In this licentiate thesis, I consider debris disks from an observational, astronomical viewpoint, but also discuss a potential astrobiological application. Debris disks are essentially disks of dust and rocks around main-sequence stars, analogue to the Kuiper- or the asteroid belt in our solar system. Their observation and theoretical modeling can help to constrain planet formation models and help in the understanding of the history of the solar system. After a general introduction into the field of debris disks and some basic debris disk physics, the thesis concentrates on the observation of gas in debris disks. The possible origins of this gas and its dynamics are discussed and it is considered what it can tell us about the physical conditions in the disk and possibly about the dust composition. In this way, the paper associated with this thesis (dealing with the gas in the β Pic debris disk) is set into context. More in detail, we observed the CII emission originating from the carbon-rich β Pic disk with Herschel HIFI and attempted to constrain the spatial distribution of the gas from the shape of the emission line. This is necessary since the gas production mechanism is currently unknown, but can be constraint by obtaining information about the spatial profile of the gas. The last part of the thesis describes our preliminary studies of the possibility of a debris disk containing biomarkers, created by a giant impact on a life-bearing exoplanet.

Thanks to a range of discovery methods that are sensitive to different regions of parameter space, we now know of over 900 planets in over 700 planetary systems. This large population has allowed exoplanetary scientists to move away from a focus on simple discovery, and towards efforts to study the bigger pictures of planetary system formation and evolution. The interactions between planets and their host stars have proven to be varied in both mechanisms and scope. In particular, tidal interactions seem to affect both the physical and dynamical properties of planetary systems, but characterising the broader implications of this has proven challenging. In this thesis I present work that investigates different aspects of tidal interactions, in order to uncover the scope of their influence of planetary system evolution. I compare two different age calculation methods using a large sample of exoplanet and brown dwarf host stars, and find a tendency for stellar model fitting to supply older age estimates than gyrochronology, the evaluation of a star's age through its rotation (Barnes 2007). Investigating possible sources of this discrepancy suggests that angular momentum exchange through the action of tidal forces might be the cause. I then select two systems from my sample, and investigate the effect of tidal interactions on their planetary orbits and stellar spin using a forward integration scheme. By fitting the resulting evolutionary tracks to the observed eccentricity, semi-major axis and stellar rotation rate, and to the stellar age derived from isochronal fitting, I am able to place constraints on tidal dissipation in these systems. I find that the majority of evolutionary histories consistent with my results imply that the stars have been spun up through tidal interactions as the planets spiral towards their Roche limits. I also consider the influence of tidal interactions on the alignment between planetary orbits and stellar spin, presenting new measurements of the projected spin-orbit alignment angle, λ, for six hot Jupiters. I consider my results in the context of the full ensemble of measurements, and find that they support a previously identified trend in alignment angle with tidal timescale, implying that tidal realignment might be responsible for patterns observed in the λ distribution.

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.

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.

The current paradigm in planet formation theory is developed around a hierarquical growth of solid bodies, from interstellar dust grains to rocky planetary cores. A particularly difficult phase in the process is the growth from meter-size boulders to planetary embryos of the size of our Moon or Mars. Objects of this size are expected to drift extremely rapid in a protoplanetary disk, so that they would generally fall into the central star well before larger bodies can form. In this thesis, we used numerical simulations to find a physical mechanism that may retain solids in some parts of protoplanetary disks long enough to allow for the formation of planetary embryos. We found that such accumulation can happen at the borders of so-called dead zones. These dead zones would be regions where the coupling to the ambient magnetic field is weaker and the turbulence is less strong, or maybe even absent in some cases. We show by hydrodynamical simulations that material accumulating between the turbulent active and dead regions would be trapped into vortices to effectively form planetary embryos of Moon to Mars mass. We also show that in disks that already formed a giant planet, solid matter accumulates on the edges of the gap the planet carves, as well as at the stable Lagrangian points. The concentration is strong enough for the solids to clump together and form smaller, rocky planets like Earth. Outside our solar system, some gas giant planets have been detected in the habitable zone of their stars. Their wakes may harbour rocky, Earth-size worlds.

