Chapter 3 X-Ray Diffraction • Bragg's Law • Laue's Condition
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Reciprocal Lattice
Appendix A THE RECIPROCAL LATTICE When the translations of a primitive space lattice are denoted by a, b and c, the vector p to any lattice point is given p = ua + vb + we. The definition of the reciprocal lattice is that the translations a*, b* and c*, which define the reciprocal lattice fulfil the following relationships: (A. I) a*.b = b*.c = c*.a = a.b* = b.c* =c. a*= 0 (A.2) It can then be easily shown that: (1) Ic* I = 1/c-spacing of primitive lattice and similarly forb* and a*. (2) a*= (b 1\ c)ja.(b 1\ c) b* = (c 1\ a)jb.(c 1\ a) c* =(a 1\ b)/c-(a 1\ b) These last three relations are often used as a definition of the reciprocal lattice. Two properties of the reciprocal lattice are particularly important: (a) The vector g* defined by g* = ha* + kb* + lc* (where h, k and I are integers to the point hkl in the reciprocal lattice) is normal to the plane of Miller indices (hkl) in the primary lattice. (b) The magnitude Ig* I of this vector is the reciprocal of the spacing of (hkl) in the primary lattice. AI ALLOWED REFLECTIONS The kinematical structure factor for reflections is given by Fhkl = I;J;exp[- 2ni(hu; + kv; + lw)] (A.3) where ui' v; and W; are the coordinates of the atoms and hkl the Miller indices of the reflection g. If there is only one atom at 0, 0, 0 in the unit cell then the structure factor will be independent of hkl since for all values of h, k and I we have Fhkl =f. -
Relativistic Dynamics
Chapter 4 Relativistic dynamics We have seen in the previous lectures that our relativity postulates suggest that the most efficient (lazy but smart) approach to relativistic physics is in terms of 4-vectors, and that velocities never exceed c in magnitude. In this chapter we will see how this 4-vector approach works for dynamics, i.e., for the interplay between motion and forces. A particle subject to forces will undergo non-inertial motion. According to Newton, there is a simple (3-vector) relation between force and acceleration, f~ = m~a; (4.0.1) where acceleration is the second time derivative of position, d~v d2~x ~a = = : (4.0.2) dt dt2 There is just one problem with these relations | they are wrong! Newtonian dynamics is a good approximation when velocities are very small compared to c, but outside of this regime the relation (4.0.1) is simply incorrect. In particular, these relations are inconsistent with our relativity postu- lates. To see this, it is sufficient to note that Newton's equations (4.0.1) and (4.0.2) predict that a particle subject to a constant force (and initially at rest) will acquire a velocity which can become arbitrarily large, Z t ~ d~v 0 f ~v(t) = 0 dt = t ! 1 as t ! 1 . (4.0.3) 0 dt m This flatly contradicts the prediction of special relativity (and causality) that no signal can propagate faster than c. Our task is to understand how to formulate the dynamics of non-inertial particles in a manner which is consistent with our relativity postulates (and then verify that it matches observation, including in the non-relativistic regime). -
The 4 Reciprocal Lattice
4 The Reciprocal Lattice by Andr~ Authier This electronic edition may be freely copied and redistributed for educational or research purposes only. It may not be sold for profit nor incorporated in any product sold for profit without the express pernfission of The Executive Secretary, International Union of Crystallography, 2 Abbey Square, Chester CIII 211[;, [;K Copyright in this electronic ectition (<.)2001 International l.Jnion of Crystallography Published for the International Union of Crystallography by University College Cardiff Press Cardiff, Wales © 1981 by the International Union of Crystallography. All rights reserved. Published by the University College Cardiff Press for the International Union of Crystallography with the financial assistance of Unesco Contract No. SC/RP 250.271 This pamphlet is one of a series prepared by the Commission on Crystallographic Teaching of the International Union of Crystallography, under the General Editorship of Professor C. A. Taylor. Copies of this pamphlet and other pamphlets in the series may be ordered direct from the University College Cardiff Press, P.O. Box 78, Cardiff CF1 1XL, U.K. ISBN 0 906449 08 I Printed in Wales by University College, Cardiff. Series Preface The long term aim of the Commission on Crystallographic Teaching in establishing this pamphlet programme is to produce a large collection of short statements each dealing with a specific topic at a specific level. The emphasis is on a particular teaching approach and there may well, in time, be pamphlets giving alternative teaching approaches to the same topic. It is not the function of the Commission to decide on the 'best' approach but to make all available so that teachers can make their own selection. -
