Dans les disques protoplanétaires, les grains micrométriques croissent jusqu'à atteindre des tailles de planétésimaux avant de finalement former des planètes. Cependant,des études dynamiques ont montré qu'une fois que les grains atteignent une taille critique, ils dérivent rapidement vers l'étoile et y sont accrétés. Ce problème est connu comme la barrière de dérive radiale. De plus, des expériences en laboratoire ont montré que les grains peuvent fragmenter ou rebondir et ainsi arrêter la croissance avant les tailles kilométriques.Afin de passer outre ces barrières, plusieurs méthodes ont été proposés comme les pièges à particules (dans les vortex ou les sillons planétaires) qui demandent des évolutions dynamiques à grande échelle. Dans ce travail, nous choisissons d'étudier les propriétés intrinsèques de la poussière pendant leur croissance et plus particulièrement leur porosité.Nous développons un modèle d'évolution de la porosité pendant la croissance en fonction de la masse des grains pour plusieurs régimes d'expansion/compression (Kataoka et al. 2013, Okuzumi et al. 2012) et l'implémentons dans notre code SPH bifluide (Barrière-Fouchet et al. 2005). Nous trouvons que la croissance des grains poreux est accélérée en comparaison aux grains compacts et leur taille peut atteindre plusieurs kilomètres. De surcroît,la dérive est légèrement ralentie pour les grains poreux qui peuvent croître jusqu'à de plus grandes tailles avant de commencer à dériver vers l'étoile. Nous constatons aussi que les grains des régions externes du disque grossissent plus que quand l'effet de la porosité est négligé. Ces deux mécanismes peuvent aider les grains à outrepasser la barrière de dérive radiale, notamment en passant dans le régime de traînée de Stokes, et ainsi former des planétésimaux.Nous étudions aussi l'effet de la fragmentation et du rebond sur le comportement des grains. En considérant un seuil de fragmentation constant, nous observons que la croissance de grains poreux est retardée un temps par la fragmentation mais qu'elle se poursuit vers de grandes tailles et par conséquent, permet de passer outre les problèmes dus à la fragmentation et à la dérive radiale. Cependant, les grains très poreux sont plus fragiles et peuvent se fragmenter plus facilement entraînant une accrétion massive des poussières dans l'étoile. De plus, nous montrons que les effets du rebond peuvent être négligés devant ceux de la fragmentation.Enfin, nous observons également que la taille des monomères et du paramètre de viscosité turbulente peut avoir une influence sur l'évolution de la porosité et donc de la poussière dans le disque.La porosité permet donc de favoriser la croissance des grains et accélérer le découplage des grains. Les grains très poreux peuvent être plus sensibles à la fragmentation.Cependant, les effets collectifs de la poussière couplés à la porosité peuvent aider les grains à outrepasser les barrières de formation planétaire. La barrière de rebond peut être négligée dans le cas de grains poreux devant les autres barrières. Enfin,l'intensité de la turbulence altère la croissance et ainsi le devenir de la poussière.La taille des monomères modifie le facteur de remplissage sans toutefois impacter le découplage des grains dans les parties internes / In protoplanetary discs, micron-sized grains should grow up to planetesimal sizes in order to ultimately form planets. However, dynamical studies show that once they reach a critical size, they drift rapidly into the accreting star. This is known as the radial-drift barrier. Moreover, laboratory experiments have shown that grains can fragment or bounce, stopping the growth towards planetesimal sizes.In order to overcome those barriers, several methods have been proposed such as particles traps (e.g. vortices or planet gaps) which all involve large-scale dynamics.In this work, we choose to investigate the intrinsic properties of the grains during their growth, in particular their porosity.We thus consider the growth of grains with variable porosity as a function of their mass in several regimes of compression/expansion (Kataoka et al. 2013, Okuzumiet al. 2012) and implement it in our 3D SPH two-fluid code (Barrière-Fouchetet al. 2005).We find that growth is accelerated for porous grains that can reach kilometersizes. On the other hand, drift is slightly slowed down for porous grains that can grow up to larger sizes before drifting towards the star. As a result, grains in the outer regions of the disc reach larger sizes than when porosity is neglected. Those two mechanisms can help grains overcome the radial-drift barrier and form planetesimals.The Stokes drag regime appears to play a substantial part in maintaining grains in the disc.Considering a constant fragmentation threshold, we also find out that growth is delayed because of fragmentation but reaching large sizes and thus overcoming problems due to fragmentation and radial drift is still possible. However, very fluffy grains are fragile and can be easily disrupted leading to a massive accretion of dust into the star. Moreover, we show that the effects due to dust bouncing can be neglected compared to fragmentation.Finally, we investigate the influence of the size of monomers and -parameter on the evolution of porosity and then dust in the disc.Dust growth is accelerated by porosity and thus promotes grains decoupling. Very fluffy grains are more affected by fragmentation. However, dust collective effects and porosity can help grains to overcome planet formation barriers. Besides,the bouncing barrier can be neglected in the case of porous dust compared to other barriers. Finally, the intensity of turbulence can alter the growth and so the outcome of dust. The size of monomers modifies the grain filling factor without impacting dust decoupling in the inner parts of the disc

