Chapter 6 Seismic Design
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Using Opensees for Analyzing a 9- Story Steel Building Under Post- Earthquake Fires
Tenth U.S. National Conference on Earthquake Engineering Frontiers of Earthquake Engineering July 21-25, 2014 10NCEE Anchorage, Alaska USING OPENSEES FOR ANALYZING A 9- STORY STEEL BUILDING UNDER POST- EARTHQUAKE FIRES N. Elhami Khorasani1 and M. E. M. Garlock2 ABSTRACT Post-earthquake fires are major hazards with possible intense consequences. Civil engineering design is moving towards the concept of resilient cities, which requires buildings with structural systems to perform adequately after extreme hazards and ensure human safety. Current codes and standards in fire engineering are mainly based on design at the component level and deterministic approaches, where uncertainties in variables are not directly incorporated in the design process. Reliability-based approaches offer better means of evaluating resilience in the face of extreme hazards. But to measure resilience in an earthquake-fire multi-hazard scenario, uncertainties in the system must be captured, and nonlinear analyses must seamlessly transfer from seismic to fire analysis. This paper discusses the successes and challenges of this seamless analysis using the open source software OpenSees. A 9-story steel building with moment resisting frames is subject to fire following earthquake while being modeled in OpenSees. With the newly added fire module in OpenSees, the software has the capacity to perform structural analysis for both seismic and thermal loads. This way, system-level analysis is performed in one software and interaction of members with each other, under both seismic and fire events, is then considered together. The current constitutive material model for steel at elevated temperature does not properly capture behavior in fire following earthquake scenario. -
Effect of Fabric Anisotropy on the Dynamic Mechanical Behavior Of
EFFECT OF FABRIC ANISOTROPY ON THE DYNAMIC MECHANICAL BEHAVIOR OF GRANULAR MATERIALS by Bo Li Submitted in partial fulfillment of the requirements For the degree of Doctor of Philosophy Dissertation Advisor: Prof. Xiangwu Zeng Department of Civil Engineering Case Western Reserve University January, 2011 CASE WESTERN RESERVE UNIVERSITY SCHOOL OF GRADUATE STUDIES We hereby approve the thesis/dissertation of Bo Li Candidate for Ph. D. degree*. (signed) Xiangwu Zeng Chair of Commitee Adel Saada Wojbor A. Woyczynski Xiong Yu (date) 11/15/2010 *We also certify that written approval has been obtained for any proprietary material contained therein Table of Contents Table of Contents I List of Tables IV List of Figures VI Acknowledgement XI Abstract XII Notation XIV Chapter 1 Introduction ........................................................................................ 1 1.1 Effect of Anisotropy on Granular Materials ........................................................................... 1 1.2 Research Objectives ............................................................................................................... 1 1.3 Outline of the Dissertation ...................................................................................................... 2 1.4 Review of the Effect of Fabric Anisotropy on Clay ............................................................... 3 1.4.1 Experimental Study on Effect of Fabric Anisotropy on Clay ......................................... 3 1.4.2 Analytical Method on Effect of Fabric Anisotropy -
Confidential Manuscript Submitted to Engineering Geology
Confidential manuscript submitted to Engineering Geology 1 Landslide monitoring using seismic refraction tomography – The 2 importance of incorporating topographic variations 3 J S Whiteley1,2, J E Chambers1, S Uhlemann1,3, J Boyd1,4, M O Cimpoiasu1,5, J L 4 Holmes1,6, C M Inauen1, A Watlet1, L R Hawley-Sibbett1,5, C Sujitapan2, R T Swift1,7 5 and J M Kendall2 6 1 British Geological Survey, Environmental Science Centre, Nicker Hill, Keyworth, 7 Nottingham, NG12 5GG, United Kingdom. 2 School of Earth Sciences, University 8 of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, United 9 Kingdom. 3 Lawrence Berkeley National Laboratory (LBNL), Earth and 10 Environmental Sciences Area, 1 Cyclotron Road, Berkeley, CA 94720, United 11 States of America. 4 Lancaster Environment Center (LEC), Lancaster University, 12 Lancaster, LA1 4YQ, United Kingdom 5 Division of Agriculture and Environmental 13 Science, School of Bioscience, University of Nottingham, Sutton Bonington, 14 Leicestershire, LE12 5RD, United Kingdom 6 Queen’s University Belfast, School of 15 Natural and Built Environment, Stranmillis Road, Belfast, BT9 5AG, United 16 Kingdom 7 University of Liege, Applied Geophysics, Department ArGEnCo, 17 Engineering Faculty, B52, 4000 Liege, Belgium 18 19 Corresponding author: Jim Whiteley ([email protected]) 20 21 Copyright British Geological Survey © UKRI 2020/ University of Bristol 2020 22 1 Confidential manuscript submitted to Engineering Geology 23 Abstract 24 Seismic refraction tomography provides images of the elastic properties of 25 subsurface materials in landslide settings. Seismic velocities are sensitive to 26 changes in moisture content, which is a triggering factor in the initiation of many 27 landslides. -
On the Wave Bottom Shear Stress in Shallow Depths: the Role of Wave Period and Bed Roughness
