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X-RAY DIFFRACTION X- Ray Sources Diffraction: Bragg’s Law
Crystal Structure Determination Elements of X-Ray Diffraction B.D. Cullity & S.R. Stock Prentice Hall, Upper Saddle River (2001) X-Ray Diffraction: A Practical Approach C. Suryanarayana & M. Grant Norton Plenum Press, New York (1998)
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Hence, X-rays can be used for the study of crystal structures
For electromagnetic radiation to be diffracted the spacing in the grating should be of the same order as the wavelength In crystals the typical interatomic spacing ~ 2-3 Å so the suitable radiation is X-rays Hence, X-rays can be used for the study of crystal structures Target X-rays Beam of electrons An accelerating (/decelerating) charge radiates electromagnetic radiation
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K K Mo Target impacted by electrons accelerated by a 35 kV potential
Characteristic radiation → due to energy transitions in the atom K White radiation Intensity 0.2 0.6 1.0 1.4 Wavelength ()
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Target Metal Of K radiation (Å) Mo 0.71 Cu 1.54 Co 1.79 Fe 1.94 Cr 2.29
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Incident X-rays Fluorescent X-rays Electrons Scattered X-rays
SPECIMEN Heat Fluorescent X-rays Electrons Scattered X-rays Compton recoil Photoelectrons Coherent From bound charges Incoherent (Compton modified) From loosely bound charges Transmitted beam X-rays can also be refracted (refractive index slightly less than 1) and reflected (at very small angles) Refraction of X-rays is neglected for now.
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(Darkens the background of the diffraction patterns)
Incoherent Scattering (Compton modified) From loosely bound charges Here the particle picture of the electron & photon comes in handy Electron knocked aside 2 No fixed phase relation between the incident and scattered waves Incoherent does not contribute to diffraction (Darkens the background of the diffraction patterns)
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Fluorescent X-rays Energy levels Characteristic x-rays
Knocked out electron from inner shell Vacuum Energy levels Characteristic x-rays (Fluorescent X-rays) (10−16s later seems like scattering!) Nucleus
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The secondary radiation is in all directions
A beam of X-rays directed at a crystal interacts with the electrons of the atoms in the crystal The electrons oscillate under the influence of the incoming X-Rays and become secondary sources of EM radiation The secondary radiation is in all directions The waves emitted by the electrons have the same frequency as the incoming X-rays coherent The emission will undergo constructive or destructive interference with waves scattered from other atoms Secondary emission Incoming X-rays
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Sets Electron cloud into oscillation
Sets nucleus (with protons) into oscillation Small effect neglected
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Oscillating charge re-radiates In phase with the incoming x-rays
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d dSin The path difference between ray 1 and ray 2 = 2d Sin
BRAGG’s EQUATION Deviation = 2 Ray 1 Ray 2 d dSin The path difference between ray 1 and ray 2 = 2d Sin For constructive interference: n = 2d Sin
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Incident and scattered waves are in phase if
In plane scattering is in phase Incident and scattered waves are in phase if Scattering from across planes is in phase
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But this is still reinforced scattering and NOT reflection
Extra path traveled by incoming waves AY These can be in phase if and only if incident = scattered Extra path traveled by scattered waves XB But this is still reinforced scattering and NOT reflection
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Note that in the Bragg’s equation:
The interatomic spacing (a) along the plane does not appear Only the interplanar spacing (d) appears Change in position or spacing of atoms along the plane should not affect Bragg’s condition !! d Note: shift (systematic) is actually not a problem!
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Note: shift is actually not a problem
Note: shift is actually not a problem! Why is ‘systematic’ shift not a problem?
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Consider the case for which 1 2
Constructive interference can still occur if the difference in the path length traversed by R1 and R2 before and after scattering are an integral multiple of the wavelength (AY − XC) = h (h is an integer)
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This is looking at diffraction from atomic arrays and not planes
Generalizing into 3D Laue’s equations S0 incoming X-ray beam S Scattered X-ray beam This is looking at diffraction from atomic arrays and not planes
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A physical picture of scattering leading to diffraction is embodied in Laue’s equations
Bragg’s method of visualizing diffraction as “reflection” from a set of planes is a different way of understanding the phenomenon of diffraction from crystals The ‘plane picture’ (Bragg’s equations) are simpler and we usually stick to them Hence, we should think twice before asking the question: “if there are no atoms in the scattering planes, how are they scattering waves?”
