ISOPHOT Serendipity Survey (ISOSS) measurements were obtained with the
C200 detector (Lemke et al. 1996), a 22 pixel array of
stressed Ge:Ga with a pixel size of 89.4
.
A broadband filter (C_160) with a reference wavelength of
170
m and a width of 89
m was used. The highest
slewing speed of the satellite was 8
/s.
During each 1/8 s integration time 4 detector
readouts were taken, i.e. the maximum read out distance on the sky
was 15
yielding one brightness value per arcminute
(see Figs. 1 and 2).
During the ISO lifetime, about 550 hours of ISOSS
measurements have been gathered, resulting in a sky
coverage of approximately 15%.
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Figure 1:
IRAS 100 ![]() ![]() |
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Figure 2:
The calibrated pixel intensities as a function
of slew length. Intensities of Pixel 2-4 are shifted
downwards in steps of 20
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A standard data processing was applied using the ISOPHOT Interactive Analysis
PIA
(Gabriel et al. 1997) Version 7.2 software package.
The detailed processing steps are given in Stickel et al. (2000).
Special care had to be taken to correct gyro drifts between subsequent
guide star acquisitions of the star tracker.
For point sources, the deglitched and background-subtracted signals of
the 4 pixels were phase-shifted according to the position angle
of the detector and co-added. Source candidates were searched for in this
co-added stream by setting a cut of 3
of the local noise.
Then, the source position perpendicular to the slew
was determined from a comparison between signal ratios with a
Gaussian source model. The flux was afterwards derived from 2-D
Gaussian fitting with fixed offset position.
In the case of long slews, the surface brightnesses were derived from a measurement of the on-board Fine Calibration Source (FCS) preceding the slew observation. For short slews the default C200 calibration was used. To tie point-source fluxes derived from ISOSS to an absolute photometric level, dedicated photometric calibration measurements of 12 sources, repeatedly crossed with varying impact parameters were compared with raster maps on the same sources (Stickel et al. 1998a). The comparison between slew and mapping fluxes showed that for brighter sources the slewing observations miss some signals, probably due to transient effects in the detector output (Acosta-Pulido et al. 2000) in combination with detector non-linearities. For sources brighter than 30 Jy, Stickel et al. (2000) found signal losses of 50%, although the true losses were not well established due to a lack of reliable sources. For fainter sources (<10 Jy) the flux loss in the slews is only 10-20%.
The SSOs were encountered at different slew speeds,
which can be characterized
by "fast'': above 3/s;
"moderate'': 1.5
/s < speed < 3
/s;
"slow'': below 1.5
/s;
"stop'': at slewends, similar to a staring observation.
But aspects like the background level, the detector history
and impact parameters also play a crucial role in source
extraction and flux calibration methods.
Method 1 is based on an automatic point source extractor
(Stickel et al. 2000)
for all slewing speeds above 1.5/s and non-saturated
crossings. All source candidates were cross correlated with the
list of SSO candidates (see Fig. 3) and
the associations found were carefully examined. Flux loss corrections
(see Sect. 2.1) have to be applied.
This method has been used at slewends, if the source was inside the detector aperture:
Not all of the ISO scientific targets are to be found in the
end-of-slew data: firstly, the 4 ISO instruments view separate areas
of the sky.
Slew end position (ISOPHOT) and target position (other instrument)
can therefore differ by up to 20.
Secondly, many observing
modes, especially for ISOPHOT, started off-target for mapping purposes
or to avoid strong detector transients.
Copyright ESO 2002