Appendix D: the Wave Vector
General Appendix D-1 2/13/2016 Appendix D: The Wave Vector In this appendix we briefly address the concept of the wave vector and its relationship to traveling waves in 2- and 3-dimensional space, but first let us start with a review of 1- dimensional traveling waves. 1-dimensional traveling wave review A real-valued, scalar, uniform, harmonic wave with angular frequency and wavelength λ traveling through a lossless, 1-dimensional medium may be represented by the real part of 1 ω the complex function ψ (xt , ): ψψ(x , t )= (0,0) exp(ikx− i ω t ) (D-1) where the complex phasor ψ (0,0) determines the wave’s overall amplitude as well as its phase φ0 at the origin (xt , )= (0,0). The harmonic function’s wave number k is determined by the wavelength λ: k = ± 2πλ (D-2) The sign of k determines the wave’s direction of propagation: k > 0 for a wave traveling to the right (increasing x). The wave’s instantaneous phase φ(,)xt at any position and time is φφ(,)x t=+−0 ( kx ω t ) (D-3) The wave number k is thus the spatial analog of angular frequency : with units of radians/distance, it equals the rate of change of the wave’s phase with position (with time t ω held constant), i.e. ∂∂φφ k =; ω = − (D-4) ∂∂xt (note the minus sign in the differential expression for ). If a point, originally at (x= xt0 , = 0), moves with the wave at velocity vkφ = ω , then the wave’s phase at that point ω will remain constant: φ(x0+ vtφφ ,) t =++ φ0 kx ( 0 vt ) −=+ ωφ t00 kx The velocity vφ is called the wave’s phase velocity. -
EMT UNIT 1 (Laws of Reflection and Refraction, Total Internal Reflection).Pdf
Electromagnetic Theory II (EMT II); Online Unit 1. REFLECTION AND TRANSMISSION AT OBLIQUE INCIDENCE (Laws of Reflection and Refraction and Total Internal Reflection) (Introduction to Electrodynamics Chap 9) Instructor: Shah Haidar Khan University of Peshawar. Suppose an incident wave makes an angle θI with the normal to the xy-plane at z=0 (in medium 1) as shown in Figure 1. Suppose the wave splits into parts partially reflecting back in medium 1 and partially transmitting into medium 2 making angles θR and θT, respectively, with the normal. Figure 1. To understand the phenomenon at the boundary at z=0, we should apply the appropriate boundary conditions as discussed in the earlier lectures. Let us first write the equations of the waves in terms of electric and magnetic fields depending upon the wave vector κ and the frequency ω. MEDIUM 1: Where EI and BI is the instantaneous magnitudes of the electric and magnetic vector, respectively, of the incident wave. Other symbols have their usual meanings. For the reflected wave, Similarly, MEDIUM 2: Where ET and BT are the electric and magnetic instantaneous vectors of the transmitted part in medium 2. BOUNDARY CONDITIONS (at z=0) As the free charge on the surface is zero, the perpendicular component of the displacement vector is continuous across the surface. (DIꓕ + DRꓕ ) (In Medium 1) = DTꓕ (In Medium 2) Where Ds represent the perpendicular components of the displacement vector in both the media. Converting D to E, we get, ε1 EIꓕ + ε1 ERꓕ = ε2 ETꓕ ε1 ꓕ +ε1 ꓕ= ε2 ꓕ Since the equation is valid for all x and y at z=0, and the coefficients of the exponentials are constants, only the exponentials will determine any change that is occurring. -
Structure Factors Again
Structure factors again • Remember 1D, structure factor for order h 1 –Fh = |Fh|exp[iαh] = I0 ρ(x)exp[2πihx]dx – Where x is fractional position along “unit cell” distance (repeating distance, origin arbitrary) • As if scattering was coming from a single “center of gravity” scattering point • Presence of “h” in equation means that structure factors of different orders have different phases • Note that exp[2πihx]dx looks (and behaves) like a frequency, but it’s not (dx has to do with unit cell, and the sum gives the phase Back and Forth • Fourier sez – For any function f(x), there is a “transform” of it which is –F(h) = Ûf(x)exp(2pi(hx))dx – Where h is reciprocal of x (1/x) – Structure factors look like that • And it works backward –f(x) = ÛF(h)exp(-2pi(hx))dh – Or, if h comes only in discrete points –f(x) = SF(h)exp(-2pi(hx)) Structure factors, cont'd • Structure factors are a "Fourier transform" - a sum of components • Fourier transforms are reversible – From summing distribution of ρ(x), get hth order of diffraction – From summing hth orders of diffraction, get back ρ(x) = Σ Fh exp[-2πihx] Two dimensional scattering • In Frauenhofer diffraction (1D), we considered scattering from points, along the line • In 2D diffraction, scattering would occur from lines. • Numbering of the lines by where they cut the edges of a unit cell • Atom density in various lines can differ • Reflections now from planes Extension to 3D – Planes defined by extension from 2D case – Unit cells differ • Depends on arrangement of materials in 3D lattice • = "Space -
