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This work deals with the analysis of reinforced concrete structures according to the currently valid standard EN 1992-1-1 (EC 2) compared with the analysis according to the American standard ACI 318-08. Static solution includes an assessment of slab in local supports, calculation of columns and footings according to 1st critical state for both standards. The slab is also assessed according to the 2st critical state according to EC 2.

Continental glaciers covered as much as thirty percent of the present-day inhabited earth during the Quaternary period. Traditionally, one-dimensional consolidation has been considered as the main process of formation for the soils deposited during glaciation. One of the outcomes of accepting one-dimensional consolidation as the main process of formation is that the geomechanical properties of soil in a horizontal plane are isotropic (known as cross-anisotropy). Recent measurements of subglacial pore pressure and preconsolidation pressure profile have indicated that this might not be the case. The role of subglacial shear action has probably been long neglected. The main objective of this research is to investigate the effects of subglacial shearing on the geomechanical properties of glaciated soils. <p> Recent research has found evidence of horizontal property anisotropy associated with the direction of the ice-sheet movement. A testing program was thus proposed to explore the relationship between the anisotropy of property and the direction of past glacier movement. The program involves several fundamental engineering parameters of soils. These parameters together with the corresponding test methods are as follows: (i) Conventional oedometer test yield stress anisotropy; (ii) Oedometer test with lateral stress measurement stiffness anisotropy; (iii) Load cell pressuremeter (LCPM) test in situ stress anisotropy. <p> The physical meaning of yield stress determined by conventional oedometer tests was interpreted as the critical state of structural collapse. The literature review and an experimental study on kaolin samples with a known stress history suggested that yield stress possesses certain dependency on the sampling direction. The anisotropy of yield stress for Battleford till from Birsay, Saskatchewan was also explored by testing directional oedometer samples. In addition, the anisotropy of stiffness was also investigated using a newly developed lateral stress oedometer that is capable of independent measurement of horizontal stresses at three different points with angles of 120 degrees. Preliminary evidence of a correlation between the direction of maximum stiffness in a horizontal plane and the known direction of glacial shear was observed. The correlation between the direction of maximum yield stress and known direction of glaciation was rather poor. Anisotropy of in situ stresses was investigated by conducting LCPM tests in Pot clay in the Netherlands. Based on the LCPM test results, it was concluded that the evidence of a correlation between the anisotropy of in situ stress and known direction of glacial advance is still rather obscure. <p> Although both the laboratory studies and field studies cannot sufficiently confirm the existence of lateral anisotropy of geomechanical properties and its relationship to the direction of the Quaternary ice-sheet movement, the effects of subglacial shearing should not be neglected in assessing the geotechnical properties of glaciated soils. In practice, it is usually found that the preconsolidation pressure profile does not follow the gravitational line as predicted by the one-dimensional consolidation theory and its magnitude is not compatible with the measured effective pressure values at the base of the glacier. It has been suggested that changes in seepage gradient (upward or downward) are responsible for the deviation of preconsolidation pressure profile away from the gravitational line. In this thesis, a new glacial process model consolidation coupled shearing was proposed. This model is based on the framework of traditional soil mechanics (critical state theory, Modified Cam-clay model and one-dimensional consolidation theory) and is consistent with the general geological and glaciological evidences. This model may provide an alternative explanation for the preconsolidation pressure patterns generally observed in practice. It can also be combined with groundwater flow characteristics to explain the diversity of the preconsolidation consolidation patterns. The proposed model was used successfully to obtain the preconsolidation pressure profile observed in Battleford till at Birsay and the subglacial shear-softening phenomenon.

