R.M. Hardy Keynote Address – Dr. Jean-Marie Konrad
Design and Analysis of Rockfill Dams: Past, Present and Future
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The 2015 R.M. Hardy lecture reviews the evolution of the design practice at Hydro-Quebec for four generations of rockfill dams. Innovative research to advance the practice is presented with particular emphasis on scale effect and particle breakage, internal erosion and contact erosion. Future developments with respect to seismic design are outlined with an emphasis on permanent deformation prediction and in situ testing in rockfill to obtain representative material parameters. Finally, analysis of rockfill dams considering evolving material properties is discussed.
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Dr. Konrad is a registered civil engineer with a Master’s degree from Université Laval and a Doctorate degree from the University of Alberta where he contributed to the development of frost heave mechanics. He worked in the private sector as a geotechnical engineer for Lavalin and James-Bay hydro electric Corporation, at the National Research Council with respect to the geotechnical aspects of the artificial drilling islands in the Beaufort Sea, development of interpretation techniques of in situ testing data in weak soils and academia at the University of Waterloo (Ontario) and Université Laval (Québec). From 1998 to 2008, he was the Chairholder of an NSERC industrial research chair on frost action in civil engineering structures. Presently he is professor of civil engineering at Université Laval, Quebec and also the Chairholder of an NSERC industrial research chair on the optimisation of the life-cycle of earthdams. Dr. Konrad is the author or co-author of over 150 technical papers. For the last twelve years, he was also a consultant for various projects related to artificial freezing, permafrost engineering, dam construction and safety assessment. Dr. Konrad is a Fellow of the Canadian Academy of Engineering and a Fellow of the Engineering Institute of Canada. |
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John Ross Mackay Lecture – Dr. Steven V. Kokelj
Retrogressive Thaw Slumps: from Slope Process to the Landscape Sensitivity of Northwestern Canada
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Retrogressive thaw slumping is a dynamic thermokarst process and an important driver of change in ice-cored, glaciogenic landscapes across the circumpolar North. In this talk, dedicated to the memory of John Ross Mackay, research on the processes and feedbacks that influence the growth of retrogressive thaw slumps is summarized with focus on studies from the Peel Plateau, northwestern Canada. Landsat imagery (1985 to 2011) and high frequency climatic and photographic time-series for the summers of 2010 and 2012 indicate that an increase in rainfall has accelerated downslope sediment flux from slump scar zones, perpetuating slump activity and intensifying this disturbance regime. Environmental impacts are significant: these mega slumps now commonly exceed 15 ha in area, displace up to 106 m3 of materials from slopes to valley bottoms, reconfigure slopes and drainage networks, and significantly increase stream sediment and solute loads.
Remote sensing of slump-impacted terrain across a 1, 275, 000 km2 area of northwestern Canada has revealed a close association with ice-rich hummocky moraine landscapes, which were deposited at the margins of the former Laurentide Ice Sheet. In conjunction with process-oriented thaw slump studies, this mapping provides a quantitative basis and a geomorphic context for evaluating the distribution of ice-cored permafrost and the potential for climate-driven landscape change across northwestern Canada. |
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| DR. STEVEN V. KOKELJ |
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Dr. Steve Kokelj, is a Permafrost Scientist with the Northwest Territories Geological Survey. He is also an Adjunct Professor in the Department of Geography and Environmental Studies, Carleton University, and in the School of Environmental Studies, University of Victoria. His research interests include the study of ground ice and chemical characteristics of permafrost, thermokarst processes, and the landscape, ecosystem and human consequences of a changing cryosphere. He has lead several multidisciplinary research projects involving collaboration between scientists, engineers and northerners. He has authored numerous scientific papers on this research and has been recognized for his communication of results to northern communities, regulators, and the scientific community. |
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| TUESDAY SEPTEMBER 22ND, 2015 |
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Keynote – Dr. Lukas U. Arenson
Cold Regions Engineering in a Changing Climate |
