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| Naji, M. |
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| Motta, Antonella |
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| Aletan, Dirar |
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| Mohamed, Tarek |
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| Ertürk, Emre |
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| Taccardi, Nicola |
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| Kononenko, Denys |
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| Petrov, R. H. | Madrid |
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| Alshaaer, Mazen | Brussels |
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| Bih, L. |
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| Casati, R. |
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| Muller, Hermance |
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| Kočí, Jan | Prague |
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| Šuljagić, Marija |
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| Kalteremidou, Kalliopi-Artemi | Brussels |
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| Azam, Siraj |
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| Ospanova, Alyiya |
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| Blanpain, Bart |
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| Ali, M. A. |
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| Popa, V. |
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| Rančić, M. |
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| Ollier, Nadège |
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| Azevedo, Nuno Monteiro |
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| Landes, Michael |
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| Rignanese, Gian-Marco |
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Ferrari, Marco
in Cooperation with on an Cooperation-Score of 37%
Topics
Publications (20/20 displayed)
- 2024Piezoelectric MEMS Flexural-Plate-Wave Transducer for Alignment of Microparticles in a Drying Dropletcitations
- 2023Flexural Plate Wave Piezoelectric MEMS Pressure Sensorcitations
- 2023Cell Alignment in Aqueous Solution Employing a Flexural Plate Wave Piezoelectric MEMS Transducercitations
- 2023Application of dissipative particle dynamics to interfacial systems: Parameterization and scalingcitations
- 2022Flexural Plate Wave Piezoelectric MEMS Transducer for Cell Alignment in Aqueous Solutioncitations
- 2022Visible and near-InfraRed (VNIR) reflectance of silicate glasses: Characterization of a featureless spectrum and implications for planetary geologycitations
- 2022Reflectance of silicate glasses in the mid-infrared region (MIR): Implications for planetary researchcitations
- 2021Mineralogical implications for the 1-micron feature in the refined average spectrum of Ceres
- 2021High-Pressure Synthesis and Gas-Sensing Tests of 1-D Polymer/Aluminophosphate Nanocompositescitations
- 2021High-Pressure Synthesis and Gas-Sensing Tests of 1-D Polymer/Aluminophosphate Nanocompositescitations
- 2019NIR and mid-IR spectroscopy on silicate glasses for the characterization of magmatic bodies on terrestrial planets.
- 2018Spectroscopy on silicate glasses from two magmatic series: implications for planetary studies.
- 2017Comparison of traditional and simplified methods for repairing CAD/CAM feldspathic ceramicscitations
- 2017FT-IR and μ-IR analysis of Carbonaceous Chondrite meteorites characterization as possible analogue of next sample returned materials
- 2016Wild 2 grains characterized combining MIR/FIR/Raman micro-spectroscopy and FE-SEM/EDS analyses
- 2014Wild 2 grains characterized combining MIR/FIR/Raman micro-spectroscopy and FE-SEM/EDS analyses
- 2014Flexural resistance of Cerec CAD/CAM system ceramic blocks. Part 2: outsourcing materials
- 2013Flexural resistance of Cerec CAD/CAM system ceramic blocks
- 2012In Situ Collection of Refractory Dust in the Upper Stratosphere: The DUSTER Facilitycitations
- 2006Acid etching surface treatment of feldspathic, alumina and zirconia ceramics: a micro-morphological SEM analysis.
Places of action
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article
Wild 2 grains characterized combining MIR/FIR/Raman micro-spectroscopy and FE-SEM/EDS analyses
Abstract
We present the analyses results of two bulk Terminal Particles, C2112,7,171,0,0 and C2112,9,171,0,0, derived from the Jupiter-Family comet 81P/Wild 2 returned by the Stardust mission. Each particle embedded in a slab of silica aerogel was pressed in a diamond cell. The aerogel, as expected, caused problems to identify the minerals and organic materials present in these particles. These problems were overcome by means of the combination of FE-SEM/EDS, IR and Raman μ-spectroscopy, three non-destructive analytical techniques, which allowed the mineral and organic information on the two bulk particles. Indeed, this approach proved to be practical for preliminary characterization, i.e. scanning particles for chemical and mineralogical heterogeneity. It can be considered as a procedure to be followed for selecting Stardust particles-of- interest using this type of bulk characterization prior to more detailed studies. TP2 and TP3 are dominated by Ca-free and low-Ca, Mg-rich, Mg,Fe-olivine. The presence of melilite in both particles is supported by IR μ-spectroscopy, but is not confirmed by Raman μ-spectroscopy possibly because the amounts are too small to be detected. TP2 and TP3 show similar silicate mineral compositions but Ni-free and low-Ni, sub-sulfur (Fe,Ni)S grains are present in TP2 only. TP2 contains indigenous amorphous carbon hot spots; no indigenous carbon was identified in TP3. These non-chondritic particles probably originated in a differentiated body. The presence of high temperature melilite group minerals (incl. gehlenite) in TP2 and TP3 reinforces the notion that collisionally-ejected refractory debris from differentiated asteroids may be common in Jupiter-Family comets. It does raise the question if similar debris and other clearly asteroidal dust could be present in Halley-type comets and if so what fractions of the dust in these comets are truly non-processed silicates and organic material. The results of this study will be relevant to the ROSETTA mission that will rendezvous with Jupiter-Family comet 67P/Churyumov-Gerasimenko during 2014 October. At the time this mission was launched our ideas of comet dust were biased by the findings of the Halley missions. The Stardust mission showed an unexpected richness of dust that originated from the inner solar system. We should be prepared for a similar mixed dust population of mono- and polymict debris in this J-F comet. Still, it would be nice if doesn't look like anything seen in comet Wild 2. The work in Stardust samples is important to the question what are the similarities and differences among comets....