Intuition What this page does
The parent note gave you five formulas. This page exercises every one of them across every case that can appear : positive and negative charge, the "obvious" limits (very close, very far, dead centre), the degenerate zeros, a real-world word problem, and an exam twist that hides two ideas in one. Work each one before reading the solution — the "Forecast" line is where the learning happens.
All symbols here were built in the parent topic ; if a symbol feels new, that note defines it.
Throughout, k ≡ 4 π ε 0 1 ≈ 8.99 × 1 0 9 N⋅m 2 / C 2 and ε 0 ≈ 8.85 × 1 0 − 12 C 2 / ( N⋅m 2 ) .
Every problem this topic can throw is one of these cells. Each worked example below is tagged with the cell it fills.
#
Cell (the scenario)
Which formula
Example
A
Point charge, positive , plain distance
k q / r 2
Ex 1
B
Point charge, negative — direction/sign
k q / r 2 , direction
Ex 2
C
Two point charges — vector superposition, a component cancels
∫ d E
Ex 3
D
Dipole, axial vs equatorial compared
2 k p / r 3 , k p / r 3
Ex 4
E
Ring, general point + the two limits (x = 0 , x ≫ R ) + max
k Q x / ( R 2 + x 2 ) 3/2
Ex 5
F
Disk general , and its degenerate infinite-sheet limit
2 ε 0 σ [ 1 − R 2 + x 2 x ]
Ex 6
G
Infinite line — real-world word problem
2 k λ / r
Ex 7
H
Exam twist : two sheets (capacitor-like), fields add vs cancel
σ /2 ε 0 superposed
Ex 8
A charge q = + 5.0 nC sits at the origin. Find the field magnitude at r = 0.20 m .
Forecast: small charge, tiny distance — do you expect thousands, or millions, of N/C? Guess the power of ten before computing.
Step 1. Use the point-charge law E = r 2 k q .
Why this step? A single point charge is the "atom" — no integration, just plug in. Nothing here breaks the sphere symmetry, so the formula applies directly.
Step 2. Substitute: q = 5.0 × 1 0 − 9 C , r = 0.20 m , r 2 = 0.040 m 2 .
E = 0.040 ( 8.99 × 1 0 9 ) ( 5.0 × 1 0 − 9 ) = 0.040 44.95 ≈ 1124 N/C .
Why this step? Just arithmetic — but keeping the 1 0 9 and 1 0 − 9 visible shows they cancel, so the answer lands near 1 0 3 , matching a sensible forecast.
Step 3. Direction: radially outward , since q > 0 .
Why this step? Sign of q sets direction; magnitude alone is an incomplete answer for a vector field.
Verify: Units: m 2 N⋅m 2 / C 2 ⋅ C = N/C . ✓ Order of magnitude ∼ 1 0 3 N/C matches forecast.
Charge q = − 3.0 nC is at the origin. What is the field at a point P located 0.10 m to the right (+ x ) of it? Give magnitude and direction.
Forecast: magnitude only depends on ∣ q ∣ — but which way does the arrow at P point?
Step 1. Magnitude uses ∣ q ∣ : E = r 2 k ∣ q ∣ .
Why this step? The formula's q carries a sign, but "how strong" is set by size, not sign. Splitting size from direction avoids losing the minus sign in arithmetic.
E = ( 0.10 ) 2 ( 8.99 × 1 0 9 ) ( 3.0 × 1 0 − 9 ) = 0.010 26.97 ≈ 2697 N/C .
Step 2. Direction: field of a negative charge points toward it.
Why this step? Field lines terminate on negative charge. P is on the + x side, so the field there points back toward the origin, i.e. in − x .
Verify: If we had used the point-charge test-charge idea — a hypothetical + 1 C at P would be pulled toward the negative charge — the force (hence field) is − x . ✓ Magnitude ≈ 2.7 × 1 0 3 N/C .
Two charges + q and + q (q = 4.0 nC ) sit on the x -axis at x = ± 0.30 m . Find the field at P = ( 0 , 0.40 ) m on the y -axis.
Forecast: by symmetry, will the field at P point along x , along y , or diagonally? Decide before computing.
Step 1. Each charge is a distance r = 0.3 0 2 + 0.4 0 2 = 0.50 m from P (a 3-4-5 triangle — see figure).
Why this step? The distance sets each individual magnitude via k q / r 2 ; the clean 3-4-5 keeps arithmetic honest.
Step 2. Magnitude of each: E 1 = r 2 k q = 0.25 ( 8.99 × 1 0 9 ) ( 4.0 × 1 0 − 9 ) = 143.8 N/C .
Why this step? Both charges are equal and equidistant, so E 1 = E 2 — this equality is exactly what makes a component cancel.
