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Astron. Astrophys. 329, 1035-1044 (1998) 3. Laboratory results on SiC powdersIn this section, we wish to illustrate and confirm the statements of Sect. 2. For this purpose, we took advantage of the advent of two new synthesis methods used in our laboratories for more general purposes: laser pyrolysis of gaseous precursors, and mechanical synthesis by milling together pure carbon and silicon. 3.1. Laser pyrolysisNanosized SiC powder has been synthesized by a gas phase laser
driven reaction using silane and acetylene precursors and a high-power
continuous wave CO2 laser emitting at 10.6
µm in resonance with an infrared absorption band
of silane. Detailed information on the synthesis process was given by
Cauchetier et al. (1988). Sample SiC212 was obtained at atmospheric
pressure under 600 W laser power, the flow rates being 600 and 300
cm3 /min of silane and acetylene respectively. A gray,
cotton-like powder is formed. The specific surface area, as measured
by adsorption-desorption of nitrogen (Brunnauer-Emmet-Teller method),
is 70 m
Chemical analysis shows the presence of 1.4 wt% of oxygen and 30.3 wt% of carbon. Neglecting hydrogen, the silicon content amounts to the remaining 68.3 wt%. From stoichiometry, the corresponding chemical composition is SiC: SiO2: free carbon = 95.7: 2.7: 1.6 wt%.
3.2. Mechanical alloyingMechanical alloying is now a widely used method to prepare all kinds of materials from elemental powder mixtures (Gilman and Benjamin,1983; LeCaer et al., 1990; Koch, 1993). A wide variety of alloys, compounds, composites have been obtained by this dry and high-energy ball-milling process often in a metastable crystalline form with a nanometric crystallite size which is typically of the order of 10 nm. Dry grinding in high-energy ball-mills is also a non-equilibrium method of processing already synthesized materials which induces changes in the ground powders such as formation of nanometre-sized crystallites with a high defect density and interface content, amorphization (Koch 1993), polymorphic transformations (for instance Begin-Colin et al. 1994), order-disorder transformations (Pochet et al. 1995). Both mechanical processes involve repeated welding, fracturing and rewelding of powder particles in a high energy ball charge. In the case of SiC, detailed studies of these processes as a function of various experimental parameters can be found in the recent literature (see for instance LeCaer et al., 1990; Matteazzi et al., 1991; Sherif El-Eskandarany et al., 1995).
Here, we have used ball-milling to refine and homogenize a
commercial product of essentially the same The X-Ray diffraction (XRD) pattern of ground SiC powder is
identical to the XRD pattern of the starting powder, but with
broadened diffraction peaks related to crystallite sizes and strains.
Grinding does not induce change in the lattice parameter of
3.3. IR SpectrometryTransmission spectra were obtained using KBr and CsI pellets in which small quantities of SiC powder were embedded homogeneously. A pellet is obtained by mixing about 1 mg of SiC and 300 mg of matrix powder, grinding for several minutes, and applying about 10 tons of pressure for 5 to 10 mn. The pellet is 13 mm in diameter and about 1 mm thick. It is mounted in the sample beam of a P-E interferometric spectrometer whose resolution is set at 4 cm-1. The absorbance spectra shown here were obtained by subtracting the spectrum of a KBr (or CsI) blank from the spectrum of an SiC-loaded pellet. Absorbances at the feature's peak range between 0.5 and 2.5. The extinction coefficient is obtained from the absorbance, A, by writing where S =1.3 cm2 is the pellet cross-section
area, If the particles are big by construction or by agglomeration, in the matrix, the spectrum can suffer dramatic changes: thus, Fig. 3 shows the full spectra of SiC from laser pyrolysis (sample SiC 212) embedded in KBr by careful grinding (a), and the same powder crammed over a blank KBr pellet (b). The effects predicted by theory (Sect. 2) are all observed on curve 3b. Similar effects are exhibited by embedded mechanically prepared SiC, when not ground or ground for excessively long times: 4 hours seems to be an optimum in avoiding size and agglomeration effects (hence sample SiC4h). By contrast, laser pyrolysis seems to produce consistently small particles.Note the very weak underlying continuum absorbance across the whole spectrum.
