New detections of CCH have been made toward nine planetary nebulae (PNe), including K4-47, K3-58, K3-17, M3-28, and M4-14. Measurements of the N = 1 -> 0 and N = 3 -> 2 transitions of this radical near 87 and 262 GHz were carried out using the new 12 m and the Sub-Millimeter Telescope (SMT) of the Arizona Radio Observatory (ARO). The presence of fine and/or hyperfine structure in the spectra aided in the identification. CCH was not observed in two PNe which are sources of C-60. The planetary nebulae with positive detections represent a wide range of ages and morphologies, and all had previously been observed in HCN and HNC. Column densities for CCH in the PNe, determined from radiative transfer modeling, were N-tot(CCH) similar to 0.2-3.3 x 10(15) cm(-2), corresponding to fractional abundances with respect to H-2 of f similar to 0.2-47 x 10(-7). The abundance of CCH was found to not vary significantly with kinematic age across a time span of similar to 10,000 years, in contrast to predictions of chemical models. CCH appears to be a fairly common constituent of PNe that are carbon-rich, and its distribution may anti-correlate with that of C-60. These results suggest that CCH may be a product of C-60 photodestruction, which is known to create C-2 units. The molecule may subsequently survive the PN stage and populate diffuse clouds. The distinct, double-horned line profiles for CCH observed in K3-45 and M3-28 indicate the possible presence of a bipolar flow oriented at least partially toward the line of sight.

What sets the observable chemical composition of exoplanetary atmospheres? The available chemical abundance of the planet's natal protoplanetary disk gas will have a deciding role in the bulk abundance of the atmosphere very early in the planet's life. While late accretion of ices and inter-atmosphere physical processing can change the observable chemical abundances. We have developed a theoretical model which connects the chemical and physical evolution of an accretion disk with the growth of a young planet to predict the bulk chemical abundance of the planetary atmosphere that is inherited from the disk. We assess what variation in atmospheric chemical abundances are attributed to different planet formation histories. We find differences in the relative abundances of primary nitrogen carriers NH$_3$ and N$_2$ depending on {\it when} the planet accreted its gas. Early ($t<1$ Myr) accreters predominately accreted warmer gas which tend to have its nitrogen in NH$_3$, while later protoplanets accrete colder, more N$_2$ dominated gas. Furthermore we compute the carbon-to-oxygen ratio (C/O) for each planets, which is used to infer {\it where} a planet forms in its accretion disk. We find that each of our planets accrete their gas very close to the water ice line, thereby accreting `pristine' gas with C/O$_{planet}$ exactly matching its host star. We extend our results by tuning our initial disk parameters to reproduce the properties of the HL Tau disk. We produce three models that span the range of measured gas masses, and one model which studies a UV quiet system. We generally find that planet formation is efficient enough to produce a Jupiter-massed planet within the predicted 1 Myr age of the disk. We find a correspondence between the radial locations of ice lines within our astrochemical model and the set of observed dust gaps in the HL Tau system. / Thesis / Doctor of Philosophy (PhD)

In this thesis, I focus on the physical and chemical evolution at the earliest stages of low-mass star formation. I report results from the Spitzer Space Telescope and molecular line observations of 9 species toward the dark cloud L43, a survey of 10 Class 0 and 6 Class I protostars with 8 molecular lines, and a survey of 9 Very Low Luminosity Objects (VeLLOs) with 11 molecular lines. From the observational results, CO depletion is extensively observed with C¹⁸O(2-1) maps. A general evolutionary trend is also seen toward the Class 0 and I samples: higher deuterium fractionation at higher CO depletion. For the VeLLO candidates and starless cores with N₂D⁺(3-2) detection, we found the deuterium ratio of N₂D⁺/N₂H⁺ is higher comparing with the Class 0 and I samples. We use DCO⁺(3-2) maps to trace the velocity structures. Also, HCO⁺(3-2) blue profiles are seen toward the VeLLO candidate L328, indicating possible infall. To test theoretical models and to interpret the observations, we adopt a modeling sequence with self-consistent calculations of dust radiative transfer, gas energetics, chemistry, and line radiative transfer. In the L43 region described in Chapter 2, a starless core and a Class I protostar are evolving in the same environment. We modeled both sources with the same initial conditions to test the chemical characteristics with and without protostellar