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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
71

Multiple Disk Gaps and Rings Generated by a Single Super-Earth

Dong, Ruobing, Li, Shengtai, Chiang, Eugene, Li, Hui 13 July 2017 (has links)
We investigate the observational signatures of super-Earths (i.e., planets with. Earth-to-Neptune. mass), which are the most common type of exoplanet discovered to date, in their natal disks of gas and dust. Combining two-fluid global hydrodynamics simulations with a radiative transfer code, we calculate the distributions of gas and of submillimeter-sized dust in a disk perturbed by a super-Earth, synthesizing images in near-infrared scattered light and the millimeter-wave thermal continuum for direct comparison with observations. In low-viscosity gas (alpha (sic) 10(-4)), a super-Earth opens two annular gaps to either side of its orbit by the action of Lindblad torques. This double gap and its associated gas pressure gradients cause dust particles to be dragged by gas into three rings: one ring sandwiched between the two gaps, and two rings located at the gap edges farthest from the planet. Depending on the. system parameters, additional rings may manifest for a single planet. A double gap located at tens of au. from a host star in Taurus can be detected in the dust continuum by the Atacama Large Millimeter Array (ALMA) at an angular resolution of similar to 0".03 after two hours of integration. Ring and gap features persist in a variety of background disk profiles, last for thousands of orbits, and change their relative positions and dimensions depending on the speed and direction of planet migration. Candidate double gaps have been observed by ALMA in systems such as. HL Tau (D5 and D6) and TW Hya (at 37 and 43 au); we submit that each double gap is carved by one super-Earth in nearly inviscid gas.
72

Morphologie et évolution des tourbillons de Rossby bidimensionnels dans les disques protoplanétaires / Structure and evolution of 2D Rossby vortices in protoplanetary disks

Surville, Clément 11 December 2013 (has links)
Le rôle des tourbillons anticycloniques dans l'évolution des disques protoplanétaires et, en particulier, dans les mécanismes de formation des planétésimaux, est au coeur des défis actuels de l'astrophysique moderne. C'est pourquoi une étude approfondie de leur structure et de leur dynamique est primordiale.Grâce à un outil numérique spécifiquement développé pour l'étude des disques, nous avons revisité l'Instabilité en Ondes de Rossby dans le régime non linéaire, et découvert l'existence d'une cascade des modes de perturbation qui permet de mieux comprendre la formation des tourbillons par cette instabilité.Leur structure à été décrite par un modèle gaussien innovant, remarquablement en accord avec les résultats numériques. Grâce à un échantillon de près de 300 tourbillons, nous avons borné le domaine des dimensions radiales, azimutales et de la vorticité. Deux familles de tourbillons possibles ont été distinguées : (i) les tourbillons incompressibles, stables et quasi-stationnaires; (ii) les tourbillons compressibles, très mobiles et associés à l'émission d'ondes de densité. Leur persistance sur plus de 1000 rotations confirme l'observabilité de tous ces tourbillons. Enfin, nous avons caractérisé leur migration vers l'étoile en fonction de leur géométrie, du gradient de pression et de l'échelle de hauteur du disque. Pour la première fois, une expression analytique permet d'estimer le taux de migration en fonction de ces paramètres; l'échelle de temps pour tomber sur étoile peut aller de 10^6 à 100 rotations. Suivant un modèle de viscosité alpha, la perte de moment cinétique pourrait être suffisante pour maintenir un taux d'accrétion significatif dans la zone morte. / The role of anticyclonic vortices in the protoplanetary disk evolution and in how do planetesimals form are among the most important chalenges of the modern astrophysics. That is why an exhaustive study of the structure and the evolution of these vortices is necessary.Thanks to a numerical code specificly designed for the study of these disks, we have revisited the Rossby Wave Instability in the nonlinear regime, and have discovered that a cascade of the perturbation modes can explain the formation of the vortices created by this instability.We have described the structure of these Rossby vortices with a new gaussian vortex model, which accurately fits the numerical results. A sample of 300 different vortices led us to define the bondaries of the radial and azimuthal extent as well as the vorticity of the vortices. We have distinguished two main families : (i) the incompressible family, which is stable and quasi stationnary ; (ii) the compressible family, moving and exciting density waves. We found them surviving more than 1000 orbits, a clear confirmation of their observability.Finaly, we have caracterized the inward migration of the vortices as a fonction of their shape, their vorticity, but also of the pressure gradient and the scale height of the disk. For the first time, we exhibit a equation relating the migration rate to these parameters. The time scale of the migration ranges from 10^6 to just 100 rotations of the disk. Extremely steep pressure gradients are needed to reverse the migration to an outward regime. Following the alpha viscosity approch, the loss of kinetic momentum due to this migration would be sufficient to sustain the accretion in the dead zone.
73

