Laplace’s Equation on a Spherebanach.millersville.edu/~bob/math467/Projects/2006/Scorzetti.pdf ·...
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Transcript of Laplace’s Equation on a Spherebanach.millersville.edu/~bob/math467/Projects/2006/Scorzetti.pdf ·...
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Laplace’s Equation on a Sphere
Pierre Simon de Laplace
Domenic Scorzetti
Millersville University [email protected]
April 25, 2006
Problem Outline A spherical shell has an inner radius ρ = 1, and an outer radius ρ = 2. The temperatures of the inner and outer surfaces are given by:
θθ cos20100)( −=fi θθ cos3050)( +=fo
a) State the boundary value problem for the steady-state temperature within the shell. b) Find the steady-state temperature inside the shell. c) Plot the steady-state temperature inside the shell for several slices parallel to the shell’s equator. Problem Cross-Section
ρ = 1
ρ = 2
2
a) Problem Statement Finding the steady-state temperature will require the use of the Laplacian operator:
0=∆u
As described above, the solution will be for the region bounded by the two surfaces. Also, note the functional dependence only on θ (in this case used as the angle from the sphere’s north pole) and the absence of φ (azimuthal angle). b) Problem Solution The spherical Laplacian with only a θ component looks like this:
(1) ⎟⎠
⎞⎜⎝
⎛⎟⎟⎠
⎞⎜⎜⎝
⎛∂∂
∂∂+
∂∂
∂∂=∆
θθ
θθρρρ
ρρuuu sin
sin212
21
Since Laplace’s equation is linear and homogeneous, I will begin solving by separation of variables. This assumes )()(),( θρθρ TRu = which is then substituted into (1):
( ) 0'sinsin21'2
21 =
∂∂+
∂∂
⎟⎠⎞⎜
⎝⎛ RTTR θ
θθρρ
ρρ
The primed variables indicate necessary regular derivatives. I continue the process by
multiplying through by RT
θρ 22 sin :
(2) ( ) 0'sinsin'22sin =∂∂+
∂∂
⎟⎠⎞⎜
⎝⎛ T
TR
Rθ
θθρ
ρθ
ρ-Dependent Portion of u To find this part, I begin by dividing equation (2) by sin2θ and rearranging the terms:
(3) ( )'sinsin
1'21 TT
RR
θθθ
ρρ ∂
∂−=∂∂
⎟⎠⎞⎜
⎝⎛
Since the left-hand side only depends on ρ and the right-hand side depends solely on θ, then both sides must equal a constant. For convenience, say this constant has the form m(m + 1) with
3
}0{∪∈ Nm (meaning m is a natural number and can also be zero). Under these assumptions, I am left with an ordinary differential equation for the LHS:
)1('21 +=∂∂
⎟⎠⎞⎜
⎝⎛ mmR
Rρ
ρ
Applying the product rule:
)1('2''21 +=+ ⎥⎦⎤
⎢⎣⎡ mmRR
Rρρ
(4) 0)1('2''2 =+−+ RmmRR ρρ
Equation (4) is Euler’s Equation (see [1]) with a solution which looks like (5), for }0{∪∈ Nm
(5) 1)( −−+= mDmCR ρρρ
θ-Dependent Portion of u Referring back to equation (3), I now isolate the θ component and set it equal to the same constant.
(6) ( ) )1('sinsin
1 +=∂∂− mmT
Tθ
θθ
Once again, apply the product rule:
[ ] )1(cos'sin''sin
1 +=+− mmTTT
θθθ
0)1(sincos''' =+−−− mm
TT
TT
θθ
Multiply through by -1 and T:
(7) 0))1((sincos''' =+++ TmmTTθθ
To further simplify the calculations, I put (7) into another form through a change of variables and by letting θcos=w (see [1]). This will require the chain rule:
(8) dwdT
ddw
dwdT
ddT θ
θθsin−==
⎟⎠
⎞⎜⎝
⎛⎟⎠
⎞⎜⎝
⎛ −==dwdT
dd
ddT
dd
dTd θ
θθθθsin2
2
4
θθθ
θ ddw
dwTd
dwdT
dTd
22
sincos22
−−=
(9) 222sincos2
2
dwTd
dwdT
dTd θθ
θ+−=
Substitute (8) and (9) into (7):
0))1((sinsincoscos2
22sin =++−+− ⎟⎟⎠
⎞⎜⎜⎝
⎛ TmmdwdT
dwdT
dwTd θ
θθθθ
0))1((coscos222sin =++−− Tmm
dwdT
dwdT
dwTd θθθ
0))1((cos2222sin =++− Tmm
dwdT
dwTd θθ
Recall the trigonometric property 1cossin 22 =+ θθ to make the following substitution:
0))1((cos222
)2cos1( =++−− TmmdwdT
dwTd θθ
Also, recall that θcos=w :
(10) 0))1((222
)21( =++−− TmmdwdTw
dwTdw
Note that equation (10) is a Legendre polynomial which has solutions of the form:
(11) Tm(w)
with }0{∪∈ Nm (see [2, Sec. 7.10.3].
