A&A 441, 773-782 (2005)
K. Jockers1 - N. Kiselev2 - T. Bonev3 - V. Rosenbush4 - N. Shakhovskoy5 - S. Kolesnikov6 - Yu. Efimov5 - D. Shakhovskoy5 - K. Antonyuk5
1 - Max-Planck-Institut für Sonnensystemforschung, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany
2 - Institute of Astronomy, Karazin Kharkiv National University, Sumskaya Str. 35, 61022 Kharkiv, Ukraine
3 - Institute of Astronomy, 1784 Sofia 72, Tsarigradsko Shose Blvd., Bulgaria
4 - Main Astronomical Observatory, NAS of Ukraine, Zabolotnoho Str. 27, 03680 Kyiv, Ukraine
5 - Crimean Astrophysical Observatory, 98409 Nauchny, Crimea, Ukraine
6 - Astronomical Observatory of Odessa National University, T.G. Shevchenko Park, 65014 Odessa, Ukraine
Received 2 May 2005 / Accepted 9 June 2005
We present results of imaging and aperture polarimetry of the dust of comet 2P/Encke at phase angles 91-105, obtained during the 2003 apparition. We investigate how strongly molecular emissions transmitted by the filters used in the observations can affect the resulting polarization of cometary dust. This problem is of particular importance for so-called gas-rich comets like comet 2P/Encke which has particularly strong molecular emission as compared to its dust continuum. Aperture polarimetry in the wide-band UBVR filters was performed at the 2.6-m Shain telescope and 1.25-m telescope of the Crimean Astrophysical Observatory on November 17-24. From these measurements a dust polarization of 8% is derived, which puts the comet in the class of comets with low polarization. The imaging observations of comet 2P/Encke were carried out at the 2-m telescope of the Bulgarian National Astronomical Observatory on November 20-22, 2003. Narrow-band filters centered on the 0-7-0 transition of the Ã2A1 - X2B1electronic band system of NH2 (662 nm) and on an adjacent red continuum at 642 nm were employed. The polarization of NH2 averaged over the 0-7-0 vibronic transition amounts to 7% at phase angles close 90, similar to the polarization of the two-atomic molecules CN and C2. The dust polarization however, when corrected for the effect of molecular emissions, is larger than 30%. We conclude that the division of comets into two polarimetric classes with one class having in the visual wavelength range a maximum polarization less than 20% is caused by ignoring the contribution of molecular emission and therefore is an artifact. Whether the comet displays a strong silicate feature (i.e. its dust grains are small) or not, the dust polarization is high.
Key words: comets: individual: 2P/Encke - comets: general - polarization - methods: observational
One of the main goals of cometary polarimetry is to determine the physical properties of cometary dust in order to learn more about its origin and formation and about the origin and formation of the comets themselves. In principle, polarimetry could be a very sensitive tool to probe the nature of cometary dust. The problem of light scattering by arbitrary dust particles, however, is still unsolved and any interpretation of polarimetric data of comets based on physical principles is uncertain as yet. Therefore, attempts have been made to find different taxonomic classes of comets by looking at their observed degree of polarization and its phase dependence. If such classes exist, one possibly could determine the ensemble properties of comets in a polarimetric class and in this way learn about the effect of these properties on polarization.
The photometric properties of comets from 0.7 to 23 m have been studied by Gehrz & Ney (1992). These authors have grouped the investigated comets into two types, type I with a color temperature close to the blackbody and an undetectable silicate feature and type II with superheated thermal infrared continuum and high-contrast silicate feature. According to early models developed by Hanner (2003,1980), both elevated color temperature and appearance of the silicate feature are associated with dust particle size. Therefore the two types of comets introduced by Gehrz & Ney (1992) are mainly distinguished by their particle size (type I: large particles, and type II: small particles) but other particle properties like porosity may also be of importance. This division of comets into two classes according to their dust particle size based on infrared observations is generally accepted at present.
Table 1: Two types of comets as defined by Gehrz & Ney (1992) in the view of later papers.
