PDF (Chapter 14. Anelasticity)
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
Stress Relaxation of Glass Using a Parallel Plate Viscometer Guy-Marie Vallet Clemson University, [email protected]
Clemson University TigerPrints All Theses Theses 8-2011 Stress relaxation of glass using a parallel plate viscometer Guy-marie Vallet Clemson University, [email protected] Follow this and additional works at: https://tigerprints.clemson.edu/all_theses Part of the Materials Science and Engineering Commons Recommended Citation Vallet, Guy-marie, "Stress relaxation of glass using a parallel plate viscometer" (2011). All Theses. 1158. https://tigerprints.clemson.edu/all_theses/1158 This Thesis is brought to you for free and open access by the Theses at TigerPrints. It has been accepted for inclusion in All Theses by an authorized administrator of TigerPrints. For more information, please contact [email protected]. TITLE PAGE STRESS RELAXATION OF GLASS USING A PARALLEL PLATE VISCOMETER A Thesis Presented to The Graduate School of Clemson University In Partial Fulfillment of the Requirements for the Degree of Master of Science Materials Science and Engineering By Guy-Marie Vallet August 2011 Accepted by: Dr. Vincent Blouin, Committee Chair Dr. Jean-Louis Bobet Dr. Evelyne Fargin Dr. Paul Joseph Dr. Véronique Jubera Dr. Igor Luzinov Dr. Kathleen Richardson ABSTRACT Currently, grinding and polishing is the traditional method for manufacturing optical glass lenses. However, for a few years now, precision glass molding has gained importance for its flexibility in manufacturing aspheric lenses. With this new method, glass viscoelasticity and more specifically stress relaxation are important phenomena in the glass transition region to control the molding process and to predict the final lens shape. The goal of this research is to extract stress relaxation parameters in shear of Pyrex® glass by using a Parallel Plate Viscometer (PPV). -
1 Revision 1 Single-Crystal Elastic Properties of Minerals and Related
Revision 1 Single-Crystal Elastic Properties of Minerals and Related Materials with Cubic Symmetry Thomas S. Duffy Department of Geosciences Princeton University Abstract The single-crystal elastic moduli of minerals and related materials with cubic symmetry have been collected and evaluated. The compiled dataset covers measurements made over an approximately seventy year period and consists of 206 compositions. More than 80% of the database is comprised of silicates, oxides, and halides, and approximately 90% of the entries correspond to one of six crystal structures (garnet, rocksalt, spinel, perovskite, sphalerite, and fluorite). Primary data recorded are the composition of each material, its crystal structure, density, and the three independent nonzero adiabatic elastic moduli (C11, C12, and C44). From these, a variety of additional elastic and acoustic properties are calculated and compiled, including polycrystalline aggregate elastic properties, sound velocities, and anisotropy factors. The database is used to evaluate trends in cubic mineral elasticity through consideration of normalized elastic moduli (Blackman diagrams) and the Cauchy pressure. The elastic anisotropy and auxetic behavior of these materials are also examined. Compilations of single-crystal elastic moduli provide a useful tool for investigation structure-property relationships of minerals. 1 Introduction The elastic moduli are among the most fundamental and important properties of minerals (Anderson et al. 1968). They are central to understanding mechanical behavior and have applications across many disciplines of the geosciences. They control the stress-strain relationship under elastic loading and are relevant to understanding strength, hardness, brittle/ductile behavior, damage tolerance, and mechanical stability. Elastic moduli govern the propagation of elastic waves and hence are essential to the interpretation of seismic data, including seismic anisotropy in the crust and mantle (Bass et al. -
Entropy Principle and Recent Results in Non-Equilibrium Theories
