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Academic literature on the topic 'Inversion linéaire'
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Journal articles on the topic "Inversion linéaire"
Passilly, N., M. Fromager, K. Aït Ameur, R. Moncorgé, J. L. Doualan, A. Hirth, and G. Quarles. "Mesure du “couplage” indice-inversion à l'origine d'un effet de lentille non-linéaire dépendant du temps dans un laser Cr3+: LiSAF." Journal de Physique IV (Proceedings) 119 (November 2004): 257–58. http://dx.doi.org/10.1051/jp4:2004119084.
Full textLaberge, Danielle, Daphné Morin, Shirley Roy, and Marielle Rozier. "Capacité d’agir sur sa vie et inflexion des lignes biographiques : le point de vue des femmes itinérantes." Santé mentale au Québec 25, no. 2 (January 30, 2007): 21–39. http://dx.doi.org/10.7202/014450ar.
Full textDufour, Jean-Marie, and Malika Neifar. "Méthodes d’inférence exactes pour un modèle de régression avec erreurs AR(2) gaussiennes." Articles 80, no. 4 (January 26, 2006): 593–618. http://dx.doi.org/10.7202/012129ar.
Full textKim, Jang Soo, Karola Mészáros, Greta Panova, and David B. Wilson. "Dyck tilings, linear extensions, descents, and inversions." Discrete Mathematics & Theoretical Computer Science DMTCS Proceedings vol. AR,..., Proceedings (January 1, 2012). http://dx.doi.org/10.46298/dmtcs.3081.
Full textHicks, Angela, and Yeonkyung Kim. "An explicit formula for ndinv, a new statistic for two-shuffle parking functions." Discrete Mathematics & Theoretical Computer Science DMTCS Proceedings vol. AR,..., Proceedings (January 1, 2012). http://dx.doi.org/10.46298/dmtcs.3027.
Full textFlavia Irene, Santamaria,. "“Un estudio multimodal y dinámico de los conocimientos numéricos de estudiantes de primer grado”." RIDAA Tesis Unicen, September 27, 2021. http://dx.doi.org/10.52278/2850.
Full textDissertations / Theses on the topic "Inversion linéaire"
Sladen, Anthony. "Modélisation non-linéaire des grands séismes de subduction." Paris 11, 2005. http://www.theses.fr/2005PA112098.
Full textWith the setting up of seismographic broad-band networks world wide in heighties, it has been possible to study the rupture process using information recorded in far-field. The inversion of seismograms to image the rupture, which is known for being highly non linear, is still commonly analysed using linearized methods. Based on this statement, we have developped an inversion method based on a stochastic algorithm called neighbourhood algorithm which has a certain number of avantages over other widely used algorithms. However, the need for a great number of variables for a kinematic inversion make it difficult to reach a good convergence. The alternative solution is to use a local exploration algorithm, the downhill simplex, in conjunction with the exploration phase. With a view to developping a simple and global method of inversion we use a simplified parametrization of the fault and the seismograms are generated from the ray theory. The methodology, aimed at pratical applications, is also a good way to evaluate the unicity of the problem and its resolution. We then set up a certain number of synthetic tests and used the well studied Antofagasta earthquake (30/07/1995) has a case study. Through this different examples we have concentrated on a certain number of essential points such as the resolution of P wave on the seismic moment, on the lateral and vertical distribution of the seismic rate and on the inversion of rupture velocity. We then invert for two major recent earthquakes : the Peruvian Aréquipa earthquake of the June 23rd, 2001 (Mw=8. 4) and of the Mexican Colima earthquake of January 22nd, 2003 (Mw=7. 6)
Agullo, Yohan. "Inversion stratigraphique multicomposante avant sommation." Paris 11, 2005. http://www.theses.fr/2005PA112338.
Full textThis thesis present the extension of monocomponent seismic prestack data stratigraphic inversion method to multicomponent data, with the objective of improving the determination of reservoir elastic parameters. In addiction to the PP pressure waves, the PS converted waves proved their interest for imaging under gas clouds ; and their potential is highly significant for the characterization of lithologies, fluids, fracturations. . . Nevertheless the simultaneous use of PP and PS data remains problematic because of their different the time scales. To jointly use the information contained in PP and PS data, we propose a method in three steps: first, monocomponent stratigraphic inversions of PP then PS data; second, estimation of the PP to PS time conversion law; third, multicomponent stratigraphic inversion. For the second point, the estimation of the PP to PS conversion law is based on minimizing the difference between the S impedances obtained from PP and PS monocomponent stratigraphic inversion. The prestack monocomponent stratigraphic inversions was adapted to the case of multicomponent data by leaving each type of data in its own time scale in order to avoid the distortion of the seismic wavelet. The results obtained on a realistic synthetic PP-PS case show on one hand that determining PP to PS conversion law (from the monocomponent inversion results) is feasible, and on the other hand that the joint inversion of PP and PS data with this conversion law improves the results compared to the monocomponent inversion ones. Although this is presented within the framework of the PP and PS multicomponent data, the developed methodology adapts directly to PP-SS data for example
Jurado, Fabrice. "Modélisation sismique et inversion non linéaire pour les milieux 3D élastiques tabulaires." Montpellier 2, 1992. http://www.theses.fr/1992MON20244.
