In Section 3.1.4, I proved that the electrostatic potential at any point

in a charge-free region is equal to its average value over any spherical surface

(radius R )centered at .Here's an alternative argument that does not rely on Coulomb's law, only on Laplace's equation. We might as well set the origin at P .Let Vave(R)be the average; first show that

dVavedR=14πR2V.da

(note that the R2in da cancels the 1/R2out front, so the only dependence on R

is in itself). Now use the divergence theorem, and conclude that if Vsatisfies

Laplace's equation, then,Vave(0)=V(P),forallR18.

Short Answer

Expert verified

It is proved that the electrostatic potential at any point P in a charge-free region is equal to its average value over any spherical surface (radius) centered at P.

Step by step solution

01

Define function

The electrostatic potential at any point P is equal to the average over any spherical surface centered at point P.

Vavg=14πR2sVDS …… (1)

Here, Vavgis the average potential, R is the radius of the sphere, dS is the small elemental surface of the sphere and V is the potential through the elemental surface area.

02

Determine the electrostatic potential at any point in a charge-free region     is equal to its average value over any spherical surface(radius ) centered at

Write the expression for the three dimensional for the element surface area of the sphere.

dS=R2sinθdθdϕ …… (2)

Here, dθand dϕare the angles of space length in xy (horizontal) and yz (vertical) direction.

Now, substitute role="math" localid="1657519318035" R2sinθdθϕfordSinequation(1).

Vavg=14πR2sVR,θ,ϕR2sinθdθdϕ=14πsVR,θ,ϕsinθdθdϕTakethederivationoftheequation(1)withrespecttoR.dVavgdR=ddR14πR2sVR,θ,ϕR2sinθdθdϕ=14πR2sVRR2sinθdθdϕ=14πR2sV.r^R2sinθdθdϕ=14πR2sVR2sinθdθdϕr^SubstituteR2sinθdθdϕfordSinaboveequationdVavgdR=14πR2sVdS.......(3)Hence,thederivativeofaveragevolumeisdVavgdR=14πR2sVdS.

03

Use divergence theorem

Use the divergence theorem,

Write the expression foe divergence theorem.

.AdV=A.dS

Applying divergence theorem to equation (3),

dVavgdR=14πR2v2VdV

Through R increases, if the average potential Vavgkept constant, then it remains as constant for increasing R.

As ,R0,

It becomes true and satisfies Laplace equation and gives the result as,

VavgR=Vavg0=VP

Hence proved.

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Most popular questions from this chapter

A "pure" dipoleρis situated at the origin, pointing in thezdirection.

(a) What is the force on a point charge q at (a,0,0)(Cartesian coordinates)?

(b) What is the force on q at (0,0,a)?

(c) How much work does it take to move q from(a,0,0)to (0,0,a)?

Four particles (one of charge q,one of charge 3q,and two of charge -2q)are placed as shown in Fig. 3.31, each a distance from the origin. Find a

simple approximate formula for the potential, valid at points far from the origin.

(Express your answer in spherical coordinates.)

(a) A long metal pipe of square cross-section (side a) is grounded on three sides, while the fourth (which is insulated from the rest) is maintained at constant potential V0.Find the net charge per unit length on the side oppositeto Vo. [Hint:Use your answer to Prob. 3.15 or Prob. 3.54.]

(b) A long metal pipe of circular cross-section (radius R) is divided (lengthwise)

into four equal sections, three of them grounded and the fourth maintained at

constant potential Vo.Find the net charge per unit length on the section opposite

to V0.[Answer to both (a) and (b) : localid="1657624161900" -ε0V0ττIn2.]

A solid sphere, radius R, is centered at the origin. The "northern" hemisphere carries a uniform charge density ρ0, and the "southern" hemisphere a uniform charge density -ρ0• Find the approximate field E(r,θ)for points far from the sphere (r>>R).

In Prob. 2.25, you found the potential on the axis of a uniformly charged disk:

V(r,0)=σ2ε0(r2+R2-r)

(a) Use this, together with the fact that PI(1)=1, to evaluate the first three terms

in the expansion (Eq. 3.72) for the potential of the disk at points off the axis, assuming r>R.

(b) Find the potential for r<Rby the same method, using Eq. 3.66. [Note: You

must break the interior region up into two hemispheres, above and below the

disk. Do not assume the coefficientsAIare the same in both hemispheres.]

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