Circular Birefringence in Crystal Optics
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Analysis of Deformation
Chapter 7: Constitutive Equations Definition: In the previous chapters we’ve learned about the definition and meaning of the concepts of stress and strain. One is an objective measure of load and the other is an objective measure of deformation. In fluids, one talks about the rate-of-deformation as opposed to simply strain (i.e. deformation alone or by itself). We all know though that deformation is caused by loads (i.e. there must be a relationship between stress and strain). A relationship between stress and strain (or rate-of-deformation tensor) is simply called a “constitutive equation”. Below we will describe how such equations are formulated. Constitutive equations between stress and strain are normally written based on phenomenological (i.e. experimental) observations and some assumption(s) on the physical behavior or response of a material to loading. Such equations can and should always be tested against experimental observations. Although there is almost an infinite amount of different materials, leading one to conclude that there is an equivalently infinite amount of constitutive equations or relations that describe such materials behavior, it turns out that there are really three major equations that cover the behavior of a wide range of materials of applied interest. One equation describes stress and small strain in solids and called “Hooke’s law”. The other two equations describe the behavior of fluidic materials. Hookean Elastic Solid: We will start explaining these equations by considering Hooke’s law first. Hooke’s law simply states that the stress tensor is assumed to be linearly related to the strain tensor. -
(Physics), June 2003, Pp 18-19
ICO topical meeting on Polarization Optics, Joensuu. eds: Asher A. Friesem and Jari Turunen, Published by University of Joensuu (Physics), June 2003, pp 18-19 The singularities of crystal optics Michael Berry and Mark Dennis H H Wills Physics Laboratory, Tyndall Avenue, Bristol BS8 1TL, United Kingdom http://www.phy.bris.ac.uk/staff/berry_mv.html This is a summary of our recent paper [1], where we reconstruct the classical theory of crystal optics [2] in a way that emphasises and extends recent ideas of singular optics [3, 4]. We concentrate on the general case where the crystal is chiral, i.e. optically active (gy- rotropic) and absorbing (dichroic) as well as biaxially anisotropic, and describe the proper- ties of the crystal as a function of propagation direction s. The refractive indices and po- larizations of plane waves are eigenvalues and eigenfunctions of the 2x2 part of the recip- rocal dielectric tensor h perpendicular to s. For transparent anisotropic crystals, h is real symmetric; addition of chirality makes h complex hermitian; addition of dichroism makes h complex nonhermitian. These different possibilities greatly influence the refractive indi- ces and eigenpolarizations. Using a new formalism involving projection from the sphere of directions s to the stereo- graphic plane R=X,Y, and associated complex variables Z=X+iY, we obtain convenient ex- plicit formulas for the two refractive indices and polarizations. Particular use is made of a representation of the polarization states as the complex ratios of their vector components. This enables three types of polarization singularity to classified and explored. First are sin- gular axes, which are degeneracies where the two refractive indices are equal. -
Experience with Ray-Tracing Simulations at the European Synchrotron Radiation Facility
Experience with ray-tracing simulations at the European Synchrotron Radiation Facility Manuel Sánchez del Río European Synchrotron Radiation Facility, BP 220, F-38043 Grenoble Cedex 9 (France) (Presented on 18 October 1995) The ESRF is the first operational third-generation synchrotron radiation hard-x-ray source. Since the beginning of its construction (1988), the ray-tracing technique proved to be an essential computer tool for the beamline optics design. The optical systems of most beamlines have been simulated by ray tracing in order to optimize the optics, fully understand their properties, and check if operation performances were as expected. In this paper, a short compilation of the experience with ray tracing and optics simulation codes at the ESRF, as well as some other in-house developments, is presented. © 1996 American Institute of Physics. I. INTRODUCTION position), the energy resolution of the monochromatized beam, and the flux or power transmitted by the beamline. The construction of the ESRF synchrotron radiation source started in 1988 as a joint project of 12 European countries. The facility is designed and optimized to supply high II. MIRROR OPTICS brilliance x-rays from insertion devices. It consists of a 200-MeV electron LINAC, a 6-GeV fast cycling booster Mirrors are used essentially to focus or collimate the x-ray synchrotron and a 6-GeV low emittance storage ring. At beam. They can also be used as x-ray filters to avoid high present, 18 beamlines constructed by the ESRF and 4 built heat load on other devices (monochromators) or as harmonic by the Collaborating Research Groups (CRG) are operational rejecters. -
