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Astron. Astrophys. 321, 305-310 (1997)
2. Method, observations, and data reduction
We observed with a standard radioastronomy receiver of wide
frequency bandpass: a linearly polarized antenna, a receiver followed
by a detector, time constant, and a recording system. No polarimeter
and no dedispersion system were used, and no calibration (except for
the ionosphere) was necessary. We recorded individual pulsar pulses,
for our purpose these pulses should have a strong linearly polarized
component. As these pulses drift downwards in frequency through the
bandpass following the delay in arrival time (due to the cold
interstellar plasma dispersion law) they will experience a rotation of
the plane of polarization (Faraday effect) (Fig. 1). It is very common
to have a pulsar pulse with a variable linearly polarized component,
and where the (intrinsic) sky angle of the direction of the linear
polarization is variable through the pulse (e.g. Rankin & Benson
1981, Stinebring et al. 1984, Rankin et al. 1989). Nevertheless, the
signal component within a pulse which has the maximum linearly
polarized flux has a well defined polarization direction in many
pulsars, and we will take this to be the dominant linear polarization
angle. The intrinsic sky angle of polarization at source
is taken to be constant over the receiver
bandpass at any given pulse longitude, including that of the dominant
linear polarization. After propagation through the interstellar medium
the direction of this dominant linearly polarized electric field
vector rotates as a function of frequency. If observed with an
antenna-receiver system that measures full intensity (e.g. two
cross-polarized antennas with a receiver each, both detected outputs
summed together) followed by our backend and recording system we will
simply see a dispersed pulse (Fig. 1b). If instead we use a single
linearly-polarized antenna-receiver system that receives a signal with
a linearly-polarized component whose electric vector rotates as a
function of frequency (Fig. 1c), then the voltage induced in the
linearly-polarized antenna is the dot product of the electric vector
and a unit vector in the direction of the antenna polarization. As a
function of time within the dispersed pulse this will result in a sine
wave: the electric vector either aligns itself with the
linearly-polarized antenna at certain frequencies, where we will have
the maximum of the sine, or is perpendicular to it at others, where we
will have the minimum of the sine, or, for in-between frequencies, we
will have the sine projection values. All other pulse components
(circularly polarized, non-polarized, etc.) will also be received by
this linearly-polarized antenna-receiver system, and will be the
non-polarized component of the pulse, as shown in Fig. 1.
![[FIGURE]](img7.gif) |
Fig. 1. Cartoon representation of the output of the pulsar pulse when observed with three different receiver systems. a Single pulse as observed with a narrowband filter (not dispersed), or at source (intrinsic). b Dispersed pulse at the output of our wideband receiver system, if we observe intensity (non-polarized system). Amount of linear polarization contribution is indicated. c Same as b but observed with a linearly polarized antenna. Alignment of the dominant linearly polarized electric vector and the antenna dipole is indicated at different frequencies (times) as the dispersed pulse descends in frequency within the passband.
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The time delay (sec) of the arrival of a
pulse at the frequency f (MHz) from the arrival at
due to interstellar medium dispersion is
![[EQUATION]](img11.gif)
where and DM is the dispersion
measure, pc cm-3. The angle of
rotation (rad) of the plane of linear polarization at the frequency
f from the intrinsic sky angle due to
Faraday rotation is
![[EQUATION]](img14.gif)
where the rotation measure RM ( )
is
![[EQUATION]](img16.gif)
![[EQUATION]](img17.gif)
where , R is the distance pulsar -
observer, in µGauss, and
if the magnetic field is pointed towards the
observer. Consider two frequencies: and
, between which the electric field vector (or
the plane of the dominant polarization) executes one half of a full
turn ( ) (that is, sinusoid maximum to maximum,
one full period)
![[EQUATION]](img23.gif)
Between and there is
a dispersion delay
![[EQUATION]](img25.gif)
Hence, for one turn of the polarization
plane there is a delay that we obtain from Eq. (2) and (3) (Smirnova
1991) (after replacing constants)
![[EQUATION]](img26.gif)
Note that depends exclusively on
here, and will be constant through the bandpass.
is a constant in the temporal domain, that is
is the same at all receiver frequencies.
does not depend on the sign of RM or
, hence it tells us their absolute value,
however, it is possible to determine indirectly the sign for new
measurements (see below). The detected output of our wideband receiver
shows the pulsar pulse as wide pulses, smeared by dispersion over the
bandpass (Fig. 1a and b). With a linearly-polarized antenna-receiver
system within these widened pulses we will see the sine modulation of
period as the dominant linearly-polarized
component of the pulsar pulse changes its angle continuously with
respect to the direction of polarization of the antenna (Fig. 1c).
