Earthquake Engineering of Large Underground Structures

Total Page:16

File Type:pdf, Size:1020Kb

Earthquake Engineering of Large Underground Structures Report No. FHWA/RD-80/195 EARTHQUAKE ENGINEERING OF LARGE UNDERGROUND STRUCTURES January 1981 Final Report Earth's Surface Underground Site DEPARTMENT OF TRANSPORTATION Dte 1 tod i LIBRARY Document is available to the public through the National Technical Information Service, Springfield, Virginia 22161 Prepared for FEDERAL HIGHWAY ADMINISTRATION Offices of Research & Development Structures and Applied Mechanics Division Washington, D.C. 20590 NATIONAL SCIENCE FOUNDATION 1800 G Street, N.W. Washington, D.C. 20550 FOREWORD This report is the result of research conducted by URS/John A. Blume Associates, Engineers, for the Federal Highway Administration (FHWA), Office of Research, under FHWA agreement 7-1-05-14 and the National Science Foundation (NSF) under NSF PFR-7706505. The report will be of interest to those researchers and engineers concerned with assessing the vulnerability of underground tunnels to strong ground motion. Specifically, the current state-of-the-art of earthquake engineering of transportation tunnels and other large underground structures is evaluated. Copies of the report are being distributed by FHWA transmittal memorandum.' Additional., copies may be obtained from the National Technical Information Service, 5285 Port Royal Road, Springfield, Virginia 22161. Charles F. ScheJ Director, Office of Research Federal Highway Administration NOTICE This document is disseminated under the sponsorship of the Department of Transportation in the interest of information exchange. The United States Government assumes no liability for its contents or use thereof. The contents of this report reflect the views of the contractor, who is responsible for the accuracy of the data pre- sented herein. The contents do not necessarily reflect the official views or policy of the Department of Transportation. This report does not constitute a standard, specification, or regulation. The United States Government does not endorse products or manufacturers Trade or manufacturers' names appear herein only because they are considered essential to the object of this document. 1 43 Technical Report Documentation Page 1. Report No. 2. Government Accession No. 3. Recipient's Catalog No. FHWA/RD-80/195 4. Title and Subtitle 5. Report Date January 1981 Earthquake Engineering of Large Underground 6. Performing Orgoni zotion Code Structures 8. Performing Organization Report No. 7. Author's) JAB-7821 G. Norman Owen and Roger E. Schol 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) 3563-^12 URS/John A. Blume & Associates, Engineers 1 1 . Controct 130 Jessie Street San Francisco, California 9^105 Period Covered 12. Sponsoring Agency Name ond Address Federal HiohwaV September 1980 National Science Administration Report Foundation and Department of Washington, D.C. 20550 Transportat ion Washington, D.C. 2059< 0H38 15. Supplementary Notes National Science Foundation Program Manager: Dr. William W. Hakala (202) 357 - 7737 Federal Highway Administration Contract Manager: Mr. James D. Cooper (703) 557~5272 16. Abstract This study identifies and evaluates the current state of the art of earthquake engineering of transportation tunnels and other large underground structures. A review of the past performance of 127 underground openings during earthquakes indi- cates that underground structures in general are less severely affected than surface structures at the same geographic location. However, some severe damage, including collapse, has been reported. Stability of tunnels during seismic motion is affected by peak ground motion parameters, earthquake duration, type of support, ground con- ditions, and in situ stresses. The literature on the nature of underground seismic motion is reviewed in detail. Although recorded underground motions tend to substantiate the idea that motion does reduce with depth, amplification at depth has been observed. The current procedures used in the seismic design of underground structures vary greatly depending upon the type of structure and the ground conditions. Procedures for subaqueous tunnels are fairly well formulated; however, procedures for structures in soil and rock are not as well formulated. Numerical procedures to predict dynamic stresses are not completely compatible with current static design procedures, which are more strongly affected by empirical methods