Letteratura scientifica selezionata sul tema "Thermo-Rhéologie"
Cita una fonte nei formati APA, MLA, Chicago, Harvard e in molti altri stili
Consulta la lista di attuali articoli, libri, tesi, atti di convegni e altre fonti scientifiche attinenti al tema "Thermo-Rhéologie".
Accanto a ogni fonte nell'elenco di riferimenti c'è un pulsante "Aggiungi alla bibliografia". Premilo e genereremo automaticamente la citazione bibliografica dell'opera scelta nello stile citazionale di cui hai bisogno: APA, MLA, Harvard, Chicago, Vancouver ecc.
Puoi anche scaricare il testo completo della pubblicazione scientifica nel formato .pdf e leggere online l'abstract (il sommario) dell'opera se è presente nei metadati.
Articoli di riviste sul tema "Thermo-Rhéologie":
CHARLES, Antoine, Thierry RIBEIRO, Marcos OLIVEIRA, Sam AZIMI, Vincent ROCHER, Jean-Christophe BAUDEZ e S. Amir BAHRANI. "Mieux comprendre l’écoulement des boues digérées : rôle de la viscosité et de la température". Techniques Sciences Méthodes 10, n. 10 (20 ottobre 2023): 35–45. http://dx.doi.org/10.36904/tsm/202310035.
Tesi sul tema "Thermo-Rhéologie":
Boudet, Chantal. "Systèmes mixtes gélatine/polymère thermo-sensible : contrôle de la gélification chimique et propriétés des films". Paris 6, 2005. http://www.theses.fr/2005PA066018.
Bailly, Laurence. "Etude du comportement de deux grades cyanates esters pour des applications structurales en matériaux composites en environnement tiède". Thesis, Toulouse, INPT, 2019. http://www.theses.fr/2019INPT0064.
Composite materials made of cyanate ester resins and in particular phenolic triazine resins such as PT15 and PT30 are selected to replace structural metal parts in aircraft at operating temperatures between 200 and 300°C. The main advantages of these resins are their high glass transition temperature, above 300°C, and their low viscosity at 80°C make them suitable for Resin Transfert Molding (RTM) process. The main goals of this work are to understand the resins’ behavior during crosslinking and then to study their durability through thermo-oxidative aging at operating temperatures. Physico-chemical characterizations of PT15 and PT30 resins at their initial state showed a similar chemical composition and spatial configuration but a different molar mass distribution. Triazine rings have only been detected in PT30 only, indicating a “pre-cured” state. These differences have consequences on the crosslinking kinetics and promote an autocatalytic mechanism for PT30. After cure optimization, PT15 has a glass transition temperature 70°C lower than the one of PT30. Among different analysis techniques, the rheological study during crosslinking provided an understanding of the networks’ structuration dissimilarities between the two grades, highlighting the formation of an intermediate structure which relaxes at lower temperatures in PT15. This different networks’ organization is the key element to understand dissimilar thermal stabilities analyzed during thermo-oxidative aging
Heinrich, Alban. "Modélisation thermomécanique de la coulée continue d'acier en 2 dimensions". Paris, ENMP, 2003. https://pastel.archives-ouvertes.fr/pastel-00001342.
In this work, we introduce a thermo-mechanical model of the steel continuous casting process, in two dimensions. With our approach, it is possible to obtain thermo-mechanical steady-state solution of the process, for the whole product. The thermo-mechanical history of the product can thus be deduced, by viewing the stress and temperature fields, for instance. One of the expected results deals with the bulging between rolls, which is known to give birth to segregation phenomena. We base our study on the global non steady-state strategy using a Lagrangian approach. The flow of matter in the studied domain is simulated through one injection tool located in the upper face of the domain. The lower face is supposed to be driven down at the starting block velocity. Thus the matter is led throughout the CC machine. Concerning the model, non-steady thermo-mechanical conservation equations are solved. The thermal problem is for the enthalpy variable. The approach to the mechanical problem is of monophasic type (velocity and pressure are the unknows). In our approach, natural convection and macrosegregation are neglected. Solid, mushy and liquid states obey respectively to elasto-viscoplastic, viscoplastic and Newtonian behaviours. The rheology of the solid state is calculated thanks laws from the litterature. The liquid and mushy states are modelled with high consistencies so that natural convection may be neglected. These developments have been validated on industrial cases, showing a good qualitative and quantitative agreement
Derouineau, Thibault. "Synthèse et étude de polymères thermo-associatifs pour le domaine des lubrifiants". Thesis, Paris Sciences et Lettres (ComUE), 2017. http://www.theses.fr/2017PSLET018.
