Issue 
A&A
Volume 498, Number 2, May I 2009



Page(s)  471  477  
Section  Interstellar and circumstellar matter  
DOI  https://doi.org/10.1051/00046361/200811518  
Published online  19 March 2009 
The Polish doughnuts revisited
I. The angular momentum distribution and equipressure surfaces
Lei Qian^{1,}^{}  M. A. Abramowicz^{1,2}  P. C. Fragile^{3,1}  J. Horák^{4,1}  M. Machida^{5}  O. Straub^{2,1}
1 
Department of Physics, Göteborg University,
41296 Göteborg, Sweden
2 
N. Copernicus Astronomical Center, Polish Academy
of Sciences,
Bartycka 18, 00716 Warszawa,
Poland
3 
Physics & Astronomy College of Charleston,
58 Coming Street Charleston SC
29424, USA
4 
Astronomical Institute, Academy of Sciences of the
Czech Republic, Bocni II/1401a, 14131 Prague, Czech Republic
5 
National Astronomical Observatory of Japan 2211 Osawa,
Mitaka, 1818588 Tokyo, Japan
Received 12 December 2008 / Accepted 10 March 2009
Abstract
We construct a new family of analytic models of black hole accretion disks in dynamical equilibria. Our construction is based on assuming distributions of angular momentum and entropy. For a particular choice of the distribution of angular momentum, we calculate the shapes of equipressure surfaces. The equipressure surfaces we find are similar to those in thick, slim and thin disks, and to those in ADAFs.
Key words: black holes physics  accretion, accretion disks
1 Introduction
In accretion disk theory one is often interested in phenomena that
occur on a ``dynamical'' timescale
much shorter
than the ``viscous'' timescale
needed for
angular momentum redistribution and the ``thermal'' timescale
needed for entropy redistribution^{},
The question whether it is physically legitimate to approximately describe the black hole accretion flows (at least in some ``averaged'' sense) in terms of stationary (independent on t) and axially symmetric (independent on ) dynamical equilibria, is not yet resolved. While observations seem to suggest that many real astrophysical sources experience periods in which this assumption is quite reasonable, several authors point out that the results of recent numerical simulations seem to indicate that the MRI and other instabilities make the black hole accretion flows genuinely nonsteady and nonsymmetric, and that the very concept of the separate timescales (1) may be questionable in the sense that locally . However, this assumption has been made in all existing comparisons between theory and observations, be they by detailed spectral fitting (e.g. Shafee et al. 2008,2007, and references there), line profile fitting (e.g. Fabian & Vaughan 2003), or studying small amplitude oscillations (see Abramowicz 2005, for references). It seems that the present understanding of the black hole accretion phenomenon rests, in a major way, on studies of stationary and axially symmetric models.
From the point of view of mathematical selfconsistency, in
modeling of these stationary and axially symmetric dynamical
equilibria, distributions of the conserved angular momentum
and entropy,
may be considered as being free functions of the Lagrangian coordinates (Ostriker et al. 1966; Bardeen 1970; Abramowicz 1970). The Lagrangian coordinates are defined by demanding that a narrow ring of matter , has the rest mass with being the rest mass density. In the full physical description, the form of the functions in (2) is not arbitrary but given by the dissipative processes, like viscosity and radiative transfer. At present, several important aspects of these processes are still unknown, so there is still no practical way to calculate physically consistent models of accretion flows from first principles, without involving some ad hoc assumptions, or neglecting some important processes. Neither the hydrodynamical simulations (that e.g. use the ad hoc const. viscosity prescription), nor the present day MHD simulations (that e.g. neglect radiative transfer) could be considered satisfactory. Furthermore, the simplifications made in these simulations are mathematically equivalent to guessing free functions (such as the entropy distribution). Bohdan Paczynski pointed out that it could often be more pragmatic to make a physically motivated guess of the final result, e.g. to guess the form of the angular momentum and entropy distributions.