than by stress-prediction models. Recommended research activities include the systematic reconnaissance of under- ground structures following major earthquakes, the placement of instrumentation for recording seismic motion in tunnels, analytical studies of underground motion, and the further development of seismic design procedures for structures in soil and rock. 17. Key Words 18. Distribution Statement Earthquake Engineering, Underground Document is available to public Structures, Earthquake Effects, through the National Technical Response, Submerged Seismic Information Service, Springfield, Tunnels, Tunnels in Soil, Tunnels in VA 22161 Rock, Seismic Design 19. Security Clossif. (of this report) 20. Security Clossif. (of this poge) 21. No. of Pages 22. Pr Unclassified Unclassified 287 Porm DOT F 1700.7 (8-72) Reproduction of completed page authorized , Contents page ACKNOWLEDGEMENTS i x SUMMARY , . , , , . xi Effects of Earthquakes on Underground Structures xi Variation of Seismic Motion with Depth xii Seismic Wave Study of a Circular Cavity xiii Analytical and Design Procedures for Underground Structures xiv Critique of the State of the Art xv Research Recommendations xvi 1. INTRODUCTION 1 2. BACKGROUND INFORMATION . 3 Underground Structures 3 Seismic Activity and Earthquake Hazard 5 Earthquake Magnitude and Intensity 11 3. OBSERVED EFFECTS OF EARTHQUAKES AND UNDERGROUND EXPLOSIONS 13 Effects of Earthquakes 13 Response Parameters 1 k Summary of Available Data ; 16 Effects of Underground Explosions 22 Conventional Blasting 23 High-Explosive Tests , 23 Underground Nuclear Explosions 27 Summary and Conclusions 35 k. SEISMIC ANALYSIS 38 Current Techniques Used in Seismic Analysis 38 Available Numerical Models 38 Analysis of Free-Field Stresses and Strains 39 Seismic Analysis of Underground Structures kS Properties Required for Seismic Analysis 64 Techniques for Measuring Soil and Rock Properties 64 Problems in Synthesizing Measured Properties 70 - - i i CONTENTS (Continued) page 5. SEISMIC WAVE PROPAGATION 7k The Nature of Underground Motion ~]k Factors Affecting Underground Motion ~lk Prediction of Underground Motion 80 Depth-Dependence of Underground Motion 82 Literature Review 82 Theoretical Formulation of Depth Dependence 86 Parametric Studies of Depth Dependence 92 Dynamic Response of Underground Cavities 105 Literature Review 107 Theoretical Formulation of Cavity Response . ., 1 08 Numerical Study of Cavity Response 113 6. CURRENT PRACTICE IN SEISMIC DESIGN 123 Submerged Tunnel s 1 25 SFBART Approach to Submerged Tunnels 128 Japanese Approach to Submerged Tunnels 139 Dynamic Analysis of Submerged Tunnels 1^5 Special Design Consideration: Seismic Joint 1^8 Underground Structures in Soil 150 SFBART Approach to Structures in Soil 151 Mononobe-Okabe Theory of Dynamic Soil Pressure 1 5*t Computer Methods for Structures in Soil 155 Special Considerations in Design 156 Underground Structures in Rock 158 Design Based on Geologic Engineering Principles 1 62 Design Based on Stress Calculations 1 66 Special Design Considerations 170 Underground Structures Intersecting Active Faults 171 Case Studies of Special Design Features 171 Recommendations for Special Design Features of Box Condu its 1 ~/h 7. CRITIQUE OF THE STATE OF THE ART 177 Effects of Earthquakes on Underground Structures 177 Underground Seismic Motion 173 Current Practice in Seismic Design of Underground Structures 179 - mi CONTENTS (Continued) page Seismic Design of Subaqueous Tunnels 179 Seismic Design of Underground Structures in Rock 180 Seismic Design of Underground Structures in Soil 1 84 8. RECOMMENDED RESEARCH ACTIVITIES 1 86 Observed Effects of Earthquakes on Underground Structures 1 86 Research Activity 1: Comprehensive Survey of Earthquake Effects on Underground Structures 1 87 Research Activity 2: Postearthquake Reconnaissance of Underground Structures 1 88 Research Activity 3: Observations of Selected Tunnels Before and After Earthquakes 1 88 Underground Seismic Motion 1 89 Research Activity 4: Recording of Seismic Motion in Deep Boreholes 192 Research Activity 5' Recording of Seismic Motion in Underground Openings 192 Research Activity 6: Development of Analytical Models for Predicting Seismic Motion at Depth 195 Seismic Analysis and Design of Underground Structures 197 Research Activity 1 \ Development of Computer Codes for Stability Evaluation of Openings in Rock 1 98 Research Activity 8: Development of Empirical Procedures for Seismic Design 199 Research