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Formation of polycyclic aromatic hydrocarbon grains using anthracene and their stability under UV irradiation

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Earth, Planets and Space201562:620010081

  • Received: 28 July 2008
  • Accepted: 5 December 2008
  • Published:


It has been known for some time that the properties of a material are changed in nanometer size. Since it is nontrivial that polycyclic aromatic hydrocarbon (PAH) grains at the nanometer scale show similar properties with that of macroscopic scale, PAH grains were synthesized by a gas evaporation method and were analyzed using a transmission electron microscope and their UV-Vis and mid-IR spectra were measured. Results from these experiments showed that condensed anthracene grains from the gas phase had a planar form and showed similar infrared peaks compared to anthracene molecules, but with somewhat wider bands and different relative intensities. Some new features were also observed. The anthracene molecules formed photodimer in their grain and showed different infrared features after UV irradiation. This would be the first report concerning nanometersized PAH grains.

Key words

  • PAH
  • infrared
  • dust
  • laboratory experiment

1. Introduction

After the discovery of unidentified infrared (UIR) bands (Gillett et al., 1973; Russell et al., 1977a; Willner et al., 1977), which are characterized by the main features at 3.3, 6.2, 7.7, 8.6 and 11.2 μms, many minor bands and the underlying broad plateaus, many candidate materials of the origin have been proposed, such as hydrogenated amorphous carbon (Duley and Williams, 1981), quenched carbonaceous composite (Sakata et al., 1984) and polycyclic aromatic hydrocarbons (PAHs) (Léger and Puget, 1984; Allamandola et al., 1985). Since the UIR bands are observed in a wide variety of objects in various stages of stellar evolution, such as Herbig Ae/Be stars, HII regions, reflection nebulae, diffuse interstellar medium, post-asymptotic giant branch (AGB) stars and planetary nebulae (e.g. Russell et al., 1977b; Roche and Aitken, 1985; Cohen et al., 1986; Onaka et al., 1996), it appears that the carriers of the UIR bands should be stable materials. Furthermore, it is expected that the carriers are ubiquitous in space. Currently, PAHs are widely being used to examine the characteristics of UIR bands and are believed to be one of the most plausible origins of these bands.

PAHs consist of carbon atoms arranged in benzene rings terminated by hydrogen atoms. They have C-C and C-H bonds that exhibit vibrational modes in the mid-IR region. Since it has been reported that the UIR bands observed in various objects show systematically different spectral features (Peeters et al., 2002; van Diedenhoven et al., 2004), the physical environments and chemical evolution in those kinds of objects can be derived from the details of band positions, relative intensities and widths of UIR bands through a series studies on PAHs. Recently, it was implied that part of the possible life cycle of PAHs depends on their distance from the central star, i.e., the ionized gas phase PAHs are dominant in the nearest region of the central star, then PAHs become neutral, and finally very small PAH grains, such as clusters of PAH molecules, become dominant at the distant region from the central star (Rapacioli et al., 2005). This also suggests a possible evolutional scenario of PAHs such that free-flying PAHs are formed from these PAH grains by photo-evaporation in photo-dissociation regions (Rapacioli et al., 2005, 2006).

