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=Spherically Symmetric Configurations=
{{LSU_HBook_header}}
{{LSU_HBook_header}}
=Spherically Symmetric Configurations=
==Principal Governing Equations==
==Principal Governing Equations==
If the self-gravitating configuration that we wish to construct is spherically symmetric, then the coupled set of multidimensional, partial differential equations that serve as our [http://www.vistrails.org/index.php/User:Tohline/PGE principal governing equations] can be simplified to a coupled set of one-dimensional, ordinary differential equations.  This is accomplished by expressing each of the multidimensional spatial operators &#8212; gradient (<math>\nabla</math>), divergence (<math>\nabla\cdot</math>), and Laplacian (<math>\nabla^2</math>) &#8212; in spherical coordinates (<math>r, \theta, \varphi</math>) (see, for example, the [http://en.wikipedia.org/wiki/Spherical_coordinate_system#Integration_and_differentiation_in_spherical_coordinates Wikipedia discussion of integration and differentiation in spherical coordinates]) then setting to zero all derivatives that are taken with respect to the angular coordinates <math>\theta</math> and <math>\varphi</math>.  After making this simplification, our governing equations become,
If the self-gravitating configuration that we wish to construct is spherically symmetric, then the coupled set of multidimensional, partial differential equations that serve as our [[User:Tohline/PGE#Principal_Governing_Equations|principal governing equations]] can be simplified to a coupled set of one-dimensional, ordinary differential equations.  This is accomplished by expressing each of the multidimensional spatial operators &#8212; gradient (<math>\nabla</math>), divergence (<math>\nabla\cdot</math>), and Laplacian (<math>\nabla^2</math>) &#8212; in spherical coordinates (<math>r, \theta, \varphi</math>) (see, for example, the [http://en.wikipedia.org/wiki/Spherical_coordinate_system#Integration_and_differentiation_in_spherical_coordinates Wikipedia discussion of integration and differentiation in spherical coordinates]) then setting to zero all derivatives that are taken with respect to the angular coordinates <math>\theta</math> and <math>\varphi</math>.  After making this simplification, our governing equations become,


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(We recognize the first of these expressions as being the statement of [http://www.vistrails.org/index.php/User:Tohline/PGE/ConservingMomentum#Time-independent_Behavior hydrostatic balance] appropriate for spherically symmetric configurations.)   
(We recognize the first of these expressions as being the statement of [[User:Tohline/PGE/ConservingMomentum#Time-independent_Behavior|hydrostatic balance]] appropriate for spherically symmetric configurations.)   


We need one supplemental relation to close this set of equations because there are two equations, but three unknown functions &#8212; {{User:Tohline/Math/VAR_Pressure01}}(r), {{User:Tohline/Math/VAR_Density01}}(r),  and {{User:Tohline/Math/VAR_NewtonianPotential01}}(r). As has been outlined in our discussion of [http://www.vistrails.org/index.php/User:Tohline/SR#Time-independent_Problems supplemental relations for time-independent problems], in the context of this H_Book we will close this set of equations by specifying a structural, barotropic relationship between {{User:Tohline/Math/VAR_Pressure01}} and {{User:Tohline/Math/VAR_Density01}}.  (See below.)
We need one supplemental relation to close this set of equations because there are two equations, but three unknown functions &#8212; {{User:Tohline/Math/VAR_Pressure01}}(r), {{User:Tohline/Math/VAR_Density01}}(r),  and {{User:Tohline/Math/VAR_NewtonianPotential01}}(r). As has been outlined in our discussion of [http://www.vistrails.org/index.php/User:Tohline/SR#Time-independent_Problems supplemental relations for time-independent problems], in the context of this H_Book we will close this set of equations by specifying a structural, barotropic relationship between {{User:Tohline/Math/VAR_Pressure01}} and {{User:Tohline/Math/VAR_Density01}}.  (See below.)


===Solution Strategies===
===Solution Strategies===
In an [http://www.vistrails.org/index.php/User:Tohline/SphericallySymmetricConfigurations/SolutionStrategies accompanying discussion], we outline three different techniques that have been used to solve the above pair of differential equations analytically, or to set them up for numerical solution once a supplemental barotropic relation has been identified.  In summary, these techniques lead to the following governing relations:
In an [[User:Tohline/SphericallySymmetricConfigurations/SolutionStrategies|accompanying discussion]], we outline three different techniques that have been used to solve the above pair of differential equations analytically, or to set them up for numerical solution once a supplemental barotropic relation has been identified.  In summary, these techniques lead to the following governing relations:




====Technique #1====
====Technique #1====
Integrating the
This technique results in the following integro-differential equation which only depends on the two unknown functions, {{User:Tohline/Math/VAR_Pressure01}} and {{User:Tohline/Math/VAR_Density01}}:
 
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{{User:Tohline/Math/EQ_SShydrostaticBalance01}}
</div>
where,
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<math>M_r \equiv \int_0^r 4\pi r^2 \rho dr</math> .
</div>


====Technique #2====
====Technique #2====
Integrating the
This technique results in the following second-order differential equation which depends only on the two unknown functions, {{User:Tohline/Math/VAR_Enthalpy01}} and {{User:Tohline/Math/VAR_Density01}}:
<div align="center">
<math>\frac{1}{r^2} \frac{d}{dr}\biggl( r^2 \frac{dH}{dr} \biggr) =-  4\pi G \rho</math> .
</div>


====Technique #3====
This technique does not immediately reduce the number of equations nor the number unknown variables, but it does change one of the governing differential equations into an algebraic relation.  The resulting pair of equations are,


====Technique #3====
<div align="center">
Integrating the
<math>\frac{1}{r^2} \frac{d }{dr} \biggl( r^2 \frac{d \Phi}{dr} \biggr)  = 4\pi G \rho </math> ,
</div>
and
<div align="center">
<math>H + \Phi = \mathrm{constant}</math> ;
</div>
the unknown functions are {{User:Tohline/Math/VAR_Enthalpy01}}, {{User:Tohline/Math/VAR_Density01}}, and {{User:Tohline/Math/VAR_NewtonianPotential01}}.