In their extensive study of polarimetric properties of comets Chernova et al. (1993) noted the tendency of gas-rich comets to have lower polarization. In their paper the degree of dustiness was defined as the so-called equivalent width W4845 introduced by Krishna Swamy (1986) and given by the ratio of light flux observed in the 5140 Å (C2) and 4845 Å filters of the International Halley Watch (IHW). This ratio is based on quantities derived from observations in the visual wavelength range where large cometary grains scatter inefficiently. Therefore it is not impossible that the comets called gas-rich by Chernova et al. (1993) in fact have the same or an even larger dust/gas mass production ratio than comets these authors called dust-rich, i.e. the denomination "gas-rich'' may be misleading. Nevertheless we will use it in this paper. Only sometimes will we use the longer, but more accurate expression "so-called gas-rich comets''. Chernova et al. (1993) attributed the lower polarization observed in gas-rich comets mainly to the influence of molecular emission of low polarization transmitted by the continuum filters of IHW but did not exclude the possibility that part of the difference may be real. Chernova et al. (1993) did not quote Gehrz & Ney (1992), but noted the association of their gas-rich comets with comets of low infrared color temperature and the absence of a silicate peak.
Later Levasseur-Regourd et al. (1996) grouped comets into two classes according to the maximum of their polarization phase curve. Like Chernova et al. (1993) they noted that comets of the class of high polarization display a strong silicate feature while in the group of low polarization comets the silicate feature is small or absent. Very recently a similar grouping into two polarimetric classes has been suggested from polarimetry of seven comets in the near-infrared wavelength range at 2.2 m (Kelley et al. 2004).
Summing up (see Table 1) we may associate type I comets as defined by Gehrz & Ney (1992) (comets having large dust grains) with the gas-rich comets as defined by Chernova et al. (1993) and with the low polarization class of Levasseur-Regourd et al. (1996). But the question posed already by Chernova et al. remains: is the low polarization observed in so-called gas-rich comets real or is it caused by low-polarized molecular emission transmitted by the filters used to measure the dust polarization?
In this paper we present observations of comet 2P/Encke obtained during its last apparition in November 2003. Comet 2P/Encke has a weak silicate feature (Gehrz et al. 1989), large dust particles (Reach et al. 2000), and is gas-rich according to the definition of Chernova et al. (1993). This would put the comet in the low polarization class. Nevertheless, as we will see, the polarization of its dust at phase angles close to 90, after correction for the presence of molecular emission, exceeds 30%. Apart from comet 2P/Encke there are other gas-rich comets (see Table 4 below) with high dust polarization. Therefore we will argue in our paper that the division of comets in two groups with one group having a maximum polarization in the visual wavelength range significantly less than 20% may no longer be tenable in the form proposed by Levasseur-Regourd et al. (1996) because of gas polarization contamination.
Table 2: Parameters of the observations.
Imaging polarimetry of comet 2P/Encke was carried out at the 2-m Ritchey-Crétien-Coudé (RCC) telescope of the Bulgarian National Astronomical Observatory (Rozhen) on November 20-22, 2003 (observers K. Jockers, T. Bonev, and G. Borisov). Aperture polarimetry of the comet was obtained with the 2.6-m Shain telescope (observers N. Kiselev, N. Shakhovskoy, and S. Kolesnikov) and 1.25-m telescope (observers Yu. Efimov, V. Rosenbush, and K. Antonyuk) of the Crimean Astrophysical Observatory on November 17-24, 2003. Weather conditions were good at both observatories. Nevertheless, the observing conditions were difficult as the comet moved rapidly at low galactic latitude in front of many field stars. In spite of the rather high total brightness (7 mag) of comet 2P/Encke, its continuum was extremely weak. At the 2-m and 1.25-m telescopes a moving guide probe was used to track the comet. Table 2 gives the heliocentric and geocentric distance, phase angle (Sun-Comet-Earth angle) and the position angle of the antisolar direction (scattering plane) and filters and pixel scale or diaphragm diameter at the time of the observations.
Standard stars with small (Serkowsky 1974; Heiles 2000) and with large polarization (Hsu & Breger 1982) were observed to determine the parameters of instrumental polarization and the zero-point of the position angle of the polarization plane for each telescope.