System Design and Verification of the Precession Electron Diffraction Technique
NORTHWESTERN UNIVERSITY System Design and Verification of the Precession Electron Diffraction Technique A DISSERTATION SUBMITTED TO THE GRADUATE SCHOOL IN PARTIAL FULFILLMENT OF THE REQUIREMENTS for the degree DOCTOR OF PHILOSOPHY Field of Materials Science and Engineering By Christopher Su-Yan Own EVANSTON, ILLINOIS First published on the WWW 01, August 2005 Build 05.12.07. PDF available for download at: http://www.numis.northwestern.edu/Research/Current/precession.shtml c Copyright by Christopher Su-Yan Own 2005 All Rights Reserved ii ABSTRACT System Design and Verification of the Precession Electron Diffraction Technique Christopher Su-Yan Own Bulk structural crystallography is generally a two-part process wherein a rough starting structure model is first derived, then later refined to give an accurate model of the structure. The critical step is the deter- mination of the initial model. As materials problems decrease in length scale, the electron microscope has proven to be a versatile and effective tool for studying many problems. However, study of complex bulk structures by electron diffraction has been hindered by the problem of dynamical diffraction. This phenomenon makes bulk electron diffraction very sensitive to specimen thickness, and expensive equip- ment such as aberration-corrected scanning transmission microscopes or elaborate methodology such as high resolution imaging combined with diffraction and simulation are often required to generate good starting structures. The precession electron diffraction technique (PED), which has the ability to significantly reduce dynamical effects in diffraction patterns, has shown promise as being a “philosopher’s stone” for bulk electron diffraction. However, a comprehensive understanding of its abilities and limitations is necessary before it can be put into widespread use as a standalone technique. -
Instantaneous Local Wave Vector Estimation from Multi-Spacecraft Measurements Using Few Spatial Points T
Instantaneous local wave vector estimation from multi-spacecraft measurements using few spatial points T. D. Carozzi, A. M. Buckley, M. P. Gough To cite this version: T. D. Carozzi, A. M. Buckley, M. P. Gough. Instantaneous local wave vector estimation from multi- spacecraft measurements using few spatial points. Annales Geophysicae, European Geosciences Union, 2004, 22 (7), pp.2633-2641. hal-00317540 HAL Id: hal-00317540 https://hal.archives-ouvertes.fr/hal-00317540 Submitted on 14 Jul 2004 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Annales Geophysicae (2004) 22: 2633–2641 SRef-ID: 1432-0576/ag/2004-22-2633 Annales © European Geosciences Union 2004 Geophysicae Instantaneous local wave vector estimation from multi-spacecraft measurements using few spatial points T. D. Carozzi, A. M. Buckley, and M. P. Gough Space Science Centre, University of Sussex, Brighton, England Received: 30 September 2003 – Revised: 14 March 2004 – Accepted: 14 April 2004 – Published: 14 July 2004 Part of Special Issue “Spatio-temporal analysis and multipoint measurements in space” Abstract. We introduce a technique to determine instan- damental assumptions, namely stationarity and homogene- taneous local properties of waves based on discrete-time ity. -
Chapter 2 X-Ray Diffraction and Reciprocal Lattice
Chapter 2 X-ray diffraction and reciprocal lattice I. Waves 1. A plane wave is described as Ψ(x,t) = A ei(k⋅x-ωt) A is the amplitude, k is the wave vector, and ω=2πf is the angular frequency. 2. The wave is traveling along the k direction with a velocity c given by ω=c|k|. Wavelength along the traveling direction is given by |k|=2π/λ. 3. When a wave interacts with the crystal, the plane wave will be scattered by the atoms in a crystal and each atom will act like a point source (Huygens’ principle). 4. This formulation can be applied to any waves, like electromagnetic waves and crystal vibration waves; this also includes particles like electrons, photons, and neutrons. A particular case is X-ray. For this reason, what we learn in X-ray diffraction can be applied in a similar manner to other cases. II. X-ray diffraction in real space – Bragg’s Law 1. A crystal structure has lattice and a basis. X-ray diffraction is a convolution of two: diffraction by the lattice points and diffraction by the basis. We will consider diffraction by the lattice points first. The basis serves as a modification to the fact that the lattice point is not a perfect point source (because of the basis). 2. If each lattice point acts like a coherent point source, each lattice plane will act like a mirror. θ θ θ d d sin θ (hkl) -1- 2. The diffraction is elastic. In other words, the X-rays have the same frequency (hence wavelength and |k|) before and after the reflection. -