heating. The physical model consists of a series of Bonner-Ebert spheres describing the pre-protostellar (PPC) stages following by standard inside-out collapse (Shu 1977). The model best matches the observed lines suggests a longer total timescale at the PPC stage, with faster evolution at the later steps with higher densities. In Chapter 3, we modeled the entire group of Class 0 and I protostars. The trend of decreasing deuterium ratio can be seen after the temperature is high enough for CO to evaporate. After the evaporation, the history of heavy depletion (e.g, from longer PPC timescales or different grain surface properties) no longer affects the line intensities of gas-phase CO. The HCO⁺ blue profiles, which are used as infall indicators, are predicted to be observed when infall is beyond the CO evaporation front. The low luminosity of VeLLOs cannot be explained by standard models with steady accretion, and we tested an evolutionary model incorporating episodic accretion to investigate the thermal history and chemical behaviors. We tested a few chemical parameters to compare with the observations and the results from Chapter 2 and 3. The modeling results from episodic accretion models show that CO and N₂ evaporate from grain mantle surfaces at the accretion bursts and can freeze back onto grain surfaces during the long periods of quiescent phases. Deuterated species, such as N₂D⁺ and H₂D⁺, are most sensitive to the temperature. Possible good tracers for the thermal history include the line intensities of gas-phase N₂H+ relative to CO, as well as CO₂ and CO ice features. / text

In this dissertation, techniques of high-resolution rotational spectroscopy have been used to measure the spectra of molecules in both laboratory and astronomical settings. In the laboratory, small metal-bearing molecules containing zinc, iron, nickel, titanium, yttrium, and scandium have been studied at microwave and millimeter/submillimeter wavelengths in order to determine their rotational, fine, and hyperfine constants. These molecules were synthesized in situ in direct-absorption and Fourier-transform microwave spectrometers using Broida-type ovens and laser ablation methods. From the spectroscopic parameters, information about fundamental physical propertes and electronic character could be obtained. Radio telescopes were used to measure the spectra of molecules in different interstellar environments. A new molecule, FeCN, was detected toward the circumstellar envelope of the carbon-rich asymtotic giant branch star, IRC+10216, marking the first iron-bearing molecule detected in the interstellar medium. The telescopes were also used to conduct a study of the evolved planetary nebula, NGC 7293, or the Helix Nebula. In the Helix, CO, HCO⁺, and H₂CO were observed at several positions offset from the central star to obtain densities and kinetic temperatures throughout the Helix. A map of the HCO⁺ J = 1→ 0 transition was also constructed, showing that HCO⁺ is widespread throughout the Helix, instead of being photodissociated and destroyed, as theoretical models of planetary nebulae predict.

Plus d'une centaine de réactions entre des molécules stables et des radicaux se sont révélées être rapides à très basse température. Les réactions entre deux espèces radicalaires ont quant à elles reçu beaucoup moins d'attention de la part des scientifiques. Les complexités de production et de mesure de concentrations de ces radicaux en sont les principales raisons. Nous avons réalisé pour la première fois des mesures de constantes de vitesse sur les réactions radical-radical N + OH, N + CN et N + CH à basse température dans un réacteur à écoulement supersonique uniforme (tuyère de Laval). Nous avons utilisé une technique de décharge micro-onde pour produire l'azote atomique et une méthode de mesure relative pour déterminer les cinétiques des réactions. Les résultats donnent un aperçu des mécanismes de formation en phase gazeuse de l'azote moléculaire dans les nuages denses du milieu interstellaire. / More than a hundred reactions between stable molecules and free radicals have been shown to remain rapid at low temperatures. In contrast, reactions between two unstable radicals have received much less attention due to the added complexity of producing and measuring excess radical concentrations. We performed kinetic experiments on the barrierless N + OH, N + CN and N + CH reactions in a supersonic flow (Laval nozzle) reactor. We used a microwave-discharge method to generate atomic nitrogen and a relative-rate method to follow the reaction kinetics. The measured rates agreed well with the results of exact and approximate quantum mechanical calculations. These results also provide insight into the gas-phase formation mechanisms of molecular nitrogen in interstellar clouds.