Activity 9: Analytical Parametric Study of Seismic Stability of Openings in Rock 199 REFERENCES 256 APPENDICES A Persons Contacted About Seismic Design of Underground Structures 200 B Abridged Modified Mercalli Intensity Scale 204 C Summary of Damage to Underground Structures from Earthquake Shaki ng 206 D A Short Review of Seismological Terms 242 E Derivation of the Green's Function for Two-Dimens ional SH Motion in a Half-Space 251 - iv - CONTENTS (Continued) page TABLES 1 Possible damage modes due to shaking for openings in rock 15 2 Test section schedule 30 3 Summary of damage in Drift C, Shot Hard Hat J,k k Approximate peak values of measured free-field quantities versus range, Shot Hard Hat 36 5 Compatibility
Recommended publications
  • 2021 Oregon Seismic Hazard Database: Purpose and Methods
    State of Oregon Oregon Department of Geology and Mineral Industries Brad Avy, State Geologist DIGITAL DATA SERIES 2021 OREGON SEISMIC HAZARD DATABASE: PURPOSE AND METHODS By Ian P. Madin1, Jon J. Francyzk1, John M. Bauer2, and Carlie J.M. Azzopardi1 2021 1Oregon Department of Geology and Mineral Industries, 800 NE Oregon Street, Suite 965, Portland, OR 97232 2Principal, Bauer GIS Solutions, Portland, OR 97229 2021 Oregon Seismic Hazard Database: Purpose and Methods DISCLAIMER This product is for informational purposes and may not have been prepared for or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to ascertain the usability of the information. This publication cannot substitute for site-specific investigations by qualified practitioners. Site-specific data may give results that differ from the results shown in the publication. WHAT’S IN THIS PUBLICATION? The Oregon Seismic Hazard Database, release 1 (OSHD-1.0), is the first comprehensive collection of seismic hazard data for Oregon. This publication consists of a geodatabase containing coseismic geohazard maps and quantitative ground shaking and ground deformation maps; a report describing the methods used to prepare the geodatabase, and map plates showing 1) the highest level of shaking (peak ground velocity) expected to occur with a 2% chance in the next 50 years, equivalent to the most severe shaking likely to occur once in 2,475 years; 2) median shaking levels expected from a suite of 30 magnitude 9 Cascadia subduction zone earthquake simulations; and 3) the probability of experiencing shaking of Modified Mercalli Intensity VII, which is the nominal threshold for structural damage to buildings.
    [Show full text]
  • Bray 2011 Pseudostatic Slope Stability Procedure Paper
    Paper No. Theme Lecture 1 PSEUDOSTATIC SLOPE STABILITY PROCEDURE Jonathan D. BRAY 1 and Thaleia TRAVASAROU2 ABSTRACT Pseudostatic slope stability procedures can be employed in a straightforward manner, and thus, their use in engineering practice is appealing. The magnitude of the seismic coefficient that is applied to the potential sliding mass to represent the destabilizing effect of the earthquake shaking is a critical component of the procedure. It is often selected based on precedence, regulatory design guidance, and engineering judgment. However, the selection of the design value of the seismic coefficient employed in pseudostatic slope stability analysis should be based on the seismic hazard and the amount of seismic displacement that constitutes satisfactory performance for the project. The seismic coefficient should have a rational basis that depends on the seismic hazard and the allowable amount of calculated seismically induced permanent displacement. The recommended pseudostatic slope stability procedure requires that the engineer develops the project-specific allowable level of seismic displacement. The site- dependent seismic demand is characterized by the 5% damped elastic design spectral acceleration at the degraded period of the potential sliding mass as well as other key parameters. The level of uncertainty in the estimates of the seismic demand and displacement can be handled through the use of different percentile estimates of these values. Thus, the engineer can properly incorporate the amount of seismic displacement judged to be allowable and the seismic hazard at the site in the selection of the seismic coefficient. Keywords: Dam; Earthquake; Permanent Displacements; Reliability; Seismic Slope Stability INTRODUCTION Pseudostatic slope stability procedures are often used in engineering practice to evaluate the seismic performance of earth structures and natural slopes.
