Recent years have seen an expansion beyond the more druggable biological targets into novel areas of biological space. However, drug discovery campaigns against these challenging targets have been afflicted with low hit rates during screening campaigns and high levels of candidate attrition during clinical trials. Subsequent studies have looked to explore the underlying factors to these challenges and have identified the lack of scaffold diversity and poor physicochemical properties in screening libraries as the leading causes. In an attempt to address this issue drug discovery strategies such as fragment-based drug discovery and lead-oriented synthesis have been developed which control and direct the compound properties within screening libraries towards relevant areas of chemical space. In addition, strategies such as diversity oriented synthesis aim to synthesise structurally complex and diverse compounds, expanding screening collections into previously under-explored areas of chemical space. This thesis reports the development of a step-efficient, modular and highly adaptable synthetic route for the synthesis of partially saturated bicyclic heteroaromatic scffolds (Figure i). The designed route takes advantage of the large chiral pool provided by amino acids, with each scaffold synthesised in just 4-6 steps from these readily available enantiopure starting materials. The mild conditions allow for excellent functional group tolerance, thus enabling the incorporation of growth vectors for chemical elaboration from the outset, a strong advantage in the drug discovery process. Overall, 29 partially saturated bicyclic heteroaromatic compounds were synthesised based around 7 different scaffolds. These demonstrated a number of possible areas for diversifation both on and around the scaffold, including variation of functional groups (Figure i, red), double (cis-diastereoisomers) and single (R2- and R3-positions) substitution patterns, variation of the 5-membered heterocycle (Figure i, green) and increased size of the saturated ring (Figure i, blue). Furthermore, careful selection of the substituents, heterocycle and size of the saturated ring would enable the synthesis of screening libraries within the constraints of fragment-like, lead-like or drug-like structures. The final library has been incorporated into the Diamond XChem high-throughput crystallography program and initial screening has identified a weakly binding hit for Activin A.

El texto completo de este trabajo no está disponible en el Repositorio Académico UPC por restricciones de la casa editorial donde ha sido publicado. / At present, the construction of highways in Andean areas the connect the various most important towns and cities in South America has become has become a key element for its development, since these routes and viaducts allow free access to cover basic needs of education, work, food and health of the population. Much of the land in these areas is clay soils whose behavior is quite unpredictable because they present abrupt volume changes according to the variation of saturation in the soil. People who travel on roads on slopes of this type of soil are at high risk due to the slippage that the slopes suffer each year. The most recent was on April 3, 2020 because of the heavy rainfall that was registered in the area; there was a landslide that affected communication channels in the department of Cajamarca in Peru [1]. In this type of slopes landslides occur when the clayey soil is specifically saturated, because under these conditions the soil is not stable and loses cohesion between its particles, therefore it is important to make slope stability studies taking into account the partially saturated soil. This article presents results of tests allow to recognize the physical characteristics of the clay soil in the province of Chepén in Cajamarca. In addition, the filter paper method is used to elaborate the soil-water characteristic curve and a series of direct shear tests are carried cut at different degrees of saturation. With these results, the partially saturate soil fault surface is constructed that allows visualizing the value of the shear stress of the soil according to the saturation to which it is subjected. This value will be important for calculating the safety factor that the slope floor must have of the resistance shear of the soil according to the saturation, this value will be important for the calculation of the safety factor that the floor of the slope must have so that it does not fall. Therefore, considering this condition of the partially saturated soil in the slope stability analysis provides values of the safety factor that are closer to reality, without the need to carry out the analysis in the most critical condition, such as what it done in classical soil mechanics.