L'objectif principal de cette thèse est de proposer de nouveaux mécanismes de transport de solides dans les disques protoplanétaires afin de résoudre le problème de la dérive radiale des solides causée par la friction du gaz. En effet, malgré d'importants efforts théoriques et expérimentaux, il reste difficile à expliquer comment de petites particules de poussière submillimétriques forment des blocs kilométriques dans les conditions qui règnent au sein des disques protoplanétaires. Je montre que les mécanismes de transport proposés dans cette thèse sont en mesure de résoudre ce problème de dérive et j'étudie leurs effets sur la formation des premiers solides. Dans un premier temps, je considère les effets de la photophorèse et des jets magnétiques sur le mouvement radial des grains dans les disques protoplanétaires. Le premier est dû aux effets thermiques du rayonnement stellaire sur la surface des grains, tandis que le deuxième est provoqué par les lignes de champ magnétique stellaire qui traversent le disque. Les résultats sont obtenus en résolvant les équations du mouvement des particules de façon numérique. Le transport induit par ces mécanismes a d'importantes conséquences pour la composition des météorites qui sont discutées dans le contexte de la nébuleuse solaire. Dans un deuxième temps, j'étudie la formation de pièges à particules causés par la présence de plusieurs planètes dans le disque grâce à des simulations hydrodynamiques. Ces résultats incluent la croissance des grains et sont directement comparés aux travaux similaires considérant une seule planète dans le disque. Le cas de l'étoile HD 100546, pour lequel les observations récentes suggèrent la présence de deux planètes dans le disque, est examiné en détail. L'évolution du disque en considérant différentes tailles de grain est étudiée au moyen de simulations hydrodynamiques SPH. Les distributions de la poussière et du gaz dans le disque sont particulièrement révélatrices car elles permettent de mettre à l'épreuve les différents scenarios proposés par les observations. L'étude de ces mécanismes montre que, selon leur taille et leur composition, les grains s'accumulent à différentes distances radiales dans le disque. Ces processus empêchent donc l'accrétion des solides par l'étoile et résolvent ainsi le problème de la barrière de dérive radiale. Les futures observations avec des instruments tels que ALMA, SPHERE et MATISSE permettront de mieux contraindre l'efficacité de ces mécanismes dans les disques protoplanétaires / The main goal of this work is to study new transport mechanisms of solids in protoplanetary disks and its implications for the composition of the first solids. The motion of solids inside the disk leads to the so-called radial-drift barrier caused by the gas aerodynamic drag, which is a severe problem for planet formation theory. In this context, it is hard to explain how sub-mm grains reach planetesimal sizes during the disk lifespan. First of all, I study the effects of photophoresis on the dust grains illuminated by the stellar radiation and quantify the efficiency of radial transport as a function of the particle properties. Then, I study the ejection of particles from the inner regions of the disk via the so-called stellar fountain model. Due to the stellar magnetic field which threads the disk, solid particles enter a jet that sends them outwards up to a few astronomical units. Both processes, photophoresis and jets, have important implications for the composition of meteorites which are discussed within the Solar Nebula scenario. In the last chapter, I study dust dynamics in multi-planetary systems through SPH simulations. The formation of particle traps in a disk with two planets is treated in detail and compared to previous work considering a single planet. Then I consider the case of HD 100546, a star with a disk which might harbor two planets according to recent observations, and study the disk evolution in different scenarios. By considering different grains sizes it is then possible to establish a link with interferometric observations of the system. We consider models with different planetary masses and radial distances in order to better constrain these quantities. The study of these mechanisms reveals that, according to particle size and composition, grains can pile up at different radial distances in the disk. This prevents the accretion by the central star by stopping the radial drift of solids, which shows that these mechanisms are good candidates to solve the radial-drift barrier. Future observations using ALMA, SPHERE and MATISSE will provide insights into the efficiency of these transport processes in protoplanetary disks