    [Show full text]
  • Living on Shaky Ground: How to Survive Earthquakes and Tsunamis
    HOW TO SURVIVE EARTHQUAKES AND TSUNAMIS IN OREGON DAMAGE IN doWNTOWN KLAMATH FALLS FRom A MAGNITUde 6.0 EARTHQUAke IN 1993 TSUNAMI DAMAGE IN SEASIde FRom THE 1964GR EAT ALASKAN EARTHQUAke 1 Oregon Emergency Management Copyright 2009, Humboldt Earthquake Education Center at Humboldt State University. Adapted and reproduced with permission by Oregon Emergency You Can Prepare for the Management with help from the Oregon Department of Geology and Mineral Industries. Reproduction by permission only. Next Quake or Tsunami Disclaimer This document is intended to promote earthquake and tsunami readiness. It is based on the best SOME PEOplE THINK it is not worth preparing for an earthquake or a tsunami currently available scientific, engineering, and sociological because whether you survive or not is up to chance. NOT SO! Most Oregon research. Following its suggestions, however, does not guarantee the safety of an individual or of a structure. buildings will survive even a large earthquake, and so will you, especially if you follow the simple guidelines in this handbook and start preparing today. Prepared by the Humboldt Earthquake Education Center and the Redwood Coast Tsunami Work Group (RCTWG), If you know how to recognize the warning signs of a tsunami and understand in cooperation with the California Earthquake Authority what to do, you will survive that too—but you need to know what to do ahead (CEA), California Emergency Management Agency (Cal EMA), Federal Emergency Management Agency (FEMA), of time! California Geological Survey (CGS), Department of This handbook will help you prepare for earthquakes and tsunamis in Oregon. Interior United States Geological Survey (USGS), the National Oceanographic and Atmospheric Administration It explains how you can prepare for, survive, and recover from them.
    [Show full text]
  • Interview with Thomas K. Caughey
    THOMAS K. CAUGHEY (1927–2004) INTERVIEWED BY CAROL BUGÉ March 25 and April 2, 1987 Photo Courtesy Caltech’s Engineering & Science ARCHIVES CALIFORNIA INSTITUTE OF TECHNOLOGY Pasadena, California Subject area Engineering Abstract Interview in two sessions in 1987 by Carol Bugé with Thomas Kirk Caughey, Professor of Applied Mechanics and Caltech alumnus (PhD, 1954). Caughey was born and educated in Scotland (bachelor's degree, University of Glasgow, 1948.) Comes to the U.S. with Fulbright to Cornell, where he completes his master's degree in mechanical engineering in 1952. He then earns his PhD at Caltech in 1954. He recalls Caltech’s engineering and physics faculty in the 1950s: H. Frederic Bohnenblust, Arthur Erdelyi, Richard P. Feynman, Tsien Hsue-shen. Begins teaching at Caltech in 1955; recalls Caltech’s Engineering Division under Frederick Lindvall; other engineers and physicists; compares engineering to other disciplines. Return to Cornell and earlier period: outstanding Cornell professors Feynman, Hans Bethe, Barney Rosser, Ed Gunder, Harry Conway; recalls grad student Ross Evan Iwanowski. Problems of physics degree program at Cornell. Professors http://resolver.caltech.edu/CaltechOH:OH_Caughey_T Gray and Bernard Hague at Glasgow University. Comparison between American and European educational systems. His research in dynamics. Earthquake research at Caltech: George Housner and Donald Hudson. Discusses physics and engineering entering a decade of decline; coming fields of genetic engineering, cognitive science and computing, neural networks, and artificial intelligence. Anecdotes about Fritz Zwicky and Charles Richter. Comments on coeducation at Caltech. Caltech personalities: Robert Millikan in his late years; Paul Epstein; Edward Simmons, Richard Gerke; William A. Fowler; further on Zwicky, Hudson; engineers Donald Clark, Alfred Ingersoll; early memories of Earnest Watson.