Au cours des conflits récents, les véhicules ont été sujet à des attaques impliquant une grande quantité d'explosif enterré. En général, les planchers sont visés, et leurs déformations absorbent une partie de l'énergie. Le véhicule subit également une impulsion, transmise par la détonation, qui peut blesser gravement les occupants. L'intensité de l'impulsion dépend principalement de trois paramètres: le degré de saturation du sol, la nature du sol dans lequel l'explosif est enterré, et la profondeur d'enfouissement de la charge. Les simulations numériques doivent reproduire le processus intégral de l'explosion, incluant l'initiale interaction entre la charge et le sol, l'expansion des produits de détonation, la propagation de l'onde de choc jusqu'au plancher du véhicule, et la grande déformation des projections de sol. L'information mécanique transmise jusqu'au niveau du plancher doit être suffisamment précise car les effets sur le véhicule constituent l'objectif des simulations. Développer un modèle constitutif de sol est par conséquent délicat.%délicat. un défi. tâche difficile. Le modèle de sol est visco-plastique avec un cap écrouissable, une surface de rupture pour limiter les contraintes de cisaillement et un cut off contre les contraintes excessives de tension. La surface de charge est entièrement lisse afin que les incréments de déformation plastique soient continus. Un mécanisme de rigidification est présenté pour tenir compte de la compression de l'air et des très grandes contraintes dans l'environnement immédiat de la charge. Le taux d'humidité du sol est également pris en compte. Deux séries d'essais ont été réalisés à DGA TT pour servir de référence pour les simulations numériques. Une première campagne a mis en jeu de petites quantités d'explosif à plusieurs profondeurs d'enfouissement. Les pressions aériennes ont été mesurées à plusieurs hauteurs et comparées aux simulations. Un moyen d'essai a été utilisé lors de la seconde campagne d'essais pour mesurer à la fois la déformation d'une plaque représentant un plancher de véhicule, mais aussi l'impulsion transmise par l'explosion enfouie. Un certain nombre de taux d'humidité, profondeurs d'enfouissement, épaisseurs de plaques et gardes au sol a été étudié. Au cours des essais, le sol STANAG, composé de sable et de graviers, défini dans l'AEP 55 relatif au STANAG 4569, a été utilisé. Des simulations Eulériennes ont été réalisées et sont en accord avec les résultats d'essais. Le rôle des trois parties de la surface de charge, des mécanismes de rigidification élastique et d'écrouissage plastique a été évalué. La masse volumique initiale du sol et la position initiale du cap sont les paramètres ayant la plus grande influence sur les pressions aériennes. Quant à l'impulsion, elle est principalement contrôlée par le degré de saturation du sol. / In recent conflicts, vehicles have been facing underbelly attacks involving a large quantity of buried explosive. A part of the energy is absorbed by the deformation of the belly. Still the vehicle is subjected to the impulse transmitted by the detonation which may severely injure occupants. The intensity of the impulse is highly dependent on three main parameters which are the degree of saturation of the soil, the nature of the soil in which the explosive is buried and the depth of burial of the charge. Computer simulations should follow the complete process of the explosion, including the early interaction of the charge with the soil, the expansion of the detonation products, the propagation of the shock wave up to the vehicle floor, and the large deformation of the soil projections. The mechanical information transmitted up to the floor level should be sufficiently accurate because the impact on the vehicle is the key target of the simulations. Developing a constitutive soil model is therefore a challenging task. The soil model is visco-plastic with a hardening cap surface, a failure surface to limit shear stresses and a cut off surface against excessive tension. The entire yield surface is smooth so that the plastic strain increments are continuous. A stiffening mechanism is introduced to account for air compression and accommodate the huge stresses in the immediate neighborhood of the charge. The water content of the soil is also taken into account. Two sets of experiments were carried out at DGA TT to serve as a reference for computer simulations. A first campaign involved small quantity of explosive at several depths of burial. The aerial pressures were measured at various heights and compared to simulations. The second set of experiments used a test rig to measure both the deformation of a floor simulating plate and the impulse transmitted by the buried explosion. A range of soil water contents, depths of burial of the explosive, plate thicknesses and stand off distances has been explored. For all the experiments, the sandy gravel STANAG soil defined in AEP 55 of STANAG 4569 has been used. Eulerian simulations were run and fit with these experiments. The roles of the three parts of the yield surface, of the elastic stiffening and plastic hardening mechanisms could be assessed. The initial soil density and the initial cap position were found to have the largest influence on aerial pressures. As for the impulse transmitted to the metallic plate, it was observed to be mostly controlled by the degree of saturation of the soil.