Controlling the viscosity of engine lubricants is a key issue to reduce the fuel consumption of engines. A new approach based on the use of thermo-associative polymers has been developed in order to compensate the natural loss of viscosity of lubricants when the temperature increases. To this aim, complementary low molecular weight polymers (for engine targeted application) that can reversibly associate with temperature through the diol-boronic ester exchange reaction have been designed and synthesized. The low molecular weights of the polymers and the dynamic behavior of the boronic ester bond decrease the high shear sensitivity of the system and so limits the shear-thinning behavior of the lubricant. The increase of polymeric function availability as the temperature rises induces polymer association. The reversibility of the thermo-associative association of polymers in non polar oil is seen over several cycles of warming-cooling with the increase of the relative viscosity of the solutions with increasing temperature. Part of the study was also dedicated to the improvement of polymers’ thermal stability in order to maintain the good lubricant properties of the thermo-associative formulations up to 150°C. Many polymers of different natures, sizes and topologies have been synthesized. The flow behavior of these polymers in both individual state in solution or in thermo-associative formulations was studied by rheology, thus enabling to determine the impact of these levers on the solutions properties as a function of temperature
Derouineau, Thibault. "Synthèse et étude de polymères thermo-associatifs pour le domaine des lubrifiants". Electronic Thesis or Diss., Paris Sciences et Lettres (ComUE), 2017. http://www.theses.fr/2017PSLET018.
Controlling the viscosity of engine lubricants is a key issue to reduce the fuel consumption of engines. A new approach based on the use of thermo-associative polymers has been developed in order to compensate the natural loss of viscosity of lubricants when the temperature increases. To this aim, complementary low molecular weight polymers (for engine targeted application) that can reversibly associate with temperature through the diol-boronic ester exchange reaction have been designed and synthesized. The low molecular weights of the polymers and the dynamic behavior of the boronic ester bond decrease the high shear sensitivity of the system and so limits the shear-thinning behavior of the lubricant. The increase of polymeric function availability as the temperature rises induces polymer association. The reversibility of the thermo-associative association of polymers in non polar oil is seen over several cycles of warming-cooling with the increase of the relative viscosity of the solutions with increasing temperature. Part of the study was also dedicated to the improvement of polymers’ thermal stability in order to maintain the good lubricant properties of the thermo-associative formulations up to 150°C. Many polymers of different natures, sizes and topologies have been synthesized. The flow behavior of these polymers in both individual state in solution or in thermo-associative formulations was studied by rheology, thus enabling to determine the impact of these levers on the solutions properties as a function of temperature
Mezri, Leila. "Rôle des fluides pendant l'exhumation continentale : modélisation hydro-thermo-mécanique". Thesis, Paris 6, 2016. http://www.theses.fr/2016PA066175.
Strain localization is essential to the existence of plate tectonic on Earth. Yet, it is the result of non-linear interaction across several temporal and spatial scales and to date no unique rheological model exists that captures the effect of all these interactions at crustal scale. The work presented here is an attempt to fill part of the gap between out- crop scale and crustal scale models, between petrological scale and crustal scale. The central question is how to measure the effects of fluids and fluid-rock interactions on the dynamics and the kinematics of continental metamorphic core complexes by the mean of crustal scale numerical models. To answer this question, we have tried to esta- blish an empirical model of fluid flow and fluid-rock interaction, which could be valid at the scale of the crust. At that specific scale, it is important to capture the effects of free fluids both on the density of rocks, because it determines the body forces that are driving the exhumation of the crust, and on the strength of rocks and particularly on shear zones which constitute the ’hand-break’, the surface tractions, which resist this exhumation. This empirical model is based on a first order observation related to the behaviour of metamorphic rocks along the retrograde P − T path of their exhumation. High-grade metamorphic rocks (amphibolite/granulite) are indeed exhumed to the sur- face with very little retromorphose except those located within the shear bands where deformation localises. This works first consisted in parameterising this observation in a manner that could be implemented into a 2D thermo-mechanical code as an hydro- thermo-mechanical coupling which could account for free-water/rock-water exchange. In second part, a simplified scheme is introduced to account for hydrothermal cooling of the crust in the late stage of exhumation. The results show that this parameterization al- lows to better account for field observation in a range of parameters that are compatible with laboratory experiments. Limiting the retromorphose of rocks by the availability of free water is shown to produce significantly different metamorphic domes kinematics as compared to prior studies. We indeed demonstrate that it is not necessary to introduce heterogeneity in crustal composition to form asymmetric structures but that the effect of water is modulated by the chemistry of the protolith rocks which influences strain localization
Charles, Antoine Henri Etienne. "Étude thermo-rhéologique de boues digérées : application à l’écoulement en conduite dans les procédés de méthanisation". Electronic Thesis or Diss., Ecole nationale supérieure Mines-Télécom Lille Douai, 2023. http://www.theses.fr/2023MTLD0008.