In practice, it is far easier to guess and use the coordinate
distributions of the specific angular momentum and entropy,
than the Lagrangian distributions (2). However, one does not known a priori the relation between the conserved and specific angular momenta (and entropy), or the functions, , . Thus, assuming (3) and (4) is not equivalent to assuming (2), and usually it should be a subject to some consistency conditions. We shall return to this point in Sect. 6.
In several ``astrophysical scenarios'' one indeed guesses a
particular form of (3) and
(4). For example, the celebrated
Shakura & Sunyaev (1973) thin disk model assumes the Keplerian
distribution of angular momentum,
and the popular colddiskplushotcorona model assumes a low entropy flat disk surrounded by high entropy, more spherical corona. These models contributed considerably to the understanding of blackhole accretion physics.
The mathematically simplest assumption for the angular momentum
and entropy distribution is, obviously,
This was used by Paczynski and his Warsaw team to introduce the thick disk models (Jaroszynski et al. 1980; Abramowicz et al. 1978; Kozowski et al. 1978; Paczynski & Wiita 1980; Abramowicz 1981; Paczynski 1982; Abramowicz et al. 1980). Thick disks have characteristic toroidal shapes, resembling a doughnut. Probably for this reason, Martin Rees coined the name of Polish doughnuts^{} for them.
Figure 1 shows a comparison of a
stateofart MHD simulation of blackhole accretion (time and
azimuth averaged) with a Polish doughnut corresponding to a
particular
.
Both models show the same characteristic
features of black hole accretion: (i) a funnel along the rotation
axis, relevant for jet collimation and acceleration; (ii) a
pressure maximum, possibly relevant for epicyclic oscillatory
modes; and (iii) a cusplike selfcrossing of one particular
equipressure surface, relevant for an inner boundary condition,
and for stabilization of the PapaloizouPringle (Blaes 1987),
thermal, and viscous instabilities (Abramowicz 1971). The cusp is
located between the radii of marginally stable and marginally
bound circular orbits,
Polish doughnuts have been useful in semianalytic studies of the astrophysical appearance of superEddington accretion (see e.g. Sikora 1971; Szuszkiewicz et al. 1996; Madau 1988) and in analytic calculations of smallamplitude oscillations of accretion structures in connection with QPOs (see e.g. Blaes et al. 2006). In the same context, numerical studies of their oscillation properties for different angular momentum distributions were first carried out by Rezzolla et al. (2003b,a). Moreover, Polish doughnuts are routinely used as convenient starting initial configurations in numerical simulations (e.g. De Villiers & Hawley 2003; Hawley et al. 2001). Recently, Komissarov (2006) has constructed analytic models of magnetized Polish doughnuts.
Figure 1: Equipressure surfaces in a very simple and analytic Polish doughnut ( left, with linear spacing), and a sophisticated, stateofart full 3D MHD numerical simulation ( right, with logarithmic spacing). Although the shapes of equipressure surfaces are remarkably similar, in the numerical model the pressure gradient is seriously larger, and visibly enhanced along roughly conical surfaces, approximately from the equatorial plane. 

