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<strong>Experimental</strong> <strong>approach</strong> <strong>of</strong> <strong>dust</strong><br />

<strong>process<strong>in</strong>g</strong> <strong>in</strong> <strong>protoplanetary</strong> <strong>disks</strong> and<br />

comparison with returned samples<br />

Mathieu Roskosz<br />

Workshop MarcoPolo-R, December 2012, CNES-Hqs<br />

Mathieu.roskosz@univ-lille1.fr


Recuits sur des précurseurs de<br />

diopsides (740°C, 10j)<br />

(thermal anneal<strong>in</strong>g)


ISM Vs. Protoplanetary disk<br />

Evaporation/condensation<br />

Thermal anneal<strong>in</strong>g<br />

Amorphous-Crystall<strong>in</strong>e<br />

F. Kemper, W. J. Vriend, and A. G. G. M. Tielens<br />

Ap. J. 609, 826–837<br />

R. van Boekel, et al.<br />

Nature 432, 479-482


A controversial m<strong>in</strong>eralogical zon<strong>in</strong>g<br />

VLT<br />

Spitzer<br />

An <strong>in</strong>ner disk dom<strong>in</strong>ated<br />

by pyroxenes<br />

An outer disk dom<strong>in</strong>ated<br />

by oliv<strong>in</strong>e<br />

Detection <strong>of</strong> SiO 2 polymorphs<br />

Watson et al., ApJS 180 (2009) 84-101<br />

Sargent et al., ApJS 182 (2009) 477-508<br />

Sargent et al., ApJ 690 (2009) 1193-1207<br />

R. van Boekel, et al.<br />

Nature 432, 479-482


<strong>Experimental</strong> details<br />

• 970-1070 K<br />

• A few hours to 2 months<br />

• Glasses and homogeneous<br />

nanoporous volatile-free<br />

gels<br />

• In situ HT X-ray Diffraction<br />

• TEM<br />

• Conventional XRD<br />

• Spectroscopies (Raman and IR)


Quelques Subsolidus résultats: crystallization 740°C, 10j<br />

Dynamical anneal<strong>in</strong>g <strong>of</strong> MgSiO 3<br />

(Roskosz et al., ApJ (2009))


Local and bulk cation dynamics control low-T<br />

<strong>dust</strong> crystallization<br />

• Even start<strong>in</strong>g from an enstatite precursor, below 700°C, only forsterite forms…<br />

MgSiO 3 amorphous Mg 2 SiO 4 +SiO 2<br />

(Roskosz et al., A&A, 2011)<br />

Mobility decoupl<strong>in</strong>gs <strong>in</strong> solids expla<strong>in</strong>s the metastable low-temperature<br />

formation <strong>of</strong> the MgO-(CaO)-rich phases<br />

(Roskosz et al., JNCS (2005) 351, 1266-1282; JNCS (2006) 352, 180-184)


Metastable low-T assemblages identified "<br />

<strong>in</strong> Star<strong>dust</strong> samples


Metastable low-T assemblages identified "<br />

<strong>in</strong> Star<strong>dust</strong> samples<br />

Conclusion et applications<br />

Al<br />

Si<br />

SiO 2<br />

1 µm<br />

Pt<br />

Mg<br />

S<br />

Fe<br />

500 nm<br />

« Fo 58 »<br />

« Fo 93 »<br />

Close association <strong>of</strong> oliv<strong>in</strong>es and quartz polymorphs (micrography H. Leroux)


Recuits sur des précurseurs de<br />

diopsides (740°C, 10j)<br />

(irradiation)


Irradiation <strong>in</strong> astrophysical environments<br />

• SN shock waves<br />

• Cosmic rays<br />

• X-w<strong>in</strong>ds<br />

• Solar flairs, outflows…<br />

Irradiation :<br />

<strong>in</strong>teractions particles-matter<br />

(photons, electrons, ions) <strong>in</strong>duc<strong>in</strong>g<br />

modifications <strong>of</strong> the material<br />

• Gra<strong>in</strong> size distribution<br />

• Lifetime<br />

• Structure<br />

• Composition<br />

• Porosity<br />

• Optical properties<br />

• Isotopic signatures<br />

L<strong>in</strong> et al., 1994, Adv. Space Res,<br />

20, 465<br />

Implantation<br />

Sputter<strong>in</strong>g


Electron irradiation<br />

Transmission<br />

Electron<br />

Microscope(MET)<br />

• Irradiation and <strong>in</strong> situ characterization<br />

(microstructure, crystall<strong>in</strong>ity, composition).


