L'étude a porté sur la conversion en presence de catalyseurs bimétaliques supportes de trois molécules modèles de polyols (érythritol, xylitol et sorbitol) en phase aqueuse à 150-240 ° C sous 30-120 bar de H2 pour obtenir sélectivement des produits linéaires C4, C5 et C6 désoxygénés qui sont des précurseurs de polymèrs. L'activité catalytique dépend fortement de la nature du support utilisé (TiO2 vs ZrO2) et la plus grande sélectivité pour les produits désoxygénés linéaires voulus C4, C5 et C6 à une conversion de 80% est de 71, 66 et 54%, respectivement, en présence de catalyseur mixte à base de rhodium et du rhenium à 200 ° C sous 80-120 bar. Les caractérisations des catalyseurs par chimisorption de CO, MET-EDX, TGA-MS et XPS suggèrent une distribution et une réductibilité différentes des espèces de Re sur les nanoparticules Rh supportées en fonction du support permettant d'expliquer ces différences / The aim of our research project reports a study of heterogeneously catalyzed conversion of three polyol model molecules (erythritol, xylitol, and sorbitol) in aqueous phase at 150-240 °C under 30-120 bar of H2 to obtain selectively linear deoxygenated C4, C5, and C6 products used as precursors for polymer applications. The activity was strongly dependent on the nature of the support (TiO2 vs ZrO2) and the highest selectivity to the desired linear deoxygenated C4, C5, and C6 products at 80% conversion reached 71, 66, and 54%, respectively, in the presence of Rh–ReOx bimetallic catalysts at 200°C under 80-120 bar. The characterizations of the catalysts by CO chemisorption, TEM-EDX, TGA-MS, and XPS suggest a different distribution and reducibility of Re species over the supported Rh nanoparticles depending on the support that can explain these differences

Ces travaux de thèse portent sur la conversion par catalyse hétérogène du furfural (produit biosourcé produit, par déshydratation du xylose issu de l'hydrolyse acide de l'hémicellulose) en acide 2,5-furane dicarboxylique (FDCA, substituant potentiel de l'acide téréphtalique, monomère de polyesters et polyamides, issu du pétrole). Cette transformation a été envisagée en deux étapes catalytiques: 1) l'hydroxyméthylation du furfural en 5-hydroxyméthylfurfural (HMF) par le formaldéhyde aqueux ou le trioxane en présence d'un catalyseur acide. Les rendements maxima de 40% ont été obtenus en utilisant le formaldéhyde aqueux en présence de nanoparticules de ZSM-5. L'instabilité du furfural et du HMF dans ces conditions réactionnelles est la principale difficulté. 2) l'oxydation aérobie du HMF en FDCA. En milieu alcalin faible (Na2CO3), en présence d'un catalyseur Pt/C promu par le Bi (rapport molaire Bi/Pt = 0,2) à 100 °C et sous 40 bar d'air, le FDCA est obtenu avec un rendement quantitatif. La modification du Pt par le bismuth permet de limiter la lixiviation du Pt dans le milieu réactionnel et de recycler le catalyseur sans prétraitement préalable et sans perte significative de l'activité, comme démontré ensuite en réacteur continu / This thesis reports a study of heterogeneously catalyzed conversion of furfural (biobased product formed from the acid-catalyzed dehydration of xylose) into 2,5-furane dicarboxylique acid (FDCA, possible replacement monomer for terephtalic acid for the production of polyethylene terephtalate). This transformation has been considered in two catalytic steps: 1) hydroxymethylation of furfural with aqueous formaldehyde or trioxane into 5-hydroxymethylfurfural (HMF) in the presence of solid acids. The maximum yields of 40% have been obtained using aqueous formaldehyde in the presence of nanoparticles of ZSM-5. The main problem was the lack of stability of furfural and HMF in reaction conditions. 