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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Mass-wasting-Congresses. ; Electronic books.
    Description / Table of Contents: First International Symposium.
    Type of Medium: Online Resource
    Pages: 1 online resource (529 pages)
    Edition: 1st ed.
    ISBN: 9789401000932
    Series Statement: Advances in Natural and Technological Hazards Research Series ; v.19
    Language: English
    Note: Intro -- Title Page -- Copyright -- TABLE OF CONTENTS -- Foreword -- Authors Index.
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  • 2
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Geography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (434 pages)
    Edition: 1st ed.
    ISBN: 9781402065125
    Series Statement: Advances in Natural and Technological Hazards Research Series ; v.27
    DDC: 551.307
    Language: English
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  • 3
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Landslides. ; Electronic books.
    Description / Table of Contents: This volume features the latest scientific research on the geological, geotechnical and geophysical aspects of slope failure in sensitive clays. It focuses on understanding the full spectrum of challenges presented by landslides in such brittle materials.
    Type of Medium: Online Resource
    Pages: 1 online resource (416 pages)
    Edition: 1st ed.
    ISBN: 9789400770799
    Series Statement: Advances in Natural and Technological Hazards Research Series ; v.36
    DDC: 551
    Language: English
    Note: Intro -- Preface -- Contents -- Contributors -- Chapter 1: Landslides in Sensitive Clays - From Geosciences to Risk Management -- 1.1 Introduction -- 1.2 Part I: Sensitive Clays: Source, Nature and Development -- 1.3 Part II: Landslide Characterization -- 1.4 Part III: Integrated Geotechnical and Geophysical Site Investigations -- 1.5 Part IV: Slope Stability, Modelling and Progressive Failure -- 1.6 Part V: Hazard Assessment, Risk Management, Regulations and Policies -- 1.7 Conclusions and Outlook -- References -- Part I: Sensitive Clay: Source, Nature and Development -- Chapter 2: Chemistry, Sensitivity and Quick-Clay Landslide Amelioration -- 2.1 Introduction -- 2.2 Sensitivity Development -- 2.2.1 Development of High Undisturbed Strength -- 2.2.1.1 Depositional Factors -- 2.2.1.2 Post-depositional Factors -- 2.2.2 Development of Low Remolded Strength -- 2.2.2.1 Depositional Factors -- 2.2.2.2 Post-depositional Factors -- 2.3 Synthesis -- 2.4 Quick Clay Landslides -- 2.4.1 Classification -- 2.4.1.1 Stepwise Landslides -- 2.4.1.2 Uninterrupted Landslides -- 2.5 Strategies for Amelioration of Landsliding in Sensitive Clays -- 2.5.1 Prevention of the Initial Failure -- 2.5.2 Prevention of Failure Zone Advancement -- 2.6 Summary -- References -- Chapter 3: Nature of Sensitive Clays from Québec -- 3.1 Introduction -- 3.2 Methodology -- 3.3 Results and Analysis -- 3.3.1 Physico-chemical Properties -- 3.3.2 Primary Minerals (Non-clay) -- 3.3.3 Clay Minerals -- 3.4 Concluding Remarks -- References -- Chapter 4: Three-Dimensional Quick-Clay Modeling of the Gothenburg Region, Sweden -- 4.1 Introduction -- 4.2 Quick-Clay Development Settings in the Gothenburg Area -- 4.3 Data and Methods -- 4.4 Three-Dimensional Quick-Clay Predictions -- 4.4.1 Model Components and Their Refinements -- 4.4.2 Possible Model Applications -- 4.5 Conclusions -- References. , Chapter 5: Ion Exchange as a Cause of Natural Restabilisation of Quick Clay - A Model Study -- 5.1 Introduction -- 5.2 The Study Area -- 5.3 Modelling -- 5.3.1 Chemistry Setup in the Model -- 5.3.2 Transport in the Model -- 5.4 Results and Discussion -- 5.4.1 Present Day Conditions -- 5.4.2 Development Over Time for the Calcium Scenario -- 5.5 Conclusions -- References -- Chapter 6: Potassium Chloride as Ground Improvement in Quick Clay Areas - A Preliminary Study -- 6.1 Introduction -- 6.2 Background -- 6.3 Laboratory Investigations -- 6.4 Results -- 6.4.1 Initial Conditions -- 6.4.2 Salt Treated Clay -- 6.4.3 Diffusion of Potassium -- 6.5 Discussion -- 6.6 Conclusions -- References -- Part II: Landslide Characterization -- Chapter 7: Inventory of Large Landslides in Sensitive Clay in the Province of Québec, Canada: Preliminary Analysis -- 7.1 Introduction -- 7.2 Definitions and Investigative Methods -- 7.3 Historical and Spatial Aspects -- 7.4 Types of Large Retrogressive Landslides -- 7.4.1 Characteristics of Flowslides -- 7.4.2 Characteristics of Spreads -- 7.5 Estimation of Retrogression Distance -- 7.6 Conclusion -- References -- Chapter 8: Characterization of Post-failure Movements of Landslides in Soft Sensitive Clays -- 8.1 Background -- 8.2 Indicators for the Extent of Post-failure Movements -- 8.3 Remolding Energy -- 8.4 Conclusions -- References -- Chapter 9: Controls on the Dimensions of Landslides in Sensitive Clays -- 9.1 Introduction -- 9.2 Material Controls -- 9.2.1 Shear Strength and Sensitivity -- 9.2.2 Remoulding Energy and Rapidity -- 9.3 Geometric and Topographic Controls -- 9.3.1 Topographic Controls -- 9.3.2 Inclination of the Rupture Surface -- 9.4 Conclusions -- References -- Chapter 10: Prehistoric Sensitive Clay Landslides and Paleoseismicity in the Ottawa Valley, Canada -- 10.1 Introduction -- 10.2 Study Area. , 10.3 Landslides in the Ottawa Valley -- 10.4 Data Source -- 10.5 Results -- 10.6 Discussion -- 10.7 Conclusions -- References -- Chapter 11: Characterization and Post-failure Analysis of the 1980 Landslide in Sensitive Clays at Havre-St-Pierre, Québec, Canada -- 11.1 Introduction -- 11.2 Review of the 1980 Landslide at Havre-Saint-Pierre -- 11.3 Morphology and Geotechnical Properties Before the Landslide -- 11.4 Morphology of the Landslide -- 11.5 Numerical Modelling of Debris Spreading -- 11.6 Discussion of the Remoulding and Mobility of the Debris -- 11.7 Conclusion -- References -- Chapter 12: The Evolution of Material Properties Within an In Situ Shear Zone in Sensitive Clay -- 12.1 Introduction -- 12.2 Site Description -- 12.3 Field and Laboratory Investigations -- 12.4 Results and Interpretations -- 12.4.1 Soil Conditions and Failure Plane -- 12.4.2 Microstructural Changes -- 12.4.3 Pore Pressure Evolution -- 12.4.4 Changes Over Time in the Failure Zone -- 12.5 Discussion and Conclusions -- References -- Part III: Integrated Geotechnical and Geophysical Site Investigations -- Chapter 13: The Use of Geophysics for Sensitive Clay Investigations -- 13.1 Introduction -- 13.2 Geo-electrical -- 13.2.1 Electrical Resistivity Tomography -- 13.2.2 Resistivity Cone (RCPT/RCPTU) -- 13.3 Electromagnetics -- 13.3.1 Radiomagnetotelluric (RMT) and Controlled Source Audio Magnetotelluric (CSAMT) Methods -- 13.3.2 Joint Inversion of ERT and CSRMT Data -- 13.4 Seismic -- 13.4.1 Seismic Refraction -- 13.4.2 Surface Wave Analysis -- 13.4.3 High Resolution Seismic Reflection -- 13.5 Relationship Between Geophysical and Geotechnical Properties -- 13.5.1 Index Parameters -- 13.5.2 Shear Strength Parameters -- 13.5.3 Small Strain Stiffness -- 13.6 Discussion and Conclusions -- References. , Chapter 14: Applications of 2D Resistivity Measurements for Quick-Clay Mapping in Mid Norway -- 14.1 Introduction -- 14.2 Methods -- 14.2.1 2D Resistivity Measurements -- 14.2.2 Geotechnical Methods -- 14.2.3 Classification of Sediments from Resistivity Values -- 14.3 Applications of 2D Resistivity Measurements in Quick- Clay Areas -- 14.3.1 Combined 2D Resistivity Measurements and Geotechnical Investigations for Quick-Clay Mapping -- 14.3.2 Mapping of Barriers Against Landslide Development -- 14.3.3 Hazard Zonation -- 14.3.4 Engineering Purposes -- 14.3.5 Landscape Development and Groundwater Drainage Pattern -- 14.4 Concluding Remarks -- References -- Chapter 15: An Integrated Approach to Quick-Clay Mapping Based on Resistivity Measurements and Geotechnical Investigations -- 15.1 Introduction -- 15.2 Field and Laboratory Work -- 15.2.1 Site Description Vålen and Smørgrav -- 15.2.2 Geotechnical Site Investigations -- 15.2.3 Laboratory Work -- 15.2.4 Electrical Resistivity Tomography (ERT) -- 15.3 Results -- 15.3.1 Resistivity and Sensitivity -- 15.3.2 Resistivity from