ν Octantis is a spectroscopic binary with a semi-major axis and period of 2.55 AU and 2.9 years, respectively. Ramm et al. (2009) discovered a 52 ms^(-1) radial-velocity (RV) perturbation with a period of 417 days in this system. All evidence, both photometric and spectroscopic, suggests the perturbation is the result of a 2.5 MJ planet orbiting the primary star. However, when assuming a “normal” prograde coplanar orbit, celestial mechanics predicts this orbit is unstable, contradicting the observed stability. Simulations by Eberle and Cuntz (2010) showed a retrograde orbit for the planet to be stable for at least 10^7 years. In this thesis, we performed a 10^8 -yr simulation of the retrograde orbit, and found it remained stable. Simulations over a range of planetary semi-major axes, eccentricities, and primary/secondary masses showed that stable retrograde orbits are not possible past a semi-major axis of 1.315 +/- 0.092 AU . Therefore, planetary retrograde orbits are most likely inherently more stable than prograde orbits owing to the absence of stability at known mean-motion resonances. Eccentricity simulations showed that the period of the planet's dominant eccentricity variation is related to the planet's semi-major axis by a second order exponential. However, retrograde orbits tend to have longer eccentricity periods than prograde orbits at the same semi-major axis. There is also evidence that this eccentricity period is connected to the orbital stability. By fitting a keplerian to both Ramm et al. (2009) and current radial velocities, the period of the ν Octantis binary was determined to be 1050.04 +/- 0.02 days with an eccentricity of 0.2359 +/- 0.001 . The planetary orbital solution for just the data reduced in this thesis gave a period of 416.9 +/- 2.1 days and an eccentricity of 0.099 +/- 0.015 , with an RMS scatter of 9.6 ms^(-1). Therefore, the orbital elements are within 1σ of the Ramm et al. (2009) elements. Assuming a retrograde coplanar orbit about the primary star then the planet has a mass of M_pl = 2.3 M_J and a semi-major axis of a_pl = 1.21 +/- 0.09 AU.