Lecture Notes
Solid State Physics PHYS 40352 by Mike Godfrey Spring 2012 Last changed on May 22, 2017 ii Contents Preface v 1 Crystal structure 1 1.1 Lattice and basis . .1 1.1.1 Unit cells . .2 1.1.2 Crystal symmetry . .3 1.1.3 Two-dimensional lattices . .4 1.1.4 Three-dimensional lattices . .7 1.1.5 Some cubic crystal structures ................................ 10 1.2 X-ray crystallography . 11 1.2.1 Diffraction by a crystal . 11 1.2.2 The reciprocal lattice . 12 1.2.3 Reciprocal lattice vectors and lattice planes . 13 1.2.4 The Bragg construction . 14 1.2.5 Structure factor . 15 1.2.6 Further geometry of diffraction . 17 2 Electrons in crystals 19 2.1 Summary of free-electron theory, etc. 19 2.2 Electrons in a periodic potential . 19 2.2.1 Bloch’s theorem . 19 2.2.2 Brillouin zones . 21 2.2.3 Schrodinger’s¨ equation in k-space . 22 2.2.4 Weak periodic potential: Nearly-free electrons . 23 2.2.5 Metals and insulators . 25 2.2.6 Band overlap in a nearly-free-electron divalent metal . 26 2.2.7 Tight-binding method . 29 2.3 Semiclassical dynamics of Bloch electrons . 32 2.3.1 Electron velocities . 33 2.3.2 Motion in an applied field . 33 2.3.3 Effective mass of an electron . 34 2.4 Free-electron bands and crystal structure . 35 2.4.1 Construction of the reciprocal lattice for FCC . 35 2.4.2 Group IV elements: Jones theory . 36 2.4.3 Binding energy of metals . -
Form and Structure Factors: Modeling and Interactions Jan Skov Pedersen, Department of Chemistry and Inano Center University of Aarhus Denmark SAXS Lab
Form and Structure Factors: Modeling and Interactions Jan Skov Pedersen, Department of Chemistry and iNANO Center University of Aarhus Denmark SAXS lab 1 Outline • Model fitting and least-squares methods • Available form factors ex: sphere, ellipsoid, cylinder, spherical subunits… ex: polymer chain • Monte Carlo integration for form factors of complex structures • Monte Carlo simulations for form factors of polymer models • Concentration effects and structure factors Zimm approach Spherical particles Elongated particles (approximations) Polymers 2 Motivation - not to replace shape reconstruction and crystal-structure based modeling – we use the methods extensively - alternative approaches to reduce the number of degrees of freedom in SAS data structural analysis (might make you aware of the limited information content of your data !!!) - provide polymer-theory based modeling of flexible chains - describe and correct for concentration effects 3 Literature Jan Skov Pedersen, Analysis of Small-Angle Scattering Data from Colloids and Polymer Solutions: Modeling and Least-squares Fitting (1997). Adv. Colloid Interface Sci. , 70 , 171-210. Jan Skov Pedersen Monte Carlo Simulation Techniques Applied in the Analysis of Small-Angle Scattering Data from Colloids and Polymer Systems in Neutrons, X-Rays and Light P. Lindner and Th. Zemb (Editors) 2002 Elsevier Science B.V. p. 381 Jan Skov Pedersen Modelling of Small-Angle Scattering Data from Colloids and Polymer Systems in Neutrons, X-Rays and Light P. Lindner and Th. Zemb (Editors) 2002 Elsevier -
Basic Four-Momentum Kinematics As
L4:1 Basic four-momentum kinematics Rindler: Ch5: sec. 25-30, 32 Last time we intruduced the contravariant 4-vector HUB, (II.6-)II.7, p142-146 +part of I.9-1.10, 154-162 vector The world is inconsistent! and the covariant 4-vector component as implicit sum over We also introduced the scalar product For a 4-vector square we have thus spacelike timelike lightlike Today we will introduce some useful 4-vectors, but rst we introduce the proper time, which is simply the time percieved in an intertial frame (i.e. time by a clock moving with observer) If the observer is at rest, then only the time component changes but all observers agree on ✁S, therefore we have for an observer at constant speed L4:2 For a general world line, corresponding to an accelerating observer, we have Using this it makes sense to de ne the 4-velocity As transforms as a contravariant 4-vector and as a scalar indeed transforms as a contravariant 4-vector, so the notation makes sense! We also introduce the 4-acceleration Let's calculate the 4-velocity: and the 4-velocity square Multiplying the 4-velocity with the mass we get the 4-momentum Note: In Rindler m is called m and Rindler's I will always mean with . which transforms as, i.e. is, a contravariant 4-vector. Remark: in some (old) literature the factor is referred to as the relativistic mass or relativistic inertial mass. L4:3 The spatial components of the 4-momentum is the relativistic 3-momentum or simply relativistic momentum and the 0-component turns out to give the energy: Remark: Taylor expanding for small v we get: rest energy nonrelativistic kinetic energy for v=0 nonrelativistic momentum For the 4-momentum square we have: As you may expect we have conservation of 4-momentum, i.e.