Continental glaciers covered as much as thirty percent of the present-day inhabited earth during the Quaternary period. Traditionally, one-dimensional consolidation has been considered as the main process of formation for the soils deposited during glaciation. One of the outcomes of accepting one-dimensional consolidation as the main process of formation is that the geomechanical properties of soil in a horizontal plane are isotropic (known as cross-anisotropy). Recent measurements of subglacial pore pressure and preconsolidation pressure profile have indicated that this might not be the case. The role of subglacial shear action has probably been long neglected. The main objective of this research is to investigate the effects of subglacial shearing on the geomechanical properties of glaciated soils. <p> Recent research has found evidence of horizontal property anisotropy associated with the direction of the ice-sheet movement. A testing program was thus proposed to explore the relationship between the anisotropy of property and the direction of past glacier movement. The program involves several fundamental engineering parameters of soils. These parameters together with the corresponding test methods are as follows: (i) Conventional oedometer test yield stress anisotropy; (ii) Oedometer test with lateral stress measurement stiffness anisotropy; (iii) Load cell pressuremeter (LCPM) test in situ stress anisotropy. <p> The physical meaning of yield stress determined by conventional oedometer tests was interpreted as the critical state of structural collapse. The literature review and an experimental study on kaolin samples with a known stress history suggested that yield stress possesses certain dependency on the sampling direction. The anisotropy of yield stress for Battleford till from Birsay, Saskatchewan was also explored by testing directional oedometer samples. In addition, the anisotropy of stiffness was also investigated using a newly developed lateral stress oedometer that is capable of independent measurement of horizontal stresses at three different points with angles of 120 degrees. Preliminary evidence of a correlation between the direction of maximum stiffness in a horizontal plane and the known direction of glacial shear was observed. The correlation between the direction of maximum yield stress and known direction of glaciation was rather poor. Anisotropy of in situ stresses was investigated by conducting LCPM tests in Pot clay in the Netherlands. Based on the LCPM test results, it was concluded that the evidence of a correlation between the anisotropy of in situ stress and known direction of glacial advance is still rather obscure. <p> Although both the laboratory studies and field studies cannot sufficiently confirm the existence of lateral anisotropy of geomechanical properties and its relationship to the direction of the Quaternary ice-sheet movement, the effects of subglacial shearing should not be neglected in assessing the geotechnical properties of glaciated soils. In practice, it is usually found that the preconsolidation pressure profile does not follow the gravitational line as predicted by the one-dimensional consolidation theory and its magnitude is not compatible with the measured effective pressure values at the base of the glacier. It has been suggested that changes in seepage gradient (upward or downward) are responsible for the deviation of preconsolidation pressure profile away from the gravitational line. In this thesis, a new glacial process model consolidation coupled shearing was proposed. This model is based on the framework of traditional soil mechanics (critical state theory, Modified Cam-clay model and one-dimensional consolidation theory) and is consistent with the general geological and glaciological evidences. This model may provide an alternative explanation for the preconsolidation pressure patterns generally observed in practice. It can also be combined with groundwater flow characteristics to explain the diversity of the preconsolidation consolidation patterns. The proposed model was used successfully to obtain the preconsolidation pressure profile observed in Battleford till at Birsay and the subglacial shear-softening phenomenon.

Der Feinkornanteil von Sanden ist einer der Einflussparameter für die Verflüssigungsneigung, welche hier anhand von Kennlinien im Rahmen des critical-state Konzeptes quantifiziert wird. Das durchgeführte Versuchsprogramm umfasste hauptsächlich statische undrainierte triaxiale Kompressionsversuche, ergänzt durch drainierte statische Triaxialversuche. Diese wurden an Hostun Sand, reinem Schluff, und Mischungen aus beiden jeweils in einem Dichtebereich von etwa 28% bis 90% relativer Lagerungsdichte durchgeführt. Die Lage und Funktion des critical-state locus (CSL) unterschiedet sich maßgeblich in den Bereichen ober- und unterhalb eines Grenzfeinkorngehaltes. Jeweils für den Bereich unterhalb und oberhalb des Grenzfeinkorngehaltes wurde eine normalisierte CSL (äquivalente CSL) ermittelt, die es erlaubt, die Verflüssigungsneigung für verschiedene Feinkorngehalte im Gültigkeitsbereich der äquivalenten CSL zu ermitteln.

