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=Virial Equilibrium of Pressure-Truncated Polytropes= {| class="PGEclass" style="float:left; margin-right: 20px; border-style: solid; border-width: 3px border-color: black" |- ! style="height: 125px; width: 125px; background-color:white;" | <font size="-1">[[H_BookTiledMenu#MoreModels|<b>Virial Equilibrium<br />of<br />Pressure-Truncated<br />Polytropes</b>]]</font> |} Here we will draw heavily from: [1] An accompanying [[SSC/FreeEnergy/PolytropesEmbedded#Pressure-Truncated_Polytropes|''Free Energy Synopsis'']]; and [2] A detailed analysis of the [[SSC/Virial/PolytropesEmbedded/SecondEffortAgain/Pt2#Plotting_Concise_Mass-Radius_Relation|Virial Equilibrium of Adiabatic Spheres]]. <br /> <br /> <br /> <br /> <br /> ==Groundwork== ===Basic Relation=== In the context of spherically symmetric, pressure-truncated polytropic configurations, the relevant free-energy expression is, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\mathfrak{G}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~W_\mathrm{grav} + U_\mathrm{int} + P_eV</math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ - 3\mathcal{A} \biggl[\frac{GM^2}{R} \biggr] + n\mathcal{B} \biggl[ \frac{K_nM^{(n+1)/n}}{R^{3/n}} \biggr] + \frac{4\pi}{3} \cdot P_e R^3 \, ,</math> </td> </tr> </table> where, when written in terms of the trio of ''[[SSC/FreeEnergy/Powerpoint#Structural_Form_Factors|structural form factors]]'', <math>\tilde{\mathfrak{f}}_A,</math> <math>\tilde{\mathfrak{f}}_M,</math> and <math>\tilde{\mathfrak{f}}_W,</math> the pair of constants, <div align="center"> <table border="0" cellpadding="5"> <tr> <td align="right"> <math>~\mathcal{A} \equiv \frac{1}{5} \cdot \frac{\tilde{\mathfrak{f}}_W}{\tilde{\mathfrak{f}}_M^2}</math> </td> <td align="center"> and </td> <td align="left"> <math>\mathcal{B} \equiv \biggl(\frac{4\pi}{3} \biggr)^{-1/n} \frac{\tilde{\mathfrak{f}}_A}{\tilde{\mathfrak{f}}_M^{(n+1)/n}} \, .</math> </td> </tr> </table> </div> ===Often-Referenced Dimensionless Expressions=== When rewritten in a suitably dimensionless form — see two useful alternatives, below — this expression becomes, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\mathfrak{G}^*</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~- a x^{-1} + bx^{-3/n} + c x^3 \, ,</math> </td> </tr> </table> where <math>~x</math> is the configuration's dimensionless radius and <math>~a</math>, <math>~b</math>, and <math>~c</math> are constants. We therefore have, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\frac{d\mathfrak{G}^*}{dx}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~\frac{1}{x^2} \biggl[ a - \biggl( \frac{3b}{n} \biggr) x^{(n-3)/n} + 3c x^4 \biggr] \, ,</math> </td> </tr> </table> and, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\frac{d^2\mathfrak{G}^*}{dx^2}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~\frac{1}{x^3} \biggl[\biggl(\frac{n+3}{n}\biggr) \biggl( \frac{3b}{n} \biggr) x^{(n-3)/n} + 6c x^4 - 2a \biggr] \, .</math> </td> </tr> </table> Virial equilibrium is obtained when <math>~d\mathfrak{G}^*/dx = 0</math>, that is, when <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\biggl( \frac{3b}{n} \biggr) x_\mathrm{eq}^{(n-3)/n} </math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ a + 3c x_\mathrm{eq}^4 \, .