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| Considering climate change is an integral part of any infrastructure design that has an extended design life and of particular importance with respect to perpetual designs. Various technical guidelines indicate that global warming should be addressed in the design but often details on how to do this are missing. Also, climate projection models have seen significant improvement over recent years, but the biggest challenge in terms of designing for climate change are not changes in air temperature, but second and third order effects, together with changes in climate extremes. Non-linear changes in precipitation, adjustments in vegetation and/or related geohazards are of relevance rather than average changes in air temperature alone, which are typically the products with the lowest uncertainties available from climate projection models. The keynote presentation provides an overview of these challenges, a summary of latest climate change modeling products and introduces the use of a systematic, risk based approach for cold regions designs considering climate change. |
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| DR. LUKAS U. ARENSON |
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Dr. Arenson is a Senior Geotechnical Engineer with BGC Engineering Inc. and specific expertise in frozen soil mechanics, periglacial risk assessments and geothermal modelling. He has worked on infrastructure and mining projects in Arctic and mountain permafrost, and on the stability of frozen slopes in the European Alps and the South American Andes. Additional work has concentrated on the thermo-mechanical processes of frozen and freezing soils at a microstructural level to better understand the hydraulic, strength and deformation properties of frozen soils with changing stress, temperature and salinity. He developed a probabilistic permafrost distribution model for mountainous terrain, extensively used in South America. He has taught permafrost engineering courses at universities and for industry, and published over 60 scientific publications on topics related to cold regions engineering. He was chair of the Cold Regions Engineering Division of the Canadian Geotechnical Society, and is currently co-chair of the Permafrost Engineering Task Force of the International Permafrost Association and an Adjunct Professor at the Civil Engineering Department of the University of Manitoba. He was the recipient of the Troy L. Péwé award in 2003 and was awarded the Roger J. E. Brown Memorial Award from the Canadian Geotechnical Society in 2010 for his contributions to permafrost engineering research and to the cold regions engineering division. |
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Keynote – Dr. Jean Hutchinson
Applications of Remote Sensing Techniques to Managing Rock Slope Instability Risk |
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| The recent development of rapid, accurate and sophisticated remote sensing tools has provided valuable rock slope change data, previously impossible to obtain. The analysis techniques discussed in this paper utilize detailed and precise models of three-dimensional geometry developed from photographs and LiDAR point clouds. Models of the rock slope from data collected at similar times can be combined, taking advantage of data at different resolutions and collected from different vantage points and platforms. Such models can be used for remote mapping of discontinuities and lithology, as well demonstrated by others. The added value for slope stability management discussed in this conference is realized when geometrical models from different times are compared. Depending upon the frequency of measurements and the rate of change of the rock slope, prior to slope failure it is possible to hypothesize the slope failure mode, the potential volume of the impending failure and in some cases, to provide an accurate estimate of the time of failure. In back analysis, it is possible to determine the distribution of the source zone(s), to assess the path of movement, and to calculate the volume of the source volume and accumulated debris. The case histories demonstrate our enhanced ability to detect and manage the risk of rock slope failure. |
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| DR. JEAN HUTCHINSON |
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Dr. Jean Hutchinson is a Professor and Department Head for Geological Sciences and Geological Engineering at Queen’s University. Jean holds degrees in GeoEngineering from the University of Toronto in 1984; Geotechnical Engineering from the University of Alberta in 1988, and Rock Engineering from the University of Toronto in 1992. Dr. Hutchinson has worked in industry (Ministry of Transportation Ontario, Klohn Crippen Consultants Ltd.), research (University of Alberta, University of Toronto, Laurentian University and CSIRO) and academic (University of Waterloo, Queen’s University) positions during her career. Dr. Hutchinson’s research areas include work on engineering geology risk assessment, natural hazards and landslides, mining induced ground subsidence, underground rock support design, insitu and remote sensing techniques for assessing ground conditions, and engineering education. Dr. Hutchinson is currently serving as a Trustee on the Board of the Canadian Foundation for Geotechnique, and as Chair of the Trailblazer Award Selection Committee for Women in Mining Canada. She is a proud Fellow of the Engineering Institute of Canada, and is delighted to have received the Thomas Roy, John Franklin and Stermac Awards from the CGS. |
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