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第21737号 / 工博第4554号 / 新制||工||1710(附属図書館) / 京都大学大学院工学研究科社会基盤工学専攻 / (主査)教授 木村 亮, 准教授 肥後 陽介, 准教授 木元 小百合 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM

The durability of concrete is of major concern in all types of concrete structures where the combined effect of exposure conditions and the type and quality of the concrete material usually determines the rate of degradation. Furthermore, there are synergy effects between different deterioration mechanisms, which means that the combined rate of degradation is higher than the sum of the individual rates of each mechanism. Therefore, to accurately predict the residual service life of existing structures or when designing new structures, it is essential to consider all these aspects. This means that various chemical and physical processes, as well as how these interact, must be taken into account in models aiming to be used for service life predictions. This thesis presents the first part of a research project with the aim to investigate common deterioration mechanisms of concrete in hydraulic structures, and to improve the knowledge how these and other related phenomena can be described using mathematical models. The objective is also to study how different mechanisms interact and to find suitable approaches to account for these interactions in the models. To this end, a literature survey on commonly detected damage in hydraulic structures is presented. In addition, it also addresses in what types of and where in hydraulic structures the various damage types are usually observed. The mathematical models presented in this part of the project are focused on long-term water absorption in air-entrained concrete as well as on freezing of partially saturated air-entrained concrete. Both models are based on a multiphase description of concrete and poromechanics to describe the coupled hygro-thermo-mechanical behaviour. The thesis also presents some of the basic concepts of multiphase modelling of porous media, including discretization of the models using the finite element method (FEM). Furthermore, it covers the simplifications that are usually introduced in the general macroscopic balance equations for mass, energy and linear momentum when modelling cement-based materials. To verify the developed models and to show their capabilities, simulation results are compared with experimental data, in situ measurements and other simulations from the literature. The results indicate that both models perform well and can be used to predict long-term moisture conditions in hydraulic structures as well as freezing-induced strains in partially saturated air-entrained concrete, respectively. Even though no interactions with other deterioration mechanisms are included in the models, the development and use of these have given insights to which parameters that are important to consider in such extensions. Furthermore, based on the insights gained, the complexity of describing the full interactions between several mechanisms in mathematical models is also discussed. It is concluded that models aiming to be used for service life predictions of hydraulic structures in day-to-day engineering work need to be simplified. However, the type of advanced models presented in this thesis can serve as a basis to study which aspects and parameters that are essential to consider in simplified prediction models. / Beständigheten hos betong är av avgörande betydelse i alla typer av betongkonstruktioner där den kombinerade effekten av exponeringsförhållanden samt typ och kvalitet på betongmaterialet vanligtvis avgör nedbrytningshastigheten. Dessutom finns synergieffekter mellan olika nedbrytningsmekanismer som innebär att den kombinerade nedbrytningshastigheten är större än summan av de enskilda nedbrytningshastigheterna. För att noggrant kunna prediktera den återstående livislängden hos befintliga konstruktioner eller vid design av nya konstruktioner är det därför viktigt att ta hänsyn till samtliga av dessa aspekter. Detta innebär att olika kemiska och fysikaliska processer, samt hur dessa interagerar med varandra, måste tas i beaktande i modeller som avses användas för livslängdsbedömningar. Den här licentiatuppsatsen presenterar den första delen av ett forskningsprojekt där målet är att studera vanligt förekommande nedbrytningsmekanismer i vattenbyggnadskonstruktioner och att öka kunskapen om hur dessa och andra relaterade fenomen kan beskrivas med matematiska modeller. Målet är också att studera hur olika nedbrytningsmekanismer samverkar och att hitta lämpliga tillvägagångssätt att ta hänsyn till dessa interaktioner i modellerna. För detta ändamål presenteras en litteraturstudie avseende vanligt förekommande skador i vattenbyggnadskonstruktioner. Dessutom behandlar denna i vilka typer av vattenbyggnadskonstruktioner och var i dessa som de olika typerna av skador vanligtvis observeras. De matematiska modeller som presenteras i denna del av projektet är inriktade på långtidsabsorption av vatten i lufttillsatt