Modelling the Optics of High Resolution Liquid Crystal Devices by the Finite Differences in the Frequency Domain Method
Modelling the optics of high resolution liquid crystal devices by the finite differences in the frequency domain method Mengyang Yang, Sally E. Day and F. Aníbal Fernández Department of Electronic and Electrical Engineering University College London, London WC1E 7JE, UK [email protected] Abstract—A procedure combining accurate liquid crystal and electromagnetic modelling is developed for the analysis of wave II. LIQUID CRYSTAL AND ELECTROMAGNETIC WAVE propagation through liquid crystal devices. This is required to PROPAGATION MODELLING study the optics of high resolution liquid crystal cells or cells containing very small features, where diffraction effects occur. It A. Liquid crystal modelling is also necessary for the study of optical waveguiding devices The liquid crystal modelling used in this work consists of a using liquid crystal as variable permittivity substrates. An variational approach to the Landau-de Gennes theory accurate finite element modelling program is used to find the implemented with the formalism of Qian and Sheng [1], [5]. permittivity tensor distribution, which is then used to find the response of the device to an excitation electromagnetic field by This is a continuum theory in which the liquid crystal means of a finite difference in the frequency domain (FDFD) orientation is defined by the order tensor Q that not only approach. describes the local orientation but also takes into account order variations. This is adequate for the accurate modelling of liquid Keywords— Liquid crystal modelling; Finite differences crystal structures containing defects or other regions of order method; Wave propagation in anisotropic inhomogeneous media; parameter variation. The permittivity distribution is then found Liquid crystal optics as εε=+Δ⊥ Inn ε where nˆ is the liquid crystal director, ε ⊥ is the relative permittivity calculated in the direction I. -
Crystal Optics Homogeneous, Anisotropic Media
Lecture 3: Crystal Optics Homogeneous, Anisotropic Media Introduction Outline material equations for homogeneous anisotropic media ~ ~ 1 Homogeneous, Anisotropic Media D = E B~ = µH~ 2 Crystals tensors of rank 2, written as 3 by 3 matrices 3 Plane Waves in Anisotropic Media : dielectric tensor 4 Wave Propagation in Uniaxial Media µ: magnetic permeability tensor examples: 5 Reflection and Transmission at Interfaces crystals, liquid crystals external electric, magnetic fields acting on isotropic materials (glass, fluids, gas) anisotropic mechanical forces acting on isotropic materials Christoph U. Keller, Utrecht University, [email protected] Lecture 3: Crystal Optics 1 Christoph U. Keller, Utrecht University, [email protected] Lecture 3: Crystal Optics 2 Properties of Dielectric Tensor Uniaxial Materials Maxwell equations imply symmetric dielectric tensor isotropic materials: n = n = n 0 1 x y z 11 12 13 for any coordinate system T = = @ 12 22 23 A anisotropic materials: 13 23 33 nx 6= ny 6= nz symmetric tensor of rank 2 ) coordinate system exists where uniaxial materials: nx = ny 6= nz tensor is diagonal ordinary index of refraction: orthogonal axes of this coordinate system: principal axes no = nx = ny elements of diagonal tensor: principal dielectric constants extraordinary index of refraction: n = n 3 principal indices of refraction in coordinate system spanned by e z principal axes rotation of coordinate system 0 2 1 around z does not change nx 0 0 ~ 2 ~ anything D = @ 0 ny 0 A E 2 0 0 nz most materials used in polarimetry are (almost) uniaxial x, y, z because principal axes form Cartesian coordinate system Christoph U. -
Soft Matter Theory
Soft Matter Theory K. Kroy Leipzig, 2016∗ Contents I Interacting Many-Body Systems 3 1 Pair interactions and pair correlations 4 2 Packing structure and material behavior 9 3 Ornstein{Zernike integral equation 14 4 Density functional theory 17 5 Applications: mesophase transitions, freezing, screening 23 II Soft-Matter Paradigms 31 6 Principles of hydrodynamics 32 7 Rheology of simple and complex fluids 41 8 Flexible polymers and renormalization 51 9 Semiflexible polymers and elastic singularities 63 ∗The script is not meant to be a substitute for reading proper textbooks nor for dissemina- tion. (See the notes for the introductory course for background information.) Comments and suggestions are highly welcome. 1 \Soft Matter" is one of the fastest growing fields in physics, as illustrated by the APS Council's official endorsement of the new Soft Matter Topical Group (GSOFT) in 2014 with more than four times the quorum, and by the fact that Isaac Newton's chair is now held by a soft matter theorist. It crosses traditional departmental walls and now provides a common focus and unifying perspective for many activities that formerly would have been separated into a variety of disciplines, such as mathematics, physics, biophysics, chemistry, chemical en- gineering, materials science. It brings together scientists, mathematicians and engineers to study materials such as colloids, micelles, biological, and granular matter, but is much less tied to certain materials, technologies, or applications than to the generic and unifying organizing principles governing them. In the widest sense, the field of soft matter comprises all applications of the principles of statistical mechanics to condensed matter that is not dominated by quantum effects. -
