In geotechnical engineering, granular flows are often studied as a means to further the understanding of the mechanisms that drive landslide motion. High quality experimental data is essential in providing evidence for the development and verification of new theoretical methods that link complex grain interactions to the extended mobility of some landslide events. At present, limited experimental data is available that captures the full range of landslide mobility. In an attempt to add to the present data sources, high quality experimental data was obtained through the use of high speed cameras and physical modelling using a geotechnical centrifuge and a large scale landslide flume. These modelling techniques allow for landslide motion, representative of field scale events, to be observed in a well-defined and controlled setting. A series of nine tests were performed in a geotechnical centrifuge under varying slope inclinations and Coriolis conditions. The effects of Coriolis on landslide mobility were evident when comparing final deposit shapes and total runout. The effects of Coriolis were more pronounced for higher velocity situations and when material was travelling on the horizontal base section opposed to the sloped section of the physical model. A series of thirty tests were performed using a large scale flume under varying source volumes and basal friction conditions, capturing the grain scale interactions and overall runout behaviour. The grain interactions and ultimately the flow behavioural regimes developed were a function of material source volume and boundary roughness. The dimensionless inertial number was used to classify flows into behavioural regimes, but was found to break down when describing transitions to the granular gas behavioural regime. The runout-time results and final deposit shapes showed significant variation between test configurations, indicating the effects of volume and basal friction on overall mobility. Using the depth averaged numerical model, DAN, it was found that a single set of empirically derived frictional parameters (i.e. specific to internal and basal friction conditions) was appropriate for matching the overall mobility of the experimental flows over a range of flow volumes and slope inclinations. / Thesis (Master, Civil Engineering) -- Queen's University, 2013-09-25 15:48:54.761

[Truncated abstract] Seismic tomography has been extensively used in geophysics for different purposes such as geological mapping and prospecting for oil and gas. In geophysics, ultrasound or electromagnetic waves are normally used to provide the tomographic information. In the geotechnical area, seismic tomography is emerging as a promising technique that can be used to determine the spatial variability of shear wave velocities and hence the small strain stiffness of geomaterials. Although some studies have been undertaken to incorporate seismic measurement into centrifuge modelling, there has been to date no attempt to build a complete seismic tomography facility with high resolution for use in a geotechnical centrifuge. Such a powerful facility can help in better understanding of soil behaviour by providing a complete picture of the spatial variation of the soil property of concern. The main aim of this study was to develop a high-resolution seismic tomography (ST) system for the beam centrifuge at the University of Western Australia (UWA) by which the shear wave velocity and hence maximum shear modulus could be determined anywhere in the centrifuge model. ... This limitation was the requirement to use an a priori model. The exact solutions in the different examples presented in this chapter were known, and they were used as a priori models into the inversion process. However, in practice the exact solution is unknown, and the aim of the tomographic inversion is to obtain a solution that best describes the measured data. Carrying out inversion without using an a priori model can yield an output model that hints at the nature of the model. This output can then be used as the starting point in an iterative process, in which the output from one step is used as an a priori model for reinverting the original data in a subsequent step. In this case, this process slightly improved the output tomogram and decreased the value of root mean squares of travel time residuals (Rrms). An alternative inversion strategy was proposed based on the results obtained in this study. It involves using a searching algorithm. A searching process can be carried out based on the output from the first iteration (without using an a priori model). The search can involve varying the parameters that describe buried anomalies, such as the size of the anomaly, the velocity value in the anomaly, and the location of the anomaly. The aim is to search for the combination of anomaly parameters that minimises the resulting error parameters (mainly Rrmx, but also the average error and the standard deviation of the error). For more subtle cases, such as the velocity model under a footing, where inversion without using an a priori model did not recover the input model, a searching algorithm involving applying perturbations to the exact Boussinesq model can be performed. Not only can the searching procedure involve adding perturbation to the velocity values in the Boussinesq model, but it can also add perturbation to the shape of the velocity distribution below the footing. The searching process can continue until a model that fits the data with a minimum error is found, i.e., minimising Rrms.

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Normalmente fundações diretas não são utilizadas em solos colapsáveis devido à falta de soluções econômicas e eficientes para melhorar essa condição crítica de terreno. Quando estes solos são inundados, a água afeta sua estrutura provocando uma redução de volume, e consequentemente grandes recalques nas fundações. Por outro lado, a maioria dos solos colapsíveis em regiões tropicais está sujeita a intenso intemperismo e laterização, os quais são responsáveis por melhorar as propriedades do solo após compactação. Por esta razão, solos lateríticos colapsíveis em forma compactada são comumente usados como aterros e materiais de construção em estradas, e têm sido empregados no Brasil para possibilitar a construção de fundações diretas. A pesquisa atual foi planejada para avaliar um aprimoramento desta técnica, que seria o uso de grupos de colunas de solos lateríticos compactados, ao invés de camadas compactadas de solo muito espessas, para permitir o uso de fundações diretas. Para este estudo, ensaios edométricos simples e duplos e de modelagem física em centrífuga foram conduzidos em um solo laterítico colapsível típico do sudeste brasileiro. Complementarmente, um modelo numérico foi ajustado, usando-se os resultados dos ensaios em centrífuga, para estimar a melhoria nas propriedades do solo reforçado. Por fim, os resultados experimentais mostraram que a técnica proposta pode reduzir os recalques de colapso induzidos por umedecimento do solo, e também melhorar o comportamento carga-recalque de fundações diretas apoiadas no solo investigado. / Normally, shallow foundations are not used in collapsible lateritic soils due to the lack of economic and efficient solutions to improve this critical ground condition. When these soils become wetted, the water breaks down soil arrangement and causes the soil to compress, and consequent large settlement of the foundations supported by them. In contrast, most collapsible soils in tropical regions are subject to intense weathering and laterization, which are responsible for good soil properties after compaction. For this reason, collapsible lateritic soils in compacted form are commonly used as fills and road construction materials, and have been utilised in Brazil to allow the construction of shallow foundations. The current research was designed in order to evaluate an enhancement of this technique, which is the use of groups of compacted lateritic soil columns, instead of very thick compacted soil layers, to allow the use of shallow foundations. For this study, single-point and double oedometer and physical model tests in centrifuge were conducted on a collapsible lateritic soil typical in the southeastern part of Brazil. Additionally, a numerical model was adjusted using the data from the centrifuge tests to estimate the improvement of the reinforced soil. The experimental results show that the proposed technique can reduce wetting-induced collapse settlements and also improve the loaddisplacement performance of shallow foundations in the soil investigated.