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2 Assumptions and definitions
We assume that the accretion flow is stationary and axially
symmetric. This assumption expressed in terms of the
BoyerLindquist spherical coordinates states that the flow
properties depend only on the radial and polar coordinates ,
and are independent on time t and azimuth .
We
also assume that the dynamical timescale is much shorter than the
thermal and viscus ones (1). Accordingly, we ignore
dissipation and assume the stressenergy tensor in the perfect
fluid form,
with p and being the pressure and energy density, respectively. The four velocity of matter u^{i} is assumed to be purely circular,
The last assumption is not fulfilled close to the cusp (see Fig. 1), where there is a transition from ``almost circular'' to almost ``freefall'' radial trajectories. Nevertheless, the transition could be incorporated in the form of the inner boundary condition (the relativistic Roche lobe overflow, see e.g. Abramowicz 1985).
One introduces the specific angular momentum ,
the
angular velocity ,
and the redshift factor A by the well
known and standard definitions,
The specific angular momentum and angular velocity are linked by
The conserved angular momentum is given by,
3 The shapes of the equipressure surfaces
In this section we briefly discuss one particularly useful result obtained by Jaroszynski et al. (1980). It states that for a perfect fluid matter rotating on circular trajectories around a black hole, the shapes and location of the equipressure surfaces const follow directly from the assumed angular momentum distribution (3) alone. In particular, they are independent of the equation of state, , and the assumed entropy distribution (4).
For a perfectfluid matter, the equation of motion
yields,
which may be transformed into,
From the second derivative commutator of the above equation,
one derives (see e.g. Abramowicz 1971) the von Zeipel condition: = const. surfaces coincide with those of , if and only if the surfaces coincide with those ^{}. Obviously, the constant angular momentum case satisfies the von Zeipel condition.
Jaroszynski et al. (1980) have also discussed a general, non barytropic
case. They wrote Eq. (14) twice, for i = r and
,
and divided the two equations side by side to get
For the Kerr metric components one knows the functions , and therefore the function in the right hand side of Eq. (17) is known explicitly in terms of r and , if one knows or assumes the angular momentum distribution . This has an important practical consequence.
Let
be the explicit equation for the
equipressure surface
const. It is,
.
If the function
in (17) is known, then Eq. (17) takes the
form of an ordinary differential equation for the equipressure
surface,
,
with the explicitly known right hand side. It may be therefore directly integrated to get all the possible locations for the equipressure surfaces.
4 The angular momentum distribution
4.1 Physical arguments: the radial distribution
Jaroszynski et al. (1980) discussed general arguments showing that the slope of the specific angular momentum should be between two extreme: the slope corresponding to and the slope corresponding to const. These two cases, together with the Keplerian one , may be considered as useful archetypes in discussing arguments relevant to the angular momentum distribution.
Indeed, far away from the black hole , these arguments are well known (see e.g. Frank et al. 2002) and together with numerous numerical simulations show that typically (i.e. in a stationary case with no shocks) the specific angular momentum should be slightly subKeplerian . There is a solid consensus on this point.
The situation close to the black hole is less clear because there is not sufficient knowledge of the nature of the stress operating in the innermost part of the flow, i.e. approximately between the horizon and the ISCO. Formally, one may consider two extreme ideal cases, depending whether the stress is very small or very large.
In the first case, the almost vanishing stress implies that the fluid is almost freefalling, and therefore the angular momentum is almost constant along fluid lines. This leads to const. Such situation is typical for the thin Shakura & Sunyaev (1973) and slim (Abramowicz et al. 1988) accretion disks. In the second case, one may imagine a powerful instability like MRI, which occurs when . It may force the fluid closer to the marginally stable state const. This situation may be relevant for ADAFs (Abramowicz et al. 1995; Narayan & Yi 1988).
Figure 2: a) and b): the distribution of angular momentum on the equatorial plane. Thick lines correspond to the angular momentum predicted by our analytic formula, dashed lines show the Keplerian angular momentum distribution and dots to the simulation data. a): Kerr geometry a=0.9 simulations by Sadowski (2008). b): PseudoNewtonian MHD simulations by Machida & Matsumoto (2008). c) and d): angular momentum off the equatorial plane, normalized to its equatorial plane value, . Lines correspond to the distribution at : longdashed , dotted , and short dashed . Points are taken from timedependent, fully 3D, MHD numerical simulations. They correspond to time and azimuthal averages at the same radial location, . c): Points from the simulations of Machida & Matsumoto (2008) in the PaczynskiWiita potential  triangle: high temperature case; square: low temperature case. d): Points from the simulations of Fragile et al. (2007) in Schwarzschild (dots) and a=0.9 Kerr (crosses) spacetimes. 