Entropy 2014, 16, 1756-1807; doi:10.3390/e16031756 OPEN ACCESS entropy ISSN 1099-4300 www.mdpi.com/journal/entropy Article Entropy Principle and Recent Results in Non-Equilibrium Theories Vito Antonio Cimmelli 1;*, David Jou 2, Tommaso Ruggeri 3 and Péter Ván 4;5;6 1 Department of Mathematics, Computer Science and Economics, University of Basilicata, Potenza 85100, Italy 2 Departament de Física, Universitat Autònoma de Barcelona, Bellaterra, and Institut d’Estudis Catalans, Barcelona, Catalonia 08193, Spain; E-Mail: [email protected] 3 Department of Mathematics and Research Center of Applied Mathematics, University of Bologna, Bologna 40123, Italy; E-Mail: [email protected] 4 Department of Theoretical Physics, Wigner Research Centre for Physics, Institute for Particle and Nuclear Physics, Budapest 1121, Hungary; E-Mail: [email protected] 5 Department of Energy Engineering, BME, Budapest 1111, Hungary 6 Montavid Thermodynamic Research Group, Budapest 1112 , Hungary * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +39-097-120-5885; Fax: +39-097-120-5896. Received: 30 December 2013; in revised form: 27 January 2014 / Accepted: 7 March 2014 / Published: 24 March 2014 Abstract: We present the state of the art on the modern mathematical methods of exploiting the entropy principle in thermomechanics of continuous media. A survey of recent results and conceptual discussions of this topic in some well-known non-equilibrium theories (Classical irreversible thermodynamics CIT, Rational thermodynamics RT, Thermodynamics of irreversible processes TIP, Extended irreversible thermodynamics EIT, Rational Extended thermodynamics RET) is also summarized. Keywords: continuum thermodynamics; entropy principle; rational thermodynamics; classical irreversible thermodynamics; extended irreversible thermodynamics; rational extended thermodynamics; exploitation of second law PACS Classification: 03.50.-z, 05.70.Ln, 05.70.Ce Entropy 2014, 16 1757 1. -
Physical Origins of Anelasticity and Attenuation in Rock I
2.17 Properties of Rocks and Minerals – Physical Origins of Anelasticity and Attenuation in Rock I. Jackson, Australian National University, Canberra, ACT, Australia ª 2007 Elsevier B.V. All rights reserved. 2.17.1 Introduction 496 2.17.2 Theoretical Background 496 2.17.2.1 Phenomenological Description of Viscoelasticity 496 2.17.2.2 Intragranular Processes of Viscoelastic Relaxation 499 2.17.2.2.1 Stress-induced rearrangement of point defects 499 2.17.2.2.2 Stress-induced motion of dislocations 500 2.17.2.3 Intergranular Relaxation Processes 505 2.17.2.3.1 Effects of elastic and thermoelastic heterogeneity in polycrystals and composites 505 2.17.2.3.2 Grain-boundary sliding 506 2.17.2.4 Relaxation Mechanisms Associated with Phase Transformations 508 2.17.2.4.1 Stress-induced variation of the proportions of coexisting phases 508 2.17.2.4.2 Stress-induced migration of transformational twin boundaries 509 2.17.2.5 Anelastic Relaxation Associated with Stress-Induced Fluid Flow 509 2.17.3 Insights from Laboratory Studies of Geological Materials 512 2.17.3.1 Dislocation Relaxation 512 2.17.3.1.1 Linearity and recoverability 512 2.17.3.1.2 Laboratory measurements on single crystals and coarse-grained rocks 512 2.17.3.2 Stress-Induced Migration of Transformational Twin Boundaries in Ferroelastic Perovskites 513 2.17.3.3 Grain-Boundary Relaxation Processes 513 2.17.3.3.1 Grain-boundary migration in b.c.c. and f.c.c. Fe? 513 2.17.3.3.2 Grain-boundary sliding 514 2.17.3.4 Viscoelastic Relaxation in Cracked and Water-Saturated Crystalline Rocks -
An Ultrasonic Study on Anelasticity in Metals
AN ULTRASONIC STUDY ON ANELASTICITY IN METALS J. P. Fulton, S. Nath, and B. Wincheski Analytical Services and Materials, Inc. 107 Research Drive Hampton, VA 23666 M. Namkung Mail Stop 231 NASA, Langley Research Center Hampton, VA 23681 INTRODUCTION Ultrasonic waves are highly sensitive to microstructural variations in materials and have been used extensively to investigate anharmonic effects in various metals and alloys[1-3]. A major focus of these studies is on the higher order elastic constants and their relation to the microstructure of the material. Ultrasonic techniques have also proven quite useful for char acterizing the stress state of a material [4-6]. Recently, while using the magnetoacoustic (MAC) method to investigate the residual stress in various steel samples, a time dependent change in the results was observed. It became apparent that the measurements were exhibit ing anelastic