Ho Sung Kim Mechanics of Solids and Fracture
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6. Fracture Mechanics
6. Fracture mechanics lead author: J, R. Rice Division of Applied Sciences, Harvard University, Cambridge MA 02138 Reader's comments on an earlier draft, prepared in consultation with J. W. Hutchinson, C. F. Shih, and the ASME/AMD Technical Committee on Fracture Mechanics, pro vided by A. S. Argon, S. N. Atluri, J. L. Bassani, Z. P. Bazant, S. Das, G. J. Dvorak, L. B. Freund, D. A. Glasgow, M. F. Kanninen, W. G. Knauss, D. Krajcinovic, J D. Landes, H. Liebowitz, H. I. McHenry, R. O. Ritchie, R. A. Schapery, W. D. Stuart, and R. Thomson. 6.0 ABSTRACT Fracture mechanics is an active research field that is currently advancing on many fronts. This appraisal of research trends and opportunities notes the promising de velopments of nonlinear fracture mechanics in recent years and cites some of the challenges in dealing with topics such as ductile-brittle transitions, failure under sub stantial plasticity or creep, crack tip processes under fatigue loading, and the need for new methodologies for effective fracture analysis of composite materials. Continued focus on microscale fracture processes by work at the interface of solid mechanics and materials science holds promise for understanding the atomistics of brittle vs duc tile response and the mechanisms of microvoid nucleation and growth in various ma terials. Critical experiments to characterize crack tip processes and separation mecha nisms are a pervasive need. Fracture phenomena in the contexts of geotechnology and earthquake fault dynamics also provide important research challenges. 6.1 INTRODUCTION cracking in the more brittle structural materials such as high strength metal alloys. -
326-97 Lab Final S.D
Geol 326-97 Name: KEY 5/6/97 Class Ave = 101 / 150 Geol 326-97 Lab Final s.d. = 24 This lab final exam is worth 150 points of your total grade. Each lettered question is worth 15 points. Read through it all first to find out what you need to do. List all of your answers on these pages and attach any constructions, tracing paper overlays, etc. Put your name on all pages. 1. One way to analyze brittle faults is to calculate and plot the infinitesimal shortening and extension directions on a lower hemisphere, stereographic projection. These principal axes lie in the “movement plane”, which contains the pole to the fault plane and the slickensides, and are at 45° to the pole. The following questions apply to a single fault described in part (a), below: (a) A fault has a strike and dip of 250, 57 N and the slickensides have a rake of 63°, measured from the given strike azimuth. Plot the orientations of the fault plane and the slickensides on an equal area projection. (b) Bedding in the vicinity of the fault is oriented 37, 42 E. Assuming that the fault formed when the bedding was horizontal, determine and plot the original geometry of the fault and the slickensides. (c) Determine the original (pre-rotation)orientation of the infinitesimal shortening and extension axes for fault. 2. All of the following questions apply to the map shown on the next page. In all of the rocks with cleavage, you may assume that both cleavage and bedding strike 024°. -
Faults and Joints
133 JOINTS Joints (also termed extensional fractures) are planes of separation on which no or undetectable shear displacement has taken place. The two walls of the resulting tiny opening typically remain in tight (matching) contact. Joints may result from regional tectonics (i.e. the compressive stresses in front of a mountain belt), folding (due to curvature of bedding), faulting, or internal stress release during uplift or cooling. They often form under high fluid pressure (i.e. low effective stress), perpendicular to the smallest principal stress. The aperture of a joint is the space between its two walls measured perpendicularly to the mean plane. Apertures can be open (resulting in permeability enhancement) or occluded by mineral cement (resulting in permeability reduction). A joint with a large aperture (> few mm) is a fissure. The mechanical layer thickness of the deforming rock controls joint growth. If present in sufficient number, open joints may provide adequate porosity and permeability such that an otherwise impermeable rock may become a productive fractured reservoir. In quarrying, the largest block size depends on joint frequency; abundant fractures are desirable for quarrying crushed rock and gravel. Joint sets and systems Joints are ubiquitous features of rock exposures and often form families of straight to curviplanar fractures typically perpendicular to the layer boundaries in sedimentary rocks. A set is a group of joints with similar orientation and morphology. Several sets usually occur at the same place with no apparent interaction, giving exposures a blocky or fragmented appearance. Two or more sets of joints present together in an exposure compose a joint system. -