betong samt på frysning i delvis vattenmättad lufttillsatt betong. Båda modellerna är baserade på en multifasbeskrivning av betong samt poromekanik för att beskriva det kopplade hydro-termo-mekaniska beteendet. Uppsatsen presenterar också några av de grundläggande koncepten gällande multifasmodellering av porösa material, inklusive diskretisering av modellerna genom användning av finita elementmetoden (FEM). Dessutom beskrivs de förenklingar som vanligtvis införs i de generella makroskopiska balansekvationerna för massa, energi och rörelsemängd då cementbaserade material modelleras. Simuleringsresultat från de utvecklade modellerna jämförs med försöksdata, fältmätningar samt andra simuleringsresultat från litteraturen för att verifiera modellerna samt visa hur de beter sig. Resultaten visar att båda modellerna ger tillfredställande resultat och kan användas för att uppskatta de långsiktiga fuktförhållandena i vattenbyggnadskonstruktioner samt frysinducerade töjningar i delvis vattenmättad lufttillsatt betong. Även om inga interaktioner mellan andra nedbrytningsmekanismer inkluderades i modellerna, så har utvecklingen samt användandet av dessa gett insikter gällande vilka parametrar som är viktiga att beakta i sådana vidareutvecklingar. Baserat på dessa insikter diskuteras också komplexiteten i att beskriva interaktionen mellan flertalet mekanismer i matematiska modeller. Det konstateras också att modeller som avses användas i dagligt ingenjörsarbete för livstidsbedömningar av vattenbyggnadskonstruktioner behöver förenklas. Däremot kan den typ av avancerade modeller som presenteras i denna uppsats användas som en grund för att studera vilka aspekter och parametrar som är viktiga att beakta i förenklade modeller. / <p>QC 20180403</p>

Les objectifs de ce travail concernent l'étude, la conception et la caractérisation d'antennes miniatures actives ou passives, large bande ou bande étroite fonctionnant en bandes MF, HF et VHF. Le manuscrit est divisé en cinq parties : La première partie présente un système de caractérisation d'antennes qui a été développé, validé et utilisé pour tous les aériens conçus. Ce système, basé sur une cellule à plaque parallèles (PPC), permet un large spectre de mesures telles que la mesure du gain, du point de compression, de l'intermodulation et de la sensibilité via une méthode rayonnée, particulièrement intéressante dans le cas des antennes actives intégrées. La deuxième partie concerne les antennes solénoïdales sur ferrite. L'utilisation de simulateurs électromagnétiques 3D a permis d'obtenir des résultats qui sont comparés à la théorie proposée dans la littérature. Les principaux systèmes d'adaptation d'impédance sont également étudiés. La troisième partie met en avant la possibilité de concevoir des antennes à substrat ferromagnétique de géométrie non conventionnelle en utilisant des matériaux composites. Deux antennes miniatures fabriquées et fonctionnant en bande VHF permettent d'illustrer ce point. Dans la quatrième partie, nous présentons un concept d'antennes à substrat ferromagnétique partiellement saturé. L'utilisation d'une source de champ magnétique statique associée à un matériau initialement dispersif permet de constater un certain nombre de phénomènes intéressants, tels que l'amélioration de l'efficacité tout en préservant l'adaptation de l'antenne ou bien la création de directivité sur des antennes électriquement très compactes. La dernière partie présente la valorisation du travail à travers un projet de télécommunication hertzienne longue portée s'inscrivant dans le cadre de la navigation maritime. / The objectives of this work concern the study, the design and the measurement of miniaturized passive and active, broadband and narrowband antennas for MF, HF and VHF frequency bands. The thesis is divided into five parts : The first part deals with a measurement system, which has been developed, validated and used for all conceived aerials. The system is based on a parallel plate cell (PPC) and allows an evaluation of the gain, the compression point, the interception point and the sensitivity using a radiative method particularly useful in the case of active integrated antennas. The second part concerns solenoidal ferrite antennas. The results obtained from electromagnetic 3D simulators were compared to the state of the art theory. Main matching technics have also been studied. The third part put the light on the possibility of development of arbitrary shaped antennas on a ferromagnetic substrate using a composite material. Two antennas developed for the VHF band, confirm this point. In the fourth part, we present a concept of antennas on a partially saturated ferromagnetic substrate. A static magnetic field associated with an initially lossy material brings up some interesting phenomena such as an increased efficiency without a degradation of the impedance matching or the directivity with very small antennas. The last part presents an application of the work across a project dedicated to long distance telecommunications in marine navigation.