    [Show full text]
  • Beyond the Angle of Repose: a Review and Synthesis of Landslide Processes in Response to Rapid Uplift, Eel River, Northern Eel River, Northern California
    Portland State University PDXScholar Geology Faculty Publications and Presentations Geology 2-23-2015 Beyond the Angle of Repose: A Review and Synthesis of Landslide Processes in Response to Rapid Uplift, Eel River, Northern Eel River, Northern California Joshua J. Roering University of Oregon Benjamin H. Mackey University of Canterbury Alexander L. Handwerger University of Oregon Adam M. Booth Portland State University, [email protected] Follow this and additional works at: https://pdxscholar.library.pdx.edu/geology_fac David A. Schmidt Univ Persityart of of the W Geologyashington Commons , Geomorphology Commons, and the Geophysics and Seismology Commons Let us know how access to this document benefits ou.y See next page for additional authors Citation Details Roering, Joshua J., Mackey, Benjamin H., Handwerger, Alexander L., Booth, Adam M., Schmidt, David A., Bennett, Georgina L., Cerovski-Darriau, Corina, Beyond the angle of repose: A review and synthesis of landslide pro-cesses in response to rapid uplift, Eel River, Northern California, Geomorphology (2015), doi: 10.1016/j.geomorph.2015.02.013 This Post-Print is brought to you for free and open access. It has been accepted for inclusion in Geology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Joshua J. Roering, Benjamin H. Mackey, Alexander L. Handwerger, Adam M. Booth, David A. Schmidt, Georgina L. Bennett, and Corina Cerovski-Darriau This post-print is available at PDXScholar: https://pdxscholar.library.pdx.edu/geology_fac/75 ACCEPTED MANUSCRIPT Beyond the angle of repose: A review and synthesis of landslide processes in response to rapid uplift, Eel River, Northern California Joshua J.
    [Show full text]
  • Strengthening the Link Between Earthquake Engineering and Architecture
    Strengthening the link between earthquake engineering and architecture A. W. Charleson School of Architecture, Victoria University of Wellington 2004 NZSEE Conference ABSTRACT: With reference mainly to the New Zealand scene, this paper reports on current initiatives to strengthen architects’ understanding and engagement with issues of earthquake engineering. The situation at the three schools of architecture in New Zealand is reviewed with mention made of some recent developments, including the introduction of earthquake structural design software and progress in integrating architectural and seismic design in studio projects. The paper notes a current earthquake engineering course organized and run by NZSEE and reviews the profile of earthquake engineering as represented in Architecture New Zealand. Overseas initiatives are also reported on. The paper concludes with recommendations for further strengthening the links between the professions. 1 INTRODUCTION Given the conference theme of ‘Earthquake Engineering: getting the message across and moving ahead’, this paper explores aspects of how the message of earthquake engineering is being communicated to architects. How strong are the links between these two allied disciplines currently, and how might they be strengthened? First, we need to ask ourselves, why are strong links important? The answer, which probably needs recalling, lies in the value of close collaboration between architects and engineers during the design process, and especially in those very early stages of design when structural layout is largely determined. Decisions made during those feasibility or preliminary design stages affect the cost- effectiveness of the structure considerably, can enable structure to integrate well with overall architectural intentions, and lead to an adequate and predictable seismic performance.
    [Show full text]
  • Earthquake/Landslide Death Scene Investigation Supplement
    Death Scene Investigation Supplement EARTHQUAKE/LANDSLIDE 1 DECEDENT PERSONAL DETAILS Last Name: First Name: Sex: Law Enforcement Case Number (if available): Male Female ME/C Case Number (if available): Law Enforcement Agency (if applicable): Date of Birth: Date of Death: Estimated Found Known MM DD YYYY MM DD YYYY Location of Injury (physical address, including ZIP code): 2 LOCATION OF THE DECEDENT Was the decedent found INDOORS? Yes No Complete 2A: OUTDOORS In what part of residence or building was the decedent found? Did the incident destroy the location? Yes No Unknown Did the incident collapse the walls or ceiling of the location? Yes No Unknown 2A OUTDOORS Was the decedent found OUTDOORS? Yes No Go to Section 3: Information