In addition to these theoretical and observational studies, therefore, experiments on the laboratory synthesis of PAHs and their grains are necessary to understand the formation and subsequent growth into PAH grains and their alteration upon UV irradiation in various objects. Several laboratory IR spectra have been reported, for example, commercial PAHs embedded in KBr pellets (Bernas et al., 1966; Flickinger and Wdowiak, 1990), carbonaceous soot formed by burning benzene (Jäger et al., 2006), PAHs distributed in an inert matrix at low temperature (Szczepanski et al., 1992; Moutou et al., 1996; Hudgins and Sandford, 1998), gas phase (Flickinger et al., 1991; Colangeli et al., 1992; Joblin et al., 1995) and IR spectra of cationic PAHs (Hudgins et al., 1994; Hudgins and Allamandola, 1995; Oomens et al., 2003). However, the IR spectra of nanometer sized PAH grains have never been observed so far. It has been shown that nanometer-sized particles show significant phenomena, which cannot be expected based on the characteristics of the bulk material. For example, the melting point of gold decreases from 1336 to 1220 to 950 K as particle size decreases from macroscopic scale to 5 to 2–3 nm (Koga et al., 2004). In addition, the diffusion coefficient of copper atoms in gold nanoparticles changes to 8.3×10-19 from 2.4×10-28 (m2 s-1) in the bulk material at 300 K (Mori et al., 1991). As a result, the time scale for forming nanoparticle alloys becomes markedly faster than that for the bulk material, i.e., from a couple of years to several seconds. Sometimes, even the stable crystal structures change for nanoparticles (Kimoto and Nishida, 1967). Actually, it has been reported that the crystal structure of pentacene is changed in thin film (Kakudate et al., 2007). Since it is nontrivial that PAH grains at the nanometer scale show similar properties with that of the macroscopic scale, we attempted to form nanometer sized PAHs grains and measured their IR spectra. Indeed, the importance of laboratory studies concerning optical spectra of nanometer sized solid particles has been suggested based on theoretical expectation. For example, the imaginary part in dielectric function becomes larger for small metallic grain compared with that of bulk. However, it is unclear how the optical properties of nanometer sized solid particles are different compared with that of bulk (Li, 2004). In this study, we performed the formation and growth of PAH grains at the nanometer scale, which are part of the life cycle of PAHs, and also performed alteration by UV irradiation, using mainly anthracene in the laboratory. This is the first report on IR spectra for nanometersized PAH grains.

2. Experimental Procedures

Anthracene has a molecular structure of three benzene rings in a straight alignment. It has two solo C-H bonds and two quartet C-H bonds, as shown in Fig. 1. The C-H out-of-plane deformation mode exhibits bands in the 11– 15 μm region depending on the number of directly adjacent H atoms, because of the coupling between the vibrating H atoms bonded to the neighboring C atoms on the ring. Anthracene grains were produced by the gas evaporation method, which is also known as the smoke experiment and has been used to produce nanometer-sized metal, oxide or semiconductor particles (Kimoto et al., 1963; Kaito, 1978). The work chamber used was a glass cylinder 17 cm in inner diameter and 33 cm in height covered with a stainlesssteal plate with electrodes on its top and connected to a high-vacuum exhaust through a valve at its bottom. An evaporation source was set 3 cm above the heater in the chamber and a glass plate was set as a collector 5 cm above the evaporation source, as shown in Fig. 2. Commercial anthracene powder (Nacalai Tesque, Inc. 99%) was charged on the upper molybdenum boat with a chromelalumel thermocouple. The chamber was evacuated down to 2.6×10-4 Pa (2×10-6 Torr) using a combination of a mechanical and a diffusion pump. After the valve was closed, He gas (99.99995% up in purity) was introduced into the chamber up to 4.0×103 Pa (30 Torr), 1.1×104 Pa (80 Torr) or 2.0×104 Pa (150 Torr). Then, the lower molybdenum boat was resistively heated. As a result, the upper boat was heated at the rate of 10 K/s by He gas convection and the temperature was controlled at 170°C. The vapor pressure of anthracene at 170°C is approximately 6.7×102 Pa (5 Torr). The evaporated anthracene molecules were homogeneously nucleated as the gas cooled and their grains were formed in the smoke. The evaporated vapor subsequently cooled and became condensed in the gas atmosphere.
Fig. 1.
Fig. 1.

Rough schematic models of (a) anthracene and (b) dianthracene molecules. The C-H out-of-plane deformation mode exhibits bands in the 11–15 μm region depending on the number of directly adjacent H atoms with individual aromatic ring. Anthracene molecule has two solo C-H bonds and two quartet C-H bonds, which exhibit 11.31 and 13.77 μm bands, respectively. Dianthracene is a photodimer of anthracene.

Fig. 2.
Fig. 2.

Schematic image of apparatus used to produce PAH grains. Commercial PAH is evaporated from upper Mo boat by heating the lower Mo boat. PAH grains are produced from the gas phase as gas cools. TEM grids were set at the same position as the glass plate.