La recherche et la détection de molécules organique à la surface de Mars est l’un des objectifs des missions martiennes actuelles (MSL, Mars Science Laboratory) et futures (ExoMars 2020). Plusieurs sources de matière organique peuvent être considérées telles que les sources abiotiques (milieu interplanétaire, hydrothermalisme, synthèses atmosphériques…) mais également les sources biotiques telles qu’une potentielle activité biologique martienne passée. A ce titre, le rover Curiosity de la mission MSL a permis la détection de composés organiques d’origine martienne chlorés et soufrés, bien que ces molécules ne soient pas liées à une quelconque activité biologique ou bien ne reflètent pas la diversité moléculaire de sources abiotiques avérées telles que le milieu interplanétaire. L’une des hypothèses pour expliquer cette faible diversité consiste à considérer que l’environnement martien n’est pas favorable à la préservation de la matière organique. Afin de comprendre l’évolution des molécules organiques à la surface de Mars et donc de guider et aider les interprétations des analyses menées in situ, j’ai travaillé sur deux expériences de simulation simulant certains paramètres de la surface de Mars (rayonnement UV, pression, température, composition minérale). La première, MOMIE (Mars Organic Matter Irradiation and Evolution), est une simulation de laboratoire mise en place au LISA (Créteil, France). La seconde est l’expérience PSS (Photochemistry on the Space Station), mise en place sur la plateforme EXPOSE R2 sur la Station Spatiale Internationale (ISS) en orbite basse terrestre, utilisant directement le flux de photons UV du Soleil filtré.J’ai étudié l’évolution de quatre molécules organiques susceptibles d’être présentes sur Mars, pures ou en présence de phases minérales analogues martiennes : la glycine (un acide aminé), l’adénine et l’uracile (deux bases azotées), et le chrysène (un hydrocarbure aromatique polycyclique). La glycine, l’adénine et le chrysène se dégradent en surface directe de Mars avec des rendements quantiques de photodissociation ϕ200-280 compris entre 6,4 ± 1,4 x 10-6 et 2,3 ± 1,0 x 10-3 molécule.photon-1. L’uracile forme des photoproduits plus stables, selon un rendement de production élevé de 1,64 ± 1,43 x 10-1 molécule.photon-1. Quatre dimères d’uracile ont pu être identifiés comme des photoproduits. Pour finir, l’ajout de phases minérales amorphe et riche en fer ou bien de perchlorates accélère la dégradation ou l’évolution des molécules organiques / Organic molecule detection at Mars is one of the main goals of the current and future Mars exploration space missions, Mars Science Laboratory (MSL, NASA) and ExoMars 2020 (ESA). Several organic sources exist : abiotic sources (interplantary medium, hydrothermalism and atmospheric synthesis) but also biotic sources such as potential past biological activity. Curiosity from the MSL mission detected chlorinated and sulfur organic compounds. However these compounds can not be linked to any biological activity and do not represent the meteoritical organic diversity.The main hypothesis to explain the low diversity of detected organic compounds at Mars is that the martian environment degrade organic matter. In order to understand organic molecule evolution at the Martian surface and be able to guide and help interpret in situ analysis, I worked on two experimental simulations mimicking some of the martian environmental conditions (UV radiation, pressure, temperature and mineral composition). MOMIE, for Mars Organic Matter Irradiation at Mars, is a laboratory experiment set up at the LISA laboratory (Créteil, France). PSS, for Photochemistry on the Space Station, has been set up on the International Space Station (ISS) in low Earth orbit, using directly filtered UV photons from the Sun.I studied the evolution of four organic molecules likely to be present at Mars with ou without a mineral phase : glycine (an amino acid), adenine and uracil (two nucleobases), and chrysene (a polycyclic aromatic hydrocarbon). Glycine, adenine and chrysene are degraded at Mars surface with quantum efficiencies of photodecomposition from 6,4 ± 1,4 x 10-6 to 2,3 ± 1,0 x 10-3 molecule.photon-1. Uracil evolve into more stable photoproducts with a production efficiency of 1,64 ± 1,43 x 10-1 molécule.photon-1. Four uracil dimers have been identified as uracil photoproducts. Finally, the studied mineral phases, an amorphous iron-rich phase and perchlorates, accelerate organics evolution or degradation

