% *======================================================================* % Cactus Thorn template for ThornGuide documentation % Author: Ian Kelley % Date: Sun Jun 02, 2002 % % Thorn documentation in the latex file doc/documentation.tex % will be included in ThornGuides built with the Cactus make system. % The scripts employed by the make system automatically include % pages about variables, parameters and scheduling parsed from the % relevant thorn CCL files. % % This template contains guidelines which help to assure that your % documentation will be correctly added to ThornGuides. 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This % will allow us to create a PDF version of the ThornGuide % via pdflatex. % - References should be included with the latex "\bibitem" command. % - Use \begin{abstract}...\end{abstract} instead of \abstract{...} % - Do not use \appendix, instead include any appendices you need as % standard sections. % - For the benefit of our Perl scripts, and for future extensions, % please use simple latex. % % *======================================================================* % % Example of including a graphic image: % \begin{figure}[ht] % \begin{center} % \includegraphics[width=6cm]{MyArrangement_MyThorn_MyFigure} % \end{center} % \caption{Illustration of this and that} % \label{MyArrangement_MyThorn_MyLabel} % \end{figure} % % Example of using a label: % \label{MyArrangement_MyThorn_MyLabel} % % Example of a citation: % \cite{MyArrangement_MyThorn_Author99} % % Example of including a reference % \bibitem{MyArrangement_MyThorn_Author99} % {J. Author, {\em The Title of the Book, Journal, or periodical}, 1 (1999), % 1--16. {\tt http://www.nowhere.com/}} % % *======================================================================* % If you are using CVS use this line to give version information \documentclass{article} % Use the Cactus ThornGuide style file % (Automatically used from Cactus distribution, if you have a % thorn without the Cactus Flesh download this from the Cactus % homepage at www.cactuscode.org) \usepackage{../../../../doc/latex/cactus} \usepackage{latexsym} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \begin{document} % The author of the documentation \author{I.~Hawke,\\ F.~Loeffler \textless loeffler@sissa.it \textgreater } %A.~Nagar \textless alessandro.nagar@polito.it\textgreater} % The title of the document (not necessarily the name of the Thorn) \title{TOVSolver} % the date your document was last changed, if your document is in CVS, % please use: % \date{$ $Date: 2009-09-17 15:39:33 -0500 (Thu, 17 Sep 2009) $ $} \date{\today} \maketitle % Do not delete next line % START CACTUS THORNGUIDE % Add all definitions used in this documentation here % \def\mydef etc \begin{abstract} This thorn solves the Tolman-Oppenheimer-Volkov equations of hydrostatic equilibrium for a spherically symmetric static star. \end{abstract} %--------------------- \section{Introduction} \label{sec:intro} %--------------------- The Tolman-Oppenheimer-Volkoff solution is a static perfect fluid ``star''. It is frequently used as a test of relativistic hydro codes. Here it is intended for use without evolving the matter terms. This provides a compact strong field solution which is static but does not contain singularities. %------------------ \section{Equations} \label{sec:eqn} %------------------ The equations for a TOV star~\cite{Tolman39,OppVol39,mtw} are usually derived in Schwarzschild coordinates. In these coordinates, the metric can be brought into the form \begin{equation} ds^2 = -e^{2\phi}dt^2 + \left(1-\dfrac{2m}{r}\right)^{-1}dr^2 + r^2 d\Omega^2 \ . \end{equation} This thorn is based on the notes of Thomas Baumgarte~\cite{Baumgarte-file} that have been partially included in this documentation. However the notation for the fluid quantities follows~\cite{Font00a}. Here we are assuming that the stress energy tensor is given by \begin{equation} \label{eq:Tmunu} T^{\mu\nu} = (\mu + P)u^{\mu}u^{\nu} + Pg^{\mu\nu}, \end{equation} where $\mu$ is the total energy, $P$ the pressure, $u^{\mu}$ the fluid four velocity, $\rho$ the rest-mass density, $\epsilon$ the specific internal energy, and \begin{eqnarray} \label{eq:fluidquantities} \mu & = & \rho (1 + \epsilon), \\ P & = & (\Gamma - 1)\rho\epsilon, \\ P & = & K \rho^{\Gamma}. \end{eqnarray} This enforces a polytropic equation of state. We note that in Cactus the units are $c = G = M_{\odot} = 1$. The equations to give the initial data are solved (as usual) in the