The Electric Field Due to an Electric Dipole — Question 4

Section 22-4 · Physics pages 3538–3539

Question 4 Equatorial finite-size corrections have the opposite approximation bias At distance r on the perpendicular bisector of a finite dipole, Eexact = kp/(r2 + a2)3/2 in magnitude. The point-dipole estimate is Ed = kp/r3. −q +q r Schematic; labels, not drawing lengths, specify the data. (a) Derive (Ed −Eexact)/Eexact and evaluate it at r = 10a. (b) Find its leading small-a/r form and compare the sign of the approximation bias with the axial case.
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Question 4 - Solution Equatorial finite-size corrections have the opposite approximation bias −q +q r (a) Method and calculation Ed Eexact = (1 + a2/r2)3/2. r = 10a : ϵ = (1.01)3/2 −1 ≈.0150374. (b) Interpretation and further calculation u = a/r ≪1 : (1 + u2)3/2 = 1 + 3 2u2 + O(u4). Ed > Eexact on the perpendicular bisector. Here each real source is farther from P than the center distance r, so the point-dipole estimate is too large. Physical check The axial and equatorial corrections need not have the same sign even for the same dipole.

Question 4

Equatorial finite-size corrections have the opposite approximation bias

At distance rr on the perpendicular bisector of a finite dipole, Eexact=kp/(r2+a2)3/2E_{\mathrm{exact}}=kp/(r^2+a^2)^{3/2} in magnitude. The point-dipole estimate is Ed=kp/r3E_d=kp/r^3.

Diagram shown in the original SVG worksheet.

  1. Derive (Ed−Eexact)/Eexact(E_d-E_{\mathrm{exact}})/E_{\mathrm{exact}} and evaluate it at r=10ar=10a.

  2. Find its leading small-a/ra/r form and compare the sign of the approximation bias with the axial case.

Question 4 - Solution

Equatorial finite-size corrections have the opposite approximation bias

Diagram shown in the original SVG worksheet.

(a) Method and calculation

EdEexact=(1+a2/r2)3/2.\frac{E_d}{E_{\mathrm{exact}}}=(1+a^2/r^2)^{3/2}.r=10a:ϵ=(1.01)3/2−1≈.0150374.r=10a:\quad\epsilon=(1.01)^{3/2}-1\approx.0150374.

(b) Interpretation and further calculation

u=a/r≪1:(1+u2)3/2=1+32u2+O(u4).u=a/r\ll1:\quad(1+u^2)^{3/2}=1+\tfrac32u^2+O(u^4).Ed>Eexacton the perpendicular bisector.E_d>E_{\mathrm{exact}}\quad\text{on the perpendicular bisector}.Here each real source is farther from P than the center distance r, so the point-dipole estimate is too large.

Physical check

The axial and equatorial corrections need not have the same sign even for the same dipole.