1. Introduction
The plane accretion discs are most considered in theoretical papers. These discs are simpler for study of various effects. Sometimes the authors mention that in general case the accretion discs can have the progressively expanding height (see e.g., Shakura & Sunyaev [
1], Abramowicz & Fragile [
2]).
Our aim is to show the change of the intensity and polarization Stokes parameters and ) for radiation emerging from cone-like inclined rotating accretion discs both in continuum and resonance lines.
We suppose that the inclined atmosphere is similar to usual atmosphere in the plane accretion disc, i.e., we study what arises if this atmosphere is cone-like inclined.
It will be demonstrated that the cone-like atmosphere considerably changes both the polarization degree and angular distribution of emerging radiation. So, it is important to know if the accretion disc is plane or not. It appears, the best technique for this is to consider the polarization angle in resonance line radiation.
The wave electric field oscillations
of the emerging radiation are parallel to the surface of a plane disc, namely
. Here
if line of sight and
is the normal to the disc. Due to symmetry of atmosphere relative to plane (
nN) the possible direction of
is to be
. Such situation corresponds to homogeneous atmosphere and the absence of the regular magnetic field. This occurs, for example, in the Milne problem (see Chandrasekhar [
3]).
Strictly speaking, the another possible polarization for homogeneous atmosphere corresponds to
lying in the plane
, but this case practically is not observed (see Dolginov et al. [
4]). Polarization of emerged radiation appears as a result of the last scatterings before escaping the homogeneous atmosphere. Inside the atmosphere the radiation can be nonpolarized.
Now we consider the rotating accretion disc with the progressive increasing (cone-like) height. We assume that small local surface
is characterized by azimuthal angle
and the normal
to the cone-like radiating atmosphere having the inclination angle
(see
Figure 1). The every
surface of cone-like atmosphere possesses the right-left symmetry and, as a consequence, the wave electric field is
(remember that oscillatting
corresponds to (
)). This occurs both for optically thick and optically thin atmospheres with right-left symmetry relative to the plane
.
In rotating accretion disc the Doppler effect gives rise to the following change of wavelength
:
Here is the central wavelength, is the wavelength in nonrotating atmosphere, is the the rotation velocity in the orbital plane (for the parameter , i.e., is small for n = 1, 2, 3, 4…). The angle is the inclination angle of the mean plane of accretion disc relative to the line of sight , is the azimuthal angle of the radiating surface . Here we take the right-hand rotation with the azimuthal rotation velocity . In this case the right part of rotating disc corresponds to larger wavelength and the left part corresponds to the less wavelength. The centre of a line corresponds to .
Note that for continuum radiation is not important whether inclined disc is rotating or not.
The observations of polarized spectral line H
-radiation and nearby continuum radiation are given in a number of papers (see, e.g., Smith et al. [
5], Afanasiev et al. [
6]). In these papers the Seyfert-1 AGNs are considered. The observations show that for the most sources the polarization (position) angle
is not constant over the spectral line wavelength
.
Below we show that in accretion disc with progressively increasing height the resonance line acquires polarization angle depending on the wavelength .
Our consideration is valid both for continuum radiation and the resonance line one. Note, that the cone inclination angle can be estimated from observed angle of a line. Our main assumption is that electric field oscillations are perpendicular to the plane . This is quite analogy to the plane accretion disc, where . Remember that the line of sight (the direction to a telescope) is characterized by the unite vector .
Due to symmetry of the atmospheres relative to the plane , the determination of polarization angle is pure geometrical problem. Let us give the solution of this problem.
2. Geometric Derivation of Polarization Angle
Let us denote
as the normal to small local surface element
on the inclined ring. This surface element is characterized by the azimuthal angle
. The angle between the normal
and the normal to the central plane of accretion disc
is the ring’s inclination angle
:
. The normal
depends on the angles
and
:
Here
and
are the unit vectors of the common coordinate system
(see
Figure 1). The line of sight
is taken in the plane
:
The angle
is the angle between vectors
and
. Frequently one denotes
. The wave electric field oscillations
of the emerging radiation from the element
of inclined atmosphere is parallel to the vector product
direction (remember that
,
,
):
Note that vector is perpendicular to the plane . The sources in the inclined ring are assumed homogeneous. The right-left symmetry of such distribution gives rise to the wave electric oscillations perpendicular to the plane , i.e., . It is convenient to choose and consider the positive axis Y as the basic one. The directed along positive Y is taken having polarization angle . It is convenient to use the vector algebra, but taking into mind that and describe the same wave electric oscillations.
The direction of -oscillations from all places of the plane accretion disc ( holds along the vector , i.e., is parallel to the Y-axis (in this case we take the polarization angle ).
Note that at
and
the direction of
, i.e., electric wave oscillations hold along
. Futher we take
), where
looks like in
Figure 1.
The wave electric vector
is perpendicular to the line of sight
. It holds in the plane
, where the unit vector
lies in the plane
(see
Figure 1):
Equation (
4) transforms to:
We take reference frame
as corresponding to the telescope coordinate system. If the radiating surface element
lies on the conical surface, then the
-vector oscillates along the direction, characterized by the angle
(see
Figure 1). Formula for
is:
The angles
and
describe the electric oscillations along the
Y-axis. Note that the vectors
and
, i.e., the angles
and
describe the same radiative oscillations. The vector
corresponds to negative signs of
and
. The values
are positive. The Equation (
7) can be written in the form:
For
the value
. It is seen that the denominator of Equation (
8) diminishes with
. This means that the polarization angle
acquires the maximum in the range of
.