Bent Crystal X-Ray Optics for the Diagnosis and Applications of Laser-Produced Plasmas
Bent crystal X-ray optics for the diagnosis and applications of laser-produced plasmas D issertation zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) seit 1558 vorgelegt dem Rat der Physikalisch-Astronomischen Fakultät der Friedrich- Schiller-U niversit ät von Dipl.-Phys. Robert Lötzsch geboren am 18.08.1980 in Jena Gutachter: 1. Prof. Dr. Eckhart Förster Institut für Optik und Quantenelektronik Friedrich-Schiller-Universität Jena 2. Prof. Dr. Helmut Zacharias Physikalisches Institut Westfälische Wilhelms-Universität Münster 3. Prof. Dr. Georg Pretzier Institut für Laser- und Plasmaphysik Heinrich-Heine-Universität Düsseldorf Tag der Disputation: 8.11.2012 Contents Motivation 3 1. Introduction 5 1.1. X-ray optics with toroidally bent crystals...................................................... 5 1.2. Interaction of short pulse lasers with so lid s................................................... 12 1.2.1. Target Normal Sheath Acceleration................................................... 14 1.2.2. Generation of ultrashort X-ray bursts................................................. 16 2. Laterally varying reflection properties of bent crystals 19 2.1. Measurement of laterally varying Bragg angles............................................. 21 2.1.1. Measurement sch em e............................................................................ 21 2.1.2. Analysis of the accuracy of the measurement system....................... 24 2.1.3. Results..................................................................................................... -
Introduction to FINITE STRAIN THEORY for CONTINUUM ELASTO
RED BOX RULES ARE FOR PROOF STAGE ONLY. DELETE BEFORE FINAL PRINTING. WILEY SERIES IN COMPUTATIONAL MECHANICS HASHIGUCHI WILEY SERIES IN COMPUTATIONAL MECHANICS YAMAKAWA Introduction to for to Introduction FINITE STRAIN THEORY for CONTINUUM ELASTO-PLASTICITY CONTINUUM ELASTO-PLASTICITY KOICHI HASHIGUCHI, Kyushu University, Japan Introduction to YUKI YAMAKAWA, Tohoku University, Japan Elasto-plastic deformation is frequently observed in machines and structures, hence its prediction is an important consideration at the design stage. Elasto-plasticity theories will FINITE STRAIN THEORY be increasingly required in the future in response to the development of new and improved industrial technologies. Although various books for elasto-plasticity have been published to date, they focus on infi nitesimal elasto-plastic deformation theory. However, modern computational THEORY STRAIN FINITE for CONTINUUM techniques employ an advanced approach to solve problems in this fi eld and much research has taken place in recent years into fi nite strain elasto-plasticity. This book describes this approach and aims to improve mechanical design techniques in mechanical, civil, structural and aeronautical engineering through the accurate analysis of fi nite elasto-plastic deformation. ELASTO-PLASTICITY Introduction to Finite Strain Theory for Continuum Elasto-Plasticity presents introductory explanations that can be easily understood by readers with only a basic knowledge of elasto-plasticity, showing physical backgrounds of concepts in detail and derivation processes -
2 Review of Stress, Linear Strain and Elastic Stress- Strain Relations
2 Review of Stress, Linear Strain and Elastic Stress- Strain Relations 2.1 Introduction In metal forming and machining processes, the work piece is subjected to external forces in order to achieve a certain desired shape. Under the action of these forces, the work piece undergoes displacements and deformation and develops internal forces. A measure of deformation is defined as strain. The intensity of internal forces is called as stress. The displacements, strains and stresses in a deformable body are interlinked. Additionally, they all depend on the geometry and material of the work piece, external forces and supports. Therefore, to estimate the external forces required for achieving the desired shape, one needs to determine the displacements, strains and stresses in the work piece. This involves solving the following set of governing equations : (i) strain-displacement relations, (ii) stress- strain relations and (iii) equations of motion. In this chapter, we develop the governing equations for the case of small deformation of linearly elastic materials. While developing these equations, we disregard the molecular structure of the material and assume the body to be a continuum. This enables us to define the displacements, strains and stresses at every point of the body. We begin our discussion on governing equations with the concept of stress at a point. Then, we carry out the analysis of stress at a point to develop the ideas of stress invariants, principal stresses, maximum shear stress, octahedral stresses and the hydrostatic and deviatoric parts of stress. These ideas will be used in the next chapter to develop the theory of plasticity. -
Multiband Homogenization of Metamaterials in Real-Space