At Rozhen Observatory the two-channel focal reducer (2CFR) of the Max-Planck-Institut für Sonnensystemforschung (Jockers 1997a; Jockers et al. 2000) was employed. At the 2m f/8 telescope it provides a pixel size in the sky of 0 88. The imaging polarimeter of 2CFR has a useful field of . It employs a split Wollaston prism located at the image of the telescope mirror (exit pupil) in the reducing optics of the focal reducer. One half of the Wollaston prism generates polarization images at position angles 0 and 90, and the other half at +45and -45 (see Geyer et al. 1996; Jockers et al. 2000). In this way four polarization images are generated simultaneously on the CCD detector. Under the prevailing conditions of a high density of background stars the simultaneity of the four polarization subimages was a great advantage as either all or none of the subimages was affected by a star trail. In order to further minimize the disturbing effect of the star trails, exposure times were kept short (5 min on Nov. 21 and 10 min on Nov. 20 and 22).
The narrow-band filters 662 (NH2, nm, FWHM = 5.9 nm), 642 (red continuum, nm, FWHM = 2.6 nm) and the wide-band filter RX ( nm, FWHM = 79.0 nm) were used. Analysis of spectra of comet 23P/1989 N1 (Brorsen-Metcalf) and 109P/1992 S2 (Swift-Tuttle) (Brown et al. 1996) and of the gas-rich comet D/1996 Q1 (Tabur) (Kiselev et al. 2001) indicate that a number of unidentified and NH2 lines of the 0-8-0 transition of the Ã2A1 - X2B1 band system fall within the pass-band of the 642 filter. Therefore, alternating with the 642 filter, polarization images were taken with the filter 662, which is centered on the 0-7-0 transition of the Ã2A1 - X2B1 band system of NH2.
We mention in passing that the labelling of the vibronic transitions of
the Ã2A1 - X2B1 band system of NH2, which are bent
in the X ground state but linear in the Ã state, depends on
which of the two states is used for the labelling. In this paper we follow
the more traditional labelling related to the Ã state. According to
Jensen et al. (2003) the labelling of the bent X state with respect to the
labelling of the linear Ã state is connected by the equation
The CCD images were processed using a program package written by K.J. in
the IDL language. The image processing included bias substraction, flat
field correction and removal of cosmic ray events. Point sources are
selected interactively in the polarization subimages and their
polarization is determined. From the standard star images the following
mean parameters of instrumental polarization on Nov. 20-22 were derived:
After correction for instrumental polarization,
the degree of polarization of the standard star differs
from the catalogue value by
% in the filters 642
and 662, respectively. The correction of position angle
the plane of polarization is equal to
in all filters. To derive polarization maps
of the comet the polarization subimages must
be aligned. Because of the low signal/noise ratio of the
individual exposures of comet Encke with 5 or 10 min duration, before determination
of the polarization all useful exposures (without
star trails in the immediate neighborhood of the comet)
were aligned to a reference image (the best exposure of the night). After alignment
the optical centers in the polarization subimages still sometimes differ by almost
1 pixel. This acts as an additional image smearing similar to seeing effects but
affects polarization only to a minor extent as the four windows are affected
in a similar way. From the aligned and added subimages,
intensity and polarization images
in the instrumental system were calculated.
Areas where the total intensity had less than 30 counts
were marked as areas not containing valid information and set to zero.
In the last step the valid parts of
were corrected for instrumental polarization, and the degree of linear polarization
and the position angle of the
The errors of polarization degree
were determined from the photon statistics of the counts (total intensity)
of comet and background contained in the sum of useful images. The following
equations were used (Geyer et al. 1996; Shakhovskoy & Efimov 1972):
|Figure 1: Data reduction steps, intensity. Left column: images. Right column: plots of average of three central rows through comet (along fan). Rows: a) Raw image in filter 662. b) Raw image in filter 642. c) NH2. d) Dust derived from filter 662. e) Dust derived from filter 642. East is to the left, north is up.|
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|Figure 2: Data reduction steps, polarization. Like Fig. 1, but instead of intensity the degree of polarization is shown. If the intensity (denominator) has fewer than 30 counts polarization data are considered invalid and the corresponding pixel is left blank.|
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As already mentioned, filter 642, designed to transmit only cometary continuum, transmits also part of the 0-8-0 transition of the Ã2A1 - X2B1 band system of NH2 and weaker unidentified emission features. In order to be able to correct for this emission and to determine the true polarization of the cometary continuum, comet 2P/Encke was also observed with the filter 662 which transmits the NH2 0-7-0 emission of the same NH2 band. In the following we must assume that the (faint) emissions transmitted by the 642 filter have the same spatial distribution as NH2. The reduction steps are illustrated in Figs. 1 and 2 for Nov. 21 where we have the best data. Figure 1 shows intensity and Fig. 2 polarization. In the left panels we give two-dimensional maps and in the right panels averages over the three rows closest to the nucleus. These cuts refer to the East-West direction and extend into comet Encke's fan.