Note, that for we have and the the expression (8) is positive for all values from up to . This corresponds to the polarization angle lying in the first quadrant of coordinates.
For we observe the all inclined atmosphere perpendicular to the central plane of accretion disc. In this case . This means that . In this case is independent of inclination angle .
Below we consider the case when a telescope observes all surface of inclined atmosphere, i.e., the angle is taken in the interval . For cases, when we observe only part of inclined atmosphere, the results depend on the unclear contribution of the lateral part of the atmosphere, which is not considered in our model. It should be noted that this restriction leaves a large field of applications.
In the case
there is the negative part of
, corresponding to negative
. In this case
where
is the angle between
and the negative part of the Y axis. The additional inclination angle relatively positive Y-axis is equal to
So, the total inclination angle is
. Instead of Formula (8) we obtain the relation:
Thus, for the expression for is to be obtained by two stages: for positive () one can use the Formula (8), and for negative () it is necessary to use Formula (11).
As an example, in
Table 1 we give the polarization angle
for
and different values of angle
.
The Case of Spectral Line
It is interesting to obtain the —dependence of polarization angle in spectral lines, which is frequently presented in atlases.
Equation (
1) gives the
—dependence of
:
Substitution of
and
into Formula (8) gives rise to
-dependence of
:
Note, that the main difficulty is to obtain from observed spectral line. The authors are working on this problem.
The polarization angle
near the centre of a line depends on
with
. Such dependence of
is frequently seen in atlases Smith et al. [
5] and Afanasiev et al. [
6].
How to estimate the inclination angle
of conical atmosphere from observed resonance line? The maximum value of
in resonance line occurs at azimuthal angle
. Equation (
7) gives for
the following formula:
Introducing this value into Formula (8) for
, we obtain the value
:
The values
can be taken from the data of observed resonance line polarization. There are many techniques to estimate the inclination angle
of mean plane of accretion disc (see, e.g., Marin [
7]). Thus, Formula (15) allows us to estimate the inclination angle
of cone-like atmosphere.
For example, let us consider the source Akn 120, where
. According to Marin [
7] we take
. From Formula (15) we obtain
. Of course, this result takes place if we assume that the source Akn 120 exists in accretion disc with progressively increasing height.
The inclination angle is related with rotation velocity . This gives an additional technique to estimate the velocity .
The polarization angle
is asymmetric function of
. This is why there exist the opposite polarization angles in red and blue wings of a spectral line. Further we consider
in the interval
. For
the angle
increases steadily from zero at
up to
and then decreases up to zero at
(see
Table 1).
We see that the polarization angle does not depend on the intensity and polarization of the radiation, emerging from the -point. The angle depends on the angles and , i.e., depends on pure geometrical values.
In particular, angle can take the values greater than for large . This case corresponds to the total observed radiation having the —ocillations in the plane . Such position angle holds in many Seyfert-1 AGNs.
3. Calculation of Observed Angular Distribution and Polarization
It is known that the Stokes parameters depend on
(see Chandrasekhar [
3]). The Stokes parameters of radiation, escaping from the inclined ring, depend on
:
The obtained formulas for are valid for every radiation—continuum or spectral one. They describe the polarization angle of radiation from inclined surface , where is the distance from the centre of an accretion disc.
We observe the radiation fluxes
and
from accretion discs visible as point-like sources:
Parameter
for continuum radiation, due to symmetry of an accretion disc, is equal to zero. The unknown factors in intensity and the radiating ring area we denoted as Const. The value R is the distance to the accretion disc,
is the angular distribution and
is the polarization degree of outgoing radiation from the plane atmospfere (
). Considering the spectral radiation, we can use the relation (see Equation (
1)):
, i.e., in this case the
—integration is related with the spectrum of the resonance line.
4. Some Results
The detailed tables of
and
in % (with
) are given in Silant’ev et al. [
8]. They describe the Milne problem in optically thick electron atmosphere (see Chandrasekhar [
3]). Using these tables, one can calculate the values of
and
for different values of parameters
and
.
The values
and
for total observed continuum radiation are given in
Figure 2 and
Figure 3. In these figures we take
, i.e., a telescope observes all surface of a radiating ring.
Figure 2 demonstrates that the radiation polarization from the total inclined ring diminishes with the increase of the inclination angle
.
Figure 3 shows that the flux of radiation sharply decreases with the increase of
. Its form becomes more flat as compared to the plane accretion disc (
).
Note that our negative corresponds to the wave electric field oscillations perpendicular to the plane . This corresponds to standard polarization angle in the Milne problem. It is very interesting that for (positive p) the oscillations hold in the plane , as in many Seyfert 1 galaxies.
Clearly, that for large the plane takes the position close to be perpendicular to the normal . In this case the -oscillations become close to the plane . Note that, if we observe such sidelong part of gas-dusty torus with , then the -oscillations will be in the plane (.
As far as resonance line, it should be noted that the rotation gives rise to an additional broadening of parameters
and
(see e.g., Silant’ev et al. [
9]).
Our theory calls in question the known technique of inclination angle estimation from measurement of radiation polarization degree. The latter uses the polarization degree for plane accretion disc. We have shown that the inclined atmosphere gives smaller values of polarization.