The society’s wastewater treatment needs are met by waste water treatment plants that produce sludges. In order to anticipate the increase in this requirement in the future, the sludge treatment processes must achieve a certain level of efficiency in terms of sludge treatment and recovery. The anaerobic digestion process significantly reduces the volume of sludge generated and can the be used for agricultural and energy purposes, in the form of digestate, biogas, electricity or heat. It is nevertheless limited by ineffective control of the transport of digested sludge within it, due to a lack of knowledge of thermo-rheology, in terms of understanding and characterisation methods, and of the hydrodynamics involved in handling these very diverse sludges. This manifests itself operationally, downstream of the sizing and design phase, in inefficient pumping, matrix heterogeneity or component clogging.It is in this context of providing scientific elements, on the one hand of the therm-rheological characerisation of digested sludge and on the other hand of the demonstration of the hydrodynamics of these fluids in operation, that the research work carried out within the framework of this thesis falls within the scope of.Firstly, protocols dedicated to the specific characterisation of each non-Newtonian behaviour have been established. The application of these protocols, at the ITM Nord Europe – Energy Environment research centre and on the industrial partner’s Characterisation plateform, shows that the thermo-rheological characteristics of digested sludge are accurately modelled by a non-modified Herschel-Bulkley model. Yield stress and shear-thinning are significantly more important than the other thermo-rheological characteristics of thixotropy, viscoelasticity and thermo-dependence. The unanticipated physical phenomon of wall slip is observed in these digested sludges, leading to heterogeneous flow hydrodynamics under conditions of low inertia and loaw wall roughness.Secondly, an experimental set-up dedicated to studying the flow of such fluids in pipe is being set up, with a visualisation to determining their hydrodynamic behaviour. Using working fluids (Carbopol solutions), it was demonstrated that these fluids undergo a rheo-inertial transition (RIT) towards turbulence. This transition is characterised by the existence of a pre-transition regime, non-existent for a Newtonian fluid, within which the flow exibits an asymmetry, which is observed by direct visualisation. These visualisations, coupled with the measurement of pressure drops, also make it possible to quantify the intermittency of the RIT on the basis of the turbulent structures visualised. This makes it possible to control the movement of such fluids through knowledge of the stabilisation of their flows and the increase in the residence time of turbulent structures, due to the non-Newtonian characteristics without viscoelasticity.Thus, this thesis manuscipt summarises the scientific elements developed within the framework of this thesis to respond to the problems of the operational obstacles encountered. As these problems stem from a lack of fundamental knowledge of the thermo-rheology and hydrodynamics of the sludge that flows through it, the study focuses its research on these two areas in order to provide the fundamentals that will make it possible to improve the control of sludge transport within the anaerobic digestion process in wastewater treatment plants
Hertgen, Solenn. "Comportement mécanique des roches et dynamique des lithosphères dans les zones de convergence". Thesis, Rennes 1, 2018. http://www.theses.fr/2018REN1B070/document.