Dans cette thèse, on étudie les écoulements oscillatoires en milieux poreux (non saturés ou partiellement saturés) dus à des oscillations tidales des niveaux d'eau dans des milieux ouverts adjacents aux milieux poreux. L'étude est centrée sur le cas des plages de sable en hydrodynamique côtière, mais les applications concernent, potentiellement et plus généralement, les problèmes d'oscillation et de variation temporelle des niveaux d'eau dans des systèmes couplés, lorsque ceux-ci mettent en jeu des interactions entre les écoulements de sub-surface (milieux poreux) et les eaux de surface (milieux ouverts) : plages naturelles et artificielles; digues portuaires; barrages en terre; berges de fleuves; estuaires. Le forçage tidal des écoulements souterrains est représenté et modélisé ici, tant expérimentalement que numériquement, par une oscillation quasi-statique du niveau d'eau dans un réservoir externe ouvert, connecté au domaine poreux. On s'intéresse plus particulièrement aux écoulements verticaux forcés par une pression oscillatoire imposée au bas d'une colonne de sol. Sur le plan expérimental, ce type de forçage est obtenu par une machine à marée équipée d'un arbre rotatif. Au total, on utilise dans ce travail trois types d'approches (expérimentale, numérique, analytique), l'objectif étant d'étudier le mouvement vertical de la surface "libre" et l'écoulement non saturé sus-jacent, de façon à prendre en compte aussi bien les pertes de charge dans la zone saturée que les gradients de pression capillaire dans la zone non saturée. […] / In this thesis, we study hydrodynamic oscillations in porous bodies (unsaturated or partially saturated), due to tidal oscillations of water levels in adjacent open water bodies. The focus is on beach hydrodynamics, but potential applications concern, more generally, time varying and oscillating water levels in coupled systems involving subsurface / open water interactions (natural and artificial beaches, harbor dykes, earth dams, river banks, estuaries). The tidal forcing of groundwater is represented and modeled (both experimentally and numerically) by quasi-static oscillations of water levels in an open water reservoir connected to the porous medium. Specifically, we focus on vertical water movements forced by an oscillating pressure imposed at the bottom of a soil column. Experimentally, a rotating tide machine is used to achieve this forcing. Overall, we use three types of methods (experimental, numerical, analytical) to study the vertical motion of the groundwater table and the unsaturated flow above it, taking into account the vertical head drop in the saturated zone as well as capillary pressure gradients in the unsaturated zone. Laboratory experiments are conducted on vertical sand columns, with a tide machine to force water table oscillations, and with porous cup tensiometers to measure both positive pressures and suctions along the column (among other measurement methods). Numerical simulations of oscillatory water flow are implemented with the BIGFLOW 3D code (implicit finite volumes, with conjugate gradients for the matrix solver and modified Picard iterations for the nonlinear problem). In addition, an automatic calibration based on a genetic optimization algorithm is implemented for a given tidal frequency, to obtain the hydrodynamic parameters of the experimental soil. Calibrated simulations are then compared to experimental results for other non calibrated frequencies. Finally, a family of quasi-analytical multi-front solutions is developed for the tidal oscillation problem, as an extension of the Green-Ampt piston flow approximation, leading to nonlinear, non-autonomous systems of Ordinary Differential Equations with initial conditions (dynamical systems). The multi-front solutions are tested by comparing them with a refined finite volume solution of the Richards equation. Multi-front solutions are at least 100 times faster, and the match is quite good even for a loamy soil with strong capillary effects (the number of fronts required is small, no more than N≈ to 20 at most). A large set of multi-front simulations is then produced in order to analyze water table and flux fluctuations for a broad range of forcing frequencies. The results, analyzed in terms of means and amplitudes of hydrodynamic variables, indicate the existence, for each soil, of a characteristic frequency separating low frequency / high frequency flow regimes in the porous system.