[pt] Muitos autores concordam que areias em estado fofo, sob carregamento não drenado crescente e granulometria favorável à liquefação, necessariamente liquefazem em algum momento. Este trabalho tem como objetivo principal avaliar se duas amostras de areia, com características muito distintas uma da outra, submetidas às mesmas condições descritas acima, entram em liquefação. A primeira amostra é uma areia limpa que foi extraída de um aterro hidráulico localizado em Camboinhas, Niterói, RJ, Brasil. A segunda é um rejeito arenoso de ferro extraído de uma barragem de rejeitos localizada em Mariana, MG, Brasil. As avalições foram feitas através de ensaios de compressão triaxial com deformação controlada. Avaliou-se o comportamento desses materiais em condições de baixa compacidade e sob diferentes tensões de confinamento, com a finalidade de observar se ocorreria a liquefação. Em caso de não ocorrência da liquefação, o objetivo era compreender os motivos de tal resposta e no caso de ocorrência, avaliar a influência da tensão de confinamento, assim como delimitar as zonas de instabilidade não drenada. Verificou-se que a areia de Camboinhas entrou em liquefação total apenas para tensões de confinamento baixas, e apresenta comportamento oposto ao comportamento normal de solos arenosos fofos, tendo baixa resistência à liquefação em baixa tensão de confinamento e alta resistência à liquefação em grandes tensões de confinamento. O rejeito arenoso de Mariana entrou em liquefação total em tensões de confinamento baixas e altas. O rejeito apresentou comportamento diferente da areia de Camboinhas e semelhante ao comportamento normalmente obtido em solos arenosos fofos sob condições não drenadas. / [en] Many authors agree that loose sands, under increasing undrained loading and liquefaction favorable granulometry, necessarily liquefy at some moment. This work has as main objective to evaluate if two sand specimens, with characteristics very different from each other, under the same conditions as described above, enter into liquefaction. The first specimen is a clean sand that was extracted from a hydraulic embankment located in Camboinhas, Niterói, RJ, Brazil. The second is a sandy tailing of iron extracted from a tailing dam located in Mariana, MG, Brazil. The evaluations were made through triaxial compression tests with controlled deformation. The behavior of these materials was evaluated under conditions of low compactness and under different confininig pressure, in order to observe if liquefaction would occur. In case of no liquefaction, the objective was understand the reasons for such response and in case of occurrence, evaluate the influence of the confining pressure, as well as mark the zones of instability undrained. It was verified that the Camboinhas sand entered in total liquefaction only for low confining pressure, and it has the opposite behavior to the normal behavior of loose granular soils, having low strength to liquefaction in low confining pressure and high strength to liquefaction in large confining pressure. The Mariana granular tailing also entered in total liquefaction for low and higth confinig pressure. The tailing showed different behavior of the Camboinhas sand and similar to the behavior normally obtained in loose granular soils under undrained conditions.