Les disques de débris orbitant dans l'environnement des étoiles proches constituent un indicateur très important des propriétés des systèmes planétaires extra-solaires. Depuis l'espace et au sol, les moyens observationnels actuels permettent de déterminer dans divers domaines de longueurs d'ondes les propriétés spatiales de ces disques et celles des grains de poussières circumstellaires. Cette thèse aborde le sujet de la modélisation des disques de débris, à partir de données fournies par de multiples instruments, en premier lieu les télescopes spatiaux Hubble et Herschel, et les interféromètres infrarouges du VLTI, CHARA, et KIN. Mes premiers projets ont pris place dans le cadre de deux programmes-clés de l'Observatoire Spatial Herschel dédiés à l'étude des disques circumstellaires autour des étoiles proches. Au sein du projet GASPS, j'ai obtenu des observations spectro-photométriques de HD 181327, une jeune étoile (12+8-4 millions d'années, Ma) de type solaire entourée d'un anneau de débris massif de 90 unités astronomique (UA) de rayon vu aussi en lumière diffusée par le télescope spatial Hubble. La bonne détermination de la géométrie de l'anneau permet de se concentrer sur la modélisation de la distribution spectrale d'énergie, afin de mieux caractériser les propriétés des poussières. J'ai utilisé le code de transfert radiatif GRaTer et démontré que le système héberge une population de planétésimaux glacés, qui pourrait représenter une source d'eau et de volatils susceptible d'être libérée sur des planètes telluriques encore en formation. Je discute quelques résultats additionnels obtenus avec Herschel à propos de disques de débris jeunes, notamment HD 32297, et d'analogues faibles de la Ceinture de Kuiper. Les disques exo-zodiacaux (exozodis), analogues du nuage Zodiacal du Système Solaire, représentent une contrepartie chaude (ou tiède) aux disques de débris, résidant proche de la zone habitable (moins de quelques unités astronomiques) et encore mal connue. Ils sont révélés par leur émission proche et moyen infrarouge et peuvent être étudiés avec la précision et la résolution requises grace à l'interférométrie optique. Dans le cas de l'étoile Beta Pictoris (12+8-4 Ma), dont le disque est vu par la tranche, une fraction significative du disque externe diffuse de la lumière vers le champ de vue des interféromètres ; une composante interne chaude doit tout de même être invoquée pour justifier de l'excès mesuré dans l'infrarouge proche. En m'appuyant sur l'exemple de l'étoile Véga (440±40 Ma), je présente la méthodologie employée et démontre que les exozodis chauds se caractérisent par une abondance de poussières sub-microniques, près de la distance de sublimation de l'étoile. D'un point de vue théorique, le mécanisme de production de ces petits grains non-liés est encore incompris. J'aborde plus en détails le cas du disque exozodiacal à deux composantes (chaude et tiède) de Fomalhaut (440±40 Ma). Je développe une nouvelle méthode de calcul des distances de sublimation et recense les processus variés qui peuvent affecter un grain de poussière afin de fournir un cadre pour l'interprétation : l'exozodi chaud à ~0.1 - 0.2 UA serait la signature indirecte d'une ceinture d'astéroïdes située à 2 UA à l'activité dynamique particulièrement intense. Finalement, je dresse un bilan des propriétés des disques de débris et de ce qu'ils peuvent nous apprendre quand on les compare au Système Solaire, et propose de futures directions de recherche pour explorer davantage les systèmes planétaires et leur dynamique. / Debris disks orbiting in the environment of nearby stars are a very important indicator of extrasolar planetary systems properties. From space and from the ground, current observational facilities enable a multi-wavelength determination of the disks structures and of the dust properties. This thesis addresses the topic of debris disks modelling, based on data from multiple instruments including first of all the Herschel and Hubble space telescopes, and the VLTI, CHARA and KIN infrared interferometers. My first research pro jects took place in the framework of two key programs from the Herschel Space Observatory dedicated to the study of circumstellar disks around nearby stars. As part of the GASPS pro ject, I obtained Herschel far-infrared spectro-photometric observations of HD 181327, a young (12+8−4 Myr) Sun-like star surrounded by a massive, 90 AU-wide debris belt, also imaged in scattered light by the Hubble Space Telescope. Proper determination of the belt geometry allows one to focus on modelling the dust properties. I used the GRaTer radiative transfer code to demonstrate that the system hosts a population of icy planetesimals that may be a source for the future delivery of water and volatiles onto forming terrestrial planets. I discuss additional results obtained with Herschel related to young debris disks, in particular HD 32297, and to faint Kuiper-Belt analogues. Exo-zodiacal disks (exozodis), those analogues to the Solar System Zodiacal cloud, represent a little known hot (or warm) counterpart of debris disks located close the habitable zone (inside of a few AUs). They are revealed by their near- to mid-infrared emission and can be assessed with the required accuracy and resolution with optical interferometers. In the case of the near edge-on star β Pictoris (12+8−4 Myr), I show that a significant fraction of the outer disk scatters light towards the small field-of-view of the interferometers; an inner hot component must nonetheless be invoked to explain the measured near-infrared excess. Based on the example of the star Vega (440 ± 40 Myr), I introduce a methodology to study inner dust disks and I show that hot exozodis are characterized by an abundance of submicron-sized grains, close to the star sublimation distance. From a theoretical point-of-view, the production mechanism for these small, unbound grains is not understood. I go into more details on the case of the Fomalhaut (440 ± 40 Ma) double-component (warm and hot) exozodiacal disk. I develop a new model for the calculation of the dust sublimation distances, and I address the various processes that can affect a dust grain in order to provide a framework for interpreting the exozodi: the hot exozodiacal disk may be the indirect signature of an asteroid belt with a particularly high dynamical activity. Lastly I draw up a summary of the properties of dusty debris disks and of what they can teach us when compared to the Solar System. I propose possible future research directions for further investigations of planetary systems and their dynamics.