effects due to some intrinsic properties of the samples. Anelasticity is a phenomena that can occur whenever there is a rapid change in the exter nal stress applied to a crystalline solid. The change in stress will cause the induced strain to adopt a new equilibrium position. If the changes in the resulting strain does not take place instantaneously, the material is said to exhibit anelastic behavior. Investigations into anelas tic relaxation in crystalline solids have been carried out for many years and provide impor tant information relating to the microstructure of the material [7-13]. The time dependence of our MAC test results led us to propose a new approach for studying the causes of anelasticity in metals. Typical studies on anelasticity use strain gauges to monitor the recovery process. -
The Mechanics of Ice
COLD REGIONS SCIENCE AND ENGINEERING Monograph ll-C2b THE MECHANICS OF ICE John W. Glen December 1975 GB 2401 CORPS OF ENGINEERS, U.S. ARMY .U58m COLD REGIONS RESEARCH AND ENGINEERING LABORATORY no.ll-C2b HANOVER, NEW HAMPSHIRE 1975 Approved for public release; distribution unlimited. 5 fl rolomis The findings in this report are not to be construed as an official Department of the Army position unless so designated by other authorized docume* s. 0 Unclassified BUREAU OF RECLAMATION pENVER UBRARY C/ 92099625 ^ Y REPORT DOCUMENTATION PAGE ...............Q ? n Q 9 f i ? 5 1. REPORT NUMBER 2. GOVT ACCESSION NO. 3. RECIPt_______________ - ..------------ Monograph II-C2b -> 5. TYPE OF REPORT ft PERIOD COVERED 4. TITLE (end Subtitle) j m MECHANICS OF ICE 6. PERFORMING ORG. REPORT NUMBER 8. CONTRACT OR GRANT NUMBER*» 7. AUTHORf» European Research Office r J.W. Glen ,r Contract DAJA37-68-C*0208 £ ■ '« • ' 1 "• - TO. PROGRAM ELEMENT, PROJECT, TASK 9. PERFORMING ORGANIZATION NAME AND ADDRESS AREA ft WORK UNIT NJUMBERS Dr. John W. Glen Department of Physics ^ DA Project 1T062112A130 University of Birmingham ( ^ Task 01 ____ Birmingham. England ____; '____ ; _______ — 11. CONTROLLING OFFICE NAME AND ADDRESS 12. REPORT DATE Office, Chief of Engineers ^ December 1975 u 13. n u m b er o f p a g e s ' Washington, D.C. 47 14. MONITORING AGENCY NAME ft ADDRESS*?/ different from Controlling Office) 15. SECURITY CLASS, (of thie report) UvS ^Army Cold Regions Research and Engineering Laboratory-^ Unclassified Hanover, New Hampshire 03755 15«. DECLASSIFICATION/ DOWNGRADING SCHEDULE 16. DISTRIBUTION STATEMENT (of thla Report) Approved for public release; distribution unlimited. -
The Anelasticity of the Mantle*
CORE Metadata, citation and similar papers at core.ac.uk ProvidedGeophys. by Caltech i. AuthorsR. astr. - Main Soc. (1967) 14, 135-164. The Anelasticity of the Mantle* Don L. Anderson Summary The attenuation of seismic waves provides the most direct data regarding the non-elastic properties of the Earth. Recent experimental results from body waves, surface waves and free oscillations provide estimates of the anelasticity in various regions of the Earth. Results to date show that the upper mantle is more attenuating than the lower mantle, the maximum attenuation is in the vicinity of the low-velocity zone, a rapid increase in attenuation occurs in the vicinity of the C-region of the mantle and com pressional waves are less attenuated than shear waves. A frequency dependence of Q has not yet been discovered. Most laboratory measurements of attenuation have been performed at ultrasonic frequencies on pure specimens of metals, glasses, plastics and ceramics. A general feature of laboratory measurements is an exponential increase of attenuation with temperature on which are superimposed peaks which can be attributed to dislocation or other defect phenomena. Measurements on natural rocks at atmospheric pressure can be attributed to the presence of cracks. The intrinsic attenuation of rocks as a function of temperature and pressure is not known. However, on other materials grain boundary phenomena dominate at high temperature. This can be attributed to increased grain boundary mobility at high temperatures. High pressure would be expected to decrease this mobility. If attenuation in the mantle is due to an activated process it is probably controlled by the diffusion rate of defects at grain boundaries. -
Anelasticity and Attenuation Part 1: Generalities Attenuation a Range Of