Step 3. Resolve. The x -components are equal and opposite → cancel. The y -components add. The y -fraction is cos θ = 0.50 0.40 = 0.80 (see the red arrow's vertical shadow in the figure).
Why this step? This is superposition's "silent hero" r ^ : choose the axis where symmetry does the work, so only one component survives.
E P = 2 E 1 cos θ = 2 ( 143.8 ) ( 0.80 ) = 230.1 N/C , along + y .
Verify: Direction is straight up (+ y ) — matches the "mirror symmetry across the y -axis kills the horizontal part" forecast. Units N/C. ✓
A dipole has p = 6.0 × 1 0 − 30 C⋅m (a water-molecule-scale value). Find the far field at r = 1.0 × 1 0 − 9 m on the axis and on the equator , and confirm the axial field is exactly twice the equatorial.
Forecast: which is larger — axial or equatorial? By how much?
Step 1. Axial: E a x = r 3 2 k p .
Why this step? On the axis the near charge dominates and the two fields point the same way, so the factor is 2 . We use r 3 (not r 2 ) because the two nearly-equal charges cancel their leading 1/ r 2 terms — the parent note's key dipole fact.
E a x = ( 1.0 × 1 0 − 9 ) 3 2 ( 8.99 × 1 0 9 ) ( 6.0 × 1 0 − 30 ) = 1.0 × 1 0 − 27 1.0788 × 1 0 − 19 ≈ 1.079 × 1 0 8 N/C .
Step 2. Equatorial: E e q = r 3 k p (half of axial).
Why this step? On the bisector the axial components add but only carry a factor 1 (not 2 ), and they point opposite to p (see figure). Same r 3 law.
E e q = 1.0 × 1 0 − 27 ( 8.99 × 1 0 9 ) ( 6.0 × 1 0 − 30 ) ≈ 5.394 × 1 0 7 N/C .
Step 3. Ratio E a x / E e q = 2 exactly.
Why this step? Confirms the structural fact — it's not a coincidence of these numbers, it's the 2 vs 1 in the formulas.
Verify: 1.079 × 1 0 8 /5.394 × 1 0 7 = 2.00 . ✓ Axial wins, forecasted correctly.
A ring of radius R = 0.10 m carries Q = 8.0 nC . Find E (a) at x = 0.20 m on the axis, (b) at the centre x = 0 , (c) as x → ∞ (show it becomes a point charge), and (d) locate the axial position of maximum field.
Forecast: will the centre give the biggest field (you're closest to all the charge) — or zero?
Step 1 (a). E = ( R 2 + x 2 ) 3/2 k Q x with R 2 + x 2 = 0.01 + 0.04 = 0.05 .
Why this step? Only the axial component of each d q survives; every d q shares the same cos θ = x / R 2 + x 2 , so it pulls out of the integral, leaving this closed form.
( R 2 + x 2 ) 3/2 = 0.0 5 1.5 = 0.011180 , E = 0.011180 ( 8.99 × 1 0 9 ) ( 8.0 × 1 0 − 9 ) ( 0.20 ) ≈ 1286 N/C .
Step 2 (b). At x = 0 : the numerator has a factor x = 0 , so E = 0 .
Why this step? By symmetry every radial pull from opposite sides of the ring cancels — closeness loses to symmetry. This is the exact mistake the parent note warns about.
Step 3 (c). For x ≫ R : ( R 2 + x 2 ) 3/2 → x 3 , so E → k Q x / x 3 = k Q / x 2 — a point charge.
Why this step? From far away the ring's radius is invisible; the field must reduce to the atom-of-everything law. A good limit check.
Step 4 (d). Maximum at x = R / 2 = 0.10/ 2 ≈ 0.0707 m (from setting d E / d x = 0 ; see the peak in the figure).
Why this step? The field grows from 0 at the centre, peaks, then falls off — so the max sits at an interior point, not at the centre.
Verify (d): Plugging x = R / 2 : field there ≈ 2769 N/C , larger than the x = 0.20 value — consistent with a peak nearer the ring. ✓
A disk of radius R = 0.050 m has σ = 2.0 × 1 0 − 6 C/m 2 . Find E (a) at x = 0.050 m on the axis, and (b) the limit x ≪ R (infinite-sheet value).
Forecast: at x = R (halfway "out" relative to the disk size) — will the field be near the full sheet value σ /2 ε 0 , or noticeably less?
Step 1 (a). E = 2 ε 0 σ [ 1 − R 2 + x 2 x ] .
Why this step? The disk is nested rings; integrating the ring result gives this bracket. The [ ⋯ ] is the "finite-size correction" that a real disk carries and an infinite sheet loses.
