Table 3
lists redshifts, absolute magnitudes, colours,
proper motion indices, and the two variability indices of
the 77 QSOs, Sey1s, and NELGs from our follow-up spectroscopy.
In a similar style, Table 4
summarises the data for
the 104 QSOs, Sey1s, and NELGs identified in the NED. The distribution
of these types over the three priority classes from the VPM survey
is given in Table 4.
In the high priority subsample, 94% of the candidates were found
to be QSOs/Sey1s, while the contamination by foreground stars is
as low as 4%. For the combined sample of high-and-medium-priority
objects the success rate (i.e., the fraction of established QSOs/Sey1s among
all candidates) is still as high as 63%.
![]() |
Figure 6:
Cumulative QSO surface density ![]() ![]() |
Figure 2 illustrates that a high fraction of all QSOs
in the field are strongly variable. The B standard deviation due to
variability is about 0.2 mag for QSOs with B<19.7. In this magnitude
range, more than 60% of the QSOs/Sey1s show the strong variability of
high-priority VPM candidates. (A detailed analysis of the
variability properties will be deferred to a separate study.)
For 90% of QSOs/Sey1s, both variability indices are above the
selection thresholds. We find that 50 out of the 53 NED
QSOs/Sey1s with B<19.7 match the selection criteria of our survey,
corresponding to a completeness of 94% for the VPM survey.
Only for two objects both variability indices fall below the selection
thresholds; another one has a proper motion index slightly above the
threshold.
The subsample of the 114 QSOs with B<19.7 is considered nearly complete.
These QSOs are homogeneously distributed over the search field
(Fig. 3). In particular, the
QSO surface density in the northern half of the field, which
is not covered by the CFHT blue grens survey, is comparable to that in the
southern part where almost all known QSOs are in the CFHT survey.
An additional three QSOs were detected by the VPM search
in the CFHT field. Two of them (No. 5, 15) have "normal'' spectra and
were obviously ignored by chance in the CFHT survey; the other one (No. 7)
shows very strong broad absorption line (BAL) features.
The subsample is of course flux-limited, and
is therefore
strongly correlated with z (Fig. 4). Only for
,
the subsample is complete with regard to luminosities
(since B<19.7 for QSOs of such z). Note that most of the
objects with z<0.55 shown in Fig. 4 are Sey1s.
The redshift distribution is shown in Fig. 5
both for (a) the subsample from Table 3
and (b) the sample of
all identified QSOs with .
The shape of
the z distribution is roughly comparable with that from the SDSS Quasar
Catalogue I. Early Data Release (Schneider et al. 2002),
corroborating the result from VPM survey in the M 92 field
(Brunzendorf & Meusinger 2002).
This impression is confirmed by the two-tailed KS two-sample test.
According to this test on a significance level
,
we have
not to reject the null hypothesis that our subsamples (a) and (b)
and the SDSS sample were drawn from the same population.
![]() |
Figure 8:
Colour-colour diagram for the M3 field. QSOs/Sey1s are shown as
![]() ![]() ![]() |
![]() |
Figure 9:
Colour-redshift relations for the the QSOs/Sey1s in the M3 field.
Panels a), b) show the objects from Table3
(![]() ![]() |
The "completeness'', or absolute efficiency, of the survey can
be estimated by comparing the QSO surface densities, i.e. number counts
per solid angle, to the densities predicted by other surveys.
Figure 6 shows the surface density of all QSOs
(i.e.,
)
with B<19.7 in our search field,
compared with mean relations from
various data samples. The cumulative density N(<B) is simply computed by
dividing the number of QSOs brighter than a given magnitude by the
effective search area where the B magnitudes were corrected for an
interstellar extinction of
mag.
The size of the
Schmidt field is
3. After subtracting the
areas of the plate margins
(not shown in Fig. 3), the calibration wedge, the crowded inner
part of M 3, and the area covered by the images of the objects
in the remaining field, the effective search area amounts to 7.8 deg2.
The resulting number-magnitude relation is roughly described
by
with
for
17.5<B<18.5and
for
18.5<B<19.5, in agreement with
the result from the M 92 field
(Brunzendorf & Meusinger 2002). The surface densities
for our total QSO sample are higher than those
derived by Hartwick & Schade (1990), especially at brighter
magnitudes. There are 9 QSOs with B<18 in our search field,
corresponding to 1.15 QSOs deg-2 mag-1, i.e.
a factor of 1.8 more than in the Hartwick & Schade data.
More recently, La Franca & Cristiani (1997)
derived surface densities of 0.76 QSOs deg-2 0.5 mag-1for
and
,
to be compared with
1.28 QSOs deg-2 0.5 mag-1 for our sample.
The surface densities based on single-epoch observations are affected
by variability and cannot be compared directly to those
based on time-averaged magnitudes. It should be noticed however
that Hartwick & Schade corrected their data for such a
variability-induced over-completeness. Note also that
the different assumptions for q0 (both Hartwick & Schade and
La Franca & Cristiani adopted q0=0.5 while we used q0=0)
make no significant difference for the number counts.
We cannot exclude that the relative overabundance of apparently
bright QSOs is due to the limitations of small-number
statistics, but note that a similar result was
found for the VPM survey in the M 92 field
(Meusinger & Brunzendorf 2001).