Coalescence growth is regarded as an important process in this method. Coalescence of the smoke particles has been explained as having two stages: a surface melting coalescence stage and a liquid-like coalescence stage (Kaito, 1978). These two stages depend mainly on grain size and temperature. The morphology and grain size are controlled by the mass density and temperature of the smoke, which depend on the atmospheric gas and gas pressure. The size of the particles also depends on their surface melting point. For example, metallic particles, such as iron or nickel with a diameter of 10–20 nm, can be produced by controlling the atmospheric gas pressure in the gas evaporation method. Since it has been suggested that the PAHs are formed in the outflows of carbon-rich AGB stars (Jura, 1987), the gas evaporation method roughly corresponds to the formation process of circumstellar PAH grains in the gas outflow from an evolved star. The produced grains are collected on a glass plate for the measurements of their IR spectra and on a standard Cu transmission electron microscope (TEM) grid supported with an amorphous carbon thin film for the observation of the size and the structure of the anthracene grains.

The mid-IR spectra, in the range from 2.5 to 25 μm, of the produced PAH grains embedded in a KBr pellet were measured with a Horiba FTIR-210 spectrometer. The wavelength resolution was 2 cm-1. The beam splitter was a Geevaporated KBr substrate, and the detector was deuteriated triglycine sulphate (DTGS). The UV-Vis spectra were measured with a Hitachi U-3300 spectrophotometer. The wavelength resolution was 0.5 nm. The produced PAH grains were also observed using a Hitachi H-7100R TEM operated at an acceleration voltage of 100 kV.

3. Synthesized PAH Grains

A typical TEM image of anthracene grains produced in He gas of 1.1×104 Pa is shown in Fig. 3(a). The size of the anthracene grains was widely distributed from 5 nm to 5 μm. The electron diffraction (ED) pattern shows Bragg reflection spots attributed to anthracene crystal, i.e., anthracene molecules never broke during evaporation. The crystal structure of anthracene is monoclinic with the axes of a = 0.9463, b = 0.6026 and c = 0.8550 nm and angles of α = γ = 90° and β = 103.57° (Mason, 1964). The ED pattern from the anthracene crystal was immediately reduced under electron beam irradiation of 10-3-10-2 A/cm2 (which is 10 times weaker than the typical intensity used in common observation) with acceleration voltage at 100 kV, and ultimately disappeared within about 60 seconds, i.e., the crystal structure of anthracene was easily broken. Although the crystal structure of anthracene grains is very sensitive to electron beam irradiation, the external geometry was retained after electron beam irradiation. During the TEM observation, the sublimation of anthracene grains was not observed.
Fig. 3.
Fig. 3.

Typical TEM images and corresponding ED patterns of anthracene grains produced in 1.1×104 Pa He gas. (a) The upper boat was heated at the rate of 10 K/s by He gas convection and the temperature was controlled at 170°C. The mean diameter of anthracene grains was 49.6 nm, which corresponds to the carbon number of 1.9×106 if the grains are hemispherical. (b) Temperature of the evaporation source was raised at a slower rate of 2.5 K/s and the temperature was controlled at 170°C. In addition to the anthracene grains, neuron-like anthracene films were formed on the amorphous carbon substrate. These TEM images were taken using the Hitachi H-7100R TEM operated at an accelerating voltage of 100 kV.

With increasing He gas pressure, the size of the anthracene grains became slightly larger owing to the increase of the collision frequency with decreasing mean free path. Figure 4 shows the size distribution of anthracene grains. The mean sizes of the anthracene grains, which were determined in 1000 particles, produced in He gas of 4.0×103, 1.1×104 and 2.0×104 Pa were 37.7, 49.6 and 58.2 nm, respectively. The number of carbon atoms is of the order of 105–106. Occasionally, significantly larger grains with micrometer diameter were seen.

When the temperature of the evaporation source was raised at a slower rate of 2.5 K/s, neuron-like anthracene films were formed on the amorphous carbon substrate along with anthracene grains, as shown in Fig. 3(b). Since the anthracene grains were also produced, the anthracene films would be formed from anthracene evaporated at a lower temperature. Because the amount of evaporant is less at lower temperatures, the anthracene grains produced in the smoke are small. Therefore, the small anthracene grains might easily migrate on the carbon substrate and form anthracene films by coalescence. The specimen including anthracene film shows the characteristic 12 μm band, as described in Section 4.