The dependence of the mass accretion rate on the stellar properties is a key constraint for star formation and disk evolution studies. Here we present a study of a sample of stars in the Chamaeleon I star-forming region carried out using spectra taken with the ESO VLT/X-shooter spectrograph. The sample is nearly complete down to stellar masses (M-star) similar to 0.1 M-circle dot for the young stars still harboring a disk in this region. We derive the stellar and accretion parameters using a self-consistent method to fit the broadband flux-calibrated medium resolution spectrum. The correlation between accretion luminosity to stellar luminosity, and of mass accretion rate to stellar mass in the logarithmic plane yields slopes of 1.9 +/- 0.1 and 2.3 +/- 0.3, respectively. These slopes and the accretion rates are consistent with previous results in various star-forming regions and with different theoretical frameworks. However, we find that a broken power-law fit, with a steeper slope for stellar luminosity lower than similar to 0.45 L-circle dot and for stellar masses lower than similar to 0.3 M-circle dot is slightly preferred according to different statistical tests, but the single power-law model is not excluded. The steeper relation for lower mass stars can be interpreted as a faster evolution in the past for accretion in disks around these objects, or as different accretion regimes in different stellar mass ranges. Finally, we find two regions on the mass accretion versus stellar mass plane that are empty of objects: one region at high mass accretion rates and low stellar masses, which is related to the steeper dependence of the two parameters we derived. The second region is located just above the observational limits imposed by chromospheric emission, at M-star similar to 0.3-0.4 M-circle dot. These are typical masses where photoevaporation is known to be effective. The mass accretion rates of this region are similar to 10(-10) M-circle dot/yr, which is compatible with the value expected for photoevaporation to rapidly dissipate the inner disk.

HD 141569 A is a pre-main sequence B9.5 Ve star surrounded by a prominent and complex circumstellar disk, likely still in a transition stage from protoplanetary to debris disk phase. Here, we present a new image of the third inner disk component of HD 141569 A made in the L' band (3.8 mu m) during the commissioning of the vector vortex coronagraph that has recently been installed in the near-infrared imager and spectrograph NIRC2 behind the W.M. Keck Observatory Keck II adaptive optics system. We used reference point-spread function subtraction, which reveals the innermost disk component from the inner working distance of similar or equal to 23 au and up to similar or equal to 70 au. The spatial scale of our detection roughly corresponds to the optical and near-infrared scattered light, thermal Q, N, and 8.6 mu m PAH emission reported earlier. We also see an outward progression in dust location from the L' band to the H band (Very Large Telescope/SPHERE image) to the visible (Hubble Space Telescope (HST)/STIS image), which is likely indicative of dust blowout. The warm disk component is nested deep inside the two outer belts imaged by HST-NICMOS in 1999 (at 406 and 245 au, respectively). We fit our new L'-band image and spectral energy distribution of HD 141569 A with the radiative transfer code MCFOST. Our best-fit models favor pure olivine grains and are consistent with the composition of the outer belts. While our image shows a putative very faint point-like clump or source embedded in the inner disk, we did not detect any true companion within the gap between the inner disk and the first outer ring, at a sensitivity of a few Jupiter masses.

Context. Accretion outbursts are key elements in star formation. ASASSN-13db is a M5-type star with a protoplanetary disk, the lowest-mass star known to experience accretion outbursts. Since its discovery in 2013, it has experienced two outbursts, the second of which started in November 2014 and lasted until February 2017. Aims. We explore the photometric and spectroscopic behavior of ASASSN-13db during the 2014-2017 outburst. Methods. We use high- and low-resolution spectroscopy and time-resolved photometry from the ASAS-SN survey, the LCOGT and the Beacon Observatory to study the light curve of ASASSN-13db and the dynamical and physical properties of the accretion flow. Results. The 2014-2017 outburst lasted for nearly 800 days. A 4.15 d period in the light curve likely corresponds to rotational modulation of a star with hot spot(s). The spectra show multiple emission lines with variable inverse P-Cygni profiles and a highly variable blue-shifted absorption below the continuum. Line ratios from metallic emission lines (Fe I/Fe II, Ti I/Ti II) suggest temperatures of similar to 5800-6000 K in the accretion flow. Conclusions. Photometrically and spectroscopically, the 2014-2017 event displays an intermediate behavior between EXors and FUors. The accretion rate (<(M)over dot> = 1-3 x 10(-7) M-circle dot/yr), about two orders of magnitude higher than the accretion rate in quiescence, is not significantly different from the accretion rate observed in 2013. The absorption features in the spectra suggest that the system is viewed at a high angle and drives a powerful, non-axisymmetric wind, maybe related to magnetic reconnection. The properties of ASASSN-13db suggest that temperatures lower than those for solar-type stars are needed for modeling accretion in very-low-mass systems. Finally, the rotational modulation during the outburst reveals that accretion-related structures settle after the beginning of the outburst and can be relatively stable and long-lived. Our work also demonstrates the power of time-resolved photometry and spectroscopy to explore the properties of variable and outbursting stars.

科学研究費補助金 研究種目:一般研究(C) 課題番号:05833001 研究代表者:渡邊 誠一郎 研究期間:1993-1994年度