from a pyrolysis experiment
(carbonization of cellulose at different temperatures,
Jaeger et al.
1998), by reflectance measurements at polished surfaces and an oscillator fit.
Data are available from the UV throughout the infrared for the following pyrolysis temperatures (indicating increasing carbonization resp. graphitization) :
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from matrix-isolation spectroscopy of non-agglomerated carbon particles
(Schnaiter et al.
1998). This unique experiment combined a molecular-beam method for extraction of carbon grains out of their condensation zone with
the isolation of the particles in rare-gas matrices. This allowed UV spectroscopy at non-agglomerated grains and
the application of simple Mie theory for evaluation of optical data.
Data are available for carbon particles condensed in : |
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from a sample of "presolar"
nano-diamonds extracted from the Allende meteorite
(Braatz et al. 2000,
Mutschke et al. 2004).
The data are based on transmission spectroscopy at VUV to IR wavelengths, taking scattering losses into account,
and electron energy loss spectroscopy performed at the Fritz-Haber-Institut Berlin :
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