Problem Set 3 Solution Phys 182 - Fall 2010 Assigned: Friday, Sept. 17 Due: Friday, Sept. 24 1 Griffiths 3.1 √ The argument is exactly the same as in Griffiths section 3.1.4, except that since z < R, z 2 + R2 − 2zR = q 1 q 1 (R − z) instead of (z − R). Hence Vavg = 4πǫ [(z + R) − (R − z)] = 4πǫ . If there is more than one 0 2zR 0 R 1 Qenc charge inside the sphere, the average potential due to interior charges is 4πǫ0 R , and the average due to Qenc the exterior charges is Vcenter , so Vavg = Vcenter + 4πǫ . 0R 2 Griffiths 3.2 A stable equilibrium is a point of local minimum in the potential energy. Here the potential energy is qV . But we know that Laplace’s equation allows no local minima for V. What looks like a minimum in the figure must in fact be a saddle point, and the box ’leaks’ through the center of each face. 3 Griffiths 3.6 Place image charges +2q at z = −d and −q at z = −3d. Total force on +q is: 1 q2 1 1 q 2q −q 1 −2q 29q 2 ẑ = − ẑ = − + − ẑ F= + + 4πǫ0 (2d)2 (4d)2 (6d)2 4πǫ0 d2 2 8 36 4πǫ0 72d2 4 Griffiths 3.7 (a) From Fig. 3.13: ı = √ √ r2 + a2 − 2ra cos θ; ı′ = r2 + b2 − 2rb cos θ.Therefore: R2 q R q′ √ , while b = = − ı′ a r2 + b2 − 2rb cos θ a q q = − q = −q 4 R2 a ar 2 r2 + R + R2 − 2ra cos θ R a2 − 2r a cos θ R Clearly, when r = R, V → 0. 1 (b) σ = −ǫ0 ∂V ∂n . In this case, ∂V ∂n = ∂V ∂r at the point r = R. Therefore: 2 1 2 ra 2 a −1 2 −ǫ0 q 2 −3/2 −3/2 2r − 2a cos θ (r + a − 2ra cos θ) (2r − 2a cos θ) + (R + ( ) − 2ra cos θ) σ(θ) = 4πǫ0 2 2 R R2 r=R 2 a q −(R2 + a2 − 2Ra cos θ)−3/2 (R − a cos θ) + (R2 + a2 − 2Ra cos θ)−3/2 =− − a cos θ 4π R a2 q (R2 + a2 − 2Ra cos θ)−3/2 R − a cos θ − + a cos θ = 4π R q 2 2 2 2 −3/2 = (R − a )(R + a − 2Ra cos θ) Z4πR Z q Induced = σda = (R2 − a2 ) (R2 + a2 − 2Ra cos θ)−3/2 R2 sin θdθdφ 4πR π −1 2 q (R2 − a2 )2πR2 (R + a2 − 2Ra cos θ)−1/2 = 4πR Ra 0 1 1 q 2 2 (a − R ) √ −√ = 2a R2 + a2 + 2Ra R2 + a2 − 2Ra p But a > R (else q would be inside), so R2 + a2 − 2Ra = a − R q 2 q 1 q 1 2 = = (a − R ) − [(a − R) − (a + R)] = (−2R) 2a a+R a−R 2a 2a qR = q′ =− a (c) The force on q due to the sphere is the same as the force of the image charge q ′ : R 2 qq ′ 1 1 q 2 Ra 1 1 − = = − q F = 4πǫ0 (a − b)2 4πǫ0 a (a − R2 /a)2 4πǫ0 (a2 − R2 )2 To bring q in from infinity to a, we do work: a Z q2 R a 1 1 q2 R q2 R 1 a′ ′ W = − da = = − 4πǫ0 ∞ (a′2 − R2 )2 4πǫ0 2 (a′2 − R2 ) ∞ 4πǫ0 2(a2 − R2 ) 5 Griffiths 3.9 (a) Image problem: λ above, −λ below. Taking an arbitrary point of reference at s = a. λ The potential of λ is V+ = − 2πǫ ln 0 λ The potential of −λ is V− = 2πǫ0 ln s+ a , s− a , where s+ is distance from λ. where s− is distance from −λ. s− λ ln Total V = 2πǫ s+ . p 0 p 2 2 , and s = y 2 + (z + d)2 , so and s+ = y + (z − d) − 2 2 +(z+d) λ ln yy2 +(z−d) V = 4πǫ 2 0 2 ∂V ∂V ∂V . Here = , evaluated at z = 0. ∂n ∂n ∂z 2(z − d) 2(z + d) λ − 2 σ(y) = −ǫ0 4πǫ0 y 2 + (z + d)2 y + (z − d)2 z=0 2λ λd d −d =− =− − 2 4π y 2 + d2 y + d2 π(y 2 + d2 ) (b) σ = −ǫ0 6 Griffiths 3.10 Image charges: −q at (a, −b) and (−a, b); q at (−a, −b). " 1 q 1 p V (x, y) = +p 2 2 2 2 4πǫ0 (x − a) + (y − b) + z (x + a) + (y + b)2 + z 2 # 1 1 −p −p (x + a)2 + (y − b)2 + z 2 (x − a)2 + (y + b)2 + z 2 2 1 1 1 q − x̂ − ŷ + √ [cos θx̂ + sin θŷ] F= 4πǫ0 (2a)2 (2b)2 (2 a2 + b2 )2 p p where cos θ = a/ a2 + b2 , sin θ = b/ a2 + b2 b a q2 1 1 = − 2 x̂ + − 2 ŷ 16πǫ0 a b (a2 + b2 )3/2 (a2 + b2 )3/2 1 1 −q 2 −q 2 q2 W = 2 +2 +2 √ 4 4πǫ0 (2a) (2b) (2 a2 + b2 ) q2 1 1 1 √ = − − 16πǫ0 a b a2 + b 2 For this to work, θ must be an integer divisor of 180◦ . Thus 180◦ , 90◦ , 60◦ , 45◦ , etc work, but no others. 7 Griffiths 3.15 The boundary conditions are: (i) V = 0 when x = 0, (ii) V = 0 when x = a, (iii) V = 0 when y = 0, (iv) (v) (vi) V = 0 when y = a, V = 0 when z = 0, V = V0 when z = a. We want sinusoidal functions in x and y, exponential in z: X(x) = A sin (kx) + B cos (kx) , Y (y) = C sin (ly) + D cos (ly) , Z(z) = Ee √ k2 +l2 z + Ge− √ k2 +l2 z (i) ⇒ B = 0; (ii) ⇒ k = nπ/a; (iii) ⇒ D = 0; (iv) ⇒ l = mπ/a; (v) ⇒ E + G = 0. Therefore p Z(z) = 2E sinh (π n2 + m2 z/a) 3 Putting this all together, and combining the constants, we have: V (x, y, z) = ∞ X ∞ X Cn,m sin (nπx/a) sin (mπy/a) sinh (π n=1 m=1 p n2 + m2 z/a) Evaluate Cn,m by imposing boundary condition (vi): i p XXh Cn,m sinh (π n2 + m2 ) sin (nπx/a) sin (mπy/a) V0 = From Eqns. 3.50 and 3.51: Cn,m sinh (π Therefore V (x, y, z) = p 2 Z a Z a if n or m is even, 0, 2 n 2 + m2 ) = V0 sin (nπx/a) sin (mπy/a)dxdy 16V0 a , if both are odd. 0 0 π 2 nm 16V0 π2 √ 1 sinh (π n2 + m2 z/a) √ sin (nπx/a) sin (mπy/a) nm sinh (π n2 + m2 ) n=1,3,5... m=1,3,5... X X 3.71-¿3.72 8 Griffiths 3.18 The polynomial is odd, so we only need P1 and P3 . V0 (θ) = k cos (3θ) = k[4 cos3 θ − 3 cos θ] = k[αP3 (cos θ) + βP1 (cos θ)] 1 5α 3 3 3 3 4 cos (θ) − 3 cos θ = α (5 cos (θ) − 3 cos θ) + β cos θ = cos θ + β − α cos θ 2 2 2 3 8 so: α = ; β = − 5 5 k and V0 (θ) = [8 cos3 θ − 3 cos θ] 5 ∞ X Al rl Pl (cos θ) sin θ), for r < R l=0 Now V (r, θ) = ∞ X Bl Pl (cos θ), for r > R rl+1 l=0 where Z 2l + 1 π V0 (θ)Pl (cos θ) sin θdθ 2Rl 0 Z π Z π 2l + 1 k 8 P (cos θ)P (cos θ) sin θdθ − 3 P (cos θ)P (cos θ) sin θdθ = 3 l 1 l 2Rl 5 0 0 2 2 k 2l + 1 8 δl3 − 3 δl1 = 5 2Rl 2l + 1 2l + 1 k 1 = [8δl3 − 3δl1 ] 5 Rl Al = 4 From continuity of V at R, we have Bl = Al R2l+1 ,so Bl = k 1 [8δl3 − 3δl1 ] 5 Rl+1 Therefore 3 r r k 8 P (cos θ) , r≤R P (cos θ) − 3 1 3 5 R R " # V (r, θ) = 2 4 k R R 8 P3 (cos θ) − 3 P1 (cos θ) , r ≥ R 5 r r Or k r r 2 2 [5 cos θ − 3] − 3 , r≤R cos θ 4 5 R R " # 2 V (r, θ) = 2 R k R 2 cos θ 4 [5 cos θ − 3] − 3 , r ≤ R 5 r r Finally σ(θ) = ǫ0 ∞ X (2l + 1)Al Rl−1 Pl (cos θ) t=0 epsilon0 k [−9P1 (cos θ) + 56P3 (cos θ)] 5R epsilon0 k cos θ[140 cos2 θ − 93] = 5R = 9 Griffiths 3.19 From Eq. 3.83 and 3.69: σ(θ) = ǫ0 ∞ X (2l + 1)Al Rl−1 Pl (cos θ) , Al = t=0 2l + 1 2Rl Z π V0 (θ)Pl (cos θ) sin θdθ 0 So we have: σ(θ) = 10 ∞ ǫ0 X (2l + 1)2 Cl Pl (cos θ) , with Cl = 2R t=0 Z π V0 (θ)Pl (cos θ) sin θdθ 0 Griffiths 3.20 Set V=0 on the equatorial plane, far from the sphere. Then the potential is the same as Ex. 3.8 plus the potential of a uniformly charged spherical shell: R2 1 Q V (r, θ) = −E0 r − 2 cos θ + r 4πǫ0 r 5