That remains constant throughout the BW
is a good assumption, since we select , where
is the center receiver frequency. We emphasize
that, having eliminated the dependence in the
measured parameter , the primary
parameter measured with our method is the magnetic field
(Eq. (4)), which is of physical interest, and
has errors due only to our measurement of and
reduction procedures. The RM is a derived parameter in
our experiment, and includes the errors of the DM measurements
done separately.
We chose the observation frequency and the bandpass so that we have
a dispersion delay over the bandpass as large
as possible, so the number of rotations of the electric vector would
be as large as possible. But it must be , where
is the pulsar period, so that consecutive
pulses do not overlap. BW should also be consistent with the receiver
(and interference!) constraints. For a proper fitting we need a
minimum of two or three sine cycles (better more), that is BW
should be larger than or
, depending in part on the signal-to-noise
ratio. If these conditions are not met a different receiver frequency
may solve the problem.
For observation we have selected mostly pulsars of a tabulated
average flux mJy at 400MHz, however, because of
signal variability some pulsars weaker than this limit produced good
results, and some pulsars stronger than this limit produced poor or no
results. If polarization characteristics were known high linear
polarization pulsars were preferred.
Observations were carried out in August - September, 1992, at
Arecibo. Strong interference at the preferred 130MHz band precluded
observations. At 318MHz seven pulsars turned out to be too weak, and
two others (PSR 1845-01 and PSR 1900 06) had no
sinusoidal modulation superimposed, presumably because of a low linear
polarization component. Positive results were obtained for seven
pulsars, all at 318MHz. Table 1 lists them, the bandwidth
BW used, their dispersion smearing and
period .
![[TABLE]](img37.gif)
Table 1. Pulsars observed at 318 MHz and their parameters: , pulsar period; BW, observational bandwidth; , dispersion delay over the observational bandwidth; N, number of points of running average; n, number of 15-minute observations used in the processing.
The detected output of the receiver (integrated by a 2 msec time
constant) was sampled with an A/D converter with a period of of 0.5
msec, and continuous 15-minute recordings on tape were done, n
recordings per pulsar (Table 1). Then the time average of the
dispersion-smeared pulse profile was obtained by folding the data with
a period , where 512 bins were distributed. No
pulse selection was done. Since the beginning of the integration had
an arbitrary pulse phase we normally rotated cyclically the integrated
pulse so that the beginning of the pulse corresponded to the low order
bins. A running average smoothing of N consecutive points
(Table 1) was done to improve the signal-to-noise ratio. To
obtain the period of the sine a least-squares fitting of the sum of a
sine and a second degree polynomial was done, and the sine frequency,
phase and amplitude, the three polynomial coefficients, and their
errors were obtained from the fit. Using higher degree polynomials did
not improve the fit. Of the fitted parameters only the frequency of
the sine is of interest. As the modulated part of the dispersed pulse
was less than only the part of the pulse period
with sinusoidal modulation was used in the fitting procedure.
Different parts of the pulse may have linear polarization
components that have different polarization sky angles. Each will
produce sines of the same frequency but different phase. Because the
sum of sines of constant frequency (which depends only on
) but arbitrary phase is also a sine of the same
frequency, we do not have to separate the contributions from different
pulse longitudes. In many pulsars the polarization angle swings over
the whole pulse longitudes range (e.g. Rankin & Benson 1981) is of
the order of or less, the resulting sine will
be of larger amplitude than the original sines. Fitting to the
resulting sine produces the same result (frequency) as fitting to
separate pulse component sines. Nevertheless, in most cases one
component at a specific pulse longitude predominated.
The signal inside the receiver goes through a square-law detector,
however, the reasoning developed above is valid for the voltage
induced by the electric field in the antenna, not the power. The
voltage sinusoid that we obtain in this experiment after going through
the square-law detector becomes the sum of a sine and double frequency
cosine. The contribution of the double-frequency cosine term is small,
and it becomes significant only if the pulse linear polarization
component approaches 100%, not common in pulsars. In any case
double-frequency distortion adds little to the error in the fitting
procedure, where we are primarily interested in the frequency of the
sine.
© European Southern Observatory (ESO) 1997
Online publication: June 30, 1998
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