about Circumstances of Death Any evidence the person was previously in a... Structure? Yes No Unknown Vehicle? Yes No Unknown 3 INFORMATION ABOUT CIRCUMSTANCES OF DEATH Does the cause of death appear to be due to any of the following? Select all potential causes of death. Complete all corresponding sections, THEN go to Section 7. Injury – Struck by (e.g., falling object)/Blunt force/Burns Complete Section 4: Injury Questions Motor Vehicle Crash Complete Section 5: Motor Vehicle Crash Questions Other (e.g., exacerbation of chronic diseases) Complete Section 6: Other Non-Injury Causes Questions 1 4 INJURY QUESTIONS How did the injury occur? Check all that apply: Hit by or struck against (Describe) Crushed (Describe) Asphyxia (Describe) Cut/laceration/impaled (Describe) Electric current or burn (Describe) Burn and/or
    [Show full text]
  • Distribution Pattern of Landslides Triggered by the 2014
    International Journal of Geo-Information Article Distribution Pattern of Landslides Triggered by the 2014 Ludian Earthquake of China: Implications for Regional Threshold Topography and the Seismogenic Fault Identification Suhua Zhou 1,2, Guangqi Chen 1 and Ligang Fang 2,* 1 Department of Civil and Structural Engineering, Kyushu University, Fukuoka 819-0395, Japan; [email protected] (S.Z.); [email protected] (G.C.) 2 Department of Geotechnical Engineering, Central South University, Changsha 410075, China * Correspondance: [email protected]; Tel.: +86-731-8253-9756 Academic Editor: Wolfgang Kainz Received: 16 February 2016; Accepted: 11 March 2016; Published: 30 March 2016 Abstract: The 3 August 2014 Ludian earthquake with a moment magnitude scale (Mw) of 6.1 induced widespread landslides in the Ludian County and its vicinity. This paper presents a preliminary analysis of the distribution patterns and characteristics of these co-seismic landslides. In total, 1826 landslides with a total area of 19.12 km2 triggered by the 3 August 2014 Ludian earthquake were visually interpreted using high-resolution aerial photos and Landsat-8 images. The sizes of the landslides were, in general, much smaller than those triggered by the 2008 Wenchuan earthquake. The main types of landslides were rock falls and shallow, disrupted landslides from steep slopes. These landslides were unevenly distributed within the study area and concentrated within an elliptical area with a 25-km NW–SE striking long axis and a 15-km NW–SE striking short axis. Three indexes including landslides number (LN), landslide area ratio (LAR), and landslide density (LD) were employed to analyze the relation between the landslide distribution and several factors, including lithology, elevation, slope, aspect, distance to epicenter and distance to the active fault.
    [Show full text]
  • Risk Analysis of Soil Liquefaction in Earthquake Disasters
    E3S Web of Conferences 118, 03037 (2019) https://doi.org/10.1051/e3sconf/201911803037 ICAEER 2019 Risk analysis of soil liquefaction in earthquake disasters Yubin Zhang1,* 1National Earthquake Response Support Service, Beijing 100049, P. R. China Abstract. China is an earthquake-prone country. With the development of urbanization in China, the effect of population aggregation becomes more and more obvious, and the Casualty Risk of earthquake disasters also increases. Combining with the characteristics of earthquake liquefaction, this paper analyses the disaster situation of soil liquefaction caused by earthquake in Indonesia. The internal influencing factors of soil liquefaction and the external dynamic factors caused by earthquake are summarized, and then the evaluation factors of seismic liquefaction are summarized. The earthquake liquefaction risk is indexed to facilitate trend analysis. The index of earthquake liquefaction risk is more conducive to the disaster trend analysis of soil liquefaction risk areas, which is of great significance for earthquake disaster rescue. 1 Risk analysis of earthquake an earthquake of M7.5 occurred in the Palu region of liquefaction Indonesia. The liquefaction caused by the earthquake is evident in its severity and spatial range. According to the Earthquake disasters often cause serious damage to us report of Indonesia's National Disaster Response Agency because they are unpredictable. Search the US Geological (BNPB), more than 3,000 people were missing in Petobo Survey (USGS) website for the number of earthquakes and Balaroa, two of Palu's worst-hit areas. These with magnitude 6 and above in the last 50 years, about situations were compared with remote sensing images 7,000times.Earthquake liquefaction has existed since before and after the disaster.