Full textSanchez, Reyes Hugo Samuel. "Inversion cinématique progressive linéaire de la source sismique et ses perspectives dans la quantification des incertitudes associées." Thesis, Université Grenoble Alpes (ComUE), 2019. http://www.theses.fr/2019GREAU026/document.
Full textThe earthquake characterization is a fundamental research field in seismology, which final goal is to provide accurate estimations of earthquake attributes. In this study field, various questions may rise such as the following ones: when and where did an earthquake happen? How large was it? What is its evolution in space and time? In addition, more challenging questions can be addressed such as the following ones: why did it occur? What is the next one in a given area? In order to progress in the first list of questions, a physical description, or model, of the event is necessary. The investigation of such model (or image) is the scientific topic I investigate during my PhD in the framework of kinematic source models. Understanding the seismic source as a propagating dislocation that occurs across a given geometry of an active fault, the kinematic source models are the physical representations of the time and space history of such rupture propagation. Such physical representation is said to be a kinematic approach because the inferred rupture histories are obtained without taking into account the forces that might cause the origin of the dislocation.In this PhD dissertation, I present a new hierarchical time kinematic source inversion method able to assimilate data traces through evolutive time windows. A linear time-domain formulation relates the slip-rate function and seismograms, preserving the positivity of this function and the causality when spanning the model space: taking benefit of the time-space sparsity of the rupture model evolution is as essential as considering the causality between rupture and each record delayed by the known propagator operator different for each station. This progressive approach, both on the data space and on the model space, does require mild assumptions on prior slip-rate functions or preconditioning strategies on the slip-rate local gradient estimations. These assumptions are based on simple physical expected rupture models. Successful applications of this method to a well-known benchmark (Source Inversion Validation Exercise 1) and to the recorded data of the 2016 Kumamoto mainshock (Mw=7.0) illustrate the advantages of this alternative approach of a linear kinematic source inversion.The underlying target of this new formulation will be the future uncertainty quantification of such model reconstruction. In order to achieve this goal, as well as to highlight key properties considered in this linear time-domain approach, I explore the Hamiltonian Monte Carlo (HMC) stochastic Bayesian framework, which appears to be one of the possible and very promising strategies that can be applied to this stabilized over-parametrized optimization of a linear forward problem to assess the uncertainties on kinematic source inversions. The HMC technique shows to be compatible with the linear time-domain strategy here presented. This technique, thanks to an efficient estimation of the local gradient of the misfit function, appears to be able to rapidly explore the high-dimensional space of probable solutions, while the linearity between unknowns and observables is preserved. In this work, I investigate the performance of the HMC strategy dealing with simple synthetic cases with almost perfect illumination, in order to provide a better understanding of all the concepts and required tunning to achieve a correct exploration of the model space. The results from this preliminary investigation are promising and open a new way of tackling the kinematic source reconstruction problem and the assessment of the associated uncertainties
Lejri, Mostfa. "Subsurface stress inversion modeling using linear elasticity : sensitivity analysis and applications." Thesis, Montpellier, 2015. http://www.theses.fr/2015MONTS212/document.
Full textToday, one of the main challenges in the oil industry, especially during the exploration phase, is the exploitation of new resources in structurally complex areas such as naturally fractured reservoirs, salt diapirs, mountain ranges, and unconventional reservoirs.We know that the geometry and sliding along active faults modifies the local stress distribution. Knowing the present day perturbed stress field is important for the study of earthquakes, for the planning of the borehole drilling and stability as well as for the prediction of fractures induced by hydro-fracturing and reactivation of natural fractures. In the other side, perturbed paleostress are responsible for the development of (pre-existing) natural fractures. The detection and modeling of the latter, are essential both in the oil industry (migration and trapping of fluids) for a cost efficient recovery of natural reserves.Understanding and quantifying the spatial and temporal development of the stress distribution has a significant economic and environmental impact. The analysis of paleo-constraints was intuitively introduced first by Anderson (1905 & 1942), then in the middle of the last century, Wallace (1951) and Bott (1959) proposed the simple hypothesis that (i) The stress field is homogeneous in space and constant in time, and that (ii) the slip direction is parallel to the traction projected on the fault plane which gives the direction of the shear stress. Many stress inversion methods are based on this hypothesis while recent studies raise doubts as to their compatibility with rock mechanics.In order to investigate the validity of the Wallace and Bott hypothesis, a comparison with vectors of slip generated with numerical models (BEM) is performed. By testing the influence of multiple parameters (geometry, boundary conditions, friction, Poisson’s coefficient , half-space, fault fluid pressure), it is shown that the complex