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4.2 The new ansatz
We suggest adopting the following assumption for the angular
momentum distribution,
The constant is defined by . For the ``hydrodynamical'' case, the function is constant,
while for the ``MHD'' case its is calculated from the condition,
Thus, there are only three dimensionless parameters in the model: (, , ). Their ranges are,
The function is the Keplerian angular momentum in the equatorial plane, , which for the Kerr metric is described by formula (5) and . An equipressure surface that starts from the cusp is marginally bound for , and .
4.3 Angular momentum on the equatorial plane
On the equatorial plane,
,
and therefore only
and
(through
)
enter the distribution
formulae (19).
when , the angular momentum is constant, , and when , it equals the Keplerian one, .
For small values of the assumed equatorial plane angular momentum (23) reproduces the characteristic shape, shown in Fig. 2, which has been found in many numerical simulations of accretion flows  including stationary, axially symmetric, viscosity, hydrodynamical ``slim disks'' (e.g. Abramowicz et al. 1988), and more recent, fully 3D, nonstationary MHD simulations (e.g. Fragile et al. 2009; Machida & Matsumoto 2008). It corresponds to a distribution that is slightly subKeplerian for large radii, and closer to the black hole it crosses the Keplerian distribution twice, at and at , forming a superKeplerian part around . For the angular momentum is almost constant.
4.4 Angular momentum off the equatorial plane
Numerical simulations show that away from the equatorial plane, the angular momentum falls off. Figure 2 shows that indeed several MHD simulations (Fragile et al. 2009; Machida & Matsumoto 2008, Figs. 2c and d respectively), feature a drop of angular momentum away from the equatorial plane. This behavior is reflected by the term in (19). One may see that this form accurately mimics the outcome of the numerical simulations. Proga & Begelman (2003a,b) also studied axisymmetric accretion flows with low specific angular momentum using numerical simulations. In their inviscid hydrodynamical case Proga & Begelman (2003a) found that the inner accretion flow settles into a pressurerotation supported torus in the equatorial region and a nearly radial inflow in the polar funnels. Furthermore, the specific angular momentum in the equatorial torus was nearly constant. This behavior changes once magnetic fields are introduced, as shown in Proga & Begelman (2003b). In the MHD case, the magnetic fields transport specific angular momentum so that in the innermost part of the flow, rotation is subKeplerian, whereas in the outer part, it is nearly Keplerian. Similar rotational profiles are also found in MHD simulations of the collapsar model of gammaray bursts (Baiotti et al. 2008; Proga et al. 2003), which use a sophisticated equation of state and neutrino cooling (instead of a simple adiabatic equation of state). Therefore, it appears that the rotational profile assumed in our model is quite robust as it has been obtained in a number of numerical experiments with various microphysics.
5 Results
Figures 3 and 4 show sequences of models calculated with the new ansatz (19) for blackhole spins a=0 and 0.5, respectively. For these models we hold fixed, while and are varied over the limits of their accessible ranges.
Figure 3: Equipressure surfaces for a = 0 and . Five rows correspond to from the top to the bottom. Four columns correspond to from the left to the right. The upper left corner shows a ``standard'' Polish doughnut. The lower right corner shows an almost Keplerian disk at the equatorial plane, surrendered by a very low angular momentum envelope. 