Os compostos de fósforo apresentam várias implicações em processos atmosféricos e interestelares. Nesta tese, será realizado um estudo ab initio em três diferentes sistemas. (i) Um destes sistemas é o radical PCO. No capítulo três, foi analisado os aspectos conformacionais do radical PCO, sendo avaliado as propriedades moleculares e termodinâmicas da espécie cíclica e das espécies lineares. Entre os isômeros do radical PCO, a espécie i3 (C&infin;V, 2&pi;) é a mais estável delas, com uma entalpia de formação a 0K de 22.33&plusmn;2.10 kcal mol-1. Considerando as barreiras de energia, que convergem em direção a espécie i3, elas apresentam valores próximos de 10 kcal mol-1, ao passo que a energia necessária para a isomerização da molécula i3 para outros isômeros é acima de 60 kcal mol-1. Estes valores de energia explicam o fato que, em condições experimentais, foi detectado apenas a espécie i3 (C&infin;V, 2&pi;). (ii) No capítulo quatro, foi elucidado o mecanismo da reação PH3 +F, assim como foi também caracterizado as propriedades eletrônicas dos intermediários observados nesta reação. Na reação PH3 +F, pode ser observado que, diferente da literatura, dois caminhos são possíveis para esta reação: (a) a reação de abstração de hidrogênio, com a formação dos produtos PH2 e HF, e a reação de adição-eliminação, com a formação das espécies PH2F e H. Analisando a energia eletrônica, é possível observar que a reação de adição-eliminação apresenta uma barreira de energia de 23 kcal mol-1 abaixo da mesma observada para a reação de abstração de hidrogênio. Considerando os intermediários formados na reação PH3 + F, são observados dois tipos de simetria: uma C1 e duas Cs. Além disso, a entalpia de formação em 298K dos intermediários variou de -22.99 to -29.74 kcal mol-1. (iii) No capítulo cinco, foi avaliada a interação da fosfina com diferentes aglomerados de água. Neste capítulo, foi realizada uma análise nos aglomerados PH3-(H2O)n (n=1-8,12,20) e avaliado a estabilidade dos potenciais isômeros, assim como as propriedades moleculares e espectroscópicas dos diferentes isômeros. Nas estruturas PH3-(H2O)n (n=1-8) foi possível observar que os modos vibracionais &delta;(PH3) e &delta;sym(PH3) apresentaram um deslocamento para o vermelho, ao passo que as freqüências de estiramento simétrico e assimétrico da fosfina apresentaram um deslocamento para o azul. No caso da estrutura PH3(H2O)20, as variações nos modos vibracionais foram similares embora que mais intensas, sendo o mesmo também observado para as respectivas intensidades. Além disso, a energia necessária para o confinamento da fosfina no interior de um aglomerado de água dodecaedro hexagonal variou de -1.81 to -6.38 kcal mol-1. / The phosphorus compounds show several implications to atmospheric and interstellar processes. In this thesis, was performed an ab initio study on three different systems. (i) One of these systems is the PCO radical. In chapter three, was studied the conformation aspects of PCO radicals, which was assessed the molecular and thermodynamic properties of the cyclic and linear species. In PCO species, it was observed that the linear specie i3 (C&infin;V, 2&pi;) is the most stable one, with the enthalpy formation at 0K of 22.33&plusmn;2.10 kcal mol-1. Considering the barrier heights, which converge into the direction of i3, they are close to 10 kcal mol-1, while the energy necessary to the isomerization of i3 to other conformations are high than 60 kcal mol-1. These energy values explain the fact that, in experimental conditions, was detected only the i3 (C&infin;V, 2&pi;) specie. (ii) In chapter four, it was elucidated the mechanism of the PH3 + F reaction, and it was also described the electronic properties of the intermediates observed in this reaction. In the PH3 + F reaction can be seen that, different from the literature, two possible pathways can be observed: (a) the hydrogen abstraction, with the formation of PH2 and HF products, (b) and the addition-elimination route, with the formation of PH2F and H species. Analyzing the electronic energy, can be observed that the barrier energy of the addition-elimination process is 23 kcal mol-1 bellow the hydrogen abstraction route. Considering the intermediates, two different point groups were detected: a C1 and two Cs. In addition, the enthalpy formation at 298K of the intermediates, in the PH3 + F reaction, range from -22.99 to -29.74 kcal mol-1. (iii) In chapter five, it was studied the interaction of phosphine with different water clusters. In this chapter was performed an analysis of the PH3-(H2O)n (n=1-8,12,20) clusters, and evaluated the stability of the potential isomers as also the molecular and spectroscopy aspects of the different species. In the PH3(H2O)n (n=1-8) structures are seen a redshift in the &delta;(PH3) and &delta;sym(PH3) vibrational modes, while is observed a blueshift from the asymmetric and symmetric stretching frequencies of phosphine. In the case of PH3(H2O)20 structure, the variations in the vibrational modes were similar however more intense, as also in their respective intensities. In addition, the necessary energy to trap phosphine in the interior of an hexagonal dodecahedron water clusters range from -1.81 to -6.38 kcal mol-1.