2) aerobic oxidation of HMF into FDCA. HMF was oxidized in alkaline aqueous solutions over Pt-based catalysts using dioxygen from air. Promotion of the catalyst with bismuth and the presence of a weak base (Na2CO3) yielded a catalytic system with a remarkable activity and selectivity. HMF was completely and exclusively converted to FDCA within 2,5 h. The catalyst could be recovered by simple filtration and reused several times without significant loss of activity and with no platinum or bismuth leaching

Cette étude se focalise sur les impacts de la réactivité en phase aqueuse de la méthacroléïne et de la méthyl vinyl cétone sur la formation des nouveaux aérosols organiques secondaires (AOS), et les impacts de la réactivité en phase aqueuse sur le vieillissement des AOS formés par l’isoprène, α-pinène et 1,3,5-triméthylbenzène en phase gazeuse. Les études de la réactivité en phase aqueuse ont été étudiées vis-à-vis des radicaux OH. Dans le but d’identifier et quantifier les produits d’oxydation des différents précurseurs d’intérêt, les échantillons en phase aqueuse ont été analysés par différents systèmes analytiques. Les résultats montrent clairement la formation de petits composés primaires et secondaires qui ont été expliqués par les mécanismes réactionnels. On a observé également la formation de composés à haute masse moléculaire par rapport à leurs précurseurs. Ces produits ont été supposés être très peu volatils et pourraient induire la formation des AOS lors de l’évaporation de l’eau. Leur capacité à former des AOS a été montrée expérimentalement par les expériences de nébulisation des solutions aqueuses à différents temps de réaction. Les résultats montrent qu’au moins une part de ces produits à haute masse moléculaire reste en phase particulaire lors de l’évaporation de l’eau, et contribue à la formation des AOS. L’ensemble de ces résultats met en évidence le fait que la réactivité en phase aqueuse atmosphérique peut induire des effets importants sur la formation et le vieillissement des AOS atmosphériques, qui peut induire une modification des propriétés physico-chimiques des aérosols. / This work focused on the impacts of aqueous phase OH-oxidation of methacrolein, methyl vinyl ketone on the SOA formation, and impacts of aqueous phase OH-oxidation on aging of SOA that are formed by isoprene, -pinene and 1,3,5-trimethylbenzene in gas phase. The chemical characterization of aqueous phase was performed by different analytical techniques. The results show the formation of small primary and secondary reaction products that were explained by suitable chemical reaction mechanisms. The formation of oligomers with high molecular mass (compared with their precursors) has also been observed during the OH-oxidation. These oligomers might be low volatile compounds that induce the formation of SOA during water evaporation. Their capacity to form SOA was experimentally demonstrated by nebulizing the aqueous phase solution at different reaction times. The results show that at least a part of oligomers remains in the particle phase during water evaporation, and contributes to the SOA formation. All of these results highlight that aqueous phase reactivity could induce important effects on the formation and aging of atmospheric SOA, which can induce modification of physico-chemical properties of SOA.