Electron irradiation: <br />

Amorphization, radiolysis, chemistry<br />

Chemical changes associated with amorphization<br />

Phase<br />

transition<br />

Oliv<strong>in</strong>e<br />

MgO<br />

+SiO 2<br />

1 µm<br />

(Carrez et al. 2002)<br />

Irradiation <strong>of</strong> MgSiO 3<br />

composition at 300 keV<br />

Oxygen bubbles formation<br />

Carrez et al., 2001<br />

San Carlos oliv<strong>in</strong>e irradiated :<br />

Differential loss <strong>of</strong> the different elements.<br />

Structure-dependent k<strong>in</strong>etics


Itokawa Dust particules collected from the<br />

Hayabusa mission<br />

Amorphization,<br />

In situ reduction <strong>of</strong> iron from<br />

m<strong>in</strong>erals <strong>in</strong>to metallic nuggets,<br />

Noble gas implantation…<br />

A closer look at experimental data<br />

may help to quantitatively describe<br />

the space weather<strong>in</strong>g<br />

Noguchi et al., Science, 2011


Electron irradiation <strong>of</strong> OM’s<br />

Polyethylene terephthalate (PET) is a<br />

semicrystall<strong>in</strong>e symetrical arrangement<br />

<strong>of</strong> aromatic groups and aliphatic cha<strong>in</strong>s<br />

Comprehensive description <strong>of</strong><br />

irradiation-<strong>in</strong>duced modifications <strong>of</strong> the<br />

IOM <strong>in</strong> relation with their D/H<br />

signatures<br />

PhD thesis <strong>of</strong> Boris Laurent, UMET <strong>in</strong> coll. MNHN<br />

http://umet.univ-lille1.fr/Projets/FrIHIDDA/<br />

12 keV, e - , PET, 2500 nm


Electron irradiation <strong>of</strong> OM’s<br />

IR spectra <strong>of</strong> electron-irradiated PET at 30 keV<br />

EPR spectroscopy <strong>of</strong> irradiated PET<br />

show<strong>in</strong>g the appearance <strong>of</strong> mono- and<br />

biradicals<br />

IR image <strong>of</strong> the grow<strong>in</strong>g band at 1600 cm -1 <strong>in</strong><br />

electron-irradiated PET at 30 keV<br />

Laurent et al. com<strong>in</strong>g LPSC


Electron irradiation <strong>of</strong> OM’s:"<br />

Wait<strong>in</strong>g for MarcoPolo-R…<br />

D/H ratios <strong>of</strong> irradiated PET as a function <strong>of</strong> Dose:<br />

Several hundreds permil fractionation, atta<strong>in</strong>ment <strong>of</strong> a steady state (??)<br />

For a detailed study <strong>of</strong> the correlations between irradiation, catalysis,<br />

structural and D/H modification <strong>of</strong> OM, please attend the com<strong>in</strong>g LPSC<br />

Laurent et al. com<strong>in</strong>g LPSC


Thanks to<br />

• H. Leroux, B. Laurent, J. Gillot, UMET<br />

• L. Rémusat, F. Robert, MNHN<br />

• H. Vez<strong>in</strong>, LASIR


<strong>Experimental</strong> <strong>approach</strong> <strong>of</strong> <strong>dust</strong><br />