Schwarzschild-like coordinates with the areal radius labelled $r$. The equations of the relativistic hydrostatic equilibrium are \begin{eqnarray} \label{eq:TOViso} \frac{d P}{d r} & = & -(\mu + P) \frac{m + 4\pi r^3 P}{r(r - 2m)}, \\ % \frac{d m}{d r} & = & 4 \pi r^2 \mu, \\ % \frac{d \phi}{d r} & = & \frac{m + 4\pi r^3 P}{r(r - 2m)} \ . \\ \end{eqnarray} Here $m$ is the gravitational mass inside the sphere radius $r$, and $\phi$ the logarithm of the lapse. Once the integration is done for the interior of the star we match to the exterior (see below). In the exterior we have \begin{align} \label{eq:TOVexterior} P & = {\tt TOV\_atmosphere}, \\ m & = M, \\ \phi & = \dfrac{1}{2} \log(1-2M / r). \end{align} In order to impose initial data in cartesian coordinates, we want to transform this solution to isotropic coordinates, in which the metric takes the form \begin{equation} \label{eq:metr_iso} ds^2 = -e^{2\phi}dt^2+e^{2\Lambda}\left(d\bar{r}^2+\bar{r}^2d\Omega^2\right) \ . \end{equation} Here $\bar{r}$ denotes the isotropic radius. Matching the two metrics, one obviously finds \begin{align} r^2 &= e^{2\Lambda}\bar{r}^2 \ , \\ \left(1-\dfrac{2m}{r}\right)^{-1} dr^2 &= e^{2\Lambda}d\bar{r}^2 \ . \end{align} As a result, we have an additional differential equation to solve in order to have $\bar{r}(r)$, that is \begin{equation} \label{eq:rbar} \frac{d (\log(\bar{r} / r))}{\partial r} = \frac{r^{1/2} - (r-2m)^{1/2}}{r(r-2m)^{1/2}} \ . \end{equation} Given such a solution, the missing metric potential is simply given by \begin{equation} e^{\Lambda} = \dfrac{r}{\bar{r}} \ . \end{equation} In the following section we concentrate on solving Eq.~(\ref{eq:rbar}) in the exterior and in the interior of the star. Then, given these one-dimensional data we interpolate to get data on the three-dimensional Cactus grid; that is, we interpolate on the three dimensional {\tt r} given by the {\tt x, y, z} variables the physical hydro and spacetime quantities that are function of the isotropic radius $\bar{r}$ computed above. Only linear interpolation is used. This avoids problems at the surface of the star, and does not cause problems if the number of points in the one dimensional array is sufficient ($1\times 10^5$ is the default, which should be sufficient for medium-sized grids). %-------------------- \subsection{Exterior} \label{sbsc:exterior} %-------------------- In the exterior of the star, $r>R$, the mass $M\equiv m(R)$ is constant, and Eq.~(\ref{eq:rbar}) can be solved analytically up to a constant of integration. Fixing this constant such that $r$ and $\bar{r}$ agree at infinity, we find \begin{equation} \bar{r} = \dfrac{1}{2}\left(\sqrt{r^2-2Mr}+r -M\right) \ , \end{equation} or, solving for $r$ [cfr. Exercise 31.7 of MTW~\cite{mtw}] \begin{equation} r=\bar{r}\left(1+\dfrac{M}{2\bar{r}}\right)^2 \ . \end{equation} The metric potential as a function of $\bar{r}$ is obviously \begin{equation} e^{2\Lambda} = \left(1+\dfrac{M}{2\bar{r}}\right)^2 \ . \end{equation} %-------------------- \subsection{Interior} \label{sbsc:interior} %-------------------- In the interior, Eq,~(\ref{eq:rbar}) can not be integrated analytically, because $m$ is now a function of $r$. Instead, we have to integrate \begin{equation} \int_0^{\bar{r}} \dfrac{d\bar{r}}{\bar{r}} = \int_0^r\left(1-\dfrac{2m}{r}\right)^{-1/2}\dfrac{dr}{r} \ . \end{equation} The left hand side can be integrated analytically, and has a singular point at $\bar{r}=0$. The right hand side cannot be integrated analytically, but will also be singular at $r=0$, which poses problems when trying to integrate the equation numerically. We therefore rewrite the right hand side by adding and subracting a term $1/r$, which yields \begin{equation} \int_0^r\dfrac{1}{r(1-2m/r)^{1/2}}dr = \int_0^r\dfrac{1-(1-2m/r)^{1/2}}{r(1-2m/r)^{1/2}}dr+\int_0^r\dfrac{dr}{r} \ . \end{equation} Since $m\sim r^3$ close to the origin, the first term on the right hand side is now regular and the second one can be integrated analytically. As a result, we find \begin{equation} \int_0^{\bar{r}}d\ln\bar{r}-\int_0^rd\ln r=\int_0^r\dfrac{1-(1-2m/r)^{1/2}}{r(1-2m/r)^{1/2}}dr \ . \end{equation} Replacing the lower limits ($r=\bar{r}=0$) temporarily with $r_0$ and $\bar{r}_0$, we can integrate the right hand side and find \begin{equation} \ln\left(\dfrac{\bar{r}}{r}\right)-\ln\left(\dfrac{\bar{r}_0}{r_0}\right)=\int_0^r\dfrac{1-(1-2m/r)^{1/2}}{r(1-2m/r)^{1/2}}dr \ , \end{equation} or \begin{equation} \bar{r} = C r \exp\left[\int_0^r\dfrac{1-(1-2m/r)^{1/2}}{r(1-2m/r)^{1/2}}dr\right] \ . \end{equation} Here the constant of integration $C$ is related to the ratio $\bar{r}_0/r_0$ evaluated at the origin (which is perfectly regular). It can be chosen such that the interior solution matches the exterior solution at the surface of the star. This requirement implies \begin{equation} C = \dfrac{1}{2R}\left(\sqrt{R^2-2MR}+R-M\right)\exp\left[\int_0^R\dfrac{1-(1-2m/r)^{1/2}}{r(1-2m/r)^{1/2}}dr\right] \ . \end{equation} In this respect, let us recall how we do initial data for the system of equations at $r=0$. Given a value of the central density $\rho_c$ (in Cactus units) we pose $P_0 = K\rho_c^{\Gamma}$, $m_0=0$, $\phi_0=0$ and $\bar{r}_0 = {\tt TOV\_Tiny}$, $r_0 = {\tt TOV\_Tiny}$. The {\tt TOV\_Tiny} number is hardwired into the code to avoid divide by zero errors; it is $10^{-20}$. Also the default parameters will give the TOV star used for the long term evolutions in~\cite{Font02a}. That is, a nonrotating $N=1$ ($\gamma=1+1/N=2$) polytropic star with gravitational mass $M=1.4M_{\odot}$, circumferential radius $R=14.15$km, central rest-mass density $\rho_c=1.28 \times 10^{-3}$ and $K=100$. %-------------------------- \section{Use of this thorn} \label{sec:use} %-------------------------- To use this thorn to provide initial data for the {\tt ADMBase} variables $\alpha$, $\beta$, $g$ and $K$ just activate the thorn and set {\tt ADMBase:initial\_data = ``TOV''}. There are two ways of coupling the matter sources to the thorn that evolves the Einstein equations. One is to use the {\tt CalcTmunu} interface. This will give the components of the stress energy tensor \emph{pointwise} across the grid. For an example of this, see thorn {\tt ADM} in {\tt CactusEinstein}. To use the {\tt CalcTmunu} interface you should \begin{itemize} \item put the lines \begin{verbatim} friend: ADMCoupling USES INCLUDE: CalcTmunu.inc USES INCLUDE: CalcTmunu_temps.inc USES INCLUDE: CalcTmunu_rfr.inc \end{verbatim} in your {\tt interface.ccl} \item In any routine requiring the matter terms, put \begin{itemize} \item {\tt \#include ``CalcTmunu\_temps.inc''} in the variable declarations \item declare {\tt CCTK\_REAL}s {\tt Ttt, Ttx, Tty, Ttz, Txx, Txy, Txz, Tyy, Tyz, Tzz}. \item Inside an {\tt i,j,k} loop put {\tt \#include ``CalcTmunu.inc''}. {\bf This must be a Fortran routine} (We could probably fix this if requested). \end{itemize} \item You then use the real numbers {\tt Ttt} etc.~as the stress energy tensor at a point. \end{itemize} As an alternative you can use the grid functions {\tt StressEnergytt, StressEnergytx}, etc.~directly to have the stress energy tensor over the entire grid. To do this you just need the line {\tt friend: ADMCoupling} in your {\tt interface.ccl}. Although this seems much simpler, you will now \emph{only} get the contributions from the {\tt TOVSolver} thorn. If you want to use other matter sources, most of the current thorns ({\tt CosmologicalConstant}, the hydro code, the scalar field code) all use the {\tt CalcTmunu} interface. You also have the possibility to use a parameter {\tt GRHydrotovsolver::TOV\_Separation} to obtain a spacetime consisting of one TOV-system for $x>0$ and a second (similar) for $x<0$. This parameter sets the separation of the centers of two neutron stars, has to be positive and should be larger than twice the radius of one star.\\ Be aware that the spacetime obtained by this is no physical spacetime and no solution of Einsteins Equations and therefore an IVP-run has to follow. This parameter was only introduced for testing purposes of the IVP-Solver and should only be considered as such. There would be better (and also easy) ways to obtain initial data for two TOVs than that. \begin{thebibliography}{10} \bibitem{Tolman39} R.~C. Tolman, Phys. Rev. {\bf 55}, 364 (1939). % \bibitem{OppVol39} J.~R. Oppenheimer and G. Volkoff, Physical Review {\bf 55}, 374 (1939). % \bibitem{mtw} C.W.~Misner, K.S.~Thorn and J.A.~Wheeler, Gravitation (Freeman and co. NY, 1973). % \bibitem{Baumgarte-file} T.~W. Baumgarte. There is a copy of his notes in this directory: \\ TOVSolver/doc. % \bibitem{Font00a} J.~A. Font, M. Miller, W. Suen and M. Tobias, Phys. Rev. {\bf D61}, 044011 (2000). % \bibitem{Font02a} J.~A. Font, T. Goodale, S. Iyer, M. Miller, L. Rezzolla, E. Seidel, N. Stergioulas, W. Suen and M. Tobias, Phys. Rev. {\bf D65}, 084024 (2002). \end{thebibliography} \include{interface} \include{param} \include{schedule} % Do not delete next line % END CACTUS THORNGUIDE \end{document}