La dernière génération de récepteurs radio, dotés à la fois d'une grande bande passante et d'une haute résolution, fait de toute observation radio-astronomique une étude spectroscopique. Dans le cas de l'imagerie à grand champ du milieu interstellaire, une telle abondance de données fournit de nouveaux outils de diagnostic, mais pose aussi de nouveaux défis en termes de traitement et d'analyse des données. L'objectif du projet ORION-B est d'observer 5 degrés carrés du nuage moléculaire OB, soit près de la moitité de la surface du nuage, dans toute la bande à 3mm. L'émission de dizaines de traceurs moléculaires à été cartographiée, ce qui inclut CO et ses isotopologues, HCO, HCN, HNC, N$_2$H$^+$, le méthanol, SO, CN...L'accès à des cartes résolues spatialement pour de nombreuse espèces chimiques nous permet d'identifier les meilleurs traceurs de la densité du gaz et de son illumination. Ces cartes ont aussi été soumises à des méthodes d'apprentissage automatique, afin de segmenter le nuage moléculaire en régions caractérisées par une émission moléculaire similaire, et de quantifier les corrélations les plus importantes entre différents traceurs moléculaires, et entre les traceurs et des quantités physiques telles que la densité ou la température des poussières.La grande surface observée, combinée à une haute résolution spatiale et spectrale, permet aussi de caractériser statistiquement la cinématique et la dynamique du gaz. La fraction de quantité de mouvement dans les modes compressifs et solénoïdaux (rotationels) de la turbulence peut être calculée, ce qui montre que le nuage est dominé par des mouvements solenoidaux, tandis que les mouvements compressifs sont concentrés dans deux régions de formation stellaire. Ce résultat est cohérent avec l a très faible efficacité de formation stellaire de ce nuage, et souligne l'importance du forçage compressif pour la formation des étoiles.Les nombreux filaments identifiés dans ce nuage moléculaire ont par ailleurs des densités relativement faibles, et sont très stables vis à vis de l'effondrement gravitationnel. La plupart des filaments sont dépourvus d'étoiles jeunes, mais ils montrent des signes de fragmentation radiale et longitudinale, ce qui indique que de la formation stellaire pourrait à l'avenir y avoir lieu. / The new generation of wide-bandwidth high-resolution receivers turns almost any radio observation into a spectral survey. In the case of wide-field imaging of the interstellar medium, such a wealth of data provides new diagnostic tools, but also poses new challenges in terms of data processing and analysis. The ORION-B project aims at observing 5 square degrees of the OB molecular cloud, or about half of the cloud's surface, over the entire 3mm band. The emission of tens of molecular tracers has been mapped, including CO isotopologues, HCO, HCN, HNC, N$_2$H$^+$, methanol, SO, CN...Having access to spatially resolved maps from many molecular species enables us to identify the best tracers of the gas density and illumination. Machine learning techniques have also been applied to these maps, in order to segment the molecular cloud into typical regions based on their molecular emission, and to quantify the most meaningful correlations of different molecular tracers with each other and with physical quantities such as density or dust temperature.The wide-field coverage, together with the spatial and spectral resolution, also allows to characterize statistically the kinematics and dynamics of the gas. The amount of momentum in the compressive and solenoidal (rotational) modes of turbulence are retrieved, showing that the cloud is dominated by solenoidal motions, with the compressive modes being concentrated in two star-forming regions. This result is in line with the overall very low star formation efficiency of the cloud, and highlights the role of compressive forcing in the star formation process.The numerous filaments identified in the molecular cloud also prove to have rather low densities, and are very stable against gravitational collapse. Most filaments are starless, but they show signs of longitudinal and radial fragmentation, which indicates that star formation might occur later on.