PANCHROMATIC IMAGING OF A TRANSITIONAL DISK: THE DISK OF GM AUR IN OPTICAL AND FUV SCATTERED LIGHT

Hornbeck, J. B., Swearingen, J. R., Grady, C. A., Williger, G. M., Brown, A., Sitko, M. L., Wisniewski, J. P., Perrin, M. D., Lauroesch, J. T., Schneider, G., Apai, D., Brittain, S., Brown, J. M., Champney, E. H., Hamaguchi, K., Henning, Th., Lynch, D. K., Petre, R., Russell, R. W., Walter, F. M., Woodgate, B. 22 September 2016 (has links)
We have imaged GM Aurigae with the Hubble Space Telescope, detected its disk in scattered light at 1400 and 1650 angstrom, and compared these with observations at 3300 angstrom, 5550 angstrom, 1.1 mu m, and 1.6 mu m. The scattered light increases at shorter wavelengths. The radial surface brightness profile at 3300 angstrom shows no evidence of the 24 au radius cavity that has been previously observed in submillimeter observations. Comparison with dust grain opacity models indicates that. the surface of the entire disk is populated with submicron grains. We have compiled a. spectral energy distribution from 0.1 mu m to 1 mm. and used it to constrain a model of the star + disk system that includes the submillimeter cavity using the Monte Carlo radiative transfer code by Barbara Whitney. The best-fit model image indicates that the cavity should be detectable in the F330W bandpass if the cavity has been cleared of both large and small dust grains, but we do not detect it. The lack of an observed cavity can be explained by the presence of submicron grains interior to the submillimeter cavity wall. We suggest one explanation for this that. could be due to a planet of mass <9 M-J interior to 24 au. A unique cylindrical structure is detected in the far-UV data from the Advanced Camera for Surveys/ Solar Blind Channel. It is aligned along the system semiminor axis, but does not resemble an accretion-driven jet. The structure is limb. brightened and extends 190 +/- 35 au above the disk midplane. The inner radius of the limb. brightening is 40 +/- 10 au, just beyond the submillimeter cavity wall.
74

Planet Traps in Protoplanetary Disks and the Formation and Evolution of Planetary Systems