Pacific Petroleum Eology
Pacific Petroleum Geology NEWSLETTER Pacific Section • American Association of Petroleum Geologists September & October• 2010 School of Rock Ridge Basin CONTENTS 2010-2011 OFF I C E RS EV E RY ISSU E President Cynthia Huggins 661.665.5074 [email protected] 4 Message from the President • C. Huggins President-Elect John Minch 805.898.9200 6 Editor’s Corner • E. Washburn [email protected] Vice President Jeff Gartland 7 PS-AAPG News 661.869.8204 [email protected] 13 Publications Secretary Tony Reid 661.412.5467 17 Member Society News [email protected] Treasurer 2009-2011 Cheryl Blume TH I S ISSU E 661.864.4722 [email protected] 8 Sharktooth Hill Fossil Fund • K. Hancharick Treasurer 2010-2012 Jana McIntyre 661.869.8231 [email protected] 10 AAPG Young Professionals • J. Allen Past President Scott Hector 11 Serpentine: The Rest of the Story • Mel 707.974.6402 [email protected] Erskine Editor-in-Chief Ed Washburn 661.654.7182 [email protected] ST AFF Web Master Bob Countryman 661.589.8580 [email protected] Membership Chair Brian Church 661.654.7863 [email protected] Publications Chair Larry Knauer 661.392.2471 [email protected] [email protected] Advisory Council Representative Kurt Neher 661.412.5203 [email protected] Cover photo of Ridge Basin outcrop courtesy Jonathan Allen Page 3 Pacific Petroleum Geologist Newsletter September & October • 2010 MESSAGE FRO M THE PRESIDENT CYNTHIA HUGGINS Do you know what Marilyn Bachman, Mike Fillipow, Peggy Lubchenco, and Jane Justus Frazier have in common? They were all recipients of the Teacher of the Year Award from AAPG, and they all came from the Pacific Section! Of the 13 recipients of this award, four have been from PSAAPG. -
AC Fischer-Cripps
A.C. Fischer-Cripps Introduction to Contact Mechanics Series: Mechanical Engineering Series ▶ Includes a detailed description of indentation stress fields for both elastic and elastic-plastic contact ▶ Discusses practical methods of indentation testing ▶ Supported by the results of indentation experiments under controlled conditions Introduction to Contact Mechanics, Second Edition is a gentle introduction to the mechanics of solid bodies in contact for graduate students, post doctoral individuals, and the beginning researcher. This second edition maintains the introductory character of the first with a focus on materials science as distinct from straight solid mechanics theory. Every chapter has been 2nd ed. 2007, XXII, 226 p. updated to make the book easier to read and more informative. A new chapter on depth sensing indentation has been added, and the contents of the other chapters have been completely overhauled with added figures, formulae and explanations. Printed book Hardcover ▶ 159,99 € | £139.99 | $199.99 The author begins with an introduction to the mechanical properties of materials, ▶ *171,19 € (D) | 175,99 € (A) | CHF 189.00 general fracture mechanics and the fracture of brittle solids. This is followed by a detailed description of indentation stress fields for both elastic and elastic-plastic contact. The discussion then turns to the formation of Hertzian cone cracks in brittle materials, eBook subsurface damage in ductile materials, and the meaning of hardness. The author Available from your bookstore or concludes with an overview of practical methods of indentation. ▶ springer.com/shop MyCopy Printed eBook for just ▶ € | $ 24.99 ▶ springer.com/mycopy Order online at springer.com ▶ or for the Americas call (toll free) 1-800-SPRINGER ▶ or email us at: [email protected]. -
Chapter 01.Pdf
Mathematical Background in Aircraft Structural Mechanics CHAPTER 1. Linear Elasticity SangJoon Shin School of Mechanical and Aerospace Engineering Seoul National University Active Aeroelasticityand Rotorcraft Lab. Basic equation of Linear Elasticity Structural analysis … evaluation of deformations and stresses arising within a solid object under the action of applied loads - if time is not explicitly considered as an independent variable → the analysis is said to be static → otherwise, structural dynamic analysis or structural dynamics Small deformation Under the assumption of { Linearly elastic material behavior - Three dimensional formulation → a set of 15 linear 1st order PDE involving displacement field (3 components) { stress field (6 components) strain field (6 components) plane stress problem → simpler, 2-D formulations { plane strain problem For most situations, not possible to develop analytical solutions → analysis of structural components … bars, beams, plates, shells 1-2 Active Aeroelasticity and Rotorcraft Lab., Seoul National University 1.1 The concept of Stress 1.1.1 The state of stress at a point State of stress in a solid body… measure of intensity of forces acting within the solid - distribution of forces and moments appearing on the surface of the cut … equipollent force F , and couple M - Newton’s 3rd law → a force and couple of equal magnitudes and opposite directions acting on the two forces created by the cut Fig. 1.1 A solid body cut by a plane to isolate a free body 1-3 Active Aeroelasticity and Rotorcraft -