==Stability &amp; Dynamics==
==Stability &amp; Dynamics==

Latest revision as of 04:39, 7 November 2012

Spherically Symmetric Configurations

Whitworth's (1981) Isothermal Free-Energy Surface
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Principal Governing Equations

If the self-gravitating configuration that we wish to construct is spherically symmetric, then the coupled set of multidimensional, partial differential equations that serve as our principal governing equations can be simplified to a coupled set of one-dimensional, ordinary differential equations. This is accomplished by expressing each of the multidimensional spatial operators — gradient (<math>\nabla</math>), divergence (<math>\nabla\cdot</math>), and Laplacian (<math>\nabla^2</math>) — in spherical coordinates (<math>r, \theta, \varphi</math>) (see, for example, the Wikipedia discussion of integration and differentiation in spherical coordinates) then setting to zero all derivatives that are taken with respect to the angular coordinates <math>\theta</math> and <math>\varphi</math>. After making this simplification, our governing equations become,

Equation of Continuity

<math>\frac{d\rho}{dt} + \rho \biggl[\frac{1}{r^2}\frac{d(r^2 v_r)}{dr} \biggr] = 0 </math>


Euler Equation

<math>\frac{dv_r}{dt} = - \frac{1}{\rho}\frac{dP}{dr} - \frac{d\Phi}{dr} </math>


Adiabatic Form of the
First Law of Thermodynamics

<math>~\frac{d\epsilon}{dt} + P \frac{d}{dt} \biggl(\frac{1}{\rho}\biggr) = 0</math>


Poisson Equation

<math>\frac{1}{r^2} \biggl[\frac{d }{dr} \biggl( r^2 \frac{d \Phi}{dr} \biggr) \biggr] = 4\pi G \rho </math>

Structure

LSU Structure still.gif

Equilibrium, spherically symmetric structures are obtained by searching for time-independent solutions to the above set of simplified governing equations. The steady-state flow field that must be adopted to satisfy both a spherically symmetric geometry and the time-independent constraint is, <math>\vec{v} = \hat{e}_r v_r = 0</math>. After setting the radial velocity, <math>v_r</math>, and all time-derivatives to zero, we see that the <math>1^\mathrm{st}</math> (continuity) and <math>3^\mathrm{rd}</math> (first law of thermodynamics) equations are trivially satisfied while the <math>2^\mathrm{nd}</math> (Euler) and <math>4^\mathrm{th}</math> give, respectively,

<math>\frac{1}{\rho}\frac{dP}{dr} =- \frac{d\Phi}{dr} </math> ,

and,

<math>\frac{1}{r^2} \biggl[\frac{d }{dr} \biggl( r^2 \frac{d \Phi}{dr} \biggr) \biggr] = 4\pi G \rho </math> .


(We recognize the first of these expressions as being the statement of hydrostatic balance appropriate for spherically symmetric configurations.)

We need one supplemental relation to close this set of equations because there are two equations, but three unknown functions — <math>~P</math>(r), <math>~\rho</math>(r), and <math>~\Phi</math>(r). As has been outlined in our discussion of supplemental relations for time-independent problems, in the context of this H_Book we will close this set of equations by specifying a structural, barotropic relationship between <math>~P</math> and <math>~\rho</math>. (See below.)

Solution Strategies

In an accompanying discussion, we outline three different techniques that have been used to solve the above pair of differential equations analytically, or to set them up for numerical solution once a supplemental barotropic relation has been identified. In summary, these techniques lead to the following governing relations:


Technique #1

This technique results in the following integro-differential equation which only depends on the two unknown functions, <math>~P</math> and <math>~\rho</math>:

LSU Key.png

<math>~\frac{dP}{dr} = - \frac{GM_r \rho}{r^2}</math>

where,

<math>M_r \equiv \int_0^r 4\pi r^2 \rho dr</math> .

Technique #2

This technique results in the following second-order differential equation which depends only on the two unknown functions, <math>~H</math> and <math>~\rho</math>:

<math>\frac{1}{r^2} \frac{d}{dr}\biggl( r^2 \frac{dH}{dr} \biggr) =- 4\pi G \rho</math> .

Technique #3

This technique does not immediately reduce the number of equations nor the number unknown variables, but it does change one of the governing differential equations into an algebraic relation. The resulting pair of equations are,

<math>\frac{1}{r^2} \frac{d }{dr} \biggl( r^2 \frac{d \Phi}{dr} \biggr) = 4\pi G \rho </math> ,

and

<math>H + \Phi = \mathrm{constant}</math> ;

the unknown functions are <math>~H</math>, <math>~\rho</math>, and <math>~\Phi</math>.

Stability & Dynamics

Stability
LSU Stable.animated.gif

SUMMARY: The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically.

Dynamics
Minitorus.animated.gif

SUMMARY: The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically. The equilibrium structure of a self-gravitating, non-rotating, uniform-density sphere can be described analytically.


Whitworth's (1981) Isothermal Free-Energy Surface

© 2014 - 2021 by Joel E. Tohline
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Recommended citation:   Tohline, Joel E. (2021), The Structure, Stability, & Dynamics of Self-Gravitating Fluids, a (MediaWiki-based) Vistrails.org publication, https://www.vistrails.org/index.php/User:Tohline/citation