ERT and RCPT -- 15.3.3 Clay Resistivity Constrained by Bedrock -- 15.4 Discussions and Conclusions -- References -- Chapter 16: Geophysical and Geotechnical Investigations for a Major Highway in a Quick-Clay Area -- 16.1 Introduction and Background -- 16.2 Setting and Project Description -- 16.3 Methods -- 16.3.1 Geotechnical Field Investigations -- 16.3.2 Laboratory Investigations -- 16.3.3 2D Resistivity Measurements -- 16.4 Results and Interpretations -- 16.4.1 Ground Conditions from Geotechnical Investigations -- 16.4.2 Interpretation of 2D Resistivity Profiles -- 16.4.3 Comparison of Geotechnical Data and 2D Resistivity Data -- 16.5 Discussion -- 16.6 Concluding Remarks -- References -- Chapter 17: Mapping of Quick Clay by ERT and CPT-R in the Göta Älv River Valley. , 17.1 Introduction -- 17.2 Site Investigation Methods -- 17.2.1 ERT -- 17.2.2 CPT-R -- 17.3 Site Description -- 17.4 Quick Clay -- 17.5 Site Investigations -- 17.6 Results and Interpretation -- 17.6.1 ERT -- 17.6.2 CPT-R -- 17.7 Analysis and Discussion -- 17.7.1 Comparison of CPT-R and ERT Results -- 17.7.2 ERT -- 17.7.3 CPT-R -- 17.8 Conclusions -- References -- Chapter 18: Geophysical Data Integration for Quick-Clay Mapping: The Hvittingfoss Case Study, Norway -- 18.1 Introduction -- 18.2 Site Description -- 18.3 Data and Methods -- 18.3.1 ERT Measurements -- 18.3.2 Seismic Measurements -- 18.3.3 GPR Measurements -- 18.3.4 Geotechnical Investigations -- 18.4 Results and Interpretation -- 18.5 Conclusions -- References -- Chapter 19: Joint Acquisition and Processing of Seismic Reflections and Surface Waves in a Sensitive Clay Deposit in the Outaouais Region (Québec), Canada -- 19.1 Introduction -- 19.2 Study Site -- 19.3 Combined MASW-SV Seismic Reflection Survey -- 19.3.1 Field Data Acquisition -- 19.3.2 MASW Processing -- 19.3.3 SV Seismic Reflection Combined Processing -- 19.3.4 Interpretation -- 19.4 Multi-offset Seismic Piezocone Penetration Test -- 19.4.1 Data Acquisition and Processing -- 19.4.2 Interpretation -- 19.5 Discussion and Conclusions -- References -- Chapter 20: Empirical Geophysical/Geotechnical Relationships in the Champlain Sea Sediments of Eastern Ontario -- 20.1 Introduction -- 20.2 Methods -- 20.2.1 Surface Seismic Methods -- 20.2.2 Basic Geotechnical Core Tests -- 20.2.3 Borehole Geophysical Logging -- 20.3 Selected Site Studies -- 20.3.1 Case 1: Undisturbed and Non-sensitive Champlain Sea Sediments West of Ottawa -- 20.3.2 Case 2: Undisturbed and Sensitive Champlain Sea Sediments in Ottawa -- 20.3.3 Case 3: Disturbed and Non-sensitive Champlain Sea Sediments Near Alfred -- 20.4 Geotechnical/Geophysical Correlations. , 20.4.1 Porosity and Bulk Density Versus Shear Wave Velocity.
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  • 4
    facet.materialart.
    Unknown
    Canadian Science Publishing
    Publication Date: 2023-11-16
    Description: Due to the recent development of well-integrated surveying techniques of the sea floor, significant improvements were achieved in mapping and describing the morphology and architecture of submarine mass movements. Except for the occurrence of turbidity currents, the aquatic environment (marine and fresh water) experiences the same type of mass failure as that found on land. Submarine mass movements, however, can have run-out distances in excess of 100 km, so their impact on any offshore activity needs to be integrated over a wide area. This great mobility of submarine mass movements is still not very well understood, particularly for cases like the far-reaching debris flows mapped on the Mississippi Fan and the large submarine rock avalanches found around many volcanic islands. A major challenge ahead is the integration of mass movement mechanics in an appropriate evaluation of the hazard so that proper risk assessment methodologies can be developed and implemented for various human activities offshore, including the development of natural resources and the establishment of reliable communication corridors.
    Type: Article , PeerReviewed
    Format: text
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