In order to determine the spatial distribution and polarization of NH2and dust from the polarization images obtained through the two filters we use the following equations:
In rows a and b of Figs. 1 and 2 the uncorrected "observed'' data in filters 662 and 642 are displayed. The image of filter 642 (continuum) is more peaked. This indicates that the dust in comet 2P/Encke probably is more concentrated to the nucleus while the NH2gas extends into the fan. This idea is confirmed when we consider the polarization observed in filter 662 (Fig. 2, row a). Within error limits the polarization becomes constant ( %) at distances into the fan larger than 1500 km. The fact of constant polarization indicates that at larger distances into the fan only NH2 gas contributes to the observed intensity. We conclude that the polarization in the 0-7-0 vibronic band averaged over the individual lines transmitted by the 662 filter equals %.
The wavelengths of 662 nm and 642 nm are close together. Therefore we can neglect
possible reddening of the cometary dust. Then the continuum contribution in both filters
is proportional to their transmission
integral multiplied by the solar intensity in both wavelengths.
This leads to the relation
Knowing from the uncorrected polarization data of filter 662 that comet Encke's pure dust
coma must be less extended into the fan than the gas coma and having the pure gas image
at our disposal we can now derive a pure dust image from equation
The dust part of the image observed in filter 662 can be calculated by multiplying by the factor 3.27 (4) and the gas part again from Eq. (3), this time for nm.
Now we can correct the observed polarization and find the true dust polarization
from the equations
For filter 662 we have determined the gas polarization and the solution of Eq. (7) is straightforward. For filter 642 (see Fig. 2, row b) the gas polarization (i.e. polarization at large distances into the fan) seems to be higher but the error bar is very large. Therefore we have assumed that the gas polarization in filter 642 is the same as in filter 662. But this assumption in principle cannot be justified as in this wavelength range the polarization of the individual NH2 lines should vary strongly from line to line. Like in OH (Le Borgne & Crovisier 1987), also in NH2 only the rotational lines with low quantum numbers are excited. Moreover Q transitions are possible which may be differently polarized (Truhins et al. 1997). In addition in the 642 filter there are unidentified lines where we have no idea of the polarization. Therefore we conclude that the degree of dust polarization derived from filter 662 (Fig. 2, row d) is more reliable and the value in row e is likely to be too high. On the other hand, the spatial distribution of polarization is better derived from filter 642 (row e) because the gas contribution in this filter is reduced.
At last, as a consistency check, using the corrected dust polarization map we can derive a map of the polarization of NH2 . This map is shown in the central row of Fig. 2. Of course, within error limits this map shows % in accordance with the polarization map at large distances from the nucleus in the fan.
The polarimetric observations at the 2.6-m Shain telescope were carried out with the one channel polarimeter (Shakhovskoy et al. 2001) operating in linear polarization measurement mode. For this, the fast rotating (33 Hz) half-wave plate (retarder) was placed in front of the fixed polaroid. Measurements of intensities were obtained for the position angles of the retarder in the order 0, 22.5, 45, ..., 157.5 with a total integration time of 4 s (133 rotations). One full exposure of the comet consisted of 64 integrations of 4 s each, i.e. 256 s. Between exposures the sky background was measured. We used the R wide-band filter and a circular diaphragm of 15 diameter. In absence of an offset guide probe the central condensation of the comet was centered by eye in the diaphragm. During one exposure the comet moved about 4 with regard to the centre of diaphragm. Thus, the real diaphragm projected at the comet was equal of about with the long dimension in the direction of the proper motion of the comet in the sky.