L’apparition massive de nids de poule sur chaussées bitumineuses a été observée en cours d’hiver sur de très courtes périodes de temps, caractérisées par l’alternance entre températures positives et fortement négatives accompagnée de précipitations pluvieuses. Ceci a conduit à rechercher un mécanisme spécifique de dégradation de couches d’enrobés bitumineux (EB) lié au comportement au gel des EB partiellement saturés en eau. Celui-ci a été étudié en laboratoire à partir d’essais à déformation libre ou empêchée, avec ajout de chaux pour certaines formules d’EB.Ces essais ont montré l’apparition de déformations de gonflement ou contraintes importantes induites lors du gel de l’eau interstitielle. D’autres essais utilisant l’IRM ont permis de visualiser le phénomène au sein du matériau. Sur la base de ces essais, nous proposons une loi de comportement thermoviscoélastique avec changement de phase pour EB. Un programme aux éléments finis a été développé (Free Fem++)pour intégrer cette loi dans le calcul de structures ; ce code couple les équations mécaniques et de diffusion de la chaleur prenant également en compte le changement de phase à travers la chaleur latente de solidification de l’eau interstitielle.Après validation du logiciel, celui-ci a été appliqué au calcul de structures bitumineuses bicouches représentatives des couches supérieures d’une chaussée. Les résultats mettent alors en évidence l’apparition de contraintes d’arrachement élevées à l’interface entre couches générées par le gel,susceptibles d’expliquer la formation de nids de poule. Un essai de laboratoire sur bicouche a confirmé la fragilisation de l’interface induite dès le premier cycle de gel. / Massive development of potholes occurring in bituminous pavements was observed during winters over short time laps characterized by temperature alternating between positive and highly negative values along with rainfalls. This led us to seek for a specific mechanism of degradation of asphalt concrete (AC) layers, related to the behavior of partially saturated AC subjected to freeze. Two types of laboratory tests were performed under traction free and restrained strain conditions to study the behavior of AC within this context, incorporating lime additive in some mix design formulations. These tests showed the development of large swelling strains or stresses induced by the phase change of pore water into ice. Additional tests using MRI allowed us to visualize this phenomenon from inside the material specimens. Based on these tests, we developed a thermoviscoelastic constitutive law including phase change for partially saturated AC. A Finite Element (FE) program was implemented (FreeFem++) to introduce the developed law instructural calculations; this FE code handles the coupling between mechanics and the heat equation, also taking into account the phase change through the latent heat of crystallization of pore water. After validating the software, this numerical tool was utilized to compute the response of bilayer bituminous structures representative of the upper layers of a pavement. The results obtained show the development of highfrost-induced pull-out stresses located at the interface between the layers, likely to explain the formation of potholes. A test carried out on a bilayer sample confirmed the weakening of the interface right after the first frost cycle.