water Article On the Wave Bottom Shear Stress in Shallow Depths: The Role of Wave Period and Bed Roughness Sara Pascolo *, Marco Petti and Silvia Bosa Dipartimento Politecnico di Ingegneria e Architettura, University of Udine, 33100 Udine, Italy; [email protected] (M.P.); [email protected] (S.B.) * Correspondence: [email protected]; Tel.: +39-0432-558-713 Received: 6 September 2018; Accepted: 25 September 2018; Published: 28 September 2018 Abstract: Lagoons and coastal semi-enclosed basins morphologically evolve depending on local waves, currents, and tidal conditions. In very shallow water depths, typical of tidal flats and mudflats, the bed shear stress due to the wind waves is a key factor governing sediment resuspension. A current line of research focuses on the distribution of wave shear stress with depth, this being a very important aspect related to the dynamic equilibrium of transitional areas. In this work a relevant contribution to this study is provided, by means of the comparison between experimental growth curves which predict the finite depth wave characteristics and the numerical results obtained by means a spectral model. In particular, the dominant role of the bottom friction dissipation is underlined, especially in the presence of irregular and heterogeneous sea beds. The effects of this energy loss on the wave field is investigated, highlighting that both the variability of the wave period and the relative bottom roughness can change the bed shear stress trend substantially. Keywords: finite depth wind waves; bottom friction dissipation; friction factor; tidal flats; bottom shear stress 1. Introduction The morphological evolution of estuarine and coastal lagoon environments is a widely discussed topic in literature, because of its complexity and the great variability of morphological patterns. -
Guideline for Extraction of Ground Motion Parameters for Scientific Hydraulic Fracturing Review Panel
Guideline for Extraction of Ground Motion Parameters for Scientific Hydraulic Fracturing Review Panel Alireza Babaie Mahani Ph.D. P.Geo. Mahan Geophysical Consulting Inc. Victoria, BC Email: [email protected] Website: www.mahangeo.com Executive Summary The Scientific Review of Hydraulic Fracturing in British Columbia (2019) provides the key findings of a scientific panel on the topic of hydraulic fracturing in British Columbia and the associated environmental risks. As indicated in the report, the panel recommends preparation of guidelines for standard calculation of earthquake magnitude and ground motion parameters. Since Babaie Mahani and Kao (2019 and 2020) have addressed the methodology for calculation of local magnitude in two publications, this report deals with standard methodologies for extraction of ground motion parameters from recorded earthquake waveforms. The guidelines include data from both types of seismic sensors that are used for induced seismicity monitoring; seismometers that record ground motion velocities and accelerometers that are designed to record strong ground accelerations at short distances. Waveforms from the November 30, 2018 induced earthquake with moment magnitude (Mw) of 4.6 that occurred in northeast British Columbia within the Montney unconventional resource play are presented for better understanding of the processing steps. Data Formats The standard format that is used to archive earthquake data is called the SEED format (Standard for the Exchange of Earthquake Data; https://ds.iris.edu/ds/nodes/dmc/data/formats/seed/). When both the time series data and metadata are archived in one file, the name full-SEED is also used. miniSEED is the stripped down version of SEED that only includes waveform data (https://ds.iris.edu/ds/nodes/dmc/data/formats/miniseed/). -
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. -
Recommended Guidelines for Liquefaction Evaluations Using Ground Motions from Probabilistic Seismic Hazard Analyses
RECOMMENDED GUIDELINES FOR LIQUEFACTION EVALUATIONS USING GROUND MOTIONS FROM PROBABILISTIC SEISMIC HAZARD ANALYSES Report to the Oregon Department of Transportation June, 2005 Prepared by Stephen Dickenson Associate Professor Geotechnical Engineering Group Department of Civil, Construction and Environmental Engineering Oregon State University ODOT Liquefaction Hazard Assessment using Ground Motions from PSHA Page 2 ABSTRACT The assessment of liquefaction hazards for bridge sites requires thorough geotechnical site characterization and credible estimates of the ground motions anticipated for the exposure interval of interest. The ODOT Bridge Design and Drafting Manual specifies that the ground motions used for evaluation of liquefaction hazards must be obtained from probabilistic seismic hazard analyses (PSHA). This ground motion data is routinely obtained from the U.S. Geologocal Survey Seismic Hazard Mapping program, through its interactive web site and associated publications. The use of ground motion parameters derived from a PSHA for evaluations of liquefaction susceptibility and ground failure potential requires that the ground motion values that are indicated for the site are correlated to a specific earthquake magnitude. The individual seismic sources that contribute to the cumulative seismic hazard must therefore be accounted for individually. The process of hazard de-aggregation has been applied in PSHA to highlight the relative contributions of the various regional seismic sources to the ground motion parameter of interest. The use of de-aggregation procedures in PSHA is beneficial for liquefaction investigations because the contribution of each magnitude-distance pair on the overall seismic hazard can be readily determined. The difficulty in applying de-aggregated seismic hazard results for liquefaction studies is that the practitioner is confronted with numerous magnitude-distance pairs, each of which may yield different liquefaction hazard results. -
5.4.5 Geological Hazards