Table 3: The mean observed and corrected degree of polarization in comet 2P/Encke.
The five-color photopolarimeter, developed at the Observatory of the University of Helsinki (Piirola 1988,1973), is standard equipment for polarization measurement at the 1.25-m telescope. The instrument was operated in linear polarization mode. In this instrument a rotating half-wave plate (retarder) with 22.5 step in front of a fixed calcite plate (polarizer) allows to measure the two orthogonally polarized intensities simultaneously. An important advantage of this instrument for the observation of faint point sources is that the sky polarization, caused e.g. by moonlight, is eliminated and only the intensity of the sky background must be taken into account. Nevertheless, the polarimeter is not suited for measurements of extended objects like comets because of superposition of the ordinary and extraordinary images. To avoid this we had to put an additional polaroid behind the calcite plate so as to extinguish one of two orthogonally polarized intensities. A single measurement consists of eight integrations in the different orientations of the retarder. Typically the integration time was 10 s. The full set of cometary measurements usually consisted of several cycles, each of 7-10 single measurements. The sky background radiation was measured before and after each cycle of cometary measurements. The photometric system is realized with four dichroic filters, which separate the light into five spectral regions, i.e. the instrument provides simultaneous measurements of polarization in the UBVRI bands (360, 440, 530, 690, and 830 nm respectively). The passbands are close to the standard UBV (Johnson) and RI (Cousins) systems. Unfortunately, because of low signal/noise ratio no reliable polarimetric data could be obtained in the R and I bands.
Before starting an exposure with either one of the aperture polarimeters the sky was visually checked for the appearance of brighter stars in the diaphragm and, if necessary, the telescope was moved away from the comet to measure the background polarization. Scans with elevated total intensity (indicating the presence of a field star in the diaphragm) were removed during data reduction.
For the five-color polarimeter the maximum of instrumental polarization was %, % and % in the UBV filters, respectively, while the instrumental polarization for aperture observations at the 2.6-m telescope did not exeed %. The main contribution to the errors in polarization degree of 2P/Encke comes from the limited signal to noise ratio for the continuum of the comet. The degree of polarization P and the position angle were calculated as in the case of the imaging polarimetry. The errors of the Stokes parameters q and u were determined from both the statistics of recorded photons (as with imaging polarimetry) and from the scatter of individual measurements (Shakhovskoy & Efimov 1972). The larger of these two errors was adopted as the accuracy measure.
Table 3 provides the degree of polarization derived from the imaging polarization measurements. The values are averaged over pixel centered on the nucleus (i.e. the pixel with maximum count rate in the intensity image). We provide the observed values in the interference filters 642, 662 and in the wide-band filter RX and the values corrected for the presence of molecular emission in the filter passband. These values are labeled "dust only''. As explained above, a correction for molecular emission is only possible if observations in both filters 642 and 662 are available. The degree of polarization measured in the red wide-band filter cannot be corrected.
For all observations the plane of polarization of the comet was perpendicular to the plane of scattering within observation errors. Therefore, in Table 3 and the following tables we do not provide the position angle of the plane of polarization. One can see that the polarization of the dust of gas-rich comet 2P/Encke at phase angles exceeds 30% i.e. the dust of the comet has a polarization higher than the average polarization of so-called dust-rich comets (see Fig. 3 below).
Table 4: Aperture polarization results for comet 2P/Encke.