La construcción de coberturas en zonas alto andinas se ha convertido en una pieza clave para disminuir los pasivos ambientales y, a la vez, contribuir el desarrollo del país gracias a la minería. Gran parte del terreno en estas zonas son suelos arcillosos cuyo comportamiento es impredecible porque presentan cambios de volumen abruptos según la variación de saturación del suelo. Quienes transitan por carreteras en taludes de este tipo de suelo, corren alto riesgo debido al deslizamiento que sufren los taludes cada año. En este tipo de taludes se producen deslizamientos cuando el suelo arcilloso se encuentra parcialmente saturado, ya que en estas condiciones el suelo no es estable. Por ello, se realizaron los estudios de estabilidad de taludes de suelo parcialmente saturado con el método de talud infinito. Se construyó la envolvente de falla del suelo parcialmente saturado con los valores del ensayo del papel filtro y corte directo de acuerdo con la saturación a la que se encuentre sometido. Estos valores serán importantes para el cálculo del factor de seguridad, el cual se obtuvo a partir de una hoja de cálculo propuesta en esta investigación. Finalmente, se validó la hoja de cálculo con el software Geostudio donde se obtuvo una variación dentro del rango de significancia +-5%. Se concluyó que el análisis de estabilidad de talud de cobertura de un suelo parcialmente saturado proporciona un valor de factor de seguridad a partir de un análisis que simula con mayor exactitud el comportamiento del suelo. / The construction of hedges in high Andean areas has become a key element in reducing environmental liabilities and, at the same time, contributing to the development of the country thanks to mining. Much of the terrain in these areas is clay soils whose behavior is unpredictable because they present abrupt volume changes depending on the variation in soil saturation. Those who travel on roads on slopes of this type of soil are at high risk due to the landslide suffered by the slopes every year. In this type of slopes, landslides occur when the clay soil is partially saturated, since under these conditions the soil is not stable. For this reason, the stability studies of partially saturated soil slopes were carried out with the infinite slope method. The partially saturated soil failure envelope was constructed with the values ​​of the filter paper test and direct cut according to the saturation to which it is subjected. These values ​​will be important for the calculation of the safety factor, which was obtained from a spreadsheet proposed in this investigation. Finally, the spreadsheet was validated with the Geostudio software, where a variation was obtained within the range of significance + -5%. It was concluded that the slope stability analysis of a partially saturated soil cover provides a factor of safety value from an analysis that more accurately simulates soil behavior. / Tesis

Cette thèse vise à étudier expérimentalement, analytiquement et numériquement, les conséquences de variations et d'oscillations hydrodynamiques à forte variabilité temporelle en milieux poreux partiellement saturés. Les problèmes que nous étudions comportent des surfaces libres tant à l'extérieur qu'à l'intérieur des milieux poreux, celles-ci étant définies comme des isosurfaces de pression d'eau égale à la pression atmosphérique (Pwater = Patm). Les différentes études expérimentales réalisées en laboratoire sont, respectivement : une expérience d'imbibition dans une boite à sable avec effets capillaires importants; la transmission d'oscillations de la surface libre à travers un massif sableux intercalaire dans un petit canal à houle (IMFT, Toulouse); l'étude de la dynamique et de la propagation des oscillations des niveaux d'eau dans un grand canal à houle (HYDRALAB, Barcelone), partiellement recouvert d'un fond sableux incliné, avec mesures de niveaux d'eau en pleine eau et sous le sable, et mesures du fond sableux (érosion/dépôts). Pour les études théoriques, nous avons développés des solutions analytiques linéarisées. Un exemple de problème traité analytiquement est: l'équation linéarisée de Dupuit-Boussinesq (D-B) transitoire à surface libre, en hypothèse d'écoulements plans et vidange/remplissage instantané : oscillations forcées, transmission et dissipation d'ondes à travers une boite à sable rectangulaire. Nous avons aussi développé une solution de l'équation faiblement non linéaire de Dupuit- Boussinesq (D-B) pour étudier le problème d'imbibition avec variation abrupte du niveau d'eau amont (suivi temporel du front de saturation). Nous avons pu étudier les différents