</math> </td> </tr> </table> And along an equilibrium ''sequence'', the ''specific'' equilibrium state that marks a transition from dynamically stable to dynamically unstable configurations — henceforth labeled as having the ''critical'' radius, <math>~x_\mathrm{crit}</math> — is identified by setting <math>~d^2\mathfrak{G}^*/dx^2 = 0</math>, that is, it is the configuration for which, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~0</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~\biggl[\biggl(\frac{n+3}{n}\biggr) \biggl( \frac{3b}{n} \biggr) x^{(n-3)/n} + 6c x^4 - 2a \biggr]_{x = x_\mathrm{eq}}</math> </td> </tr> <tr> <td align="right"> <math>~\Rightarrow ~~~ x_\mathrm{crit}^4 </math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \frac{a}{3^2c}\biggl(\frac{n - 3}{n+1}\biggr) \, . </math> </td> </tr> </table> Inserting the adiabatic exponent in place of the polytropic index via the relation, <math>~n = (\gamma - 1)^{-1}</math>, we have equivalently, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~ x_\mathrm{crit}^4 </math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \frac{a}{3^2c}\biggl(\frac{4-3\gamma}{\gamma}\biggr) \, . </math> </td> </tr> </table> ===Useful Recognition=== By comparing various terms in the first two algebraic ''Setup'' expressions, above, It is clear that, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~W^*_\mathrm{grav} = -ax^{-1}</math> </td> <td align="center"> and, </td> <td align="left"> <math>~U^*_\mathrm{int} = bx^{-3/n} \, .</math> </td> </tr> </table> Notice, then, that in every equilibrium configuration, we should find, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~- \frac{U^*_\mathrm{int}}{W^*_\mathrm{grav}}\biggr|_\mathrm{eq}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \biggl(\frac{b}{a}\biggr) x_\mathrm{eq}^{(n-3)/n} = \frac{n}{3a} \biggl[ a + 3cx^4_\mathrm{eq} \biggr] </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \frac{n}{3} \biggl[ 1 + \biggl(\frac{3c}{a}\biggr) x^4_\mathrm{eq} \biggr] \, . </math> </td> </tr> </table> And, specifically in the ''critical'' configuration we should find that, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~- \frac{U^*_\mathrm{int}}{W^*_\mathrm{grav}}\biggr|_\mathrm{crit}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \frac{1}{3(\gamma-1)} \biggl[ 1 + \frac{1}{3}\biggl(\frac{4-3\gamma}{\gamma}\biggr) \biggr] = \frac{4}{3^2\gamma(\gamma-1)} </math> </td> </tr> <tr> <td align="right"> <math>~\Rightarrow ~~~\frac{S^*_\mathrm{therm}}{W^*_\mathrm{grav}}\biggr|_\mathrm{crit}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ -\frac{2}{3\gamma} \, . </math> </td> </tr> </table> The equivalent of this last expression also appears at the end of subsection <b><font color="maroon" size="+1">⑦</font></b> of an [[SSC/SynopsisStyleSheet#Stability|accompanying ''Tabular Overview'']]. ==Equilibrium Sequences== In all of the polytropic configurations being considered here, {{ Math/MP_PolytropicConstant }} is a constant — that is, the specific entropy of all fluid elements is assumed to be the same, both spatially and temporally. ===Fix Mass While Varying External Pressure=== In this case, we want to examine undulations of a two-dimensional free-energy surface that results from allowing <math>R</math> and <math>P_e</math> to vary while holding <math>M</math> fixed. In our [[SSC/FreeEnergy/PolytropesEmbedded#Case_M|accompanying, more detailed discussion]], this is referred to as '''Case M'''. Adopting the normalizations, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>R_\mathrm{norm}</math> </td> <td align="center"> <math>\equiv</math> </td> <td align="left"> <math> \biggl[ \biggl( \frac{G}{K_n} \biggr)^n M^{n-1} \biggr]^{1/(n-3)} \, , </math> </td> <td align="center"> </td> <td align="right"> <math>P_\mathrm{norm}</math> </td> <td align="center"> <math>\equiv</math> </td> <td align="left"> <math> \biggl[ \frac{K_n^{4n}}{G^{3(n+1)} M^{2(n+1)}} \biggr]^{1/(n-3)} </math> </td> <td align="center"> and, </td> <td align="right"> <math>E_\mathrm{norm}</math> </td> <td align="center"> <math>\equiv</math> </td> <td