<strong>process<strong>in</strong>g</strong> <strong>in</strong> <strong>protoplanetary</strong> <strong>disks</strong> and<br />

comparison with returned samples<br />

Mathieu Roskosz<br />

Workshop MarcoPolo-R, December 2012, CNES-Hqs<br />

Mathieu.roskosz@univ-lille1.fr


Exemple 1: composition enstatite<br />

Cristallisation sous la température de transition vitreuse<br />

a<br />

b<br />

c<br />

200 nm


Durée de vie de l’assemblage Forsterite+SiO 2 <br />

Thickness ^2 (microns)<br />

120<br />

100<br />

80<br />

60<br />

40<br />

20<br />

580MPa<br />

450 MPa<br />

210 MPa<br />

1 Wt% H 2 O<br />

1000°C<br />

Thickness^2 (microns)<br />

25<br />

20<br />

15<br />

10<br />

5<br />

nom<strong>in</strong>ally anhydrous<br />

0,1 Wt% H2O<br />

1 Wt% H2O<br />

210 MPa<br />

1000°C<br />

thickness^2 (microns)<br />

700<br />

600<br />

500<br />

400<br />

300<br />

200<br />

100<br />

0<br />

0<br />

0 10 20 30 40 50 60 70 80 90 100<br />

time (h)<br />

1450°C<br />

1400°C<br />

1350°C<br />

0 Wt% H 2 O<br />

1 bar<br />

0 20 40 60 80 100 120<br />

time (h)<br />

0<br />

0 10 20 30 40 50 60 70 80 90 100<br />

time (h)<br />

Fo+SiO 2 DOIT se transformer en<br />

enstatite<br />

La vitesse de cette transformation<br />

dépend fortement de P, H 2 O, et T<br />

Que se passe-t-il à basse P, T et<br />

sans eau (sous 1000°C) ?<br />

Data from Yund, 97, CMP; Fisler et al., 97, PCM


Durée de vie de l’assemblage Forsterite+SiO 2 <br />

Recuits sur un assemblage de f<strong>in</strong> gra<strong>in</strong>s de forsterite encapsulés dans une<br />

matrice de silice pure formée par sol-gel.<br />

Recuits à 1000°, 1100° et 1250°C jusqu’à 1 mois<br />

Les extrapolations arrhéniennes des données HP ou HT avec et sans eau<br />

prédisent une vitesse de croissance de la couche d’enstatite d’au mo<strong>in</strong>s<br />

10 -11 m.s -1 à 1100°C


Durée de vie de l’assemblage Forsterite+SiO 2 <br />

500 nm 200 nm<br />

Mo<strong>in</strong>s de 4 10 -16 m.s -1<br />

Pourtant la diffusion cationique<br />

opère (murissement des textures)<br />

La nucléation d’enstatite est<br />

<strong>in</strong>hibée à l’<strong>in</strong>terface<br />

Fo/SiO 2 par un<br />

ΔV global de -6%<br />

En l’absence de pression de<br />

conf<strong>in</strong>ement et d’eau<br />

L’assemblage Fo+SiO 2 peut être<br />

préservé à T


M<strong>in</strong>eralogical zon<strong>in</strong>g


Conclusion et applications


M<strong>in</strong>eralogical zon<strong>in</strong>g


Irradiation <strong>in</strong> astrophysical environments<br />

• Nature des particules (photon, électrons, ions)<br />

• Flux des particules (particules cm -2 s -1 )<br />

• Fluence (particules cm -2 )<br />

• Spectre d’énergie (eV, keV or MeV ?)<br />

Stone et al., 2008, Adv. Space Res, 454, 71<br />

L<strong>in</strong> et al., 1994, Adv. Space Res, 20, 465


Irradiation par des ions: exemple 2/3<br />

amorphisation<br />

Conditions<br />

experimentales:<br />

He sur oliv<strong>in</strong>e<br />

Energie: 4 keV<br />

5 10 16 ions/cm 2 10 17 ions/cm 2<br />

Implantation<br />

5 10 17 ions/cm 2 10 18 ions/cm 2<br />

Porosité des<br />

poussières<br />

Implantations de gaz<br />

rares<br />

Réduction de la taille<br />

des poussières dans<br />

l’ISM ?<br />

Surpression, fracturation<br />

Demyk et al., 2001,<br />

Carrez et al., 2002


Le grand recyclage stellaire<br />

X

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