geometry faults subject to specific boundary conditions can yield slip vectors with significant discrepancies with the maximum shear stress resolved on the fault plane. Conversely, the presence of a high sliding friction, allows under certain conditions, to validate the hypothesis of Wallace and Bott.We then focus on the task to compare the results of stress inversions based on the assumption of Wallace and Bott (called classical stress inversion methods) to a geomechanical method. For this, a complex fault geometry is used in a sensitivity analysis (boundary conditions, friction, sampling) to evaluate the uncertainty of the results of the two inversion methods. This analysis is then compared to a case study, Chimney Rock (Utah, USA), showing the advantages and disadvantages of the classical stress inversion methods.One of the main challenges of the oil industry is the exploitation of resource in structurally complex oil fields such as naturally fractured reservoirs. Knowing the heterogeneous paleostress allows to optimize the modeling of these natural fractures. Since slip on faults is hardly observed in petroleum reservoirs, fracture orientation data (joints, faults, stylolites) are naturally taken into account during the inversion of stresses. It is shown, using various field and industry examples, that in such cases the use of mechanical stress inversions is much more appropriate.However, it is sometimes difficult to determine the fracture kinematics observed along wellbores, and very often the studied regions underwent multiple tectonic phases. The final section aims to address the problem of data with unknown kinematic (joints, faults, stylolites ...) and expends the mechanical stress inversion to the separation of tectonic phases
Kormendi, Françoise. "Inversion non linéaire de sismogrammes TAU-P en milieu stratifié élastique à l'aide du critère des moindres carrés." Brest, 1989. http://www.theses.fr/1989BRES2009.
Full textCrusem, René. "Simulation de signaux sismiques et étude de sources nucléaires souterraines par inversion de moments." Châtenay-Malabry, Ecole centrale de Paris, 1986. http://www.theses.fr/1986ECAP0054.
Full textPašović, Mirza. "Tissue harmonic reduction : application to ultrasound contrast harmonic imaging." Thesis, Lyon 1, 2010. http://www.theses.fr/2010LYO10060.
Full textUltrasound contrast agents are small micro bubbles that respond nonlinearly when exposed to ultrasound wave. The nonlinear response gives possibility of harmonic ultrasound images which has many advantages over fundamental imaging. However, to increase ultrasound contrast harmonic imaging performance we must first understand nonlinear propagation of ultrasound wave. Nonlinear propagation distorts the propagating wave such that higher harmonics appear as the wave is propagating. The theory that was laid down, was allowed implementing a new method of modelling nonlinear ultrasound propagation. The knowledge obtained during this process was used to construct a multiple component second harmonic reduction signal for reduction of their harmonics generated due to the tissue nonlinearities. As a consequence detection of ultrasound contrast agents at higher harmonics was increased. Further more, a powerful ultrasound imaging technique called Pulse Inversion, was further enhanced with multiple component second harmonic reduction signal. What was learned during investigation of the Pulse Inversion, technique lead to a new phase coded ultrasound contrast harmonic method called second harmonic inversion;. Also it was noted that for different type of media the level of distortion of ultrasound pulse is different. It depends largely on the nonlinear parameter B / A. Although the work on this parameter has not been finished it is very important to continue in this direction since B / A imaging with ultrasound contrast agents has a lot of potential
Lévesque, Martin. "Modélisation du comportement mécanique de matériaux composites viscoélastiques non linéaires par une approche d'homogénéisation." Paris, ENSAM, 2004. https://pastel.archives-ouvertes.fr/pastel-00001237.
Full textThe main objective of this thesis is to develop a model, based on homogenisation, for predicting the mechanical response of nonlinear viscoelastic composites. The model is applied to a glass beads reinforced polypropylene in which the beads are randomly distributed. The initial part of the thesis is concerned with the development of a three dimensional nonlinear viscoelastic constitutive law that can be applied to this polypropylene composite. The second stage of the thesis deals with the development and identification of the homogenisation model while this theoretical model is presented in Chapter Three. This approach allows material models, for which the response does not depend on the load history, to be applied to nonlinear viscoelastic materials. The approach involves transforming the initial nonlinear viscoelastic problem into one which is linear viscoelastic with a history of stress-free deformations. This problem is solved with the linear viscoelastic correspondence principle and Laplace-Carson transforms. Chapter Four deals with the numerical implementation of such a model. The implementation is achieved in such a way that the comparison materials, which represent the new linear viscoelastic problem, satisfy all thermodynamic requirements. Moreover, a new algorithm has been developed to numerically invert the Laplace-Carson transforms with good accuracy. The final part of the thesis validates the theoretical model through means of finite element models of typical microstructures and the numerical implementation of the nonlinear viscoelastic constitutive law. Comparisons are also presented between the predictions of the homogenisation model, the fi(…)
Saari, Hammoud. "Commande répétitive de procédés échantillonnés à déphasage non minimal." Chambéry, 1996. http://www.theses.fr/1996CHAMS006.
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