Les avalanches sont susceptibles d’affecter le réseau routier et les infrastructures bâties, mettant en péril la population. L’extension des avalanches est généralement évaluée à l’aide de modèles physiques et/ou statistiques. Ces modèles sont très performants pour simuler des événements relativement fréquents, cependant, les incertitudes augmentent dès lors que l’on considère des événements plus rares. Il est donc indispensable de valider les procédures de modélisation afin de confirmer les prédictions qui en découlent. Dans ce travail, la dendrogéomorphologie a été utilisée comme un outil de validation. Cette approche se fonde sur le fait que les arbres forment un cerne de croissance par année et que les individus affectés par des processus naturels enregistrent l’évidence d’une perturbation dans leurs cernes. Cette thèse a permis de proposer une nouvelle approche pour l’identification des événements avalancheux fondée sur l’expertise du dendrogéomorphologue et d’évaluer la qualité de l’approche dendrogéomorphologique. Il a également été possible de réaliser une validation croisée entre des avalanches extrêmes prédites par un modèle statistique-dynamique et des informations sur des périodes de retour d’avalanches similaires obtenues à l’aide de l’approche dendrogéomorphologique. Les résultats montrent une très bonne concordance pour des événements dont la période de retour est égale ou inférieure à 300 ans. Finalement, une analyse des relations statistiques avalanche-climat a montré que les arbres enregistrent préférentiellement les événements qui ont eu lieu durant des épisodes froids associés à des tempêtes hivernales accompagnées de fortes précipitations. / Snow avalanches are a significant natural hazard that impact roads, structures and threaten human lives in mountainous terrain. The extent of avalanches is usually evaluated using topographic or statistic models. These models are well capable to simulate contemporary events, but uncertainties increase as soon as longer return periods are investigated. Thus, there is a real need for validation of modelling procedures to corroborate model predictions. In the present work, dendrogeomorphology has been used as a validation tool. This approach is based on the fact that trees affected by mass movements record the evidence of geomorphic disturbance in their growth-ring series and thereby provide a precise geochronological tool for the reconstruction of past mass movement activity. This PhD thesis presents a new tree-ring-based semi-quantitative approach for the identification of avalanche events based on the analytical skills of the dendrogeomorphic expert and proposes an evaluation of the completeness of tree-ring records. Furthermore, this work proposes the first cross-validation of high return period avalanches derived from a locally calibrated statistical-dynamical model and the long-term, higher-return period information gathered from tree-ring records. Comparison of relations between runout distances and return periods between both approaches shows very good agreement for events with return periods of < 300 yr. Finally, a statistical analysis of avalanche-climate relations suggests that tree rings preferentially record events that occurred during cold winter storms with heavy precipitation.

Avalanche photodiodes are the primary choice for photodetection in optical access networks, due to their capacity to meet the current requirements of bandwidth and sensitivity introduced by NG-PON2. This work provides an effective tool for modeling and predicting the operation of an avalanche photodiode, paving the way to making better performing receivers. We employed Lumerical to obtain several steady state and transient parameters for a silicon germanium SACM waveguide avalanche photodiode, where close agreement is illustrated between our findings and measurements reported on fabricated devices. The utility of our work is further demonstrated by implementing and modeling a device, designed to meet certain fabrication specifications, where optimization guidelines are suggested afterwards. By providing an accurate approximation of the avalanche photodiode operation, we offer a cost-effective approach to address the problem of fabricating better devices in optical access networks. The introduced methods can be similarly used for other types of photodiodes, contributing to a vast range of applications. / Graduate