Fracture and Deformation of Soft Materials and Structures
Iowa State University Capstones, Theses and Graduate Theses and Dissertations Dissertations 2018 Fracture and deformation of soft am terials and structures Zhuo Ma Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/etd Part of the Aerospace Engineering Commons, Engineering Mechanics Commons, Materials Science and Engineering Commons, and the Mechanics of Materials Commons Recommended Citation Ma, Zhuo, "Fracture and deformation of soft am terials and structures" (2018). Graduate Theses and Dissertations. 16852. https://lib.dr.iastate.edu/etd/16852 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. Fracture and deformation of soft materials and structures by Zhuo Ma A dissertation submitted to the graduate faculty in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Major: Engineering Mechanics Program of Study Committee: Wei Hong, Co-major Professor Ashraf Bastawros, Co-major Professor Pranav Shrotriya Liang Dong Liming Xiong The student author, whose presentation of the scholarship herein was approved by the program of study committee, is solely responsible for the content of this dissertation. The Graduate College will ensure this dissertation is globally accessible and will not permit alterations after a degree is conferred. Iowa State University Ames, Iowa 2018 Copyright © Zhuo Ma, 2018. All rights reserved. ii TABLE OF CONTENTS Page LIST OF FIGURES .......................................................................................................... -
Folds and Folding
Chapter ................................ 11 Folds and folding Folds are eye-catching and visually attractive structures that can form in practically any rock type, tectonic setting and depth. For these reasons they have been recognized, admired and explored since long before geology became a science (Leonardo da Vinci discussed them some 500 years ago, and Nicholas Steno in 1669). Our understanding of folds and folding has changed over time, and the fundament of what is today called modern fold theory was more or less consolidated in the 1950s and 1960s. Folds, whether observed on the micro-, meso- or macroscale, are clearly some of our most important windows into local and regional deformation histories of the past. Their geometry and expression carry important information about the type of deformation, kinematics and tectonics of an area. Besides, they can be of great economic importance, both as oil traps and in the search for and exploitation of ores and other mineral resources. In this chapter we will first look at the geometric aspects of folds and then pay attention to the processes and mechanisms at work during folding of rock layers. 220 Folds and folding 11.1 Geometric description (a) Kink band a a It is fascinating to watch folds form and develop in the laboratory, and we can learn much about folds and folding by performing controlled physical experiments and numerical simulations. However, modeling must always be rooted in observations of naturally folded Trace of Axial trace rocks, so geometric analysis of folds formed in different bisecting surface settings and rock types is fundamental. Geometric analy- (b) Chevron folds sis is important not only in order to understand how various types of folds form, but also when considering such things as hydrocarbon traps and folded ores in the subsurface. -
The Role of Flexural Slip in the Development of Chevron Folds
Scholars' Mine Masters Theses Student Theses and Dissertations Spring 2018 The role of flexural slip in the development of chevron folds Yuxing Wu Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Petroleum Engineering Commons Department: Recommended Citation Wu, Yuxing, "The role of flexural slip in the development of chevron folds" (2018). Masters Theses. 7788. https://scholarsmine.mst.edu/masters_theses/7788 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. 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]. i THE ROLE OF FLEXURAL SLIP IN THE DEVELOPMENT OF CHEVRON FOLDS by YUXING WU A THESIS Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE IN PETROLEUM ENGINEERING 2018 Approved by Andreas Eckert, Advisor John Patrick Hogan Jonathan Obrist Farner ii 2018 Yuxing Wu All Rights Reserved iii ABSTRACT Chevron folds are characterized by straight limbs and narrow hinge zones. One of the conceptual models to initiate and develop chevron folds involves flexural slip during folding. While some kinematical models show the necessity for slip to initiate during chevron folding, recent numerical modeling studies of visco-elastic effective single layer buckle folding have shown that flexural slip does not result in chevron folds. In this study, several 2D finite element analysis models are run, distinguished by 1) geometry of the initial perturbation (sinusoidal and white noise), 2) varying thewavelength of the initial perturbation (10%, 50%, and 100% of the dominant wavelength) and 3) variation of the friction coefficient (high and low friction coefficient between interlayers). -
