Meteoritics and Planetary Science · 2008 · 102 citations · 101 references
Natural SciencesChemistryEarth SciencesElemental AnalysisInterstellar MediumSpectroscopyInfrared SpectroscopyInterstellar DustRaman SpectroscopyCarbonaceous DustCometary Infrared EmissionField EmissionInterplanetary DustLabile Carbon PoolsOrganic Molecules In CometsRaman Data AnalysisRaman Microscopy
Abstract— We report combined micro‐infrared, micro‐Raman, and field emission scanning electron microscope (FESEM) analyses of particles collected by the Stardust spacecraft during its flyby of comet 81P/Wild 2 on 2 January 2004 and successfully returned back to Earth on 15 January 2006. We present mid‐infrared (IR) spectra of six of these particles. The CH 2 /CH 3 ratios inferred from the infrared data are greater than those seen in organics in the diffuse interstellar medium, possibly indicating the presence of longer or less branched aliphatic chains. The micro‐Raman data offer insights into the state of the order of the carbonaceous component present in the particles. Raman parameters for most of the particles span a similar range to that observed in interplanetary dust particles (IDPs) and the most primitive meteorites. Both the IR and Raman data imply the presence of a very labile carbonaceous component. Hydrated silicates may be present in two particles of Track 35, one of which may also contain carbonates, but further investigations with other techniques need to be performed to confirm these findings. In some cases, the analyses are difficult to interpret because of the presence of compressed aerogel mixed with the grains.
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