This dissertation outlines the study and development of a Solid-state Impact-ionization Multiplier (SIM). The SIM is a stand-alone current amplifier designed with optical detection systems in mind. The SIM amplifies signals utilizing impact ionization as a source of gain. The SIM is fabricated on silicon in order to take advantage of its favorable impact ionization coefficients. Utilizing silicon in impact ionization based gain devices makes low noise and high gains attainable. Because it is a stand-alone device, it can be wired to an arbitrary current source making it capable of receiving an input from photodiodes of any material. This makes it possible to amplify a signal from a photodiode that has been optimized for a given wavelength. In this way, the SIM attempts to separate the absorption and multiplication portions in modern day optical detection/amplification devices such as in Avalanche Photodiodes (APDs). This flexibility allows it to be utilized in many different systems. The SIM has gone through several iterations in the last few years. Each change has been with the purpose of increasing gain, frequency response or yield. The progression of the device has come at the hand of much thought, theory, simulation, fabrication, and testing. One of the challenges encountered in its development has been gain controllability due to poor carrier confinement and premature breakdown. Increased gain control was developed through simulation and fabrication of a confining oxide layer. Yield and difficulties in consistent fabrication were also addressed by altering the input metallization and doping processes. The frequency response of the device has been the largest challenge in device development. Issues such as space charge, floating node voltage, edge effects and low signal amplification have caused limitations. Successes and attempts at overcoming these, and other, challenges is the basis of this dissertation of work.

Avalanche paths are unique ecosystems that represent a significant portion of the landscape in the northern Rocky Mountains. Frequent avalanche disturbance results in vegetative cover that is unlike the adjacent coniferous forest. These high relief environments have the potential to remove carbon from the atmosphere at rates differing from those of the surrounding forest, and to regulate matter and/or energy fluxes to downslope ecosystems. This thesis attempts to estimate organic carbon on south-facing avalanche paths in the southern portion of Glacier National Park, Montana. I am specifically interested in total organic carbon density, compartmental carbon density, and change in organic carbon over time as a function of shrub and tree diameter. Using an integrated sampling method, estimates of total organic carbon on avalanche paths appear to be different than those of the adjacent forest and similar to those of other shrub formation types in the area. However, the potentially moveable litter compartment is consistently larger. Organic carbon from shrub and trees growing on paths appears to be increasing at a continuous rate leading up to disturbance, while a typical individual's rate of increase appears to be slowing. The organic material temporarily stored on avalanche paths could serve as an important outside carbon source for near and distant aquatic ecosystems.

- Les instabilités de dépôts granulaire sont omniprésentes dans la nature, elles présentent un comportement solide et liquide comme en témoigne les avalanches et les écoulements de boue qui sont a l'origine de nombreuses catastrophes humaines et économiques. Malgré son importance pratique, ces phénomènes sont encore loin d'être compris et bien décrit notamment en raison du manque de compréhension de leur rhéologie. Ce manuscrit présente une étude expérimentale d'avalanche se propageant sur une couche granulaire érodable. Dans la première partie, l'équilibre d'une couche granulaire sur un plan incline est étudiée, aussi bien dans l'air que dans l'eau. A partir de ce dépôt granulaire, la méthode de propagation d'avalanche est expliquée dans ces différentes phases. La rhéologie des écoulements stationnaires de sable est déduite et comparée aux résultats communément trouvés. Des mesures expérimentales, dites "méthode de la lame de suie" et "méthodes des feuillets colorées", montrent l'existence d'une couche statique prenant place sous l'écoulement. Dès lors la rhéologie précédemment établie est modifiée permettant ainsi de décrire les avalanches en termes de rhéologie locales. En appliquant cette rhéologie aux cas des ondes solitaires érosives, le profil d'érosion en est extrait. Pour le sable sur la feutrine il ressort que l'onde ne creuse pas la couche jusqu'au fond tandis que pour les ondes de billes la couche est entièrement érodée. Dans la dernière partie la stabilité de ces ondes est étudiée. Au delà d'un seuil les ondes se déstabilisent transversalement. Après une longueur d'onde initiale, un phénomène de coalescence par fusion est observé. Ce dernier est lui-même stoppé par la formation de doigts. Une étude expérimentale de stabilité a montré que c'est une instabilité linéaire à grande longueur d'onde et à nombre d'onde nul. Toutes les longueurs d'onde mesurées aussi bien dans l'air que dans l'eau se regroupent autour d'une même courbe dès lors qu'elles sont adimensionnées par la taille des grains.

This thesis presents a comprehensive assessment of breakdown and operational voltage constraints in state-of-the-art silicon-germanium (SiGe) heterojunction bipolar transistor (HBT) BiCMOS technology. Technology scaling of SiGe HBTs for high frequency performance results on lower breakdown voltages, making operating voltage constraints an increasingly vital reliability consideration in SiGe HBTs from both a device and circuits perspective.