align="left"> <math> P_\mathrm{norm} R^3_\mathrm{norm} \, , </math> </td> </tr> </table> — which, as is detailed in an [[SSCpt1/Virial#Choices_Made_by_Other_Researchers|accompanying discussion]], are similar but not identical to the normalizations adopted by {{ Horedt70full }} and by {{ Whitworth81full }} — the coefficients in the above-presented [[#Basic_Relations|Basic Relations]] become, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~a</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~3\mathcal{A} \, , </math> </td> <td align="center"> </td> <td align="right"> <math>~b</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~n\mathcal{B} </math> </td> <td align="center"> and, </td> <td align="right"> <math>~c</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~\frac{4\pi}{3}\biggl( \frac{P_e}{P_\mathrm{norm}} \biggr) \, . </math> </td> </tr> </table> The relevant dimensionless free-energy surface is, then, given by the expression, <table border="1" cellpadding="8" align="center"> <tr> <th align="center" colspan="1">''Case M'' Free-Energy Surface</th> </tr> <tr><td align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\mathfrak{G}_{K,M}^* \equiv \frac{\mathfrak{G}_{K,M}}{E_\mathrm{norm}} </math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ -3\mathcal{A} \biggl(\frac{R}{R_\mathrm{norm}}\biggr)^{-1} +~ n\mathcal{B} \biggl(\frac{R}{R_\mathrm{norm}}\biggr)^{-3/n} +~ \biggl( \frac{4\pi}{3} \biggr) \frac{P_e}{P_\mathrm{norm}} \biggl(\frac{R}{R_\mathrm{norm}}\biggr)^3 \, . </math> </td> </tr> </table> </td></tr> </table> ===Fix External Pressure While Varying Mass=== In this case, we want to examine undulations of a two-dimensional free-energy surface that results from allowing <math>~R</math> and <math>~M</math> to vary while holding <math>~P_e</math> fixed. In our [[SSC/FreeEnergy/PolytropesEmbedded#Case_P|accompanying, more detailed discussion]], this is referred to as '''Case P'''. Motivated by the published work of {{ Stahler83full }}, here we adopt the normalizations, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~R_\mathrm{SWS}</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~\biggl( \frac{n+1}{nG} \biggr)^{1/2} K_n^{n/(n+1)} P_\mathrm{e}^{(1-n)/[2(n+1)]} \, ,</math> </td> <td align="center"> </td> <td align="right"> <math>~M_\mathrm{SWS}</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~\biggl( \frac{n+1}{nG} \biggr)^{3/2} K_n^{2n/(n+1)} P_\mathrm{e}^{(3-n)/[2(n+1)]} </math> </td> <td align="center"> and,</td> </tr> <tr> <td align="right"> <math>~E_\mathrm{SWS}</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left" colspan="6"> <math>~ \biggl( \frac{n}{n+1} \biggr) \frac{GM_\mathrm{SWS}^2}{R_\mathrm{SWS}} = \biggl( \frac{n+1}{n} \biggr)^{3/2} G^{-3/2}K_n^{3n/(n+1)} P_\mathrm{e}^{(5-n)/[2(n+1)]} \, .</math> </td> </tr> </table> the coefficients in the above-presented [[#Basic_Relations|Basic Relations]] become, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~a</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~3 \mathcal{A} \biggl( \frac{n+1}{n} \biggr)\biggl( \frac{M}{M_\mathrm{SWS}}\biggr)^2 \, , </math> </td> <td align="center"> </td> <td align="right"> <math>~b</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~n\mathcal{B} \biggl(\frac{M}{M_\mathrm{SWS}}\biggr)^{(n+1)/n} </math> </td> <td align="center"> and, </td> <td align="right"> <math>~c</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~\frac{4\pi}{3} \, , </math> </td> </tr> </table> where the pair of constants, <math>\mathcal{A}</math> and <math>\mathcal{B}</math>, have the same definitions in terms of the ''[[SSC/FreeEnergy/Powerpoint#Structural_Form_Factors|structural form factors]]'' as provided above. The relevant dimensionless free-energy surface is, then, given by the