O presente trabalho de pesquisa aborda a aplicação de análise por elementos finitos a maciços escavados por túneis, revisando relevantes estudos sobre análise numérica deste tipo de obra e realizando modelagem numérica própria, bi e tridimensional, voltada ao caso do Túnel Paraíso do Metrô de São Paulo (obra com dados de instrumentação e de ensaios), com uso do consagrado programa de elementos finitos Imperial College Finite Element Program (ICFEP), desenvolvido nos últimos trinta anos no Imperial College de Londres. Dentre os modelos constitutivos adotados nestas análises, destaca-se o Cinemático com Duas Superfícies Modificado do Imperial College, modelo elasto-plástico com endurecimento cinemático e isotrópico, baseado no estado crítico, com grande capacidade de representar as características de rigidez de argilas sobreadensadas (como são as argilas da região do Túnel Paraíso), cujas principais características são levantadas através de revisão bibliográfica. Da observação da etapa de reprodução numérica de ensaios e dos resultados conseguidos com as análises da escavação do túnel, são feitas considerações sobre o desempenho de todos os modelos constitutivos adotados (além do Cinemático com Duas Superfícies Modificado, o Cam-Clay Modificado e o elasto perfeitamente plástico com critério de ruptura de Mohr-Coloumb), bem como sobre a performance dos modelos numéricos desenvolvidos. / This research approaches the application of finite element analysis to tunnel excavation, making a survey of some numerical relevant studies of this kind of construction and performing a range of plane-strain and three-dimensional analyses, focused on the Paraíso Tunnel from Sao Paulo Underground (with field instrumentation and lab tests), using a powerful finite element program, the Imperial College Finite Element Program (ICFEP), developed in the last thirty years at Imperial College London. Among the constitutive models adopted in those analyses, it is highlighted the Modified Two Surfaces Kinematic from Imperial College, a elasto-plastic model with kinematic and isotropic hardening, based on the critical state, with great ability to represent the pre-failure stiffness of overconsolidated clays (as are the clays around Paraíso Tunnel), whose main features are raised through a literature survey. From the results of numerical simulation of lab tests and from the predictions of the tunnelling analyses, it is discussed the performance of all constitutive models adopted (including Modified Cam-Clay and elastic perfectly plastic model with Mohr-Coloumb failure criterion) and of the numerical models developed.

Procurando diminuir as incertezas a respeito do comportamento de estacas em perfis arenosos, desenvolveu-se um campo experimental localizado em Araquari-SC, conduzido pela Universidade Federal do Rio Grande do Sul, no qual foram executados (a) ensaios de campo para definir as condições geotécnicas do solo, (b) estacas escavadas e hélice continua e (c) provas de carga estática nos elementos estruturais. O presente trabalho tem como objetivo estudar as variáveis que intervêm no mecanismo de transferência de carga ao solo. Mediante ensaios de laboratório, caracterizou-se o solo presente no campo experimental, definiram-se os parâmetros de resistência, mineralogia, forma, distribuição e tamanho das partículas, para serem usadas na retro análise do coeficiente de pressão de solo (ks) das provas de carga. Para esta finalidade foram analisados os resultados medidos em estacas escavadas executadas com bentonita e polímero. A retro análise foi realizada através do método beta (β), abordagem que permite a obtenção da capacidade lateral das estacas construídas em perfis arenosos, baseado nas tensões verticais, no coeficiente de pressão de solo e no ângulo de atrito da interface solo-estaca. Devido à interação entre as partículas do solo e concreto da estaca, estas são mobilizadas a elevados níveis de deformações, o ângulo de atrito da interface é considerado próximo ao ângulo de atrito no estado crítico da areia. O solo presente no campo experimental corresponde a areia fina com lentes de silte. Assim, os parâmetros de resistência definidos foram o ângulo de atrito no estado crítico e de pico com valores de 33,0° e 33,4° respetivamente. O ângulo no estado crítico foi utilizado na retro análise das provas de carga e como resultado foi obtido o ks, para posteriormente ser comparado ao coeficiente de empuxo no repouso (k0). Os resultados mostraram que com a profundidade o valor ks aproxima-se ao valor de k0, apresentado uma relação de ks/k0 próxima a unidade. Conclui-se que, o mecanismo de transferência de carga entre o solo e a estaca pode ser avaliado em função das tensões iniciais do depósito, expressas a partir de k0 estimado com base nos ensaios de laboratório. / In order to reduce the uncertainties regarding the behavior of piles in sandy profiles, an experimental field was developed by the Federal University of Rio Grande do Sul in Araquari-SC, where were executed (a) field tests to define soil geotechnical conditions, (b) bored and continuous flight auger piles and (c) static load tests on the structural elements. The aim of this research was to study the variables that intervene in the soil load transfer mechanism. The soil at the experimental field was characterized by laboratory tests, and parameters of resistance, mineralogy, particle shape, distribution and size were obtained for use in the back analysis of the soil pressure coefficient (ks) of the load tests. For this purpose, were analyzed the results measured on bored piles executed with bentonite and polymer. The back analysis was made using the beta method (β), which allows to estimate the lateral capacity of the piles constructed in sandy profiles, based on vertical stresses, soil pressure coefficient and friction angle of the soil-pile interface. Due to the interaction between the soil particles and the pile concrete, the first are mobilized at high deformation levels, the friction angle of the interface is considered close to the friction angle in the sand critical state. The soil present in the experimental field corresponds to fine sand with silt lenses. Thus, the resistance parameters defined were the critical state and peak friction angle with values of 33.0 ° and 33.4 ° respectively. The critical state angle was used in the back analysis of the load tests, and as a result the ks was obtained, to be subsequently compared to the at rest lateral earth pressure coefficient (k0). The results showed that, with depth, the value ks approaches the value of k0, with a relation of ks / k0 close to unity. It is concluded that the load transfer mechanism between the soil and the pile can be evaluated as a function of the initial stresses of the deposit, expressed from an estimated k0 based on the laboratory tests.

