lunes, 15 de febrero de 2010

Diffraction theory



Summary notes, equations and figures

Introduction: a constrast of two interactions of radiation with matter
Spectroscopy (absorption): measure the variation of intensity with n or l in one direction, to obtain a spectrum.
Crystallography (diffraction): measure the variation of intensity with direction for one l, to obtain a diffraction pattern.

Fundamental properties of a wave, important in diffraction
Wavelength  l  (distance between two adjacent crests or troughs of the wave)
Amplitude  |F|  (size of wave, half the difference between crest and trough); intensity I µ |F|2
Phase  f  (position of a crest or maximum relative to other waves, measured as a fraction of the wavelength or as an angle in the range 0 to 360°)

Analogy between a microscope and X-ray crystallography
X-ray crystallography works essentially like an X-ray microscope, but in two stages:
1. scattering of X-rays by a small crystalline sample (lots of identical molecules regularly arranged and scattering cooperatively); record the diffraction pattern;
2. recombination of scattered waves mathematically by computer, to give a representation of the time-averaged electron density distribution in the sample (effectively, the positions of atoms); this can not be carried out physically as in an optical microscope.

Fundamentals of the crystalline state

Translation symmetry is essential; other symmetry (rotation, reflection, inversion) may also be present.  Translation symmetry is characterised by a lattice, and its basic repeat unit is the unit cell; geometry is specified by 3 lengths and 3 angles, some of which take special values/relationships if rotation/reflection symmetry is present.
Space group: the collection of all symmetry operations for a crystal structure.  Symbol is a combination of letters and numbers, indicating the symmetry present.  There are 230 space groups.
Asymmetric unit: the unique part of the structure (a fraction of a unit cell).  Operation of symmetry except for pure translation generates the unit cell, then operation of translation symmetry generates the complete crystal structure.
Crystal systems
For the essential symmetry, each type of rotation axis is generic; it could be a proper or improper rotation or a screw axis, and mirrors can also be glide planes.  The unit cell types shown in parentheses can be converted into standard types not in parentheses by a different choice of axes, but are used in some cases in order to satisfy other conventions or conveniences regarding symmetry and geometry.
Crystal system
Essential symmetry
Unit cell restrictions
Unit cell types
triclinic
none
none

P

monoclinic
2 and/or m for one axis
a=g=90°
P, C (I)
orthorhombic
2 and/or m for three axes
a=b=g=90°
P, C (A), I, F
tetragonal
4 for one axis
a=b; a=b=g=90°
P, I
trigonal
3 for one axis
a=b; a=b=90°, g=120°
P (R)
hexagonal
6 for one axis
a=b; a=b=90°, g=120°

P

cubic
3 for four directions
a=b=c; a=b=g=90°
P, I, F

Any line, and any plane (or set of regularly spaced parallel planes) in a 3D lattice (crystal structure) can be specified by 3 numbers; for lines joining lattice points, and sets of planes passing through lattice points, these numbers are integers.  For planes, they are called Miller indices, represented by the letters h,k,l.

Crystals and their diffraction patterns
X-rays are used because their wavelengths are comparable to the sizes of atoms and molecules, giving rise to diffraction effects by crystals.
Geometry of diffraction pattern (positions of spots on film/detector, directions of diffracted beams) is related to unit cell (lattice) geometry.
Symmetry of diffraction pattern is related to symmetry of crystal structure (space group).
Intensities of diffraction pattern are related to the nature and positions of atoms within the asymmetric unit.

Diffraction by crystals (geometry): reciprocal lattice, Bragg equation, and Ewald sphere

Direct lattice (crystal structure lattice) is defined by three vectors: a, b, c.  Define a reciprocal lattice (a*, b*, c*), such that
a* = (b ´ c) / V     b* = (c ´ a) / V     c* = (a ´ b) / V
V = a × (b ´ c) = b × (c ´ a) = c × (a ´ b)
Hence:   a × a* = b × b* = c × c* = 1
and  a × b* = a × c* = b × a* = b × c* = c × a* = c × b* = 0
This means that a* is perpendicular to both b and c, etc.  If every set of parallel lattice planes is represented by a point such that its distance from the origin is 1/d (the reciprocal of the spacing between planes) and the direction is perpendicular to the planes, then all the possible points lie at reciprocal lattice points, and the coordinates of each point (counting from the origin in three dimensions) are the Miller indices of the plane: (ha* + kb* + lc* = d*hkl, a vector with length 1/dhkl).  As a consequence of the Bragg equation (below), the reciprocal lattice is a convenient representation for the geometry of the diffraction pattern, and every diffracted beam (X-ray reflection) is labelled by the three indices h,k,l, specifying the associated lattice planes.

path difference = a sinyi + a sinyd = hl

where yi and yd are the angles of the incident and diffracted beams as shown, l is the wavelength, a is the one-dimensional lattice spacing, and h is an integer (positive, zero, or negative).  For a given value of yi (a fixed incident beam), each value of h corresponds to an observed diffraction maximum and the equation can be used to calculate the permitted values of yd, the directions in which intensity is observed.  The result is a set of bright fringes. 
Using vector notation: if s and s0 are unit vectors along the directions of the diffracted and incident beams, and a is the lattice translation vector, then
a · (s - s0) = hl
There are three such equations, one for each dimension, and all must be satisfied simultaneously (Laue equations); this requires three integers h, k, l and reference to all three lattice vectors a, b, c.
Alternative representation for three dimensions (right): for rays reflected by two adjacent planes
path difference = 2dhkl sinq = (n) l
Using vector notation: if d*hkl is the reciprocal lattice vector for the reflecting planes, then this vector is parallel to s - s0 and
(s - s0)/l = d*hkl = ha* + kb* + lc*
The Ewald sphere construction is a way of showing geometrically how rotation of a crystal (and its reciprocal lattice with it) leads to the Bragg equation being satisfied in certain orientations, generating observed diffracted beams.  A sphere of radius 1/l is centred on the crystal, with the incident beam in a fixed direction.  The origin of the reciprocal lattice is placed on the sphere opposite the incident beam, and the crystal rotates.  Whenever a reciprocal lattice point touches the surface of the sphere, the Bragg equation is satisfied for this set of lattice planes, and a Bragg reflection occurs; the direction of the diffracted beam is from the centre of the sphere to the reciprocal lattice point.  This allows us to predict both where and when diffraction will occur, if the lattice parameters and crystal orientation are known.

Diffraction by crystals (symmetry)
To a first approximation, all diffraction patterns have inversion symmetry (Friedel's Law); the point group symmetry of the pattern is related to the space group of the crystal and is called the Laue group.  There are 11 possible Laue groups.  Other aspects of the space group symmetry are revealed in 'systematic absences', special subsets of the data that systematically have zero intensity.
For a non-centrosymmetric crystal structure, if the X-ray wavelength is close to an absorption edge of an element in the compound, Friedel's Law breaks down, and I(h,k,l) ¹ I(-h,-k,-l).  The (usually small) intensity differences can be measured and used to determine absolute configuration for chiral structures.


Ider Guerrero



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