expression, <table border="1" cellpadding="8" align="center"> <tr> <th align="center" colspan="1">''Case P'': Free-Energy Surfaces</th> </tr> <tr><td align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\mathfrak{G}_{K,P_e}^* \equiv \frac{\mathfrak{G}_{K,P_e}}{E_\mathrm{SWS}}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~- 3 \mathcal{A} \biggl( \frac{n+1}{n} \biggr)\biggl( \frac{M}{M_\mathrm{SWS}}\biggr)^2 \biggl(\frac{R}{R_\mathrm{SWS}}\biggr)^{-1} + n\mathcal{B} \biggl(\frac{M}{M_\mathrm{SWS}}\biggr)^{(n+1)/n} \biggl(\frac{R}{R_\mathrm{SWS}}\biggr)^{-3/n} + \frac{4\pi}{3} \biggl( \frac{R}{R_\mathrm{SWS}}\biggr)^3 \, . </math> </td> </tr> </table> </td></tr> </table> Across this '''Case P''' free-energy surface, extrema — and, hence, equilibrium configurations — will arise wherever the virial-equilibrium condition is met, that is, wherever <table border="1" cellpadding="8" align="center"> <tr> <th align="center" colspan="1">''Case P'': Virial Equilibrium Sequences</th> </tr> <tr><td align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~0</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \biggl( \frac{R}{R_\mathrm{SWS}}\biggr)^4 -\frac{3\mathcal{B}}{4\pi} \biggl(\frac{M}{M_\mathrm{SWS}}\biggr)^{(n+1)/n} \biggl( \frac{R}{R_\mathrm{SWS}}\biggr)^{(n-3)/n} + \frac{3 \mathcal{A}}{4\pi} \biggl( \frac{n+1}{n} \biggr)\biggl( \frac{M}{M_\mathrm{SWS}}\biggr)^2 \, .</math> </td> </tr> </table> </td></tr> </table> An equilibrium model ''sequence'' is thereby defined for each chosen polytropic index in the range, <math>0 \le n < \infty</math>. Along each equilibrium sequence for which <math>3 \le n < \infty</math>, there is one ''specific'' equilibrium state that marks a transition from dynamically stable to dynamically unstable configurations. For a given mass, the radius of this ''critical'' configuration is identified by the relation, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math> \biggl( \frac{R_\mathrm{eq}}{R_\mathrm{SWS}}\biggr)_\mathrm{crit}^4 </math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math> \frac{\mathcal{A}}{4\pi}\biggl(\frac{n - 3}{n}\biggr) \biggl( \frac{M}{M_\mathrm{SWS}}\biggr)^2 \, . </math> </td> </tr> </table> ---- Below, we will examine the behavior of individual virial-equilibrium sequences, using various physical arguments to justify our choice of specific expressions for the coefficients, <math>\mathcal{A}</math> and <math>\mathcal{B}.</math> Here, in an effort to provide a broad overview, we set, <div align="center"> <math>\mathcal{A} = \frac{4\pi n}{3(n+1)}</math> and <math>\mathcal{B} = \biggl( \frac{4\pi}{3} \biggr) \, ,</math> </div> and display, in a single diagram, the behaviors of equilibrium sequences having seven different polytropic indexes. Specifically, each curve in the left-hand panel of Figure 1 results from the mass-radius expression, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>0</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math> \biggl( \frac{R}{R_\mathrm{SWS}}\biggr)^4 - \biggl( \frac{R}{R_\mathrm{SWS}}\biggr)^{(n-3)/n} \biggl( \frac{M}{M_\mathrm{SWS}} \biggr)^{(n+1)/n} + \biggl( \frac{M}{M_\mathrm{SWS}}\biggr)^2 \, .</math> </td> </tr> </table> <span id="StahlerSchematic">(As has been demonstrated</span> in an [[SSC/Virial/PolytropesEmbedded/SecondEffortAgain/Pt2#modNormalizations|accompanying discussion]], we could alternatively have obtained this same algebraic relation by shifting to a different pair of mass- and radius-normalizations — namely, <math>M_\mathrm{mod}</math> and <math>R_\mathrm{mod}</math> — instead of choosing these specific values of <math>\mathcal{A}</math> and <math>\mathcal{B}.