Section 5.4.5: Risk Assessment – Geological Hazards 5.4.5 Geological Hazards The following section provides the hazard profile (hazard description, location, extent, previous occurrences and losses, probability of future occurrences, and impact of climate change) and vulnerability assessment for the geological hazards in Sussex County. 2016 Plan Update Changes The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, probability of future occurrence, and potential change in climate and its impacts on the geological hazards is discussed. The geological hazards is now located in Section 5 of the plan update. It includes landslide, land subsidence and sinkholes, all of which were profiled separately in the 2011 HMP. New and updated figures from federal and state agencies are incorporated. U.S. 2010 Census data was incorporated, where appropriate. Previous occurrences were updated with events that occurred between 2008 and 2015. A vulnerability assessment was conducted for the geological hazards and it now directly follows the hazard profile. 5.4.5.1 Profile Hazard Description Geological hazards are any geological or hydrological processes that pose a threat to humans and natural properties. Every year, severe natural events destroy infrastructure and cause injuries and deaths. Geologic hazards may include volcanic eruptions and other geothermal related features, earthquakes, landslides and other slope failures, mudflows, sinkhole collapses, snow avalanches, flooding, glacial surges and outburst floods, tsunamis, and shoreline movements. For the purpose of this HMP update, only landslides and land subsidence/sinkholes will be discussed in the Geological Hazard profile. Landslides According to the U.S. -
1. Geology and Seismic Hazards
8 PUBLIC SAFETY ELEMENT As required by State law, the Public Safety Element addresses the protection of the community from unreasonable risks from natural and manmade haz- ards. This Element provides information about risks in the Eden Area and delineates policies designed to prepare and protect the community as much as possible from the effects of: ♦ Geologic hazards, including earthquakes, ground-shaking, liquefaction and landslides. ♦ Flooding, including dam failures and inundation, tsunamis and seiches. ♦ Wildland fires. ♦ Hazardous materials. This Element also contains information and policies regarding general emer- gency preparedness. Each section includes background information on the particular hazard followed by goals, policies and actions designed to minimize risk for Eden Area residents. The Public Safety Element establishes mechanisms to prepare for and reduce death, injuries and damage to property from public safety hazards like flood- ing, fires and seismic events. Hazards are an unavoidable aspect of life, and the Public Safety Element cannot eliminate risk completely. Instead, the Element contains policies to create an acceptable level of risk. 1. GEOLOGY AND SEISMIC HAZARDS Earthquakes and secondary seismic hazards such as ground-shaking, liquefac- tion and landslides are the primary geologic hazards in the Eden Area. This section provides background on the seismic hazards that affect the Eden Area and includes goals, policies and actions to minimize these risks. 8-1 COUNTY OF ALAMEDA EDEN AREA GENERAL PLAN PUBLIC SAFETY ELEMENT A. Background Information As is the case in most of California, the Eden Area is subject to risks from seismic activity. The Eden Area is located in the San Andreas Fault Zone, one of the most seismically-active regions in the United States, which has generated numerous moderate to strong earthquakes in northern California and in the San Francisco Bay Area. -
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. -
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. -
A Review of the Seismic Hazard Zonation in National Building Codes in the Context of Eurocode 8
A REVIEW OF THE SEISMIC HAZARD ZONATION IN NATIONAL BUILDING CODES IN THE CONTEXT OF EUROCODE 8 Support to the implementation, harmonization and further development of the Eurocodes G. Solomos, A. Pinto, S. Dimova EUR 23563 EN - 2008 A REVIEW OF THE SEISMIC HAZARD ZONATION IN NATIONAL BUILDING CODES IN THE CONTEXT OF EUROCODE 8 Support to the implementation, harmonization and further development of the Eurocodes G. Solomos, A. Pinto, S. Dimova EUR 23563 EN - 2008 The mission of the JRC is to provide customer-driven scientific and technical support for the conception, development, implementation and monitoring of EU policies. As a service of the European Commission, the JRC functions as a reference centre of science and technology for the Union. Close to the policy-making process, it serves the common interest of the Member States, while being independent of special interests, whether private or national. European Commission Joint Research Centre Contact information Address: JRC, ELSA Unit, TP 480, I-21020, Ispra(VA), Italy E-mail: [email protected] Tel.: +39-0332-789989 Fax: +39-0332-789049 http://www.jrc.ec.europa.eu Legal Notice Neither the European Commission nor any person acting on behalf of the Commission is responsible for the use which might be made of this publication. A great deal of additional information on the European Union is available on the Internet. It can be accessed through the Europa server http://europa.eu/ JRC 48352 EUR 23563 EN ISSN 1018-5593 Luxembourg: Office for Official Publications of the European Communities © European Communities, 2008 Reproduction is authorised provided the source is acknowledged Printed in Italy Executive Summary The Eurocodes are envisaged to form the basis for structural design in the European Union and they should enable engineering services to be used across borders for the design of construction works.