Cette thèse de doctorat porte sur la réponse des fondations caisson dans du sable pour les éoliennes en mer soumises à des chargements monotones et cycliques combinés. Le processus de défaillance et l’enveloppe de rupture (diagramme de capacité portante) d’une fondation en caisson dans du sable soumise à des chargements monotones combinés sont premièrement étudiés à l’aide du modèle constitutif de Mohr-Coulomb. La méthode Lagrangian-Smoothed Particle Hydrodynamics Combinée (CLSPH) est adoptée pour prendre en compte les grandes déformations et les limites de l'approche sont mises en évidence. Une loi constitutive basée sur la notion de l’état critique pour le sable récemment mis au point (SIMSAND) est ensuite introduite et utilisée avec la méthode CLSPH. Des tests d’effondrement du sol dans un canal rectangulaire et d’une colonne granulaire en prenant en compte différentes géométries sont simulés afin de valider l’approche en termes de morphologie de dépôt final, des profils d’écoulement et de zones non perturbées. La méthode CLSPH et le modèle SIMSAND sont ensuite utilisés pour étudier le diagramme de capacité portante des fondations caisson dans du sable. Différents paramètres ayant une incidence sur la forme et la taille de l'enveloppe de rupture sont pris en compte, tels que la densité et la rigidité du sol, la résistance au frottement, la rupture des grains, la géométrie et les dimensions de la fondation. Une formule analytique est introduite pour décrire la surface de rupture 3D capable à reproduire les résultats numériques. Sur la base de la formule analytique proposée, un macro-élément pour des fondations caisson dans du sable soumises à des chargements monotones et cycliques est finalement développé dans le cadre de l'hypoplasticité. L’outil numérique proposé est validé avec des résultats expérimentaux. / This PhD thesis deals with the response of caisson foundations in sand for offshore wind turbines submitted to combined monotonic and cyclic loadings. First, the failure process and failure envelope (or bearing capacity diagram) of a caisson foundation in sand under combined monotonic loadings is investigated using the conventional Mohr-Coulomb constitutive model. A Combined Lagrangian-Smoothed Particle Hydrodynamics(CLSPH) method is adopted to consider large deformations and the limitations of the approach are highlighted. A recently developed critical state model for sand (SIMSAND) is then introduced and combined with the CLSPH method. Rectangular channel soil collapse tests and granular column collapse tests considering different aspect ratios are simulated to validate the approach in terms of final deposit morphologies, flow profiles and undisturbed areas.The CLSPH method and the SIMSAND model are then used to investigate the bearing capacity diagram of the caisson foundation in sand. Different parameters affecting the shape and size of the failure envelope are considered, as soil density and stiffness, friction strength, grain breakage, geometry and aspect ratio of the foundation. An analytical formula is introduced to describe the 3D failure surface reproducing the numerical results. Based on the proposed analytical formula, a macro-element for the caisson foundation in sand submitted to monotonic and cyclic loadings is finally developed within the framework of hypoplasticity. Validation is provided through comparison with experimental results.