La nouvelle fenêtre spectroscopique dans le sub-millimétrique, ouverte par l’avènement del’observatoire spatial Herschel, a permis la détection d’espèces azotées simples, les hydruresd’azote NH, NH2 et NH3, dans les enveloppes froides de proto-étoiles. Ces enveloppes sontconstituées de gaz dense et froid caractéristique des conditions physico-chimiques des nuagesmoléculaires. L’observation d’hydrures d’azote dans de tels environnements a donc permis d’apporterde nouvelles contraintes sur la chimie interstellaire de ces nuages, et nous a donné enparticulier l’occasion de ré-explorer la chimie de l’azote.L’objectif de mon travail de thèse a été d’analyser en détail cette chimie interstellaire etprincipalement la formation en phase gazeuse d’espèces polyatomiques simples : les hydruresd’azote. Dans des conditions de gaz dense et froid (n = 104 cm−3, T = 10 K), la chimie de cesderniers est initiée par une chimie lente (la conversion de N en N2 par réactions neutre-neutre),contrairement à celles de ses analogues oxygénés et carbonés. Nous nous sommes particulièrementintéressés à cette étape de la chimie de l’azote, au vu des récents travaux théoriqueset expérimentaux menés par plusieurs équipes d’experts (Bordeaux, Besançon). De plus, lesrécents travaux concernant la conversion ortho-para de l’hydrogène moléculaire et les nouveauxcalculs de rapports de branchement de spins nucléaires pour les voies de production des hydruresd’azote dans leurs configurations ortho et para, menés à l’IPAG, nous ont permis d’entreprendrele calcul auto-cohérent des différentes symétries de spin des hydrures d’azote et de l’hydrogènemoléculaire. Nous avons ainsi pu développer un nouveau réseau chimique de l’azote, bénéficiantdes taux cinétiques les plus à jour pour les réactions critiques impliquées dans la chimie deshydrures d’azote.Ce nouveau réseau est utilisé pour modéliser l’évolution temporelle des abondances desespèces azotées dans des conditions de gaz dense et froid ( 103 < n < 106 cm−3, T ≤ 50 K).Les résultats à l’état stationnaire sont comparés aux observations de NH, NH2 et NH3, dans lesenveloppes froides de proto-étoiles de faible masse, en étudiant l’influence des abondances totalesen phase gazeuse du carbone, de l’oxygène et du soufre. Nos modèles chimiques reproduisent lesabondances des hydrures d’azote observés et leurs rapports pour un rapport C/O élementaire, enphase gazeuse, de ∼ 0.8 et à condition que l’abondance totale de soufre soit déplétée d’au moinsun facteur 2. Les rapports ortho/para prédits par nos modèles, pour NH2 et NH3, respectivement∼ 2.3 et ∼ 0.7, sont compatibles avec les observations de ces derniers dans des nuages diffusfroids. Les abondances des hydrures d’azote, dans des conditions de nuages sombres, sont donccohérentes avec une synthèse purement en phase gazeuse. De plus, nos résultats soulignent lefait que NH provient d’une voie de formation différente de celle de NH2 et NH3. NH vient de larecombinaison dissociative de N2H+ alors que la formation de NH2 et NH3 est principalementdue à la recombinaison dissociative de l’ion ammonium (NH+4 ), lui même molécule fille deN+. Ainsi, NH2 et NH3 procèdent de l’échange de charge dissociatif N2 + He+, tandis que NHprovient de la réaction N2 + H+3 . / The new spectroscopic window opened by the advent of the Herschel Space Observatory,has enabled the detection of simple nitrogen species, the nitrogen hydrides NH, NH2, and NH3,in the cold envelope of protostars. These envelopes are made of dense cold gas characteristicof the physico-chemical conditions of molecular clouds. The observation of nitrogen hydrides insuch environments has brought new constraints on the interstellar chemistry of these kind ofclouds, and gives, in particular, the opportunity to revisit the chemistry of nitrogen.The aim of my thesis was to comprehensively analyse the interstellar chemistry of nitrogen,focussing on the gas-phase formation of the simplest polyatomic species, namely nitrogen hydrides.Under dense, cold gas conditions (n = 104 cm−3, T = 10 K), the chemistry of theselatter is initiated by a slow chemistry (the conversion from N to N2 with neutral-neutral reactions),in contrast to their carbonated and oxygenated analogues. We have investigated andrevisited this specific part of the nitrogen chemistry in the light of recent theoretical and experimentalwork carried out by several expert teams (Bordeaux, Besançon). In addition, recentwork about the ortho-para conversion of molecular hydrogen and new calculations of nuclearspin branching ratios for the production pathways of nitrogen hydrides in their ortho and paraconfigurations conducted at IPAG, enabled us to treat self-consistently the different spin symmetriesof the nitrogen hydrides together with the ortho and para forms of molecular hydrogen.We were able to develop a new network of chemical nitrogen in which the kinetic rates of criticalreactions involved in the nitrogen chemistry have been updated.This new network is used to model the time evolution of the nitrogen species abundancesin dense cold gas conditions (T ≤ 50 K, 103 < n < 106 cm−3). The steady-state resultsare compared to observations of NH, NH2 and NH3 towards a sample of low-mass protostars,with a special emphasis on the influence of the overall amounts of gaseous carbon, oxygen, andsulphur. Our chemical models reproduced the nitrogen hydrides abundances and their ratios fora gas-phase elemental C/O ratio of ∼ 0.8, provided that the total amount of sulphur is depletedby at least a factor of two. Our predicted ortho-to-para ratios for NH2 and NH3, ∼ 2.3 and∼ 0.7 respectively, are in good agreement with the observations towards cold diffuse clouds.Then, in dark gas conditions, the nitrogen hydride abundances are consistent with a pure gasphasesynthesis. Moreover, our results are based on the fact that NH is coming from a differentpathway than NH2 and NH3. NH is the daughter molecule of N2H+, deriving from the reactionN2+H+3 , while NH2 and NH3 proceed from NH+4 , itself daughter molecule of N+, resulting fromthe dissociative charge exchange N2 + He+.

La formation des planètes a lieu dans les disques protoplanétaires constitués de gaz et de poussières. Si ces dernières ne représentent que 1% de la masse totale du disque, elles jouent un rôle fondamental pour l’évolution chimique des disques en agissant comme catalyseurs pour la formation des molécules. Comprendre cette chimie est essentiel pour remonter aux conditions physiques initiales qui ont permis la naissance des planètes.Au cours de ma thèse, j’ai étudié la chimie à la surface des grains de poussières et son impact sur l’évolution chimique du nuage moléculaire, condition initale de la formation du disque, et du disque protoplanétaire. Grâce à des simulations numériques, à l’aide du code de chimie gaz-grain Nautilus, j’ai pu montrer l’importance des réactions de diffusion et des interactions gaz-grain pour les abondances des espèces en phase gazeuse. Les résultats du modèle couplés aux observations ont également mis en évidence les effets de la structure physique (température, densité, AV) sur la distribution des molécules dans les disques. / Planetary formation occurs in the protoplanetary disks of gas and dust. Although dust represents only 1% of the total disk mass, it plays a fundamental role in disk chemical evolution since it acts as a catalyst for the formation of molecules. Understanding this chemistry is therefore essential to determine the initial conditions from which planets form.During my thesis, I studied grain-surface chemistry and its impact on the chemical evolution of molecular cloud, initial condition for disk formation, and protoplanetary disk. Thanks to numerical simulations, using the gas-grain code Nautilus, I showed the importance of diffusion reactions and gas-grain interactions for the abundances of gas-phase species. Model results combined with observations also showed the effects of the physical structure (in temperature, density, AV) on the molecular distribution in disks.