Hasegawa, Yasuhiro 10 1900 (has links)
<p>One of the most fundamental problems in theories of planet formation in protoplanetary disks is planetary migration that arises from resonant, tidal interactions of forming planets with the natal disks. This rapid inward migration, also known as type I migration, leads to the well-known problem that its timescale is about two orders of magnitude shorter than the typical disk lifetime, so that (proto)planets plunge into the host stars within the disk lifetime. This provides a huge hurdle for understanding the statistical properties of observed extra solar planets that now amount to more than 700.</p> <p>In this thesis, we focus on one of the most general properties of protoplanetary disks - inhomogeneities. A large amount of theoretical and observational work currently suggests that protoplanetary disks are most likely to possess several kinds of inhomogeneities. Planetary migration is highly sensitive to the disk properties such as the surface density and temperature of disks, and the sensitivity leads to the formation of trapping sites for rapid type I migration at disk inhomogeneities. These local sites capturing planets undergoing migration are referred to as planet traps. We perform both analytical and numerical studies for exploring formation mechanisms of planet traps at disk inhomogeneities and their consequences for the formation and evolution of planetary systems. We focus on three kinds of the disk inhomogeneities: dead zones, ice lines, and transitions of heat sources in protoplanetary disks we refer to as heat transitions. Dead zones are an inevitable consequence of disk turbulence originating from magnetorotational instabilities (MRIs) that take place in (partially) ionized disks threaded by weak magnetic fields. One of the fundamental properties of the dead zone is a low level of turbulence there, which is the outcome of the high density, preventing the region from being ionized due to X-rays from the central stars and cosmic rays. Ice lines are formed due to low disk temperatures which lead to condensation of specific molecules there. Heat transitions arise as a consequence of the switching of the dominant heating process from viscous heating to stellar irradiation as the distance to the host stars increases.</p> <p>We summarize our major findings. 1) rapid dust settling arising in dead zones leaves a dusty wall at the outer edge of the dead zones beyond which the disks are quite turbulent, so that dust is fully mixed with the gas. Efficient heating of the wall by stellar irradiation and the subsequent backward heating of the dead zones by the wall result in a positive temperature gradient in the dead zones. This inversion in the temperature profiles leads to outward migration there. 2) Any protoplanetary disk is likely to possess up to three types of planet traps that are specified by characteristic disk radii (dead zone, ice line and heat transition traps). Disk evolution, driven by disk viscosity, lowers both the accretion rate and surface density of gas and moves traps inward at different rates. This suggests that the interactions of (proto)planets captured at different traps play the dominant role in constructing planetary system architectures. Furthermore, the distribution of planet traps depends largely on stellar masses and accretion rates, so that they are one of the principle parameters for regulating the (initial) scale of planetary systems. 3) Both multiplicity and mobility of planet traps are crucial for understanding the statistical properties of observed extra solar planets. For instance, the mass-period relation - observational manifestation that planetary mass is an increasing function of orbital periods - can be understood by constructing and following evolutionary tracks of accreting planets in planet traps. These three contribution are new results in the field.</p> / Doctor of Philosophy (PhD)
75

Environnements stellaire : des étoiles lambda Boötis aux disques protoplanétaires