4. Infrared Spectra of Anthracene Grains

The anthracene grains produced were embedded in KBr pellets and their mid-IR spectra were measured. The IR spectra of anthracene grains produced in He gas of 4.0×103, 1.1×104 and 2.0×104 Pa showed many significant features including 11.31- and 13.77-μm bands, which are attributed to the vibrations of aromatic solo and quartet C-H out-of-plane bending modes, respectively. The typical IR spectrum of anthracene grains with a mean diameter of 49.6 nm produced in 1.1×104 Pa He gas, corresponding to the anthracene grains in Fig. 3(a) is shown in Fig. 5(iii). Characteristic features are coincident with the spectrum measured for anthracene molecules dispersed in an Ar matrix at 10 K (Hudgins and Sandford, 1998). The IR spectrum, ranging from 5 to 20 μm, of the molecule was taken from the following webpage ( and modified, as shown in Fig. 5(i). The characteristic features and most plausible candidates of their origin are listed in Table 1. Some differences in the full width of halfmaximum, peak intensities and positions between IR spectra of grains and molecules are visible. In particular, the IR spectra of the grains and the commercial powder have an extra peak at 10.21 μm and two additional peaks at 13.43 and 13.56 μms along with the peak at 13.77 μm compared with the spectra of matrix isolated molecules as indicated by arrows in Fig. 5(iv). In order to see the influence of impurities, a shutter was prepared just below the glass plate. As a result, impurities with sublimation temperatures lower than anthracene could be eliminated. However, the IR spectral features did not change. In addition, although the commercial anthracene powder of the evaporant remained during the experiment, the change of the IR spectra was negligible, i.e., there is no influence of impurities with higher sublimation temperature. Therefore, the bands produced are attributed to new transition bands caused by the aggregation of anthracene molecules independent with crystalline size.

In the spectrum of anthracene films and grains corresponding to Fig. 3(b), a 12-μm band newly appears compared with that of anthracene grains, which is shown in Fig. 5(iv). The 12-μm band has similarly appeared in the spectra of anthracene grains produced with lower heating rates in 4.0×103 and 2.0×104 Pa He gas. Although the 12-μm band is very weak, it significantly shows up in the spectra of condensed anthracene. Previously, although existence of a feature was calculated at 12.3 μm for longaxis polarization, it was not found in solution spectra and in stretched polyethylene spectra, and finally it was not assigned (Radziszewski and Michl, 1985). Since the 12-μm band has never appeared in the spectra of molecules and commercial bulk powder, nor in that of anthracene grains excluding film, we considered that the 12-μm band was caused by the anthracene film. There are other two possible origins of the 12-μm band: the duo or trio C-H out-ofplane bending mode and group vibrations of (CH) n (n = 2 or 3). However, since the features, such as relative intensity or peak position, of the 12-μm band remained the same in all experimental runs with various He gas pressures, we believe that the origin of the 12-μm band is anthracene itself.
Fig. 4.
Fig. 4.

Size distribution of nanometer-sized anthracene grains produced by the gas evaporation method. The mean sizes of the grains produced in He gas of 4.0×103, 1.1×104 and 2.0×104 Pa were 37.7, 49.6 and 58.2 nm, respectively.

Fig. 5.
Fig. 5.

Mid-IR spectra corresponding to (i) molecule in Ar matrix, (ii) commercial powder of anthracene in KBr pellet, (iii) laboratory-produced grains shown in Fig. 2(a) and (iv) laboratory-produced films and grains shown in Fig. 2(b). The IR spectrum of molecule (i) was extracted from the on-line database of IR spectra of PAHs by Hudgins et al. on the Astrochemistry Laboratory website ( and was modified. It has not been recorded at wavelengths longer than 20 μm. A significant 12 μm band appeared in the spectrum of anthracene grains. It corresponds to the plateau feature in astronomically observed spectra. IR spectra (ii) and (iii) of the samples embedded in KBr pellets were measured with a Fourier-transform infrared spectrometer (Horiba Inc. FT210). The wavelength resolution was 2 cm-1. The spectra were arbitrarily-positioned for clarity in the direction of longitudinal axis.