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.

The past decade has seen significant progress on the direct detection and characterization of young, self-luminous giant planets at wide orbital separations from their host stars. Some of these planets show evidence for disequilibrium processes like transport-induced quenching in their atmospheres; photochemistry may also be important, despite the large orbital distances. These disequilibrium chemical processes can alter the expected composition, spectral behavior, thermal structure, and cooling history of the planets, and can potentially confuse determinations of bulk elemental ratios, which provide important insights into planet-formation mechanisms. Using a thermo/photochemical kinetics and transport model, we investigate the extent to which disequilibrium chemistry affects the composition and spectra of directly imaged giant exoplanets. Results for specific "young Jupiters" such as HR 8799 b and 51 Eri b are presented, as are general trends as a function of planetary effective temperature, surface gravity, incident ultraviolet flux, and strength of deep atmospheric convection. We find that quenching is very important on young Jupiters, leading to CO/CH4 and N-2/NH3 ratios much greater than, and H2O mixing ratios a factor of a few less than, chemical-equilibrium predictions. Photochemistry can also be important on such planets, with CO2 and HCN being key photochemical products. Carbon dioxide becomes a major constituent when stratospheric temperatures are low and recycling of water via the H-2 + OH reaction becomes kinetically stifled. Young Jupiters with effective temperatures less than or similar to 700 K are in a particularly interesting photochemical regime that differs from both transiting hot Jupiters and our own solar-system giant planets.

O presente trabalho tem por objetivo a caracterização dinâmica dos sistemas múltiplos de planetas extrassolares. O critério de classificação escolhido é baseado na proposta publicada inicialmente em Ferraz-Mello et al. (2005) e posteriormente modicada em Michtchenko et al. (2007). Para a obtenção dos parâmetros planetários orbitais foi feita uma pesquisa em diversos catálogos e artigos disponíveis para posterior criação de um catálogo próprio. Este incluiu somente sistemas extrassolares múlltiplos, ou seja, sistemas que contêm dois ou mais planetas orbitando a estrela. Foram feitas simulações numéricas de estabilidade dinâmica dos sistemas do catálogo próprio com tempos de integração de 200 mil até 21 milhões de anos. Ao todo, foram analisados 37 sistemas múltiplos extrassolares, divididos em 50 subsistemas considerando-se a estrela e dois planetas em órbitas consecutivas. Ao todo, foram analisados 37 sistemas múltiplos extrassolares, divididos em 50 subsistemas considerando-se a estrela e dois planetas em órbitas consecutivas. Estes foram submetidos ao total de 68 simulações computacionais. Os sistemas que apresentaram um cenário de estabilidade dinâmica foram posteriormente separados em três classes: ressonantes, seculares ou hierárquicos. Mais ainda, o comportamento secular desses sistemas foi classificado conforme o movimento do ângulo \"Deltavarpi\" : oscilatório em torno de 0º, oscilatório em torno de 180º ou circulatório. Os resultados das simulações são mostrados para todos os sistemas estudados. / The aim of the present work is a dynamic classification of multiple extrasolar systems. The characterization criterion used is based on a criterion proposed initially in Ferraz-Mello et al. (2005) and modified in Michtchenko et al. (2007). To obtain orbital parameters of the extrasolar systems, a search was done into several available catalogues and the scientific literature. A new catalogue was compiled containing only multiple extrasolar systems, that is, systems with two or more planets in orbit of the host star. Numerical simulations of dynamical stability of the cataloged systems were done considering pairs of planets on the consecutive orbits. Totally, 37 multiple extrasolar systems were analyzed, decomposed in 50 sub-systems each one consisting of the host star and two planets. The time evolution of those were simulated over time spans from 200 thousand years to 21 million years in 68 numerical simulations. The systems which have presented a dynamical stability were subsequently classified in resonants, secular or hierarchical and their secular behavior was classified with respect of the angle \"Deltavarpi\" as oscillation around 0º, oscillation around 180º or circulation. The result of all simulations are presented here for the analyzed systems.