Submitted preprint. 1 Multiband Homogenization of Metamaterials in Real-Space: 2 Higher-Order Nonlocal Models and Scattering at External Surfaces 1, ∗ 2, y 1, 3, 4, z 3 Kshiteej Deshmukh, Timothy Breitzman, and Kaushik Dayal 1 4 Department of Civil and Environmental Engineering, Carnegie Mellon University 2 5 Air Force Research Laboratory 3 6 Center for Nonlinear Analysis, Department of Mathematical Sciences, Carnegie Mellon University 4 7 Department of Materials Science and Engineering, Carnegie Mellon University 8 (Dated: March 3, 2021) Dynamic homogenization of periodic metamaterials typically provides the dispersion relations as the end-point. This work goes further to invert the dispersion relation and develop the approximate macroscopic homogenized equation with constant coefficients posed in space and time. The homoge- nized equation can be used to solve initial-boundary-value problems posed on arbitrary non-periodic macroscale geometries with macroscopic heterogeneity, such as bodies composed of several different metamaterials or with external boundaries. First, considering a single band, the dispersion relation is approximated in terms of rational functions, enabling the inversion to real space. The homogenized equation contains strain gradients as well as spatial derivatives of the inertial term. Considering a boundary between a metamaterial and a homogeneous material, the higher-order space derivatives lead to additional continuity conditions. The higher-order homogenized equation and the continuity conditions provide predictions of wave scattering in 1-d and 2-d that match well with the exact fine-scale solution; compared to alternative approaches, they provide a single equation that is valid over a broad range of frequencies, are easy to apply, and are much faster to compute. -
Stress, Cauchy's Equation and the Navier-Stokes Equations
Chapter 3 Stress, Cauchy’s equation and the Navier-Stokes equations 3.1 The concept of traction/stress • Consider the volume of fluid shown in the left half of Fig. 3.1. The volume of fluid is subjected to distributed external forces (e.g. shear stresses, pressures etc.). Let ∆F be the resultant force acting on a small surface element ∆S with outer unit normal n, then the traction vector t is defined as: ∆F t = lim (3.1) ∆S→0 ∆S ∆F n ∆F ∆ S ∆ S n Figure 3.1: Sketch illustrating traction and stress. • The right half of Fig. 3.1 illustrates the concept of an (internal) stress t which represents the traction exerted by one half of the fluid volume onto the other half across a ficticious cut (along a plane with outer unit normal n) through the volume. 3.2 The stress tensor • The stress vector t depends on the spatial position in the body and on the orientation of the plane (characterised by its outer unit normal n) along which the volume of fluid is cut: ti = τij nj , (3.2) where τij = τji is the symmetric stress tensor. • On an infinitesimal block of fluid whose faces are parallel to the axes, the component τij of the stress tensor represents the traction component in the positive i-direction on the face xj = const. whose outer normal points in the positive j-direction (see Fig. 3.2). 6 MATH35001 Viscous Fluid Flow: Stress, Cauchy’s equation and the Navier-Stokes equations 7 x3 x3 τ33 τ22 τ τ11 12 τ21 τ τ 13 23 τ τ 32τ 31 τ 31 32 τ τ τ 23 13 τ21 τ τ τ 11 12 22 33 x1 x2 x1 x2 Figure 3.2: Sketch illustrating the components of the stress tensor. -
Geophysical Journal International Provided by RERO DOC Digital Library Geophys
View metadata, citation and similar papers at core.ac.uk brought to you by CORE Geophysical Journal International provided by RERO DOC Digital Library Geophys. J. Int. (2010) 180, 225–237 doi: 10.1111/j.1365-246X.2009.04415.x A combination of the Hashin-Shtrikman bounds aimed at modelling electrical conductivity and permittivity of variably saturated porous media A. Brovelli1 and G. Cassiani2 1Laboratoire de technologie ecologique,´ Institut d’ingenierie´ l’environnement, Batimentˆ GR, Station No. 2, Ecole Polytechnique Fed´ erale´ de Lausanne, CH-1015 Lausanne, Switzerland. E-mail: alessandro.brovelli@epfl.ch 2Dipartimento di Geoscienze, Universita` di Padova, Via Giotto 1, 35127 Padova, Italy Accepted 2009 October 9. Received 2009 October 8; in original form 2009 March 4 SUMMARY In this paper, we propose a novel theoretical model for the dielectric response of variably satu- rated porous media. The model is first constructed for fully saturated systems as a combination of the well-established Hashin and Shtrikman bounds and Archie’s first law. One of the key advantages of the new constitutive model is that it explains both electrical conductivity—when surface conductivity is small and negligible—and permittivity using the same parametrization. The model for partially saturated media is derived as an extension of the fully saturated model, where the permittivity of the pore space is obtained as a combination of the permittivity of the aqueous and non-aqueous phases. Model parameters have a well-defined physical meaning, can be independently measured, and can be used to characterize the pore-scale geometrical features of the medium. Both the fully and the partially saturated models are successfully tested against measured values of relative permittivity for a wide range of porous media and saturat- ing fluids.