Table 1.
Table 1.

Absorption peak positions (μm) of each spectrum and known assignments.

5. Stability on UV Irradiation

It has been suggested that when the PAHs consisting of 25 carbon atoms form grains via van der Waals forces, the PAH grains are easily broken by far-UV photon absorption (Léger and Puget, 1984; Tielens et al., 1999). It has also been suggested that the PAH grains are photo-evaporated, which produces free-flying PAHs in photo-dissociation regions (Rapacioli et al., 2005; Sakon et al., 2007). Anthracene has roughly two absorption features at 210–290 and 340–410 nm in the range of 200 to 800 nm, as shown in Fig. 6. In order to elucidate the stability of anthracene grains to UV irradiation, the anthracene grains, which were produced in 1.1×104 Pa of He gas and embedded in a KBr pellet, corresponding to Fig. 3(a), were irradiated for 1–100 hours with UV radiation at 254 and 365 nm. The UV lamps at 254 and 365 nm have a width of about 20 nm. The two different irradiation wavelengths correspond to the central wavelength of the absorption features. The intensities at 254 and 365 nm of the UV lamp are 61 and 74 mW/cm2, respectively. The absorption efficiencies at 254 and 365 nm regions are similar. In the case of irradiation for 15 hours, the total fluxes at 254 and 365 nm are 4.2×1021 and 7.4×1021 photons/cm2, respectively.
Fig. 6.
Fig. 6.

Spectral change in UV-Vis spectra of anthracene grains produced in 1.1×104 Pa He gas embedded in KBr pellets after UV irradiation for 1–100 hours at (a) 254 and (b) 365 nm. The intensities at 254 and 365 nm of the UV lamp are 61 and 74 mW/cm2, respectively. The total fluxes at 254 nm are 4.2×1021, 1.1×1022, 1.7×1022, 2.8×1022 and 8.4×1022 photons/cm2, for 15, 40, 60, 80 and 100 hours, respectively. The total fluxes at 365 nm are 5.0×1020, 1.0×1021, 2.0×1021, 3.0×1021, 4.0×1021, 5.0×1021 and 7.6×1021 photons/cm2 for 1, 2, 4, 6, 8, 10 and 15 hours, respectively. Anthracene has roughly two absorption features at 210–290 and 310–440 nm in the range of 200 to 800 nm, as seen in spectra (i). (a) The feature at 210–290 nm gradually disappeared after UV irradiation at 254 nm. The feature at 310–440 nm still remained after as long as 100 hour. (b) Both features immediately and simultaneously disappeared after UV irradiation at 365 nm. The spectra were arbitrarily-positioned for clarity in the direction of longitudinal axis.