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Figure 4: Equipressure surfaces for a = 0.5 and . Five rows correspond to from the top to the bottom. Four columns correspond to from the left to the right. The upper left corner shows a ``standard'' Polish doughnut. The lower right corner shows an almost Keplerian disk at the equatorial plane, surrendered by a very low angular momentum envelope. 

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5.1 Equipressure surfaces on the axis of rotation
Figures 3 and 4
show an interesting change of
the behavior of equipressure surfaces close to the axis with
increasing .
No equipressure surface can cross the symmetry
axis when the dependence of the angular momentum on
is
weak. This is the case for the first three columns of
Fig. 3 where
.
On the
other hand, for the angular momentum distributions with higher
the equipressure surfaces cross the axis perpendicularly.
This happens in plots of the last column of Fig. 3. This behavior can be understood easily
from the limit of
as
.
In
Schwarzschild spacetime Eqs. (17) and
(18) give
The limit on the righthand side is either 0, 1 or , depending on the value of . When , and no equipressure surface goes across the axis. On the other hand, when equipressure surfaces cross the axis perpendicularly. Of course, a stationary torus may exist only within an equipotential surface located inside the Roche lobe, i.e., the critical selfcrossing equipotential within the cusp (Abramowicz 1985).
5.2 Comparison with numerical simulations
Figure 5 illustrates that the results of the analytic models are well matched with results of modern 3D MHD numerical simulations (here taken from Fragile et al. 2009,2007). For the correct choice of parameters, the model can reproduce many of the relevant features of the numerical results, including the locations of the cusp and pressure maximum, as well as the vertical thickness of the disk. At this stage, such qualitative agreement is all that can be hoped for. One notable difference between the analytic and numerical solutions is the behavior inside the cusp. While the analytic equipressure surfaces formally diverge toward the poles, the numerical solution maintains a fairly constant vertical height, which is also evident in Fig. 1. This is because in the region inside the cusp, our assumption (10) about the form of the velocity is not valid  velocity cannot be consistent with a pure rotation only, . In this region the radial velocity u^{r} must be nonzero and large. Thus, accuracy of our analytic models may only be trusted in the region outside the cusp, .
6 Discussion
In this paper we assumed a form of the angular momentum distribution (19) and from this calculated the shapes and locations of the equipressure surfaces. This may be used in calculating spectra (in the optically thick case) by the same ``surface'' method as used in works by Sikora (1971) and Madau (1988).
We plan to construct the complete physical model of the interior
in the second paper of this series. Here, we only outline the
method by considering a simplified toy model. Let us denote
.
We assume a toy (nonbarytropic) equation of
state and an entropy distribution, by writing,
Let us, in addition, define two functions connected to the entropy distribution,
From the obvious condition that the second derivative commutator of pressure vanishes, , and Eqs. (25), (26) and (17) one derives,
where G_{r} and are defined as
and can be calculated from the angular momentum distribution using Eq. (14). From (27) it is obvious that one cannot independently assume the functions and ^{}. Assuming is equivalent with assuming the shapes of isentropic surfaces. Indeed, from (26) one concludes that the function that describes an isentropic surface is given by the equation,
that may be directly integrated. Then the condition (27) gives the physical spacing (``labels'') to the isentropic surfaces, and through the equation of state (25) also to equipressure surfaces and isopicnic ( ) surfaces.
Note, that a possible choice corresponds, obviously, to the ``von Zeipel'' case in which equipressure and isentropic surfaces coincide. In this case the denominator in (27) vanishes, implying a singularity unless the numerator also vanishes. The condition for the numerator to vanish is, however, equivalent to the von Zeipel condition.
Figure 5: Comparison of pressure distributions between the analytic model ( dark lines) and numerical simulations ( colors). The results of MHD simulations (taken from Fragile et al. 2009,2007) have been timeaveraged over one orbital period at . Upper panel: Schwarzschild black hole (a=0); the analytic model parameters are , , and . Lower panel: Kerr black hole (a=0.5); the analytic model parameters are , , and . 