Thèse de doctorat : Dispositifs de l'Electronique Intégrée : Villeurbanne, INSA : 2000. / Titre provenant de l'écran-titre. Bibliogr. p. 207-211.

This thesis reports a rock slope hazard investigation located in the Central Andes of Chile, where two significant rock mass wasting events were recognized. Dating using cosmogenic nuclide for ³⁶Cl showed that the deposits were post-glacial in age, corresponding to the Upper Pleistocene Portillo Rock Avalanche (PRA) and a Holocene rock slump and rockslide. The pre-historic landslide deposits underlie both a key transportation route between Chile and Argentina and an important ski resort. The purpose of this research was to investigate the likely failure mechanism and characterise the runout path and volume of the PRA. The insights gained on the back analysis of the slope were used in later stages to assess the hazard potential of a recurring major rockslide. The distinct element code UDEC was used to evaluate the failure mechanism. Elasto-plastic modelling results showed that sliding and shearing along the bedding planes together with brittle fracturing and shearing through the toe of the slope likely had occurred. Runout simulations were carried out using DAN3D. Combinations of rheologies were tested and ranked based on their ability to represent the current distribution of the debris by means of pre-failure topography reconstruction and volume estimates of the deposits. Results showed that the best basal rheological combination for the PRA was frictional during the rockslide and Voellmy when entrainment became important. In contrast, a constant frictional basal rheology best represented the Holocene rock slump. The performance of the present-day state of the slope was tested under different scenarios. Under static condition the slope proved to be stable indicating a stabilized geometrical profile with time. Also, the slope proved to be stable under increased pore water pressures at its toe. Finally the modelled slope was subjected to a seismic load (M=7.8) and its crest failed due to an outward rotation of blocks, probably aided by topographic amplification. The runout simulations showed that the leading edge of the flow could override part of the International Santiago-Mendoza Corridor with no direct impact to the Portillo Ski Resort. Overall, though, under this highly unlikely dynamic condition for the site, the hazard level is very low.

This thesis reports a rock slope hazard investigation located in the Central Andes of Chile, where two significant rock mass wasting events were recognized. Dating using cosmogenic nuclide for ³⁶Cl showed that the deposits were post-glacial in age, corresponding to the Upper Pleistocene Portillo Rock Avalanche (PRA) and a Holocene rock slump and rockslide. The pre-historic landslide deposits underlie both a key transportation route between Chile and Argentina and an important ski resort. The purpose of this research was to investigate the likely failure mechanism and characterise the runout path and volume of the PRA. The insights gained on the back analysis of the slope were used in later stages to assess the hazard potential of a recurring major rockslide. The distinct element code UDEC was used to evaluate the failure mechanism. Elasto-plastic modelling results showed that sliding and shearing along the bedding planes together with brittle fracturing and shearing through the toe of the slope likely had occurred. Runout simulations were carried out using DAN3D. Combinations of rheologies were tested and ranked based on their ability to represent the current distribution of the debris by means of pre-failure topography reconstruction and volume estimates of the deposits. Results showed that the best basal rheological combination for the PRA was frictional during the rockslide and Voellmy when entrainment became important. In contrast, a constant frictional basal rheology best represented the Holocene rock slump. The performance of the present-day state of the slope was tested under different scenarios. Under static condition the slope proved to be stable indicating a stabilized geometrical profile with time. Also, the slope proved to be stable under increased pore water pressures at its toe. Finally the modelled slope was subjected to a seismic load (M=7.8) and its crest failed due to an outward rotation of blocks, probably aided by topographic amplification. The runout simulations showed that the leading edge of the flow could override part of the International Santiago-Mendoza Corridor with no direct impact to the Portillo Ski Resort. Overall, though, under this highly unlikely dynamic condition for the site, the hazard level is very low.

Thesis (Ph. D.)--Electrical and Computer Engineering, Georgia Institute of Technology, 2008. / William Doolittle, Committee Member ; Joy Laskar, Committee Member ; Russell Dupuis, Committee Chair ; David Citrin, Committee Member ; Srinivas Garimella, Committee Member.