In the following, therefore, we consider only sample powders SiC212
and SiC4h and restrict the spectral range to the feature extent, 700
to 1000 cm-1, as in Fig. 4 and 5
3.4. DiscussionIn order to lay down sound bases for the comparison of laboratory with astronomical spectra (Sect. 4), we wish first to use our results as a test of the fundamental assumptions that: 1) the feature shape is determined mainly by the distribution of particle shapes and 2) the bulk optical constants (Eq. 12) apply to our powders. Indeed, as expected, all extinction features are confined between
The red shift of the feature on going from a KBr matrix
( 1) Considering the weakness of the damping constant,
2) For each wavenumber 3) Using (8), compute the corresponding resonance wavenumber in the other matrix, n: where 4) Note that the ratio of spectral intensities,
where This procedure was applied to the spectrum (Fig. 2b) of SiC212 in
CsI (matrix m) to deduce the expected spectrum in KBr (matrix
n), which is compared in Fig. 6 to the measured spectrum (Fig.
4a). The fit is particularly sensitive to the exact value assumed for
Finally, compare the measured and expected extinctions. The
measured values of If the SiC particles were all small spheres, we
would, from Eq. 7, expect their peak extinction coefficient,
Similar huge "discrepancies" were previously blamed on the use of
bulk SiC optical constants to interpret the spectra of powders. Note,
however, that micrographs show that the particles are not mostly
isolated spheres. Besides, if they were, their spectrum would be a
Lorentzian curve of width Given the purity and crystallinity of our materials, the
observed spectral profiles should rather be interpreted in terms of
continuous distributions of grain shapes. In this case, it is
indeed expected that the feature peak should be depressed relative to
in agreement with the numbers in (17), to within errors on SiC masses embedded in the pellets. Since our fundamental assumptions are validated by this test and
previous remarks, we retain these assumptions for further discussion.
Thus, Fig. 7 gives, for each wavenumber, a) the calculated red shift
We now proceed to discuss the spectra within this framework. First
note that the "blue" peak of SiC212 in KBr (Fig. 4a) occurs at
The other peak in Fig. 4 (820 cm-1 or12.2 µm) and the single peak of Fig. 5 (870 cm-1 or 11.5 µm) must be due to oblate and/or prolate spheroids. The position of this peak mainly depends on the particular shape distribution, i.e. on the production process and preparation technique. Thus, the single peak in the spectra of Friedman et al. (1981) occurs near 840 cm-1 while that of 600GWS, the purest and finest powder of Borghesi et al. (1985), falls at 860 cm-1. The samples of Koike (1987) cover the whole range from 820 to 885 cm-1. Since all these spectra were taken in KBr matrices, it can be deduced from Fig. 5 that the corresponding L 's range from 0.05 to 0.25. For ellipsoids, the corresponding ellipticities fall between 0.7 and 0.88 (Bohren and Huffman, 1983), and the ratio of large to small size, between 1.4 and 50. This is compatible with the flakes and /or strings of spheroids seen under the microscope. To us, the correlation that seems to exist between polytype and feature peak position (Kaito et al., 1994) only implies that crystal polytypes may come in prefered shapes of particles, not that they have different bulk optical constants. This is borne out by the large variety of spectra that can be obtained by the same laboratory, for the same polytype. Only exceptionally does the literature mention a strong peak near
Neither small nor large spheres exhibit the 12.6 µm feature; only intermediate-sized spheres do so, but this feature is then dwarfed by the characteristic feature of spheres at L =1/3 (Bohren and Huffman, Fig. 12.1). Finally, it is useful to recall here the attempt of
Pégourié (1988) to infer the optical constants of
We conclude that all observed laboratory spectra, to our knowledge, can be interpreted by using the bulk optical properties and allowing for the distribution of particle shapes. If the latter is unknown, it can be inferred from the extinction spectrum (cf. Fig. 6), provided the particles are small enough. However, there is no way to infer the bulk optical properties from the spectrum, if the shape distribution is unknown. The assumption that the particles are spherical is generally not tenable. Even a continuous distribution is a better approximation. ![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 1998 Online publication: December 16, 1997 ![]() |