m = 0 T0(w) = 1 T0(cosθ) = 1 m = 1 T1(w) = w T1(cosθ) = cosθ m = 2 T2(w) = 0.5(3w2-1) T2(cosθ) = 0.5(3cos2θ -1)
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General Solution This is found by combining equations (5) and (11) inside an infinite series:
(12) )(cos0
)1(),( θρρθρ ∑∞
=−−+=
m mTmmDm
mCu
However, notice my original problem consists of only a finite sum of constants and cosines, so I can find an exact solution with ρ = 1 and ρ = 2 per equation (12). Additionally, I only need to sum through m = 1 since there are no squared cosine terms to account for. ρ = 1
)(cos0
)(cos20100)(),1( θθθθ ∑∞
=+=−==
m mTmDmCfiu
)(cos1)11()(cos0)00(cos20100 θθθ TDCTDC +++=−
By substitution from the solution table above:
(13) θθ cos)11()00(cos20100 DCDC +++=−
ρ = 2
)(cos0
)122(cos3050)(),2( θθθθ ∑∞
=−−+=+==
m mTmmDm
mCfou
)(cos1)1121121()(cos0)120
020(cos3050 θθθ TDCTDC −−++−+=+
)(cos1)141
12()(cos0)021
0(cos3050 θθθ TDCTDC +++=+
By substitution from the solution table above:
(14) θθ cos)141
12()021
0(cos3050 DCDC +++=+
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Using equations (13) and (14) I will match up coefficients and find C0, D0, C1, and D1 and use these in my exact solution by plugging them into equation (12).
00100 DC += 1120 DC +=−
021
050 DC += 141
1230 DC +=
For clarity, the details of the coefficient calculations are in Appendix A. These calculations yield:
C0 = 0 C1 = 20 D0 = 100 D1 = -40
Here I will construct the final form of the steady-state temperature using equation (12) and my tables of Legendre solutions and coefficients:
)(cos1)111
11()(cos0)1
00
0(),( θρρθρρθρ TDCTDCu −−++−+=
))(cos240120()11000(),( θρρρθρ −−+−+=u
(15) θρ
ρρ
θρ cos24020100),(
⎟⎟⎟
⎠
⎞
⎜⎜⎜
⎝
⎛−+=u
Equation (15) represents the steady-state temperature for the spherical shell.
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c) Plot the Solution For my solution plot, I used the fact that the problem is symmetrical with respect to φ the azimuthal direction. I then used Mathematica’s DensityPlot function for slices parallel to the equator and through the region of interest, from θ = 0 to θ = π and between ρ = 1 and ρ = 2. In the schematic diagram below, the shaded red box depicts one slice and the red outlined rectangle shows the orientation of the output plot. You can think of the plot being the blue area bent straight instead of curved.
The color scheme shows cooler light greens and yellows with warmer dark blue and violet tones. Notice the temperature is relatively uniform around the north pole and becomes increasingly varied between the surfaces approaching the south pole. Lastly, note the hottest temperature distribution near the inner surface and the coolest temperatures near the outer surface and south pole.
0 0.5 1 1.5 2 2.5 31
1.2
1.4
1.6
1.8
2
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References [1] Dr. Robert Buchanan, “Laplace’s Equation on a Sphere”, <http://banach.millersville.edu/~bob/math467/sampleproject.pdf> [2] Richard Haberman, Applied Partial Differential Equations with Fourier Series and Boundary Value Problems, 4th Edition, Pearson Prentice Hall, Upper Saddle River, NJ 2004. Appendix A
00 100 DC −= 00 =C ______________________________
( ) 00 2110050 DD +−=
02110050 D−=
5021
0 =D
1000 =D _______________________________
11 20 DC −−= 201 =C _______________________________
( ) 11 4120230 DD +−−=
11 4124030 DD +−−=
1474030 D−−=
14770 D−=
401 −=D _______________________________