The low-resolution spectra of the objects from Table 3
are shown in Fig. 7. The spectra are dominated by the typical
AGN-emission lines:
Ly+N V
,
Si IV+O IV]
,
C IV
,
C III]
,
Mg II
,
[O III]
,
and the Balmer series.
A few objects (Nos. 10, 19, 64, 50, 11, 69, 7) apparently have relatively
weak lines. Unfortunately, many of these spectra were taken at
relatively bad atmospheric transparency, and poorly
removed telluric lines may effect the equivalent widths of
the QSO emission lines.
Therefore we do not quantitatively discuss the
distribution of the equivalent widths in this paper.
The analysis of the QSOs from the VPM survey in the M 92 field
(where most of the spectra were taken under
better weather conditions) has shown that the sample-averaged
line equivalent widths for the VPM QSOs are in good agreement
with those from other samples of radio-quiet QSOs
(Meusinger & Brunzendorf 2001).
Broad absorption troughs are indicated in the spectra of the
QSOs Nos. 3, 49, 37, 57, 7, 44, 75, 33, 65, and 70. For some other QSOs
absorption features may be hidden due to the low
signal-to-noise. The fraction of BAL QSOs is about 10%, in good
agreement with the
BAL percentage in the SDSS Early Data Release (Schneider et al.
2002). There is only one object with an unusual spectrum:
the BAL QSO No. 7 where the emission lines are almost completely
masked by extremely broad absortion lines. The best guess for the
emission redshift is
,
compared to
for the strongest absorption lines
(C IV
,
Al III
,
and the
Fe II-multiplet at
). This object is a high-priority
VPM QSO candidate with quite red colours (see below). There is no entry in
the NED at this position. Objects like No. 7 are not very
likely to be recognized by most other optical QSO surveys.
For a few other QSOs/Sey1s, the spectra in Fig. 7
have unusually red continua (Nos. 42, 64, 48, 3).
However, the U-B indices (Table 3) of these objects
closely follow the mean colour-redshift relation (Fig. 9)
and thus the missing blue light in the spectra is interpreted by
the slit-loss effect due to atmospheric dispersion (Sect. 1).
We conclude that, up to the limit of the survey, the fraction of QSOs
with unusual spectra is at maximum a few percent. This conclusion is
again in agreement with the statistics from the (still incomplete) SDSS
data (Hall et al. 2002).
In Paper I, a colour-colour diagram of the QSO candidates was presented showing a broad scatter of their colour indices and a large fraction of red QSO candidates. The distribution of the spectroscopically classified objects on the U-B versus B-V plane is shown in Fig. 8. The most important result is the fact that all candidates with extremely red colours proved to be foreground stars, in agreement with what we found from the VPM survey in the M 92 field. Obviously, the QSOs from Table 3 populate essentially the same area as the QSOs from the CFHT grens survey. For z<2.2 this area is well defined by the selection criteria of classical colour surveys. There are only 7 low-redshift (z<2.2) QSOs located beyond the demarcation line for colour selection discussed in Paper I. A typical fluctuation of about 0.35 mag per colour index is expected due to photometric errors and variability (as the time-lines for the three colour bands are not identical). In addition, a scatter may be produced by intrinsic differences in the continuum slope and/or the strength of emision lines and/or absorption troughs. Remarkably, the strongest deviation from the colour selection line is measured for the two absorption line QSOs Nos. 7 and 75.
The same conclusion is reached from the colour-redshift relations (Fig. 9). Apart from the scatter due to variability and photometric errors, the QSOs from our sample closely follow the mean relation of QSOs from the Véron-Cetty & Véron (2001) catalogue. Among the QSOs from Table 3, the strongest deviation is measured again for Nos. 7 and 75. The QSO No. 28, which is the faintest object in Table 3, shows a strong deviation in B-V. Fainter QSOs tend to have larger colour indices B-V (Fig. 9d).
Data from the 2 Micron All Sky Survey (2MASS; Skrutskie
et al. 1997), March 2000 data release are available
for 25% of the field. With an identification radius of 10 arcsec
we identified six QSOs from our whole sample with catalogued 2MASS sources.
For all six
objects the
colour index is smaller than 4, i.e.
smaller than for the red QSOs found by Webster et al. (1995)
among the flat-spectrum radio-loud QSOs.
For the M 92 field we have estimated that the fraction of
QSOs with unusually red B-V colour indices must be less than 3% up
to B=19.8 (Brunzendorf &
Meusinger 2002). From the data in the M 3 field we
estimate a similar fraction of about 2% up to B=19.7.
Although a survey in the B-band is obviously not an ideal
approach to derive strong conclusions about the underlying population of
possibly highly reddened QSOs, the unbiased VPM QSO sample
provides a constraint of its properties.
Let us assume for simplicity that there are
two QSO populations of comparable size: normal QSOs and reddened QSOs with an
intrinsic dust reddening equivalent to
EB-V = 0.5 - a not
unreasonable level in a dusty system - implying an extinction of about
2 mag in the B-band (assuming a galactic extinction curve). Using
the number-magnitude relation from Fig. 6, we would expect to
detect about 5-7 strongly reddened QSOs up to
in each
search field. This is clearly more than what we found,
indicating that the red QSOs are either redder on average or less frequent.
A more detailed
discussion of this question has to be deferred to a separate study.
Copyright ESO 2002