Gonzalez, Jean-François 03 June 2005 (has links) (PDF)
J'ai effectué une étude des éléments C, N, et O dans les atmosphères d'étoiles chimiquement particulières de la séquence principale, où ils sont sous-abondants et répartis de manière inhomogène. J'ai recensé les processus physiques qu'il faut inclure dans les calculs d'accélération radiative et montré leur importance relative. Des améliorations majeures par rapport aux approximations usuelles ont été obtenues grâce à l'utilisation systématique des données atomiques du projet OPACITY. Elles permettent de calculer précisément la dépendance en fréquence des opacités, et d'améliorer l'évaluation des largeurs de raies. Les contributions des raies et de la photoionisation sont calculées pour chaque ion et l'accélération totale sur un élément donné est obtenue grâce à un modèle prenant en compte les réactions rapides entre ions. Les accélérations radiatives calculées pour le carbone, l'azote, et l'oxygène, les poussant vers le haut, apparaissent inférieures à la gravité dans tous les modèles d'enveloppe considérés (étoiles de type A à F), pour une large gamme de paramètres, expliquant leurs déficits marquées à la surface de la plupart des étoiles chimiquement particulières. Des tables donnant d'une part l'opacité de ces éléments, d'autre part leur accélération radiative sur une grille contenant de nombreuses conditions de plasma permettent d'effectuer des calculs d'évolution stellaire prenant en compte tous les aspects de la diffusion des éléments C, N, et O, les plus abondants après H et He. <br /> <br />Je me suis ensuite intéressé aux étoiles de type lambda Bootis, un petit sous-groupe singulier d'étoiles chimiquement particulières, dont les anomalies d'abondance ne sont pas expliquées par le modèle de la diffusion radiative. Il s'agirait plutôt d'étoiles jeunes, encore entourées des restes du disque à partir duquel elles se sont formées, et dont elles accrèteraient un gaz appauvri en éléments lourds, ceux-ci s'étant condensés en grains. Afin de vérifier cette hypothèse, nous avons recherché la signature de matière circumstellaire dans le spectre de ces étoiles. Peu d'étoiles de notre échantillon montrent un tel indice et nos résultats suggèrent une anti-corrélation entre la présence de gaz ou de poussières, pouvant caractériser deux états différents dans l'évolution du disque protostellaire. Au cours de cette étude, nous avons découvert par hasard le premier cas de pulsations non radiales dans une étoile de type lambda Bootis, puis montré qu'elles sont communes dans ce groupe. L'identification des modes de pulsation permet de remonter à la structure interne de ces étoiles et à leur état d'évolution, permettant ainsi de tester le modèle d'accrétion. <br /> <br />Mon étude des environnements circumstellaires des étoiles lambda Bootis m'a conduit à m'intéresser aux disques protoplanétaires. Jusqu'à récemment, nous n'avions observé qu'un seul système solaire (le nôtre) dans lequel nous pouvions tester notre compréhension du processus de formation de planètes. Maintenant, plus d'une centaine de planètes ont été découvertes autour d'autres étoiles et les contraintes sur les modèles théoriques sont devenues très serrées. Nous savons que, dans la nébuleuse solaire, les particules de poussière de la taille du micron se sont agglomérées pour former des planètes, objets 10^13 à 10^14 fois plus grands. Bien qu'il y ait beaucoup de travail réalisé sur les dernières étapes de cette formation, et sur la migration de planètes déjà formées, peu de travail a été fait pour développer des modèles hydrodynamiques décrivant l'interaction du gaz et de la poussière dans les disques proto-planétaires. Nous développons un code hydrodynamique SPH permettant de modéliser cette interaction, principalement par la force de friction, entre deux phases: du gaz et des grains de poussière d'une taille donnée. Nous obtenons ainsi la répartition spatiale des grains dans le disque en fonction de leur taille. Ce travail correspond à la thèse de Laure Barrière-Fouchet, qui se termine en 2005. Nous projetons ensuite d'ajouter les mécanismes de coagulation, croissance, et évaporation des grains de poussière en modélisant plusieurs phases pour différentes tailles de grains et la variation du nombre de particules dans chaque phase qui en résulte. Ceci permettra de caractériser les zones du disque les plus favorables à la formation de planétésimaux. Ensuite, il s'agira d'explorer plus profondément les mécanismes de formation de planètes. En effet, si l'on arrive assez bien à faire croître les grains microscopiques jusqu'à une taille de l'ordre du centimètre, les collisions entre ces gros grains les refragmentent et empêchent de dépasser cette taille. Plusieurs solutions sont à envisager pour permettre de passer ce cap: diminution des vitesses de collisions dans les régions plus denses, rôle de la turbulence, etc... <br /> <br />Un peu à part de mes travaux précédents, avec mes collègues de l'ESO, j'ai observé et pris le premier spectre de la contrepartie optique du sursaut gamma GRB980425, qui s'est avéré être une supernova très particulière: SN1998bw. Son spectre en évolution rapide ne permettait pas de classer cette supernova, la première à être associée à un sursaut gamma, dans les types connus. Notre équipe a suivi régulièrement l'évolution de sa courbe de lumière et de son spectre, la somme de données recueillie ayant conduit à un modèle d'hypernova.
76

The Sizes and Depletions of the Dust and Gas Cavities in the Transitional Disk J160421.7-213028