types de problèmes transitoires liés aux expériences citées plus haut par simulation numérique. En particulier, nous avons simulé des écoulements partiellement saturés et insaturés, en coupe verticale, à l'aide d'un code de calcul (BIGFLOW 3D) qui résoud l'équation de Richards généralisée en régime transitoire. Nous avons ainsi étudié numériquement en régime non saturé, l'expérience d'imbibition dans un sable initialement sec à frontières verticales (IMFT sandbox), puis l'expérience de propagation d'ondes dans le grand canal à houle de Barcelone (laboratoire HYDRALAB) comportant une plage de sable inclinée, avec un couplage complètement intégré entre les zones micro-poreuse (sable) et “macro-poreuse” (pleine eau). Pour analyser les résultats de cette dernière expérience et les comparer aux simulations, nous avons utilisé plusieurs méthodes de traitement et d'analyse des signaux : analyse de Fourier (spectres de fréquences) ; ondelettes discrètes multi-résolution (Daubechies) ; analyses corrélatoires simple et croisée. Ces méthodes sont combinées avec des méthodes de préfiltrage pour estimer dérives et résidus (moyennes mobiles ; ondelettes multi-résolution). Cette analyse des signaux a permis de comprendre et quantifier la propagation à travers une plage de sable. Au total, les différentes approches de modélisation mis en oeuvre, associé à des procédures de calage en situation de couplage transitoire non linéaire ont permis de reproduire globalement les phénomènes de propagation de teneur en eau et de niveau d'eau dans les différentes configurations étudiées. / This thesis aims at investigating experimentally, analytically and numerically, the consequences of hydrodynamic variations and oscillations with high temporal variability in partially saturated porous media. The problems investigated in this work involve “free surfaces” both outside and inside the porous media, the free surface being defined as the “atmospheric” water pressure isosurface (Pwater = Patm). The laboratory experiments studied in this work are, respectively: Lateral imbibition in a dry sand box with significant capillary effects; Transmission of oscillations of the free surface through a vertical sand box placed in a small wave canal (IMFT, Toulouse); Dynamics of free surface oscillations and wave propagation in a large wave canal (HYDRALAB, Barcelona), partially covered with sand, with measurements of both open water and groundwater levels, and of sand topography (erosion / deposition). For theoretical studies, we have developed linearized analytical solutions. Here is a sample problem that was treated analytically in this work: The linearized equation of Dupuit-Boussinesq (DB) for transient free surface flow, assuming horizontal flow and instantaneous wetting/drainage of the unsaturated zone: forced oscillations, wave transmission and dissipation through a rectangular sandbox. We also developed a weakly nonlinear solution of the Dupuit-Boussinesq equation to study the sudden imbibition (temporal monitoring of the wetting front). We have studied the different types of transient flow problems related to the experiments cited above by numerical simulation. In particular, we have simulated unsaturated or partially saturated transient flows in vertical cross-section, using a computer code (BIGFLOW 3D) which solves a generalized version of Richards’ equation. Thus, using the Richards / BIGFLOW 3D model, we have studied numerically the experiment of unsaturated imbibition in a dry sand (IMFT sandbox), and then, with the same model, we have also studied the partially saturated wave propagation experiment in the large Barcelona wave canal (HYDRALAB laboratory), focusing on the sloping sandy beach, with coupling between the micro-porous zone (sand) and the “macro-porous” zone (open water). To interpret the results of the latter experiment and compare them to simulations, we use several methods of signal analyzis and signal processing, such as: Fourier analysis, discrete multi-resolution wavelets (Daubechies), auto and cross-correlation functions. These methods are combined with pre-filtering methods to estimate trends and residuals (moving averages; discrete wavelet analyses). This signal analyzis has allowed us to interpret and quantify water propagation phenomena through a sandy beach. To sum up, different modeling approaches, combined with model calibration procedures, were applied to transient nonlinear coupled flow problems. These approaches have allowed us to reproduce globally the water content distributions and water level propagation in the different configurations studied in this work.