PGE/PoissonOrigin: Difference between revisions

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<math>~ \Phi(\vec{x})</math>
<math>\Phi(\vec{x})</math>
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<math>~\equiv</math>
<math>\equiv</math>
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<math>~ -G \int \frac{\rho(\vec{x}^{~'})}{|\vec{x}^{~'} - \vec{x}|} d^3x^' \, .</math>
<math>-G \int \frac{\rho(\vec{x}^{~'})}{|\vec{x}^{~'} - \vec{x}|} d^3x^' \, .</math>
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[<b>[[User:Tohline/Appendix/References#BT87|<font color="red">BT87</font>]]</b>], p. 31, Eq. (2-3)<br />
[<b>[[Appendix/References#BT87|<font color="red">BT87</font>]]</b>], p. 31, Eq. (2-3)<br />
[<b>[[User:Tohline/Appendix/References#EFE|<font color="red">EFE</font>]]</b>], &sect;10, p. 17, Eq. (11)<br />
[<b>[[Appendix/References#EFE|<font color="red">EFE</font>]]</b>], &sect;10, p. 17, Eq. (11)<br />
[<b>[[User:Tohline/Appendix/References#T78|<font color="red">T78</font>]]</b>], &sect;4.2, p. 77, Eq. (12)
[<b>[[Appendix/References#T78|<font color="red">T78</font>]]</b>], &sect;4.2, p. 77, Eq. (12)
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(Note: &nbsp; As we have detailed in a [[User:Tohline/VE#Setting_the_Stage|separate discussion]], throughout [<b>[[User:Tohline/Appendix/References#EFE|<font color="red">EFE</font>]]</b>] Chandrasekhar adopts a ''different sign convention'' as well as a different variable name to represent the gravitational potential.)  Recognizing that the gradient of the function, <math>~|\vec{x}^{~'} - \vec{x}|^{-1}</math>, with respect to <math>~\vec{x}</math> is,
(Note: &nbsp; As we have detailed in a [[User:Tohline/VE#Setting_the_Stage|separate discussion]], throughout [<b>[[Appendix/References#EFE|<font color="red">EFE</font>]]</b>] Chandrasekhar adopts a ''different sign convention'' as well as a different variable name to represent the gravitational potential.)  Recognizing that the gradient of the function, <math>~|\vec{x}^{~'} - \vec{x}|^{-1}</math>, with respect to {{ Template:Math/VAR_PositionVector01 }} is,
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<math>~\nabla_x \biggl[ \frac{1}{|\vec{x}^{~'} - \vec{x}|} \biggr]</math>
<math>\nabla_x \biggl[ \frac{1}{|\vec{x}^{~'} - \vec{x}|} \biggr]</math>
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<math>~=</math>
<math>=</math>
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   <td align="left">
   <td align="left">
<math>~
<math>
\frac{\vec{x}^{~'} - \vec{x}}{|\vec{x}^{~'} - \vec{x}|^3} \, ,
\frac{\vec{x}^{~'} - \vec{x}}{|\vec{x}^{~'} - \vec{x}|^3} \, ,
</math>
</math>
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[<b>[[User:Tohline/Appendix/References#BT87|<font color="red">BT87</font>]]</b>], p. 31, Eq. (2-4)
[<b>[[Appendix/References#BT87|<font color="red">BT87</font>]]</b>], p. 31, Eq. (2-4)
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and given that, in the above expression for the gravitational acceleration, the integration is taken over the volume that is identified by the ''primed'' <math>~(\vec{x}~{'})</math>, rather than the unprimed <math>~(\vec{x})</math>, coordinate system, <font color="#007700">we find that we may write</font> the gravitational acceleration as,
and given that, in the above expression for the gravitational acceleration, the integration is taken over the volume that is identified by the ''primed'' <math>(\vec{x}~{'})</math>, rather than the unprimed <math>(\vec{x})</math>, coordinate system, <font color="#007700">we find that we may write</font> the gravitational acceleration as,
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<math>~\vec{a}(\vec{x})</math>
<math>\vec{a}(\vec{x})</math>
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<math>~=</math>
<math>=</math>
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   <td align="left">
<math>~\int G\rho(\vec{x}^{~'})  \nabla_x \biggl[ \frac{1}{|\vec{x}^{~'} - \vec{x}|} \biggr]d^3 x'
<math>\int G\rho(\vec{x}^{~'})  \nabla_x \biggl[ \frac{1}{|\vec{x}^{~'} - \vec{x}|} \biggr]d^3 x'
</math>
</math>
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<math>~=</math>
<math>=</math>
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<math>~ \nabla_x \biggl\{ G \int \biggl[ \frac{\rho(\vec{x}^{~'}) }{|\vec{x}^{~'} - \vec{x}|} \biggr]d^3 x'\biggr\}</math>
<math>\nabla_x \biggl\{ G \int \biggl[ \frac{\rho(\vec{x}^{~'}) }{|\vec{x}^{~'} - \vec{x}|} \biggr]d^3 x'\biggr\}</math>
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<math>~=</math>
<math>=</math>
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<math>~-\nabla_x \Phi \, .</math>
<math>-\nabla_x \Phi \, .</math>
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[<b>[[User:Tohline/Appendix/References#BT87|<font color="red">BT87</font>]]</b>], p. 31, Eq. (2-5)
[<b>[[Appendix/References#BT87|<font color="red">BT87</font>]]</b>], p. 31, Eq. (2-5)
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Revision as of 10:35, 2 July 2021