Dong, Ruobing, Marel, Nienke van der, Hashimoto, Jun, Chiang, Eugene, Akiyama, Eiji, Liu, Hauyu Baobab, Muto, Takayuki, Knapp, Gillian R., Tsukagoshi, Takashi, Brown, Joanna, Bruderer, Simon, Koyamatsu, Shin, Kudo, Tomoyuki, Ohashi, Nagayoshi, Rich, Evan, Satoshi, Mayama, Takami, Michihiro, Wisniewski, John, Yang, Yi, Zhu, Zhaohuan, Tamura, Motohide 21 February 2017 (has links)
We report ALMA Cycle 2 observations of 230 GHz (1.3 mm) dust continuum emission, and (CO)-C-12, (CO)-C-13, and (CO)-O-18 J = 2-1 line emission, from the Upper Scorpius transitional disk [PZ99] J160421.7-213028, with an angular resolution of similar to 0''.25 (35 au). Armed with these data and existing H-band scattered light observations, we measure the size and depth of the disk's central cavity, and the sharpness of its outer edge, in three components: sub-mu m-sized "small" dust traced by scattered light, millimeter-sized "big" dust traced by the millimeter continuum, and gas traced by line emission. Both dust populations feature a cavity of radius similar to 70 au that is depleted by factors of at least 1000 relative to the dust density just outside. The millimeter continuum data are well explained by a cavity with a sharp edge. Scattered light observations can be fitted with a cavity in small dust that has either a sharp edge at 60 au, or an edge that transitions smoothly over an annular width of 10 au near 60 au. In gas, the data are consistent with a cavity that is smaller, about 15 au in radius, and whose surface density at 15 au is 10(3 +/- 1) times smaller than the surface density at 70 au; the gas density grades smoothly between these two radii. The CO isotopologue observations rule out a sharp drop in gas surface density at 30 au or a double-drop model, as found by previous modeling. Future observations are needed to assess the nature of these gas and dust cavities (e.g., whether they are opened by multiple as-yet-unseen planets or photoevaporation).
77

What is the Mass of a Gap-opening Planet?

Dong, Ruobing, Fung, Jeffrey 24 January 2017 (has links)
High-contrast imaging instruments such as GPI and SPHERE are discovering gap structures in protoplanetary disks at an ever faster pace. Some of these gaps may be opened by planets forming in the disks. In order to constrain planet formation models using disk observations, it is crucial to find a robust way to quantitatively back out the properties of the gap-opening planets, in particular their masses, from the observed gap properties, such as their depths and widths. Combining 2D and 3D hydrodynamics simulations with 3D radiative transfer simulations, we investigate the morphology of planet-opened gaps in near-infrared scattered-light images. Quantitatively, we obtain correlations that directly link intrinsic gap depths and widths in the gas surface density to observed depths and widths in images of disks at modest inclinations under finite angular resolution. Subsequently, the properties of the surface density gaps enable us to derive the disk scale height at the location of the gap h, and to constrain the quantity M-p(2)/alpha, where Mp is the mass of the gap-opening planet and a characterizes the viscosity in the gap. As examples, we examine the gaps recently imaged by VLT/SPHERE, Gemini/GPI, and Subaru/HiCIAO in HD 97048, TW Hya, HD 169142, LkCa. 15, and RX J1615.3-3255. Scale heights of the disks and possible masses of the gap-opening planets are derived assuming each gap is opened by a single planet. Assuming a = 10(-3), the derived planet masses in all cases are roughly between 0.1 and 1M(J).
78

Revolution evolution : tracing angular momentum during star and planetary system formation