Environmental pollution has become a global concern as consequence of industrializa-tion and urbanization. The ongoing subsurface contamination by dense non-aqueous phase liquids (DNAPLs) bears tremendous hazardous potential for humans and ecosys-tems including aquifer systems. Intended or accidental spill events have led to a vast number of registered sites affected by DNAPL type chemicals. Despite the existence of novel techniques for their exploration, characterization and remediation, economical constraints often limit efforts for risk prevention or reduction, so that information and data to characterize highly complex DNAPL contamination scenarios are often insuffi-cient and compensated by natural attenuation of groundwater-dissolved contaminant plumes. Especially, knowledge on the DNAPL source zone geometry (SZG) and source zone formation are critically required yet very scarce. Against the previously stated background, this cumulative doctoral dissertation critically examined the processes of DNAPL source zone formation at laboratory scale. A comprehensive literature review identified current limitations and open research questions in the latter research field, revealing evidence for the relevance of SZG for plume response at different scales. Giv-en only a limited number of published studies related to DNAPL source zone formation, two simplified experimental setups mimicking source zone formation in an initially fully water-saturated aquifer were developed and intensively tested. The performance of aqueous and non-wetting phase dyes was evaluated for DNAPL release into three non-consolidated porous media using reflective optical imaging in combination with a cus-tom-made image processing and analysis (IPA) framework. The latter suite allowed for the generation of physically plausible DNAPL saturation distributions with determinable level of uncertainty. Then, a limited number of DNAPL release experiments were per-formed under controlled ambient as well as with boundary and initial conditions to generate robust observation data, while further adopting the IPA framework. The latter data was introduced into a numerical multiphase flow model. While most system pa-rameters could be directly determined, the parameters defining the capillary pressure-saturation and relative permeability-saturation retention curves were inversely deline-ated through a classical Monte Carlo analysis. Overall, the successfully calibrated nu-merical setup mimicking the transient DNAPL source zone formation allowed to quanti-fy uncertainties related to the experiment, IPA framework and model setup configura-tion. In addition, a number of new research questions pointing towards future im-provements of laboratory-scale methodologies to understand DNAPL contamination were derived. Especially in light of numerous existing contaminated sites with unclear history and even more vague future, given by potential impacts through climate change and anthropogenic activity, an increasing need for sophisticated strategies to better un-derstand DNAPL contamination and to reduce hazard potential is expected.:Statement I List of publications II Abstract VI Acknowledgements and funding information IX List of figures XIII List of tables XIV Abbreviations and symbols used in the main text XV 1 Introduction and background 1-1 1.1 Motivation of this thesis 1-1 1.2 Incorporation of this thesis in research projects 1-4 1.3 Definition of objectives and workflow strategy of this thesis 1-5 1.4 Formal structure of this thesis 1-11 2 Existing knowledge on DNAPL contamination 2-1 3 Fundamentals of DNAPL migration in porous media 3-1 3.1 Basic concepts for multiphase flow in porous media 3-1 3.2 Capillary pressure-saturation correlation 3-3 3.3 Relative permeability-saturation correlation 3-5 3.4 Balance equations for laminar fluid phase flow in porous media 3-7 4 Core research complex A : Development of a framework for the semi-automatized generation of DNAPL saturation distribution observation data 4-1 5 Core research complex B : Experimental and model-based simulation of DNAPL source zone formation 5-1 6 Summary and conclusions 6-1 6.1 Summary of perceptions for each main section of this thesis 6-1 6.2 New research questions with regard to DNAPL source zone formation at the laboratory scale 6-5 6.3 General recommendations for future works related to DNAPL contamination 6-8 References Ref-1 Appendix I : ENGELMANN ET AL. (2019a) App I-1 Published journal article App I-1 Appendix II : ENGELMANN ET AL. (2019b) App II-1 Published journal article App II-1 Electronic Supplementary Material 1 : Unprocessed raw TIFF format images used for IPA frame-work evaluation App II-26 Electronic Supplementary Material 2 : Sensitivities for color model change and binary conversion algorithms App II-36 Electronic Supplementary Material 3 :Relevance of spatially non-uniform illumination correction and background exclusion App II-76 Appendix III : ENGELMANN ET AL. (2021) App III-1 Published journal article App III-1 Electronic Supplementary Material 1 : Unprocessed raw TIFF format images for IPA framework ap-plication App III-30 Electronic Supplementary Material 2 : Processed images with all intermediate steps of IPA frame-work application App III-58 Electronic Supplementary Material 3 : IPA fitness App III-86 Electronic Supplementary Material 4 : Partial objective functions App III-87 Electronic Supplementary Material 5 : Model verification App III-93

