( V B − V A ) = ( 1.6 × 1 0 − 19 ) ( 9.0 ) = 1.44 × 1 0 − 18 J .
Positive — the agent must push a + charge up the potential hill.
Why this step? Sign discipline: agent work = + q Δ V against the field.
Step 3 — Spacing of 3.0 V sheets.
Δ x = 4500 3.0 = 6.67 × 1 0 − 4 m = 0.667 mm .
Three sheets fill the 2.0 mm gap.
Why this step? Equal-Δ V spacing again — the everyday capacitor picture.
Verify: 3 × 0.667 mm = 2.0 mm = d ✓. W agent = 1.6 × 1 0 − 19 × 9.0 = 1.44 × 1 0 − 18 J ✓. Units: C ⋅ V = J ✓.
Worked example Between two plates, the left plate is at
V = + 40 V and the right at V = + 10 V , separated by d = 0.020 m . A student writes "E points from left to right because left is more positive... wait, or is it the other way?" Find E 's magnitude and correct direction.
Forecast: Left plate is at higher potential. Does E point away from it or toward it?
Step 1 — Magnitude.
E = d ∣ V left − V right ∣ = 0.020 ∣40 − 10∣ = 0.020 30 = 1500 V/m .
Why this step? Only the potential difference and the gap set the strength; the absolute values (40 vs 10 ) don't matter.
Step 2 — Direction from E = − ∇ V . The field points downhill in V , i.e. from the higher-potential left plate (40 V ) toward the lower-potential right plate (10 V ) — so left → right . See Gradient and Directional Derivative : − ∇ V points toward decreasing V .
Why this step? The trap is thinking "+ plate repels, so field goes... ?" The clean rule is always "field points from high V to low V ", no repulsion story needed.
Step 3 — Perpendicularity check. Equipotentials here are vertical planes (x = const ); E is horizontal (along x ) — meets them at 9 0 ∘ . ✓
Verify: E = 30/0.020 = 1500 V/m ✓. Direction: high→ low = left→ right ✓. (Had both plates been negative , say − 40 and − 10 , the field would still point from − 40 toward − 10 , i.e. toward the less negative plate — the absolute sign never enters, only the difference.)
Recall Quick self-test across the matrix
Sign flip changes what about a point charge's equipotentials? ::: Only the field direction (and the sign of V ); the spherical shape is unchanged.
At a zero-field saddle point, is E ⊥ equipotential? ::: Vacuously yes — there is no field direction, so no violation; and the crossing hyperbolas are the same V , not two different surfaces.
Work sliding a charge along one equipotential? ::: Zero, for any path — the force is conservative and V A = V B .
As r → ∞ for a point charge, equal-Δ V spheres get... ::: farther apart (field weakens as 1/ r 2 ).
Direction of E between plates at + 40 V and + 10 V ? ::: From the 40 V plate toward the 10 V plate (high V → low V ).
Mnemonic The whole page in one line
Shape from the r -dependence, direction from the sign, strength from the spacing, work from the endpoints.