2 ε 0 σ = 2 ( 8.85 × 1 0 − 12 ) 2.0 × 1 0 − 6 = 1.130 × 1 0 5 N/C .
R 2 + x 2 x = 0.0025 + 0.0025 0.050 = 0.0707 0.050 = 0.7071.
E = 1.130 × 1 0 5 ( 1 − 0.7071 ) = 1.130 × 1 0 5 ( 0.2929 ) ≈ 3.310 × 1 0 4 N/C .
Step 2 (b). As x ≪ R : R 2 + x 2 x → 0 , bracket → 1 , so E → 2 ε 0 σ = 1.130 × 1 0 5 N/C .
Why this step? Close to a big disk you can't tell it's finite — it looks infinite. WHY constant: backing away reveals more sheet, which cancels the 1/ r 2 falloff exactly.
Verify: At x = R the field (3.3 × 1 0 4 ) is only ≈ 29% of the sheet value (1.13 × 1 0 5 ) — so the forecast "noticeably less" is right; edge effects matter once x is comparable to R . ✓
A long straight power-line wire carries a linear charge density λ = 3.0 × 1 0 − 7 C/m . A bird lands r = 2.0 m away. What field magnitude does it sit in, and which direction does the field point?
Forecast: compared to a point charge's 1/ r 2 , a line's 1/ r falls off slower . Should the field feel weaker or stronger than "your intuition from point charges" at a few metres?
Step 1. Use Gauss's cylindrical result E = 2 π ε 0 r λ = r 2 k λ .
Why this step? Cylindrical symmetry lets E leave the flux integral (only the curved wall contributes) — so we get a clean formula without integrating, unlike a ring.
E = 2.0 2 ( 8.99 × 1 0 9 ) ( 3.0 × 1 0 − 7 ) = 2.0 5394 ≈ 2697 N/C .
Step 2. Direction: radially outward, perpendicular to the wire (since λ > 0 ).
Why this step? The field of a line points away from the line along the shortest (perpendicular) path — the same direction the Gaussian cylinder's curved normal points.
Verify: Halving the distance to 1.0 m should double E (because 1/ r , not 1/ r 2 ): 2 × 2697 = 5394 N/C — that's exactly 2 k λ /1.0 . ✓ Slower falloff confirmed.
Two large parallel sheets carry + σ and − σ with σ = 4.0 × 1 0 − 6 C/m 2 . Find the field (a) between the sheets and (b) outside them.
Forecast: the "twist" — do the two single-sheet fields (σ /2 ε 0 each) add or cancel between the plates? Outside?
Step 1. Each isolated sheet makes E 1 = 2 ε 0 σ pointing away from + σ and toward − σ .
Why this step? A single sheet is the degenerate disk limit; its field is uniform, so the whole problem is a superposition of two known uniform fields.
E 1 = 2 ( 8.85 × 1 0 − 12 ) 4.0 × 1 0 − 6 = 2.260 × 1 0 5 N/C .
Step 2 (a) — between: both fields point the same way (from + toward − ), so they add:
E in = 2 E 1 = ε 0 σ = 4.520 × 1 0 5 N/C .
Why this step? This is the capacitor field σ / ε 0 — the missing factor of 2 the parent note flags as a common mistake, recovered here by counting both sheets, not both faces of one.
Step 3 (b) — outside: the two fields point in opposite directions and cancel:
E out = E 1 − E 1 = 0.
Why this step? Outside, you're on the far side of both sheets; the + sheet pushes out while the − sheet pulls in — equal magnitudes, opposite signs.
Verify: E in = σ / ε 0 = 4.0 × 1 0 − 6 /8.85 × 1 0 − 12 = 4.520 × 1 0 5 N/C = 2 × 2.260 × 1 0 5 . ✓ And E out = 0 , matching an ideal Parallel plate capacitor . ✓
Recall Why is the ring's field zero at its centre but not at
x = R / 2 ?
At the centre ::: every d q has an opposite partner pulling equally the other way, so all field vectors cancel — symmetry beats closeness; the field then rises to a maximum at x = R / 2 before decaying as 1/ x 2 .
Recall Between two oppositely-charged sheets the field is
σ / ε 0 , outside it is what?
Zero ::: the two single-sheet fields (σ /2 ε 0 each) add inside but cancel outside.
Mnemonic Direction shortcut
Positive charge → arrows out ; negative charge → arrows in . Magnitude never carries the sign — direction does. Compute size with ∣ q ∣ , then place the arrow by the charge's sign.
Related: Gauss's law · Coulomb's law · Flux and field lines · Electric dipole in a uniform field · Electric potential .