The results of photoelectric measurements of polarization through wide-band filters and large diaphragms are given in Table 4. The low observed integrated polarization of 8% in the wide-band U, B, V, and R filters is caused by the emission of the radicals CN, C3, C2, and NH2 which according to Osip et al. (1992) and Fink & Hicks (1996) are the predominant molecular components in the spectrum of comet 2P/Encke. The polarization of molecules CN and C2 and C3 and its phase angle dependence is well studied theoretically (Le Borgne & Crovisier 1987, and references therein). The phase dependence of polarization is described by the expression:
|Figure 3: Degree of polarization of comet 2P/Encke in the red spectral range obtained in different diaphragms as compared to two-atomic molecules (Eq. (8), dotted line) and typical dusty comets (red spectral range, Eq. (9), dashed line). Open symbols, , and +: measurements. Filled symbols: values corrected for the influence of gas emissions in the filter passband. All symbols refer to imaging polarimetry of this paper, with two exceptions: +: aperture measurements at the 2.6-m telescope, this paper. : imaging polarimetry (Kiselev et al. 2004).|
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Figure 3 shows the polarization of comet 2P/Encke derived from imaging
polarimetry for several square apertures and from photoelectric
observations. Data from the previous paper (Kiselev et al. 2004) for an area
of 2000 km2 are also included. The full line presents the phase angle dependence of polarization
for resonance fluorescence according to Eq. (8). The dashed line is the "standard'' phase curve
of polarization of dusty comets (Kiselev 2003; see also
in the red continuum filter (684.0/9.0 nm), calculated from the fit
It is very likely that the low polarization measured in other gas-rich comets also is an artifact caused by molecular emissions transmitted by the filters used for the cometary observations. The improved sensitivity of astronomical spectrographs caused by the advent of the sensitive CCD-detectors has considerably increased the number of known emission lines in cometary spectra (Brown et al. 1996; Arpigny 1995). Many of them are still unidentified. As we know now, it is virtually impossible to find spectral continuum windows entirely free of cometary molecular emissions. As was recently shown by Kiselev et al. (2001), even the special narrowband continuum filters transmit a significant number of faint molecular emission lines. When the intrinsic continuum caused by the light scattering of cometary dust is weak, the contribution of these lines can significantly reduce the observed polarization even if the intrinsic polarization of the light scattered by the dust particles is high. Attempts of some investigators (Eaton et al. 1992; Levasseur-Regourd et al. 1996) to carry out polarimetric measurements with broad-band filters in the red spectral region did not improve the situation because faint molecular lines are present also in this part of the cometary spectrum. Here the most important molecules are NH2 and H2O+.
The second difficulty of measurements of the intrinsic dust polarization is related to the low spatial resolution of most aperture observations of comets. The small dust grains contributing most to the visible light scattered by cometary dust are released from the nucleus. Even if they are altered by fractionation or loss of volatiles their distribution peaks sharply at the cometary nucleus. Cometary neutrals observable in the visual wavelength range, however, are daughter molecules. Close to the nucleus they have a shallower distribution than cometary dust grains. Therefore it is expected that in gas-rich comets, because the gas/dust ratio increases with distance from the nucleus, if the filters transmit molecular emissions, the observed polarization will decrease with distance from the nucleus and, in case of aperture measurements, with increasing aperture of the polarimeter. A good example is provided by the observations of gas-rich Comet D/1996 Q1 (Tabur) (Jockers 1997b; Kiselev et al. 2001). Instead of a gas coma surrounding the nucleus from all sides comet 2P/Encke has a gas jet pointing toward West. Nevertheless our observations clearly demonstrate that the observed polarization is reduced when observed with a larger diaphragm.
Table 5: Polarization and infrared emission data for gas-rich comets observed at large phase angles.
The polarization data available in the literature for gas-rich comets in the red spectral region are collected in Table 5 together with the corresponding infrared data. In this table from left to right the columns indicate the name of the comet, the phase angle of the observation and the corresponding degree of polarization , the diameter of diaphragm or size of box projected on the comet, and the typical degree of polarization observed in dust-rich comets. This column was calculated from the trigonometric fit for dust-rich comets (Eq. (9)). Comets with large difference between observed polarization and polarization calculated from Eq. (9) are attributed to the class of low polarization. At first sight it seems indeed that gas-rich comets belong to the class of low-polarization comets as postulated by Levasseur-Regourd et al. (1996). But there are exceptions besides comet 2P/Encke. Comet C/1983 H1 (Iras-Araki-Alcock) approached the Earth very closely. Because of this even a polarimeter with a medium-size diaphragm would pick up only the innermost part of the coma. A high polarization was observed despite the fact that this comet showed almost no dust continuum or silicate feature. Other gas-rich comets, C/1982 M1 (Austin), C/1989 Q1 (Okasaki-Levy-Rudenko) and D/1996 Q1 (Tabur), when observed through small diaphragms, showed high polarization. We are forced to dismiss the temptingly simple idea that the dust of gas-rich comets has low intrinsic polarization, and must face the fact that the large grains, constituting the majority of dust present in gas-rich comets, have a polarization as high as the grains in dust-rich comets or possibly even higher.