    [Show full text]
  • Landslide Triggering Mechanisms
    kChapter 4 GERALD F. WIECZOREK LANDSLIDE TRIGGERING MECHANISMS 1. INTRODUCTION 2.INTENSE RAINFALL andslides can have several causes, including Storms that produce intense rainfall for periods as L geological, morphological, physical, and hu- short as several hours or have a more moderate in- man (Alexander 1992; Cruden and Vames, Chap. tensity lasting several days have triggered abun- 3 in this report, p. 70), but only one trigger (Varnes dant landslides in many regions, for example, 1978, 26). By definition a trigger is an external California (Figures 4-1, 4-2, and 4-3). Well- stimulus such as intense rainfall, earthquake shak- documented studies that have revealed a close ing, volcanic eruption, storm waves, or rapid stream relationship between rainfall intensity and acti- erosion that causes a near-immediate response in vation of landslides include those from California the form of a landslide by rapidly increasing the (Campbell 1975; Ellen et al. 1988), North stresses or by reducing the strength of slope mate- Carolina (Gryta and Bartholomew 1983; Neary rials. In some cases landslides may occur without an and Swift 1987), Virginia (Kochel 1987; Gryta apparent attributable trigger because of a variety or and Bartholomew 1989; Jacobson et al. 1989), combination of causes, such as chemical or physi- Puerto Rico (Jibson 1989; Simon et al. 1990; cal weathering of materials, that gradually bring the Larsen and Torres Sanchez 1992)., and Hawaii slope to failure. The requisite short time frame of (Wilson et al. 1992; Ellen et al. 1993). cause and effect is the critical element in the iden- These studies show that shallow landslides in tification of a landslide trigger.
    [Show full text]
  • Case Study on Slope Stability Changes Caused by Earthquakes—Focusing on Gyeongju 5.8 ML EQ
    sustainability Article Case Study on Slope Stability Changes Caused by Earthquakes—Focusing on Gyeongju 5.8 ML EQ Sangki Park , Wooseok Kim *, Jonghyun Lee and Yong Baek Korea Institute of Civil Engineering and Building Technology, 283, Goyang-daero, Ilsanseo-gu, Goyang-si 10223, Gyeonggi-do, Korea; [email protected] (S.P.); [email protected] (J.L.); [email protected] (Y.B.) * Correspondence: [email protected]; Tel.: +82-31-910-0519 Received: 16 July 2018; Accepted: 16 September 2018; Published: 27 September 2018 Abstract: Slope failure is a natural hazard occurring around the world and can lead to severe damage of properties and loss of lives. Even in stabilized slopes, changes in external loads, such as those from earthquakes, may cause slope failure and collapse, generating social impacts and, eventually causing loss of lives. In this research, the slope stability changes caused by the Gyeongju earthquake, which occurred on 12 September 2016, are numerically analyzed in a slope located in the Gyeongju area, South Korea. Slope property data, collected through an on-site survey, was used in the analysis. Additionally, slope stability changes with and without the earthquake were analyzed and compared. The analysis was performed within a peak ground acceleration (PGA) range of 0.0 (g)–2.0 (g) to identify the correlation between the slope safety factor and peak ground acceleration. The correlation between the slope safety factor and peak ground acceleration could be used as a reference for performing on-site slope stability evaluations. It also provides a reference for design and earthquake stability improvements in the slopes of road and tunnel construction projects, thus supporting the attainment of slope stability in South Korea.
    [Show full text]
  • Selection of Method for Seismic Slope Stability Analysis
    Missouri University of Science and Technology Scholars' Mine International Conferences on Recent Advances 1991 - Second International Conference on in Geotechnical Earthquake Engineering and Recent Advances in Geotechnical Earthquake Soil Dynamics Engineering & Soil Dynamics 14 Mar 1991, 2:00 pm - 3:30 pm Selection of Method for Seismic Slope Stability Analysis Neven Matasovic University of California, Los Angeles, CA Follow this and additional works at: https://scholarsmine.mst.edu/icrageesd Part of the Geotechnical Engineering Commons Recommended Citation Matasovic, Neven, "Selection of Method for Seismic Slope Stability Analysis" (1991). International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics. 25. https://scholarsmine.mst.edu/icrageesd/02icrageesd/session07/25 This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This Article - Conference proceedings is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics by an authorized administrator of Scholars' Mine. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. /\ Proceedings: Second International Conference on Recent Advances In Geotechnical Earthquake Engineering and Soil Dynamics, ~ March 11-15, 1991, St. Louis, Missouri, Paper No. 7.20 5election of Method for Seismic Slope Stability Analysis "even Matasovic' 3raduate Student, University of California, Los Angeles, .:alifornla SYNOPSIS: The seismic stability of natural slopes in clayey materials is a subject about which much uncertainty still exists. Therefore, selection of the method for the seismic slope stability analysis is an important part of solving the problem.
    [Show full text]