We have observed the CO
(115 GHz) and
HCN
(88.6 GHz) lines in a sample of 20 Seyfert
galaxies. The Southern sample was observed in December 1997 and
October 1998 with the 15 m SEST
at La Silla, Chile. Since the
100 GHz and 115 GHz can be used simultaneously with the 150 GHz and
the 230 GHz receivers, respectively, we also observed
CS
(147 GHz) and CO
(230 GHz). All
receivers were tuned to the single-band mode and typical system
temperatures, on the
-scale, were 150 K at 89 GHz, 200 to 300 K
at 115 GHz, 200 K at 150 GHz and 300 K at 230 GHz. The HPBWs are
57'', 45'', 34'', and 22'', respectively. The backends were
acousto-optical spectrometers with 1440 channels and a channel width
of 0.7 MHz. We used dual-beam switching with a throw of about
in azimuth, with pointing errors being typically
rms on each axis. The intensity was calibrated using the
chopper-wheel method. For the first observing run the weather was
excellent, and only the removal of linear baselines was
required. However, two of the sources, NGCs 6814 and 7130, were within
the sun-limit and, after the application for more time, were observed
during the second run under similarly good conditions.
Transition | ![]() |
HPBW [''] |
![]() |
||
OSO | SEST | OSO | SEST | ||
HCN
![]() |
89 | 44 | 57 | 0.59 | 0.75 |
CO
![]() |
115 | 33 | 45 | 0.50 | 0.70 |
CS
![]() |
147 | - | 34 | - | 0.66 |
CO
![]() |
230 | - | 22 | - | 0.50 |
The Northern sample was originally observed in February 1998 with the
20 m telescope at Onsala Space Observatory (OSO). During this session,
however, the weather was unfavourable and more time was awarded for
the following November. Both the CO
and
HCN
transitions were observed with the SIS 100 GHz
receiver. The HPBWs are 33'' and 44'', respectively. The backend
was a filter-bank with a bandwidth of 512 MHz and a channel
separation of 1 MHz. We used a similar dual-beam switching as the SEST
observations and obtained similar pointing errors. Although far from
ideal for most of the session, the weather was a great improvement
over the previous run, with HCN being observed when the weather was
poorest. Typical system temperatures were around 500 K for CO. This is
considerably worse than the optimal 300 K, but given the improved
receivers, is comparable with the system temperatures of
Heckman et al. (1989). Some of the Northern sources were re-observed in April
1999 when the excellent weather gave system temperatures of
K and
K for the HCN and CO lines,
respectively. As with the SEST data, only linear baselines were
removed.
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