The faintest sources visible on the objective prism plate have
,
while the depth of the direct plate is comparable with the blue plate of the
POSS I. X-ray sources with no optical counterpart on the HQS direct plate
were searched on the red POSS plate, and most of them were found.
As has been noted before, low resolution HI surveys gave an average value
of for galactic
hydrogen in HS 47.5/22. A new and better resolved map was obtained with the
100 m RT at Effelsberg (9' beam) to allow individual corrections. The
observations were performed during two observing runs in 1989, resulting in a
grid with separations
and
, slightly incomplete at the edges.
The measurements are contaminated by stray radiation arising from the sidelobes of the telescope, which can be removed through an all sky deconvolution provided the complete antenna pattern is known. Kalberla et al. (1980) use this method to correct their measurements with the 100 m RT. Lockman et al. (1986) take a different approach, they combine their spectra to synthetize the beam of the Stark Survey, which is practically uncontaminated (Stark et al. 1992). Any differences between the combined data and the corresponding Stark Survey spectra are attributed to stray radiation present in the former and are therefore subtracted.
Both approaches give a good accuracy but need large amounts of computer time
and storage capacity. For the present work, the much easier though less
accurate ( in
) time independent correction
presented in Kalberla et al. (1980, their Sect. 4.2) is used. They
found with several assumptions that the corrected main beam brightness
temperature
is
where is the observed profile area expressed in
, and
is the measured antenna temperature.
The small size of HS 47.5/22 means that the distance to the Milky Way does not
vary greatly so that it is possible to use one common correction factor.
This factor is obtained by dividing
values from the
Stark Survey by the uncorrected 100 m RT values at the same positions, and
averaging the results:
Figure 5 (click here) shows a contour plot of the corrected column density in
HS 47.5/22. Empty grid positions have been filled with the weighted means of
the neighbouring positions for the plot.
Figure 5: Contour plot of in HS 47.5/22. Contours are plotted in
steps of
, starting at
(contour 1). Coordinates are B1950.0
Variations of a factor
, already
indicated in the low resolution surveys, could be confirmed on scales of less
than 30'. Regions with high
can be found near the eastern
and along the southern borders of HS 47.5/22 and in the north western edge.
The lowest value in the area between is less than
. A high velocity cloud found by Hulsbosch &
Wakker (1988) is present in our data as well. It is, however, not the
reason for the variations in
since the column density peaks
of the cloud do not coincide with the overall maxima.
HS 47.5/22 was surveyed with the DRAO interferometer (Penticton/Canada) at 21cm and 74cm in March 1993. A full analysis of the DRAO observations is under way and will be published elsewhere.
In addition, HS 47.5/22 is located inside the area of several radio continuum
surveys which became available during the project. Table 2 (click here) gives
an overview of position accuracies and flux limits of these surveys. These
catalogues are crosscorrelated with the X-ray source list. A source is
considered identified if the X-ray and radio positions agree within the
errors. Only a few X-ray sources match with objets from either catalogue;
they are listed in Table 3 (click here). Two sources match with
phase calibration sources in Patnaik et al. (1992); they are included
in the table.
References | flux limit | pos.err. | |
87GB (6cm) | (1) | ![]() | ![]() |
GB 1.4 GHz | (2) | 100mJy | ![]() |
B3 408 MHza | (3) | 100mJy | 15''/35''b |
Texas 365 MHz | (4) | ![]() | ![]() |
DRAO 21cm | (5) | ![]() | ![]() |
DRAO 74cm | (5) | ![]() | ![]() |
a: covers |
b: errors in ![]() | ||
c: ![]() |
![]() | RXJ | (1) | (2) | (3) | (4) | (5) | |
9 | 0943.5+4633 | 3'' | D | ||||
27 | 0944.6+4638 | 19'' | D | ||||
53 | 0945.6+4636 | 3'' | 8'' | 9'' | 4'' | 5'' | D |
64 | 0945.9+4619 | 12'' | gal. cand. | ||||
180 | 0950.2+4553 | 28'' | BLLaccand.a | ||||
284 | 0953.6+4625 | 26'' | 40'' | 25'' | D | ||
317 | 0954.7+4608 | 43'' | 37'' | D | |||
321 | 0954.8+4715 | 17'' | 10'' | D | |||
347 | 0955.6+4721 | 22'' | 19'' | D | |||
424 | 0957.7+4848 | 60'' | 23'' | D | |||
425 | 0957.7+4745 | 21'' | AGNa | ||||
443 | 0958.3+4608 | 36'' | AGNa | ||||
446 | 0958.3+4725 | 4'' | 9'' | 18'' | 5'' | OK492b | |
534 | 1000.9+4640 | 13'' | 29'' | AGN cand. | |||
555 | 1001.5+4659 | 23'' | AGN groupa | ||||
571 | 1003.1+4757 | 28'' | unident. | ||||
a: identified in this work. | |||||||
b: Peterson et al. (1978). |