Davies, Claire L. January 2015 (has links)
Stars form via the gravitational collapse of molecular clouds during which time the protostellar object contracts by over seven orders of magnitude. If all the angular momentum present in the natal cloud was conserved during collapse, stars would approach rotational velocities rapid enough to tear themselves apart within just a few Myr. In contrast to this, observations of pre-main sequence rotation rates are relatively slow (∼ 1 − 15 days) indicating that significant quantities of angular momentum must be removed from the star. I use observations of fully convective pre-main sequence stars in two well-studied, nearby regions of star formation (namely the Orion Nebula Cluster and Taurus-Auriga) to determine the removal rate of stellar angular momentum. I find the accretion disc-hosting stars to be rotating at a slower rate and contain less specific angular momentum than the disc-less stars. I interpret this as indicating a period of accretion disc-regulated angular momentum evolution followed by near-constant rotational evolution following disc dispersal. Furthermore, assuming that the age spread inferred from the Hertzsprung-Russell diagram constructed for the star forming region is real, I find that the removal rate of angular momentum during the accretion-disc hosting phase to be more rapid than that expected from simple disc-locking theory whereby contraction occurs at a fixed rotation period. This indicates a more efficient process of angular momentum removal must operate, most likely in the form of an accretion-driven stellar wind or outflow emanating from the star-disc interaction. The initial circumstellar envelope that surrounds a protostellar object during the earliest stages of star formation is rotationally flattened into a disc as the star contracts. An effective viscosity, present within the disc, enables the disc to evolve: mass accretes inwards through the disc and onto the star while momentum migrates outwards, forcing the outer regions of the disc to expand. I used spatially resolved submillimetre detections of the dust and gas components of protoplanetary discs, gathered from the literature, to measure the radial extent of discs around low-mass pre-main sequence stars of ∼ 1−10 Myr and probe their viscous evolution. I find no clear observational evidence for the radial expansion of the dust component. However, I find tentative evidence for the expansion ofthe gas component. This suggests that the evolution of the gas and dust components of protoplanetary discs are likely governed by different astrophysical processes. Observations of jets and outflows emanating from protostars and pre-main sequence stars highlight that it may also be possible to remove angular momentum from the circumstellar material. Using the sample of spatially resolved protoplanetary discs, I find no evidence for angular momentum removal during disc evolution. I also use the spatially resolved debris discs from the Submillimetre Common-User Bolometer Array-2 Observations of Nearby Stars survey to constrain the amount of angular momentum retained within planetary systems. This sample is compared to the protoplanetary disc angular momenta and to the angular momentum contained within pre-stellar cores. I find that significant quantities of angular momentum must be removed during disc formation and disc dispersal. This likely occurs via magnetic braking during the formation of the disc, via the launching of a disc or photo-evaporative wind, and/or via ejection of planetary material following dynamical interactions.
79

Imagerie de l'environnement protoplanétaire des étoiles jeunes par interférométrie optique / Imaging the protoplanetary environment of young stellar objects by optical interferometry