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Diffraction = Reinforced Coherent Scattering
Bragg’s equation is a negative law If Bragg’s eq. is NOT satisfied NO reflection can occur If Bragg’s eq. is satisfied reflection MAY occur Diffraction = Reinforced Coherent Scattering Reflection versus Scattering Reflection Diffraction Occurs from surface Occurs throughout the bulk Takes place at any angle Takes place only at Bragg angles ~100 % of the intensity may be reflected Small fraction of intensity is diffracted X-rays can be reflected at very small angles of incidence
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n is an integer and is the order of the reflection
n = 2d Sin n is an integer and is the order of the reflection For Cu K radiation ( = 1.54 Å) and d110= 2.22 Å n Sin 1 0.34 20.7º First order reflection from (110) 2 0.69 43.92º Second order reflection from (110) Also written as (220)
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In XRD nth order reflection from (h k l) is considered as 1st order reflection from (nh nk nl)
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A B C Intensity of the Scattered electrons Scattering by a crystal
Polarization factor B Atom Atomic scattering factor (f) C Unit cell (uc) Structure factor (F)
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A Scattering by an Electron Coherent (definite phase relationship)
Emission in ‘all’ directions Sets electron into oscillation Coherent (definite phase relationship) Scattered beams The electric field (E) is the main cause for the acceleration of the electron The moving particle radiates most strongly in a direction perpendicular to its motion The radiation will be polarized along the direction of its motion
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Intensity of the scattered beam due to an electron (I) at a point P
For an polarized wave z P For a wave oscillating in z direction r x Intensity of the scattered beam due to an electron (I) at a point P such that r >> The reason we are able to neglect scattering from the protons in the nucleus The scattered rays are also plane polarized
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For an unpolarized wave
E is the measure of the amplitude of the wave E2 = Intensity IPy = Intensity at point P due to Ey Total Intensity at point P due to Ey & Ez IPz = Intensity at point P due to Ez
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Sum of the squares of the direction cosines =1
Hence In terms of 2
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In general P could lie anywhere in 3D space
x z r P 2 In general P could lie anywhere in 3D space For the specific case of Bragg scattering: The incident direction IO The diffracted beam direction OP The trace of the scattering plane BB’ Are all coplanar OP is constrained to be on the xz plane
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For an unpolarized wave E is the measure of the amplitude of the wave
E2 = Intensity IPy = Intensity at point P due to Ey The zx plane is to the y direction: hence, = 90 IPz = Intensity at point P due to Ez
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Scattered beam is not unpolarized
Very small number Forward and backward scattered intensity higher than at 90 Scattered intensity minute fraction of the incident intensity
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Polarization factor Comes into being as we used unpolarized beam
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B Scattering by an Atom f → (Å−1) →
Scattering by an atom [Atomic number, (path difference suffered by scattering from each e−, )] Scattering by an atom [Z, (, )] Angle of scattering leads to path differences In the forward direction all scattered waves are in phase f → (Å−1) → 0.2 0.4 0.6 0.8 1.0 10 20 30 Schematic
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Incoherent (Compton) scattering
Coherent scattering Incoherent (Compton) scattering Z Sin() /
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B Scattering by an Atom BRUSH-UP
The conventional UC has lattice points as the vertices There may or may not be atoms located at the lattice points The shape of the UC is a parallelepiped (Greek parallēlepipedon) in 3D There may be additional atoms in the UC due to two reasons: The chosen UC is non-primitive The additional atoms may be part of the motif
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C Scattering by the Unit cell (uc)
Coherent Scattering Unit Cell (UC) is representative of the crystal structure Scattered waves from various atoms in the UC interfere to create the diffraction pattern The wave scattered from the middle plane is out of phase with the ones scattered from top and bottom planes
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x d(h00) a B A R S B M N C Ray 1 = R1 Ray 3 = R3 Ray 2 = R2
Unit Cell x R S Ray 2 = R2 B d(h00) a M N (h00) plane C
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Independent of the shape of UC
Extending to 3D Independent of the shape of UC Note: R1 is from corner atoms and R3 is from atoms in additional positions in UC
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In complex notation If atom B is different from atom A the amplitudes must be weighed by the respective atomic scattering factors (f) The resultant amplitude of all the waves scattered by all the atoms in the UC gives the scattering factor for the unit cell The unit cell scattering factor is called the Structure Factor (F) Scattering by an unit cell = f(position of the atoms, atomic scattering factors) For n atoms in the UC Structure factor is independent of the shape and size of the unit cell If the UC distorts so do the planes in it!!