</math>) <table border="1" align="center" cellpadding="8"> <tr> <th align="center" colspan="2">Figure 1: Virial-Analysis-Based Equilibrium Sequences</th> </tr> <tr> <td align="center" rowspan="2"> [[File:MassRadiusVirialLabeled.png|350px|Virial Theorem Mass-Radius Relation]] </td> <td align="center"> [[File:Stahler1983TitlePage0.png|300px|center|Stahler (1983) Title Page]] </td> </tr> <tr> <td align="center" bgcolor="white"> [[File:Stahler_MRdiagram1.png|300px|center|Stahler (1983) Figure 17 (edited)]] </td> </tr> </table> For comparison, the ''schematic'' diagram displayed on the righthand side of the figure is a reproduction of Figure 17 from Appendix B of {{ Stahler83 }}. It seems that our derived, analytically prescribable, mass-radius relationship — which is, in essence, a statement of the scalar virial theorem — embodies most of the attributes of the mass-radius relationship for pressure-truncated polytropes that were already understood, and conveyed schematically, by Stahler in 1983. ---- Below, we will examine the behavior of individual virial-equilibrium sequences, using various physical arguments to justify our choice of specific expressions for the coefficients, <math>\mathcal{A}</math> and <math>\mathcal{B}.</math> Here, in an effort to provide a broad overview, we set all three structural form factors to unity, in which case the pair of coefficients, <div align="center"> <math>\mathcal{A} = \frac{1}{5}</math> and <math>\mathcal{B} = \biggl( \frac{3}{4\pi} \biggr)^{1/n}</math>, </div> and the resulting mass-radius relation of equilibrium sequences is governed by the algebraic mass-radius relation, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>0</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math> \biggl( \frac{R}{R_\mathrm{SWS}}\biggr)^4 - \biggl( \frac{R}{R_\mathrm{SWS}}\biggr)^{(n-3)/n}\biggl[ \biggl(\frac{3}{4\pi} \biggr) \frac{M}{M_\mathrm{SWS}}\biggr]^{(n+1)/n} + ~\frac{3}{20\pi} \biggl( \frac{n+1}{n}\biggr) \biggl( \frac{M}{M_\mathrm{SWS}}\biggr)^2 \, .</math> </td> </tr> </table> The left-hand panel of Figure 1 displays this behavior for equilibrium sequences having seven different values of the polytropic index, as labeled. As has been demonstrated in an [[SSC/Virial/PolytropesEmbedded/SecondEffortAgain/Pt2#Plotting_Concise_Mass-Radius_Relation|accompanying discussion]], this governing mass-radius relation can be analytically manipulated into a form that provides either an explicit <math>M(R)</math> or <math>R(M)</math> relation for the cases labeled, <math>n = 1, 3,</math> and <math>\infty</math>; a generic root-finding technique has been used to generate [[SSC/Virial/PolytropesEmbedded/SecondEffortAgain/Pt2#TabulatedValues|points along each of the other depicted equilibrium sequences]]. <table border="1" align="center" cellpadding="8"> <tr> <th align="center" colspan="2">Figure 1: Virial-Analysis-Based Equilibrium Sequences</th> </tr> <tr> <td align="center" rowspan="2"> [[File:MassRadiusVirialLabeled.png|350px|Virial Theorem Mass-Radius Relation]] </td> <td align="center"> [[File:Stahler1983TitlePage0.png|300px|center|Stahler (1983) Title Page]] </td> </tr> <tr> <td align="center" bgcolor="white"> [[File:Stahler_MRdiagram1.png|300px|center|Stahler (1983) Figure 17 (edited)]] </td> </tr> </table> For comparison, the ''schematic'' diagram displayed on the righthand side of the figure is a reproduction of Figure 17 from Appendix B of {{ Stahler83 }}. It seems that our derived, analytically prescribable, mass-radius relationship — which is, in essence, a statement of the scalar virial theorem — embodies most of the attributes of the mass-radius relationship for pressure-truncated polytropes that were already understood, and conveyed schematically, by Stahler in 1983.
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