La pollution atmosphérique liée aux aérosols organiques secondaire (SOA) représente un des enjeux majeurs du XXIème siècle. La photochimie multiphasique des SOA constitue le coeur et l'originalité de cette thèse.Le réacteur photochimique permet de simuler en laboratoire, l'oxydation en phase aqueuse atmosphérique des composés organiques volatils biogéniques (BVOC), et notamment, la méthyl vinyl cétone (MVK), afin d'étudier la formation ces SOA.Nous étudions la réactivité de la MVK en présence de ●OH et sa capacité à oligomériser en fonction des concentrations initiales de MVK, d'oxygène, et de ●OH. Une large stratégie analytique basée sur la chromatographie liquide couplée à la spectrométrie de masse (MS) permet d'identifier des produits de réaction, et d'établir un mécanisme réactionnel, expliquant la formation des oligomères, leurs rendements et leur vieillissement.Les données colligées servent d'entrées à un modèle de boîte multiphasique, afin d'explorer la sensibilité de l'oligomérisation aux conditions atmosphériques.Ensuite, nous comparons la réactivité de la MVK en présence de ●OH à celle induite par la photolyse de l'acide pyruvique; puis nous mesurons la tension de surface engendrée par ces deux systèmes d'oligomères. Enfin, la mobilité ionique couplée à la MS permet d'observer la co-oligomérisation d'une gamme étendue de BVOC en présence de ●OH.L'oligomérisation atmosphérique implique (i) une concentration minimale de précurseurs pouvant être atteinte dans les aérosols humides via la co-oligomérisation; (ii) une réactivité en compétition avec l'oxygène dissous dans la phase aqueuse, et dont la pertinence atmosphérique reste à explorer. / Air pollution caused by secondary organic aerosol (SOA) is one of the major challenges of this century. We focus this thesis on SOA , through an innovative approach, i.e. multiphase photochemistry.The photochemical reactor allows to simulate in laboratory, the atmospheric aqueous phase oxidation of biogenic volatile organic compounds (BVOC) and in particular, methyl vinyl ketone (MVK), and thus, to study SOA.We study the reactivity of MVK in the presence of ●OH and its ability to oligomerize under various initial concentrations of oxygen, MVK and ●OH. A wide analytical strategy based on liquid chromatography-mass spectrometry is used to identify the reaction products, and establish a chemical mechanism. We focus on these oligomers systems, formation, yield and aging. Collected data are used as inputs to a multiphase box model to explore the sensitivity of oligomerization to the variations of physical and chemical atmospheric parameters. The photochemistry of pyruvic acid generates radical chemistry and initiates MVK oligomerization. We closely compare this reaction to MVK ●OH oxidation. Then, we measure the surface activity of both systems. The ability of oligomers to partition to the interface could affect the climate. Finally, we used ion mobility - mass spectrometry to observe ●OH co-oligomerization of a mixture of organic compounds most representative of the atmosphere.Atmospheric oligomerization implies (i) a minimal concentration of precursors that could be reached in wet aerosol via the co-oligomerization; (ii) a reactivity in competition with the addition of the dissolved oxygen, whose the atmospheric relevance remains to be explored.

<p dir="ltr">The chemical constituents of terrestrial and atmospheric waters originate from biomass burning, fertilizer runoff, and anthropogenic activity, among other sources, and their multi-phase chemistry is complex. Sunlight plays an essential role in aquatic chemistry. Photosensitizers in terrestrial and atmospheric waters absorb light to form highly reactive species such as triplet excited carbon (³C*), hydroxyl radical (•OH), and singlet oxygen (¹O₂), driving the photochemical transformations of dissolved organic matter (DOM) in the aqueous phase. Of note, these reactive species transform DOM compounds that do not undergo direct photolysis. DOM frequently undergoes a change in optical properties following photochemical processing, with implications for air quality, water quality, and human and animal health. The presence of inorganic minerals, such as the fertilizer compound struvite, in terrestrial or atmospheric waters introduces further complexity and impacts the photochemical processes that occur. Simplified proxy systems are created in the laboratory to simulate aquatic photochemical processes and evaluate the formation and/or photodegradation of photoproducts. These mixtures typically consist of a representative organic carbon (OC) compound and a photosensitizer, along with struvite or another inorganic mineral.</p>