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7 Conclusions
The new ansatz (19) captures two essential features of the angular momentum distribution in black hole accretion disks:
 1.
 On the equatorial plane and far from the black hole, the angular momentum in the disk differs only little from the Keplerian one being slightly subKeplerian, but closer in it becomes (slightly) superKeplerian and still closer, in the plunging region, subKeplerian again and nearly constant.
 2.
 Angular momentum may significantly decrease off the equatorial plane, and become very low (even close to zero, in a nonrotating ``corona'').
Acknowledgements
We thank Daniel Proga and Luciano Rezzolla for helpful comments and suggestions. Travel expenses connected to this work were supported by the China Scholarship Council (Q.L.), the Polish Ministry of Science grant N203 0093/1466 (M.A.A.), and the Swedish Research Council grant VR Dnr 62120063288 (P.C.F.).
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Footnotes
 ...^{}
 Permanent address: Department of Astronomy, Peking University Cheng Fu St. 209, 100871 Beijing, PR China.
 ... redistribution^{}
 We use the spherical BoyerLindquist coordinates , the geometrical units c = 1 = G and the + signature. The Kerr metric is described by the ``geometrical'' mass M and the ``geometrical'' spin parameter 0 < a < 1, that relate to the ``physical'' mass and angular momentum by the rescaling, , . Partial derivatives are denoted by and covariant derivatives by .
 ... doughnuts^{}
 However, real Polish doughnuts (called paczki in Polish) have spherical shapes. They are definitely nontoroidal  see e.g. http://en.wikipedia.org/wiki/Paczki
 ...^{}
 The best known Newtonian version of the von Zeipel condition states that for a barytropic fluid , both angular velocity and angular momentum are constant on cylinders, , , with being the distance from the rotation axis.
 ...^{}
 A somewhat similar situation in the case of rotating stars is known as the von Zeipel paradox (Tassoul 1978): Pseudobarytropic models in a state of permanent rotation cannot be used to describe rotating stars in strict radiative equilibrium.
All Figures
Figure 1: Equipressure surfaces in a very simple and analytic Polish doughnut ( left, with linear spacing), and a sophisticated, stateofart full 3D MHD numerical simulation ( right, with logarithmic spacing). Although the shapes of equipressure surfaces are remarkably similar, in the numerical model the pressure gradient is seriously larger, and visibly enhanced along roughly conical surfaces, approximately from the equatorial plane. 

Open with DEXTER  
In the text 
Figure 2: a) and b): the distribution of angular momentum on the equatorial plane. Thick lines correspond to the angular momentum predicted by our analytic formula, dashed lines show the Keplerian angular momentum distribution and dots to the simulation data. a): Kerr geometry a=0.9 simulations by Sadowski (2008). b): PseudoNewtonian MHD simulations by Machida & Matsumoto (2008). c) and d): angular momentum off the equatorial plane, normalized to its equatorial plane value, . Lines correspond to the distribution at : longdashed , dotted , and short dashed . Points are taken from timedependent, fully 3D, MHD numerical simulations. They correspond to time and azimuthal averages at the same radial location, . c): Points from the simulations of Machida & Matsumoto (2008) in the PaczynskiWiita potential  triangle: high temperature case; square: low temperature case. d): Points from the simulations of Fragile et al. (2007) in Schwarzschild (dots) and a=0.9 Kerr (crosses) spacetimes. 

Open with DEXTER  
In the text 
Figure 3: Equipressure surfaces for a = 0 and . Five rows correspond to from the top to the bottom. Four columns correspond to from the left to the right. The upper left corner shows a ``standard'' Polish doughnut. The lower right corner shows an almost Keplerian disk at the equatorial plane, surrendered by a very low angular momentum envelope. 

Open with DEXTER  
In the text 
Figure 4: Equipressure surfaces for a = 0.5 and . Five rows correspond to from the top to the bottom. Four columns correspond to from the left to the right. The upper left corner shows a ``standard'' Polish doughnut. The lower right corner shows an almost Keplerian disk at the equatorial plane, surrendered by a very low angular momentum envelope. 

Open with DEXTER  
In the text 
Figure 5: Comparison of pressure distributions between the analytic model ( dark lines) and numerical simulations ( colors). The results of MHD simulations (taken from Fragile et al. 2009,2007) have been timeaveraged over one orbital period at . Upper panel: Schwarzschild black hole (a=0); the analytic model parameters are , , and . Lower panel: Kerr black hole (a=0.5); the analytic model parameters are , , and . 

Open with DEXTER  
In the text 
Copyright ESO 2009
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