In the case of irradiation at 254 nm, almost all features shown in the spectrum for 0 hour in Fig. 7(a), such as peaks at 6.17, 6.90, 7.59, 8.72, 10.02, 10.45, 11.31, 13.77, 21.12 and 21.56 μm, gradually decreased with increasing irradiation time. In contrast, new bands appeared at 8.19, 8.62, 9.70, 10.59, 12.27 and 14.69 μm, and the band at 16.62 μm seemed to be shifted to 16.72 μm and appeared with higher intensity. Then, the feature at 254 nm disappeared and the feature at 365 nm decreased, as shown in Fig. 6(a). In the case of irradiation at 365 nm, the peaks in the mid-infrared region were changed similarly to the case of 254 nm irradiation, although the change was rapid compared with the case of 254 nm, as indicated in Fig. 7(b). The features completely disappeared within 15 hours upon irradiation at 365 nm, although initial bands remained after 100 hours of 254 nm irradiation. At this time, the absorption features at 254 nm also disappeared, as did the absorption feature corresponding to the irradiated wavelength at 365 nm, as shown in Fig. 6(b). Namely, irradiation at 365 nm had a greater effect on anthracene grains than that at 254 nm in spite of its weaker energy. This result implies that the alteration of PAHs by UV irradiation depends on the wavelength. Photon fluxes for the disappearance of half-values of the features were 2.25×1022 and 2.02×1021 photons/cm2 at 254 and 365 nm, respectively. The value of the appearance features doubled upon irradiation at similar photon fluxes. The decreasing rates of the absorption intensity at the 11.3 μm feature under irradiation of both wavelengths are shown in Fig. 8. The photon fluxes in various environments have been reported as 3.4×1012 photons cm-2 s-1 in a reflection nebula NGC 7023, which is illuminated by a young star (Rogers et al., 1995), 1.4×103 and 4.8×103 photons cm-2 s-1 in a dense molecular cloud (Prasad and Tarafdar, 1983; Mennella et al., 2003), 108 photons cm-2 s-1 at the edge of such a cloud (Mathis et al., 1983) and 6.4×109 photons cm-2 s-1 at a heliocentric distance of 5 AU, which corresponds to the distance between Jupiter and the Sun, from the coronal photon flux of the young Sun (Dorren et al., 1995). The experimental photon flux for the disappearance of half-values of the features under 365 nm corresponds to that for 1.9×101, 1.3–4.4×1010, 105 and 9.8×103 year, respectively. This rough estimation suggests that although the spectral alteration of anthracene does not appear around dense molecular clouds, it may occur in reflection nebula and young stellar environments if anthracene grains survive into that stage.
Fig. 7.
Fig. 7.

Mid-IR spectra of anthracene grains produced in 1.1×104 Pa He gas. Spectral change by UV irradiation at (a) 254 nm and (b) 365 nm is shown for 1–100 hours. The intensities at 254 and 365 nm of the UV lamp are 61 and 74 mW/cm2, respectively. The total fluxes at 254 nm are 4.2×1021, 1.1×1022, 1.7×1022, 2.8×1022 and 8.4×1022 photons/cm2, for 15, 40, 60, 80 and 100 hours, respectively. The total fluxes at 365 nm are 5.0×1020, 1.0×1021, 2.0×1021, 3.0×1021, 4.0×1021, 5.0×1021 and 7.6×1021 photons/cm2 for 1, 2, 4, 6, 8, 10 and 15 hours, respectively. (a) In the case of irradiation at 254 nm, the spectral change gradually takes place with increasing irradiation time. (b) In contrast, in the case of irradiation at 365 nm, the spectral change was similarly to that at 254 nm irradiation but the change was very fast compared with that at 254 nm. Photon fluxes for the disappearance of the half-value of the features were 2.25×1022 and 2.02×1021 photons/cm2 at 254 and 365 nm, respectively. The value of the appearance features became twice upon irradiation at similar photon fluxes. The spectra were arbitrarily-positioned for clarity in the direction of longitudinal axis.

Fig. 8.
Fig. 8.

The correlation between the absorption intensity at the 11.3 μm feature and the irradiation time under (a) 254 and (b) 365 nm, respectively. The times and total photon fluxes at the half-value of the intensity at the 11.3 μm feature are 80 and 4 hours and 2.25×1022 and 2.02×1021 photons/cm2, respectively.

The disappearance of UV-Vis features shown in Fig. 6(b) implies that the band gaps of anthracene were varied by UV irradiation. In addition, since the infrared features drastically changed, the C-H bonding of anthracene molecules should be altered. After several studies, we concluded that the new features are caused by dianthracene, i.e., a photodimer of anthracene was produced (Fig. 1). The features have been compared with those of a previously reported spectrum in Table 1. It is known that dianthracene reverts to anthracene upon UV irradiation at 300 nm or shorter. Nevertheless, dianthracene was formed by irradiation at 254 nm in this experiment. This might be the reason behind the slower change of the spectral features by UV irradiation at 254 nm compared to 365 nm.