If we accept the idea discussed earlier that so-called gas-rich comets have predominantly large dust grains, how can it be possible that large cometary dust grains have high polarization? There is further observational evidence that large dust grains can be highly polarized. When comet D/1999 S4 (LINEAR) disintegrated it left behind a highly reddened cloud of dust (Bonev et al. 2002), which could be observed for several days. When this cloud was visible, the phase angle decreased from a maximum of to . There cannot be any doubt that the cloud consisted of large particles, as small particles are quickly removed by solar radiation pressure. From aperture polarimetry (Kiselev et al. 2002) a polarization of 30% was observed at a phase angle of 104. Imaging polarimetry (Hadamcik & Levasseur-Regourd 2003) indicates even higher polarization values. At a phase angle of 109 (slightly earlier than the measurement by Kiselev et al.) a maximum polarization of 40% was observed on the sunward side of the remainig dust cloud.
The polarization properties of cometary dust particles are still not well understood from the theoretical side. The most successful models describe cometary dust as aggregates of constituent particles of submicron size (Petrova et al. 2000; Xing & Hanner 1997; Mann et al. 2004; West 1991; Petrova et al. 2004; Tishkovets et al. 2004; Kimura 2001). With the exception of Xing & Hanner (1997) all quoted papers have used spheres as constituent particles. Unfortunately, aggregate particles with sizes large compared to the wavelength, which could model realistic cometary dust grains, cannot be calculated with presently available algorithms and computers. At phase angles around 90 existing aggregate models of cometary dust grains predict a polarization of 50% or higher for grains comparable to or slightly larger than the wavelength. For aggregates of larger size the polarization may decrease. The polarization is also likely to decrease for all aggregates irrespective of their size, if the constituent particles are nonspherical and have a wide size distribution. So we conclude that at present models of cometary dust grains do not contradict the idea of the existence of large cometary dust grains with a degree of polarization between 30-40%. The reason for this may be that, besides the dependence on refractive index, polarization is sensitive to surface structure and compactness of the dust grains on scales comparable to the wavelength but to a much lesser extent to particle size. In this respect the observations of Kelley et al. (2004), seemingly confirming the existence of two polarimetric classes in the near infrared spectral region, are of great importance. It seems, however, premature to include them into the discussion of this paper. More work is needed on cometary spectroscopy and polarimetry of molecules and dust in the K band.
During its apparition in November 2003 polarimetric observations of comet 2P/Encke were carried out at the Bulgarian National Observatory (Institute of Astronomy, Bulgarian Academy of Sciences) and the Crimean Astrophysical Observatory, Ukraine (CrAO). Imaging polarimetry was obtained in Bulgaria and aperture measurements were performed at CrAO. The aim of the study was to verify the existence of two polarimetric classes of comets, i.e. a class of gas-rich, low-polarization comets versus a class of dust-rich high-polarization comets. Comet 2P/Encke was an appropriate target, as it is a well studied gas-rich comet and its dust grains are known to be large. For the imaging observations we used two adjacent filters. The filter 642 (center wavelength in nanometers) transmits a so-called continuum window, and the filter 662 is centered on one of the main emissions of the NH2 radical found at 662 nm. As was shown, the polarimetric and photometric data in the two filters allow us to unambiguously separate gas and dust in comet 2P/Encke. The data reduction steps are illustrated in Figs. 1 (photometry) and 2 (polarimetry). The aperture polarimetry was performed in the classical way through wide-band filters. The following results were obtained.
We are grateful for generous allocation of observing time at the 2-m telescope of the National Observatory of the Bulgarian Academy of Sciences and at the 2.6-m and 1.25-m telescopes of the Crimean Astrophysical Observatory. N.K. and T.B. have been supported by fellowship grants of the Max Planck Society. K.J. acknowledges a useful discussion with Prof. Per Jensen, University of Wuppertal, Germany, about the vibronic states of the NH2molecule.