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Formulas/physics/Electric Charges Fields/Field on Axis of Uniformly Charged Disc

Field on Axis of Uniformly Charged Disc

Field at axial distance x from centre of a disc of radius R and surface charge density σ. Reduces to infinite plane result (σ/2ε₀) as R→∞.
Class 12
Derivation

Setup

A disc of radius RR has uniform surface charge density σ\sigma. Treat the disc as a collection of concentric rings, each of radius rr' and width drdr'.

Charge on a ring of radius rr':

dq=σ2πrdrdq = \sigma \cdot 2\pi r'\, dr'

Using the ring result

From the axial field of a ring (formula ef22-field-ring-axis), the contribution from ring rr' at axial point xx:

dE=dqx4πε0(x2+r2)3/2=σxrdr2ε0(x2+r2)3/2dE = \frac{dq \cdot x}{4\pi\varepsilon_0(x^2 + r'^2)^{3/2}} = \frac{\sigma x\, r'\, dr'}{2\varepsilon_0(x^2 + r'^2)^{3/2}}

Integration

E=0Rσxr2ε0(x2+r2)3/2drE = \int_0^R \frac{\sigma x\, r'}{2\varepsilon_0(x^2 + r'^2)^{3/2}}\, dr'

Substitute u=x2+r2u = x^2 + r'^2, du=2rdrdu = 2r'\, dr':

E=σx4ε0x2x2+R2u3/2du=σx4ε0[2u1/2]x2x2+R2E = \frac{\sigma x}{4\varepsilon_0}\int_{x^2}^{x^2+R^2} u^{-3/2}\, du = \frac{\sigma x}{4\varepsilon_0}\left[-2u^{-1/2}\right]_{x^2}^{x^2+R^2} E=σx2ε0[1x1x2+R2]E = \frac{\sigma x}{2\varepsilon_0}\left[\frac{1}{x} - \frac{1}{\sqrt{x^2+R^2}}\right] E=σ2ε0(1xx2+R2)\boxed{E = \frac{\sigma}{2\varepsilon_0}\left(1 - \frac{x}{\sqrt{x^2+R^2}}\right)}

Limiting cases

Infinite plane (RR \to \infty): x/x2+R20x/\sqrt{x^2+R^2} \to 0, so Eσ/2ε0E \to \sigma/2\varepsilon_0. Recovers the infinite sheet result.

Far field (xRx \gg R): expand using (1+R2/x2)1/21R2/2x2(1 + R^2/x^2)^{-1/2} \approx 1 - R^2/2x^2:

Eσ2ε0R22x2=σπR24πε0x2=Q4πε0x2E \approx \frac{\sigma}{2\varepsilon_0} \cdot \frac{R^2}{2x^2} = \frac{\sigma \pi R^2}{4\pi\varepsilon_0 x^2} = \frac{Q}{4\pi\varepsilon_0 x^2}

The disc looks like a point charge at large distances.

At the surface (x0x \to 0): Eσ/2ε0E \to \sigma/2\varepsilon_0, consistent with the plane sheet result.

Remember
This derivation illustrates the general strategy for continuous distributions: reduce to a known result (here, the ring) then integrate over the parameter describing the distribution (here, $r'$).