Anelasticity and Attenuation Part 1: Generalities SIO 227C Bernard Minster April 2004 1 2 Attenuation A range of rheologies . Energy is lost to heat . Elasticity . Not explained by theory of elasticity . Inelasticity . Many mechanisms, most of which operate at . Plasticity the microscopic level . Viscosity . “slight” departure from elastic behavior . Viscoelasticity . Rheology based on simple considerations of . Visco-plasticity near-equilibrium thermodynamics. Elasto-plasticity . As much as possible, stick to linear theory . Anelasticity 3 4 1 Elasticity Viscosity . Linear elasticity (Green) . Linear viscosity Stress Stress . Hooke’s law σ = Kε σ = κε˙ . Nonlinear elasticity . Nonlinear viscosity Strain . Example. Strain rate σ = F(ε) σ ∝ε˙1 / N Stress Stress . Fully reversible deformation: . For instance, for water ice,N=3 Loading and unloading paths . Perhaps for the mantle as well are the same . Large stress leads to low effective . Equilibrium reached instantly Strain viscosity Strain rate . Deformation nonrecoverable 5 6 Plasticity Inelasticity . Instantaneous plasticity Stress . Nonlinear, . Rigid-plastic nonrecoverable . Time-dependent Strain . (example: material Stress Stress failure) . Elasto-plasticity Strain Strain rate 7 8 2 Anelasticity postulates Some Comments 1. For every stress there is a unique . Anelasticity is just like elasticity, plus the equilibrium value of strain and vice time dependence postulate versa . There can be an elastic component of the deformation in addition to the time-dependent 2. The equilibrium response is achieved component only after the passage of sufficient . Recovery is also time dependent time . Linearity is taken in the mathematical sense: 3. The stress-strain relationship is linear σ(αε1 + βε2) = ασ(ε1) + βσ(ε2) 9 10 Comparison of Rheologies Thermodynamic Substance Unique equilibrium Instan- Linear . -
Boltzmann Equation 1
Contents 5 The Boltzmann Equation 1 5.1 References . 1 5.2 Equilibrium, Nonequilibrium and Local Equilibrium . 2 5.3 Boltzmann Transport Theory . 4 5.3.1 Derivation of the Boltzmann equation . 4 5.3.2 Collisionless Boltzmann equation . 5 5.3.3 Collisional invariants . 7 5.3.4 Scattering processes . 7 5.3.5 Detailed balance . 9 5.3.6 Kinematics and cross section . 10 5.3.7 H-theorem . 11 5.4 Weakly Inhomogeneous Gas . 13 5.5 Relaxation Time Approximation . 15 5.5.1 Approximation of collision integral . 15 5.5.2 Computation of the scattering time . 15 5.5.3 Thermal conductivity . 16 5.5.4 Viscosity . 18 5.5.5 Oscillating external force . 20 5.5.6 Quick and Dirty Treatment of Transport . 21 5.5.7 Thermal diffusivity, kinematic viscosity, and Prandtl number . 22 5.6 Diffusion and the Lorentz model . 23 i ii CONTENTS 5.6.1 Failure of the relaxation time approximation . 23 5.6.2 Modified Boltzmann equation and its solution . 24 5.7 Linearized Boltzmann Equation . 26 5.7.1 Linearizing the collision integral . 26 5.7.2 Linear algebraic properties of L^ ............................. 27 5.7.3 Steady state solution to the linearized Boltzmann equation . 28 5.7.4 Variational approach . 29 5.8 The Equations of Hydrodynamics . 32 5.9 Nonequilibrium Quantum Transport . 33 5.9.1 Boltzmann equation for quantum systems . 33 5.9.2 The Heat Equation . 37 5.9.3 Calculation of Transport Coefficients . 38 5.9.4 Onsager Relations . 39 5.10 Appendix : Boltzmann Equation and Collisional Invariants . -
Effects of Glass Transition and Structural Relaxation on Crystal
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 31 August 2020 doi:10.20944/preprints202008.0719.v1 Effects of Glass Transition and Structural Relaxation on Crystal Nucleation: Theoretical Description and Model Analysis J¨urnW. P. Schmelzer(1;∗), Timur V. Tropin(2), Vladimir M. Fokin(3), Alexander S. Abyzov(4), and Edgar D. Zanotto(3) (1) Institut f¨urPhysik der Universit¨atRostock, Albert-Einstein-Strasse 23-25, 18059 Rostock, Germany (2) Frank Laboratory of Neutron Physics, Joint Institute for Nuclear Research, ul. Joliot-Curie 6, 141980 Dubna, Russia (3) Vitreous Materials Laboratory, Department of Materials Engineering, Federal University of S~aoCarlos, UFSCar 13565-905, S~aoCarlos-SP, Brazil (4) National Science Center Kharkov Institute of Physics and Technology, 61108 Kharkov, Ukraine Submitted to Entropy, August 27, 2020 Keywords: Nucleation, crystal growth, general theory of phase transitions, glasses, glass transition PACS numbers: 64.60.Bd General theory of phase transitions 64.60.Q- Nucleation 81.10.Aj Theory and models of crystal growth 64.70.kj Glasses 64.70.Q- Theory and modeling of the glass transition; 65.40.gd Entropy * Corresponding author: Dr. J¨urnW. P. Schmelzer Phone: +49 381 498 6889, Fax: +49 381 498 6882 Email: [email protected] 1 © 2020 by the author(s). Distributed under a Creative Commons CC BY license. Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 31 August 2020 doi:10.20944/preprints202008.0719.v1 Abstract In the application of classical nucleation theory (CNT) and all other theoretical models of crystallization of liquids and glasses it is always assumed that nucleation proceeds only after the supercooled liquid or the glass have completed structural relaxation processes towards the metastable equilibrium state. -
Anelastic Behavior of Small Dimensioned Aluminum
metals Article Anelastic Behavior of Small Dimensioned Aluminum Enrico Gianfranco Campari 1 , Stefano Amadori 1, Ennio Bonetti 1, Raffaele Berti 1 and Roberto Montanari 2,* 1 Department of Physics and Astronomy, Bologna University, Viale Berti Pichat 6/2, I-40127 Bologna, Italy; [email protected] (E.G.C.); [email protected] (S.A.); [email protected] (E.B.); raff[email protected] (R.B.) 2 Department of Industrial Engineering, Rome University “Tor Vergata”, Via del Politecnico, 1-00133 Roma, Italy * Correspondence: [email protected]; Tel.: +39-0672597182 Received: 18 March 2019; Accepted: 9 May 2019; Published: 11 May 2019 Abstract: In the present research, results are presented regarding the anelasticity of 99.999% pure aluminum thin films, either deposited on silica substrates or as free-standing sheets obtained by cold rolling. Mechanical Spectroscopy (MS) tests, namely measurements of dynamic modulus and damping vs. temperature, were performed using a vibrating reed analyzer under vacuum. The damping vs. temperature curves of deposited films exhibit two peaks which tend to merge into a single peak as the specimen thickness increases above 0.2 µm. The thermally activated anelastic relaxation processes observed on free-standing films are strongly dependent on film thickness, and below a critical value of about 20 µm two anelastic relaxation peaks can be observed; both their activation energy and relaxation strength are affected by film thickness. These results, together with those observed on bulk specimens, are indicative of specific dislocation and grain boundary dynamics, constrained by the critical values of the ratio of film thickness to grain size. -
Relaxation Processes in Glass and Polymers Lecture 2
MITT Ulrich Fotheringham: Relaxation Processes in Glass and Polymers, Lecture 2 Relaxation Processes in Glass and Polymers Lecture 2: Phenomenology of viscoelasticity & glass transition Dr. Ulrich Fotheringham Research and Technology Development SCHOTT AG MITT Ulrich Fotheringham: Relaxation Processes in Glass and Polymers, Lecture 2 In the following, examples from the progress of relaxation research in glass will be shown in order to illustrate what relaxation is about. It is neither a comprehensive picture of the history of relaxation research nor a balanced assessment of the contributions of all individuals involved. To illustrate glass properties, references will be made to different companies. These references have been picked arbitrarily for educational reasons, copyright issues etc., not to provide a balanced view of the achievements of different companies. Despite its careful preparation, the manuscript may contain errors. Dr. Ulrich Fotheringham MITT Ulrich Fotheringham: Relaxation Processes in Glass and Polymers, Lecture 2 Observation 1a (before 1912!): Glass, if heated to high temperatures and cooled down rapidly, shows birefringence like Calcite: (calcite birefringence picture from Carl Zeiss AG, information on polarisation microscopy) In contrast to the permanent birefrigence of Calcite, the birefringence in glass is stress-induced. Otto Schott found that it will relax if the sample is held for 24h at a minimum temperature which depends on the composition: crown flint (historic example: (historic example: window glass) lead