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====Summary==== From the above derivations, we can describe the properties of a spherical {{Math/MP_PolytropicIndex}} = 1 polytrope as follows: * <font color="red">Mass</font>: : Given the density, <math>\rho_c</math>, and the radius, <math>R</math>, of the configuration, the total mass is, <div align="center"> <math>M = \frac{4}{\pi} \rho_c R^3 </math> ; </div> : and, expressed as a function of <math>M</math>, the mass that lies interior to radius <math>r</math> is, <div align="center"> <math>\frac{M_r}{M} = \frac{1}{\pi} \biggl[ \sin\biggl(\frac{\pi r}{R} \biggr) - \biggl(\frac{\pi r}{R} \biggr)\cos\biggl(\frac{\pi r}{R} \biggr) \biggr]</math> . </div> * <font color="red">Pressure</font>: : Given values for the pair of model parameters <math>( \rho_c , R )</math>, or <math>( M , R )</math>, or <math>( \rho_c , M )</math>, the central pressure of the configuration is, <div align="center"> <math>P_c = \frac{2 G}{\pi} \rho_c^2 R^2 = \frac{\pi G}{8}\biggl( \frac{M^2}{R^4} \biggr) = \biggl[ \frac{1}{2\pi} G^3 \rho_c^4 M^2 \biggr]^{1/3}</math> ; </div> : and, expressed in terms of the central pressure <math>P_c</math>, the variation with radius of the pressure is, <div align="center"> <math>P(r)= P_c \biggl[\frac{R}{\pi r} \sin\biggl(\frac{\pi r}{R}\biggr) \biggr]^2</math> . </div> * <font color="red">Enthalpy</font>: : Throughout the configuration, the enthalpy is given by the relation, <div align="center"> <math>H(r) = \frac{2 P(r)}{ \rho(r)} = \frac{GM}{R} \biggl[\frac{R}{\pi r} \sin\biggl(\frac{\pi r}{R}\biggr) \biggr]</math> . </div> * <font color="red">Gravitational potential</font>: : Throughout the configuration — that is, for all <math>r \leq R</math> — the gravitational potential is given by the relation, <div align="center"> <math>\Phi_\mathrm{surf} - \Phi(r) = H(r) = \frac{GM}{R} \biggl[\frac{R}{\pi r} \sin\biggl(\frac{\pi r}{R}\biggr) \biggr] </math> . </div> : Outside of this spherical configuration— that is, for all <math>r \geq R</math> — the potential should behave like a point mass potential, that is, <div align="center"> <math>\Phi(r) = - \frac{GM}{r} </math> . </div> : Matching these two expressions at the surface of the configuration, that is, setting <math>\Phi_\mathrm{surf} = - GM/R</math>, we have what is generally considered the properly normalized prescription for the gravitational potential inside a spherically symmetric, {{Math/MP_PolytropicIndex}} = 1 polytropic configuration: <div align="center"> <math>\Phi(r) = - \frac{G M}{R} \biggl\{ 1 + \biggl[\frac{R}{\pi r} \sin\biggl(\frac{\pi r}{R}\biggr) \biggr] \biggr\} </math> . </div> * <font color="red">Mass-Radius relationship</font>: : We see that, for a given value of <math>\rho_c</math>, the relationship between the configuration's total mass and radius is, <div align="center"> <math>M \propto R^3 ~~~~~\mathrm{or}~~~~~R \propto M^{1/3} </math> . </div> * <font color="red">Central- to Mean-Density Ratio</font>: : The ratio of the configuration's central density to its mean density is, <div align="center"> <math>\frac{\rho_c}{\bar{\rho}} = \biggl(\frac{\pi M}{4 R^3} \biggr)\biggl(\frac{3 M}{4 \pi R^3} \biggr) = \frac{\pi^2}{3} </math> . </div> <table border="1" cellpadding="8" align="right"> <tr> <th align="center">[[File:DataFileButton02.png|right|60px|file = Dropbox/WorkFolder/Wiki edits/EmbeddedPolytropes/n1.xlsx --- worksheet = Sheet1]]Figure 1: Mass vs. Radius <br />for n = 1 polytrope</th> </tr> <tr> <td align="center">[[File:N100SequenceA.png|300px|n = 1 mass vs. radius diagram]]</td> </tr> </table> For the purposes of comparing the internal structure of configurations having different polytropic indexes — see, for example [[SSC/Structure/Polytropes/Numerical#Fig4|Figure 4 in an accompanying chapter]] — we have found it useful in each case to graphically illustrate how the normalized mass, <math>~M/M_\mathrm{SWS}</math>, varies with the normalized radius, <math>~R/R_\mathrm{SWS}</math>, where the definition of these two functions is drawn from an [[SSC/Structure/PolytropesEmbedded#Stahler.27s_Presentation|accompanying discussion of pressure-truncated polytropic configurations]]. In the case of an <math>~n=1</math> polytrope, both functions are expressible analytically; specifically, we have, <div align="center"> <table border="0" cellpadding="3"> <tr> <td align="right"> <math> ~\frac{R}{R_\mathrm{SWS}}\biggr|_{n=1} </math> </td> <td align="center"> <math>~\equiv~</math> </td> <td align="left"> <math> \biggl( \frac{1}{4\pi} \biggr)^{1/2} \xi \, ; </math> </td> </tr> <tr> <td align="right"> <math> ~\frac{M}{M_\mathrm{SWS}}\biggr|_{n=1} </math> </td> <td align="center"> <math>~=~</math> </td> <td align="left"> <math> \biggl( \frac{1}{4\pi} \biggr)^{1/2} \biggl[ \frac{\xi^2}{\theta_n} \biggl| \frac{d\theta_n}{d\xi} \biggr| ~\biggr]_{n=1} </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=~</math> </td> <td align="left"> <math> \biggl( \frac{1}{4\pi} \biggr)^{1/2} \frac{\xi^3}{\sin\xi} \biggl[\frac{\sin\xi - \xi\cos\xi}{\xi^2} \biggr] </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=~</math> </td> <td align="left"> <math> \biggl( \frac{1}{4\pi} \biggr)^{1/2} \xi \biggl[1 - \xi\cot\xi \biggr] \, . </math> </td> </tr> </table> </div> As Figure 1 illustrates, this normalized mass increases monotonically with radius. Given that the surface of the configuration is associated with the parameter value, <math>~\xi = \pi</math>, we recognize that, at the surface, <math>~R/R_\mathrm{SWS} = \sqrt{\pi/4} \approx 0.8862269</math> and <math>~M/M_\mathrm{SWS}</math> formally climbs to infinity.
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