Collision Orogeny
Downloaded from http://sp.lyellcollection.org/ by guest on October 6, 2021 PROCESSES OF COLLISION OROGENY Downloaded from http://sp.lyellcollection.org/ by guest on October 6, 2021 Downloaded from http://sp.lyellcollection.org/ by guest on October 6, 2021 Shortening of continental lithosphere: the neotectonics of Eastern Anatolia a young collision zone J.F. Dewey, M.R. Hempton, W.S.F. Kidd, F. Saroglu & A.M.C. ~eng6r SUMMARY: We use the tectonics of Eastern Anatolia to exemplify many of the different aspects of collision tectonics, namely the formation of plateaux, thrust belts, foreland flexures, widespread foreland/hinterland deformation zones and orogenic collapse/distension zones. Eastern Anatolia is a 2 km high plateau bounded to the S by the southward-verging Bitlis Thrust Zone and to the N by the Pontide/Minor Caucasus Zone. It has developed as the surface expression of a zone of progressively thickening crust beginning about 12 Ma in the medial Miocene and has resulted from the squeezing and shortening of Eastern Anatolia between the Arabian and European Plates following the Serravallian demise of the last oceanic or quasi- oceanic tract between Arabia and Eurasia. Thickening of the crust to about 52 km has been accompanied by major strike-slip faulting on the rightqateral N Anatolian Transform Fault (NATF) and the left-lateral E Anatolian Transform Fault (EATF) which approximately bound an Anatolian Wedge that is being driven westwards to override the oceanic lithosphere of the Mediterranean along subduction zones from Cephalonia to Crete, and Rhodes to Cyprus. This neotectonic regime began about 12 Ma in Late Serravallian times with uplift from wide- spread littoral/neritic marine conditions to open seasonal wooded savanna with coiluvial, fluvial and limnic environments, and the deposition of the thick Tortonian Kythrean Flysch in the Eastern Mediterranean. -
Elastic Plastic Fracture Mechanics Elastic Plastic Fracture Mechanics Presented by Calvin M
Fracture Mechanics Elastic Plastic Fracture Mechanics Elastic Plastic Fracture Mechanics Presented by Calvin M. Stewart, PhD MECH 5390-6390 Fall 2020 Outline • Introduction to Non-Linear Materials • J-Integral • Energy Approach • As a Contour Integral • HRR-Fields • COD • J Dominance Introduction to Non-Linear Materials Introduction to Non-Linear Materials • Thus far we have restricted our fractured solids to nominally elastic behavior. • However, structural materials often cannot be characterized via LEFM. Non-Linear Behavior of Materials • Two other material responses are that the engineer may encounter are Non-Linear Elastic and Elastic-Plastic Introduction to Non-Linear Materials • Loading Behavior of the two materials is identical but the unloading path for the elastic plastic material allows for non-unique stress- strain solutions. For Elastic-Plastic materials, a generic “Constitutive Model” specifies the relationship between stress and strain as follows n tot =+ Ramberg-Osgood 0 0 0 0 Reference (or Flow/Yield) Stress (MPa) Dimensionaless Constant (unitless) 0 Reference (or Flow/Yield) Strain (unitless) n Strain Hardening Exponent (unitless) Introduction to Non-Linear Materials • Ramberg-Osgood Constitutive Model n increasing Ramberg-Osgood −n K = 00 Strain Hardening Coefficient, K = 0 0 E n tot K,,,,0 n=+ E Usually available for a variety of materials 0 0 0 Introduction to Non-Linear Materials • Within the context of EPFM two general ways of trying to solve fracture problems can be identified: 1. A search for characterizing parameters (cf. K, G, R in LEFM). 2. Attempts to describe the elastic-plastic deformation field in detail, in order to find a criterion for local failure. -
Fracture Cleavage'' in the Duluth Complex, Northeastern Minnesota
Downloaded from gsabulletin.gsapubs.org on August 9, 2013 Geological Society of America Bulletin ''Fracture cleavage'' in the Duluth Complex, northeastern Minnesota M. E. FOSTER and P. J. HUDLESTON Geological Society of America Bulletin 1986;97, no. 1;85-96 doi: 10.1130/0016-7606(1986)97<85:FCITDC>2.0.CO;2 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes Geological Society of America Downloaded from gsabulletin.gsapubs.org on August 9, 2013 "Fracture cleavage" in the Duluth Complex, northeastern Minnesota M.