In order to elucidate the conditions of spectral change, several experiments were performed. The spectrum change was not observed when anthracene, before being embedded in KBr, was irradiated with UV in He of 4.0×104 Pa (300 Torr). In the case of irradiation in air, the spectral features did not change, although the color of anthracene became yellowish. It has been observed that yellow anthraquinone is formed by irradiation in the presence of oxygen. Nevertheless, the spectrum of the yellowish sample does not correspond with anthraquinone. The spectral evolution was completely duplicated with the irradiation of anthracene embedded in KCl or NaCl. Namely, potassium and bromide do not affect the formation of dianthracene. When anthracene and KBr were mixed and irradiated with UV before being made into a pellet under pressure, the spectral change was negligible. Accordingly, the pressure in forming the pellet is a clue to the spectral evolution. To form a KBr pellet, the mixture of anthracene and KBr powders was pressed at 6×103 kg/cm2. It is known that the formation of dianthracene is accelerated depending on the domain structure of anthracene crystals (Ramdas et al., 1980). Actually, formation of dianthracene in KBr pellets has been previously reported using bulk anthracene crystals with similar trends even in nanometer sized anthracene grains (Bernas et al., 1966; Chandross and Ferguson, 1966). Since the crystal structure of anthracene may be fragile because it is a molecular crystal, pressing will reduce the crystallinity of anthracene grains. However, the absorption features attributed to the anthracene molecule were not changed after it was embedded in the KBr pellet. Similar spectral changes were observed even when the pressure for pressing the KBr pellet was as low as 7.5×102 kg/cm2. When a similar irradiation experiment was performed on other PAHs, such as phenanthrene, naphthacene (tetracene), pentacene, pyrene, chrysene and coronene, no alteration of the spectral features was observed except for anthracene, even when xenon white light was irradiated.

6. Astronomical Implications

Our experimental result concerning the 12 μm band caused by anthracene films implied that if anthracene and possibly other PAHs deposited on the previously condensed solid grains, such as silicon carbide, graphitic carbon, iron or possibly oxide, PAHs would grow on the grain in a twodimensional structure and form PAH films. Then, the surface PAH layer might be the cause of the plateau feature at 11–15 μm. Indeed, silicon carbide grains with PAHs on their surface have been found in a carbonaceous meteorite (Frenklach et al., 1989). Two-dimensional PAHs can also exist in the gas phase. The PAH surface layer will later be coated by an ice layer in the cooler region. If those particles are transferred to a molecular cloud, photodimers should be produced in the carbonaceous layer between the core and the surface ice layer. In the case of freeflying PAH molecules, they emit after excitation by absorption of single UV photons. Since nanometer sized grains have a larger heat capacity than PAH molecules, the grains have to be heated by other source or photodimers have to be released from the grain surface for efficient emission from photodimers. In that case, the infrared spectrum will become broader, because many peaks appear in the midinfrared region. In addition to anthracene, it is known that naphthacene and coronene can form dimers. Therefore, although infrared spectra of neutral, anionic and cationic PAHs were measured actively, it is necessary to obtain the infrared spectrum of PAH dimers, because UV rays are present ubiquitously in space. Our experimental results suggest the possibility that the disappearance of UIR bands in the HII region is a result of the broadness of infrared features caused by the formation of photodimers.

7. Summary

Anthracene grains with 35–60 nm mean diameter were produced by evaporating commercial anthracene powder in He gas. The anthracene grains showed somewhat different features concerning width, relative intensities and positions from anthracene molecules. In addition, the 12-μm band, which has never appeared in the spectra of molecular and commercial powder of anthracene, was observed from the anthracene films. After UV irradiation, the characteristic mid-IR features of the anthracene grains were dramatically changed owing to the formation of anthracene photodimers, i.e., dianthracene, depending on the irradiated wavelength. Currently, similar experiments are being performed in order to understand the growth mechanisms and the cause of the significant optical properties of PAHs and their grains using other PAHs, such as naphthacene, naphthalene, pyrene, chrysene and coronene.



This work was supported in part by a Grant-in-Aid for Young Scientists (start-up) from the KAKENHI (19840048) of JSPS.

Authors’ Affiliations

Institute for Molecular Science, National Institutes of Natural Sciences, Okazaki, Aichi 444-8585, Japan
Department of Astronomy, School of Science, University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan
Laboratory for Nano-Structure Science, Department of Physics, Ritsumeikan University, 1-1-1 Nojihigashi, Kusatsu-shi, Shiga 525-8577, Japan
Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan


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