Convergence zones are key objects to the understanding of the lithosphere dynamics. They are the location correspond to places of intense deformation as evidenced by the concentration and magnitude of recorded earthquakes. On a larger scale of time and space, these deformations generally result in nappes stacking whose study offers access to the different structural levels involved in the mountain belt structuration. Precisely characterizing the structuring dynamics of these units as well as the parameters controlling this dynamic is a crucial step that would allow in particular a better quantification of lithospheric dynamics. The aim of this thesis is twofold: (1) clarifying the rheological behavior of rocks in the Pressure-Temperature (P-T) conditions of the eclogitic facies at the subduction interface and (2) characterizing and quantifying the influence of the overriding plate rheology, and more specifically, the role of its crustal part, on the spatio-temporal evolution of convergence zones. For this, I used a multi-disciplinary approach. First, I present a multi-scale analysis combining fieldwork and metamorphic petrology, which allowed me to study the deformation within High Pressure-Low Temperature (HP-LT) rocks at the subduction interface in the Mont-Emilius klippe (Western Alps, Italy). Then, I show the results of a quantitative study combining 3D and 2D thermo-mechanical modeling of convergence zones. The entire set of models allowed me to analyze different parameters influencing the rheological structure of the overriding plate, such as the initial geotherm, the thicknesses of the lithosphere and the crust, and the nature of the involved materials. All the performed models are constrained/compared by/with data from natural examples. The results of the study on deformed rocks within the subduction interface highlight the possible brittle behavior of rocks at pressure and temperature conditions on the order of 2.15-2.40 GPa and 500-550 °C, i.e., in the eclogitic facies. The recording of such a deformation mode is of paramount importance because it challenges the paradigm of subduction interface caracterized by ductile behavior without resistance. The results obtained with the numerical models show that the rheology of the overriding plate, as well as that of only its crustal part, has a first-order influence on the overall dynamics of the convergence zones by modifying the mode of subduction, trench kinematics, the mode of exhumation during collision, the timing for slab break-off and back-arc basin formation, the location and intensity of deformation within the overriding plate. The combination of petrology and numerical modeling methods allowed me to obtain a quantified analysis of the influence of the rheology of the lithospheres involved in convergence zones on the dynamics of these zones. This thesis presents new constraints for our understanding of the mechanical response of the lithosphere at different spatial scales as a function of its rheological structure. The new data presented here reveal the major impact of the lithosphere rheology in convergence zones. This parameter leads us to reconsider our current view of the convergence zones
Mezri, Leila. "Rôle des fluides pendant l'exhumation continentale : modélisation hydro-thermo-mécanique". Electronic Thesis or Diss., Paris 6, 2016. http://www.theses.fr/2016PA066175.
Strain localization is essential to the existence of plate tectonic on Earth. Yet, it is the result of non-linear interaction across several temporal and spatial scales and to date no unique rheological model exists that captures the effect of all these interactions at crustal scale. The work presented here is an attempt to fill part of the gap between out- crop scale and crustal scale models, between petrological scale and crustal scale. The central question is how to measure the effects of fluids and fluid-rock interactions on the dynamics and the kinematics of continental metamorphic core complexes by the mean of crustal scale numerical models. To answer this question, we have tried to esta- blish an empirical model of fluid flow and fluid-rock interaction, which could be valid at the scale of the crust. At that specific scale, it is important to capture the effects of free fluids both on the density of rocks, because it determines the body forces that are driving the exhumation of the crust, and on the strength of rocks and particularly on shear zones which constitute the ’hand-break’, the surface tractions, which resist this exhumation. This empirical model is based on a first order observation related to the behaviour of metamorphic rocks along the retrograde P − T path of their exhumation. High-grade metamorphic rocks (amphibolite/granulite) are indeed exhumed to the sur- face with very little retromorphose except those located within the shear bands where deformation localises. This works first consisted in parameterising this observation in a manner that could be implemented into a 2D thermo-mechanical code as an hydro- thermo-mechanical coupling which could account for free-water/rock-water exchange. In second part, a simplified scheme is introduced to account for hydrothermal cooling of the crust in the late stage of exhumation. The results show that this parameterization al- lows to better account for field observation in a range of parameters that are compatible with laboratory experiments. Limiting the retromorphose of rocks by the availability of free water is shown to produce significantly different metamorphic domes kinematics as compared to prior studies. We indeed demonstrate that it is not necessary to introduce heterogeneity in crustal composition to form asymmetric structures but that the effect of water is modulated by the chemistry of the protolith rocks which influences strain localization
Costes, Frédéric. "Modélisation thermomécanique tridimensionnelle par éléments finis de la coulée continue d'aciers". Phd thesis, École Nationale Supérieure des Mines de Paris, 2004. http://pastel.archives-ouvertes.fr/pastel-00001334.