Kluska, Jacques 06 October 2014 (has links)
Une manière efficace de contraindre la formation des planètes est l'étude des disques protoplanétaires. Les premières images de ces disques ont été obtenues dans les années 80 en infrarouge et en millimétrique. Ces images dévoilaient pour la première fois la morphologie de l'excès infrarouge vu dans les distributions spectrales d'énergies des étoiles jeunes. Depuis, de nets progrès ont été faits et, outre la détection directe de planètes, nous sommes capables de distinguer les perturbations que celles-ci pourraient engendrer dans ces disques. La région interne de ces disques, où la majorité des planètes sont détectées, est complexe car étant le théâtre de nombreux phénomènes encore mal contraints (sublimation de la poussière, vents, accrétion). Pour les étoiles jeunes les plus proches, observer ces régions revient à atteindre une résolution angulaire de l'ordre de la milliseconde d'arc, inatteignable avec un télescope monolithique. L'interférométrie optique permet de satisfaire cette contrainte. Cette technique consiste à combiner la lumière de deux télescopes ou plus afin de la faire interférer. Ces interférences permettent de contraindre la morphologie de l'objet observé à l'aide de modèles. Mais afin de comprendre les phénomènes en jeu il est nécessaire d'avoir une image indépendante de ces modèles. La reconstruction d'images est possible avec l'avènement récent d'interféromètres à 4 télescopes ou plus. Les premières images ont ainsi pu être reconstruites. Cependant, l'étoile centrale ne permet pas d'accéder facilement à l'image de l'environnement. Ma thèse a donc consisté à outrepasser cette difficulté en développant une méthode de reconstruction d'image adaptée à l'environnement protoplanétaire des étoiles jeunes. Elle consiste à séparer l'étoile centrale de l'image afin de reconstruire son environnement tout en prenant en compte la différence de température entre ces deux éléments. Grâce à cette méthode et aux instruments interférométriques du VLTI, j'ai pu reconstruire les images des premières unités astronomiques d'une douzaine d'étoiles de Herbig et de révéler leurs morphologies. J'ai ainsi pu appliquer une analyse géométrique originale afin de les caractériser. Enfin, j'ai analysé plus en détail un étoile particulière, MWC158, dont j'ai imagé la variabilité qui pourrait être interprétée comme une éjection de matière. Ma thèse démontre l'importance de la prise en compte des aspects chromatiques dans la reconstruction d'image ainsi que de l'adaptation de cette méthode à la spécificité des étoiles jeunes. / An effective way to understand the formation of planets is the study of protoplanetary disks. The first images of these disks were obtained in the infrared and the millimeter in the 80s. These images unveiled for the first time the morphology of the infrared excess seen in the spectral energy distributions of young stellar objects. Since then, significant progress has been made and, in addition to the direct detection of planets, we are able to distinguish the disruption they could cause in these disks. The inner region of these disks, where the majority of planets are found, is complex as being the scene of many phenomena still poorly constrained (dust sublimation, winds, accretion). For the closest young stars, observing these regions amounts to achieve an angular resolution of the order of a milliarcsecond, unattainable with monolithic telescopes. The optical interferometry can reach such a small angle. This technique consists in combining the light of two or more telescopes to make it interfere. These interferences can be used to constrain the morphology of the observed object by using models. But to understand the phenomena involved in the inner parts of young stellar objects, it is necessary to have an independent image. Image reconstruction is possible with the recent advent of interferometers with 4 or more telescopes. The first images were able to be rebuilt. However, the central star does not allow easy access to the environment morphology. The goal of my thesis was to bypass this difficulty by developing a method of image reconstruction which is adapted to the protoplanetary environment of young stars. It consists in separating the central star of the image to reconstruct its environment while taking into account the temperature difference between the two. With this method and the VLTI interferometric instruments, I reconstructed the images of the first astronomical unit of a dozen of Herbig stars and revealed their morphologies. I was able to apply a novel geometric analysis to characterize them. Finally, I have analyzed in more detail a particular star, MWC158, which I imaged the variability that could be interpreted as a matter ejection. My thesis demonstrates the importance of the inclusion of chromatic aspects in image reconstruction and adaptation of this method to the specific characteristics of young stars.
80

Effet de la structure du disque sur la formation et la migration des planètes / Effect of the disc structure on planets formation and migration

Cossou, Christophe 28 November 2013 (has links)
Au delà du système solaire et de ses planètes, nous avons maintenant un catalogue de quasiment 1000 exoplanètes qui illustrent la grande diversité des planètes et des systèmes qu'il est possible de former. Cette diversité est un défi que les modèles de formation planétaire tentent de relever. La migration de type 1 est un des mécanismes pour y parvenir. En fonction des propriétés du disque protoplanétaire, les planètes peuvent s'approcher ou s'éloigner de leur étoile. La grande variété des modèles de disques protoplanétaires permet d'obtenir une grande variété de systèmes planétaires, en accord avec la grande diversité que nous observons déjà pour l'échantillon limité qui nous est accessible. Grâce à des simulations numériques, j'ai pu montrer qu'au sein d'un même disque, il est possible de former des super-Terres ou des noyaux de planètes géantes selon l'histoire de migration d'une population d'embryons. / In addition to the Solar System and its planets, we now have a database of nearly 1000 planets that emphasize the huge diversity of planets and systems that can be formed. This diversity is a challenge for planetary formation models. Type I migration is one of the mechanisms possible to explain this diversity. Depending on disc properties, planets can migrate inward or outward with respect to their host star. The huge parameter space of protoplanetary disc models can form a huge diversity of planetary systems, in agreement with the diversity observed in the nonetheless small sample accessible to us. Thanks to numerical simulations, I showed that within the same disc, it is possible to form super-Earths or giant planet cores, depending on the migration history of an initial population of embryos.

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