Origin of the Poisson Equation

In deriving the,

Poisson Equation

∇2Φ=4πGρ

we will follow closely the presentation found in §2.1 of [BT87].


According to Isaac Newton's inverse-square law of gravitation, the acceleration, a→(x→), felt at any point in space, x→, due to the gravitational attraction of a distribution of mass, ρ(x→), is obtained by integrating over the accelerations exerted by each small mass element, ρ(x→′)d3x′, as follows:

a→(x→)

=

∫[x→′−x→|x→′−x→|3]Gρ(x→′)d3x′,

[BT87], p. 31, Eq. (2-2)

where, G is the universal gravitational constant.

Step 1

In the astrophysics literature, it is customary to adopt the following definition of the,

Scalar Gravitational Potential

Φ(x→)

≡

−G∫ρ(x→′)|x→′−x→|d3x'.

[BT87], p. 31, Eq. (2-3)
[EFE], §10, p. 17, Eq. (11)
[T78], §4.2, p. 77, Eq. (12)

(Note:   As we have detailed in a separate discussion, throughout [EFE] Chandrasekhar adopts a different sign convention as well as a different variable name to represent the gravitational potential.) Recognizing that the gradient of the function, |x→′−x→|−1, with respect to x→ is,

∇x[1|x→′−x→|]

=

x→′−x→|x→′−x→|3,

[BT87], p. 31, Eq. (2-4)

and given that, in the above expression for the gravitational acceleration, the integration is taken over the volume that is identified by the primed (x→'), rather than the unprimed (x→), coordinate system, we find that we may write the gravitational acceleration as,

a→(x→)

=

∫Gρ(x→′)∇x[1|x→′−x→|]d3x′

 

=

∇x{G∫[ρ(x→′)|x→′−x→|]d3x′}

 

=

−∇xΦ.

[BT87], p. 31, Eq. (2-5)

Step 2

Next, we realize that the divergence of the gravitational acceleration takes the form,

∇x⋅a→(x→)

=

∇x⋅∫[x→′−x→|x→′−x→|3]Gρ(x→′)d3x′

 

=

∫Gρ(x→′){∇x⋅[x→′−x→|x→′−x→|3]}d3x′.

[BT87], p. 31, Eq. (2-6)

Examining the expression inside the curly braces, we find that,

∇x⋅[x→′−x→|x→′−x→|3]

=

−3|x→′−x→|3+3[(x→′−x→)⋅(x→′−x→)|x→′−x→|5]

(Note:   Ostensibly, this last expression is the same as equation 2-7 of [BT87], but apparently there is a typesetting error in the BT87 publication. As printed, the denominator of the first term on the right-hand side is |x→′−x→|1, whereas it should be |x→′−x→|3 as written here.) When (x→′−x→)≠0, we may cancel the factor |x→′−x→|2 from top and bottom of the last term in this equation to conclude that,

∇x⋅[x→′−x→|x→′−x→|3]=0

      when,      

(x→′≠x→).

[BT87], p. 31, Eq. (2-8)

Therefore, any contribution to the integral must come from the point x→′=x→, and we may restrict the volume of integration to a small sphere … centered on this point. Since, for a sufficiently small sphere, the density will be almost constant through this volume, we can take ρ(x→')=ρ(x→) out of the integral. Via the divergence theorem (for details, see appendix 1.B — specifically, equation 1B-42 — of [BT87]), the remaining volume integral may be converted into a surface integral over the small volume centered on the point x→′=x→ and, in turn, this surface integral may be written in terms of an integral over the solid angle, d2Ω, to give:

∇x⋅a→(x→)

=

−Gρ(x→)∫d2Ω

 

=

−4πGρ(x→).

[BT87], p. 32, Eq. (2-9b)

Step 3

Finally, combining the results of Step 1 and Step 2 gives the desired,

Poisson Equation

User:Tohline/Math/EQ Poisson01

which serves as one of the principal governing equations in our examination of the Structure, Stability, & Dynamics of Self-Gravitating Fluids.

See Also

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