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Structure factor calculations
Simple Cubic A Atom at (0,0,0) and equivalent positions F is independent of the scattering plane (h k l)
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Real C- centred Orthorhombic
Atom at (0,0,0) & (½, ½, 0) and equivalent positions C- centred Orthorhombic Real (h + k) even Both even or both odd e.g. (001), (110), (112); (021), (022), (023) Mixture of odd and even (h + k) odd e.g. (100), (101), (102); (031), (032), (033) F is independent of the ‘l’ index
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If the blue planes are scattering in phase then on C- centering the red planes will scatter out of phase (with the blue planes- as they bisect them) and hence the (210) reflection will become extinct This analysis is consistent with the extinction rules: (h + k) odd is absent
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In case of the (310) planes no new translationally equivalent planes are added on lattice centering this reflection cannot go missing. This analysis is consistent with the extinction rules: (h + k) even is present
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Real Body centred Orthorhombic
Atom at (0,0,0) & (½, ½, ½) and equivalent positions Real (h + k + l) even e.g. (110), (200), (211); (220), (022), (310) (h + k + l) odd e.g. (100), (001), (111); (210), (032), (133)
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Real Face Centred Cubic
Atom at (0,0,0) & (½, ½, 0) and equivalent positions Face Centred Cubic (½, ½, 0), (½, 0, ½), (0, ½, ½) Real (h, k, l) unmixed e.g. (111), (200), (220), (333), (420) (h, k, l) mixed e.g. (100), (211); (210), (032), (033) Two odd and one even (e.g. 112); two even and one odd (e.g. 122)
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Mixed indices Mixed indices CASE h k l A o e B (h, k, l) mixed
Two odd and one even (e.g. 112); two even and one odd (e.g. 122) Mixed indices CASE h k l A o e B (h, k, l) mixed e.g. (100), (211); (210), (032), (033) Unmixed indices All odd (e.g. 111); all even (e.g. 222) Unmixed indices CASE h k l A o B e (h, k, l) unmixed e.g. (111), (200), (220), (333), (420)
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E Na+ at (0,0,0) + Face Centering Translations (½, ½, 0), (½, 0, ½), (0, ½, ½) Cl− at (½, 0, 0) + FCT (0, ½, 0), (0, 0, ½), (½, ½, ½) NaCl: Face Centred Cubic
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Zero for mixed indices Mixed indices CASE h k l A o e B Mixed indices
(h, k, l) mixed e.g. (100), (211); (210), (032), (033)
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If (h + k + l) is even If (h + k + l) is odd Unmixed indices CASE h k
B e Unmixed indices (h, k, l) unmixed e.g. (111), (222); (133), (244) If (h + k + l) is even e.g. (222),(244) If (h + k + l) is odd e.g. (111), (133)
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Presence of additional atoms/ions/molecules in the UC can alter the intensities of some of the reflections
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Reflections which may be present Reflections necessarily absent
Selection / Extinction Rules Bravais Lattice Reflections which may be present Reflections necessarily absent Simple all None Body centred (h + k + l) even (h + k + l) odd Face centred h, k and l unmixed h, k and l mixed End centred h and k unmixed C centred h and k mixed C centred Bravais Lattice Allowed Reflections SC All BCC (h + k + l) even FCC h, k and l unmixed DC h, k and l are all odd Or all are even & (h + k + l) divisible by 4
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h2 + k2 + l2 SC FCC BCC DC 1 100 2 110 3 111 4 200 5 210 6 211 7 8 220 9 300, 221 10 310 11 311 12 222 13 320 14 321 15 16 400 17 410, 322 18 411, 330 19 331
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Reciprocal Lattice BASIS VECTORS B
Properties are reciprocal to the crystal lattice BASIS VECTORS B The reciprocal lattice is created by interplanar spacings
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A reciprocal lattice vector is to the corresponding real lattice plane
The length of a reciprocal lattice vector is the reciprocal of the spacing of the corresponding real lattice plane Planes in the crystal become lattice points in the reciprocal lattice ALTERNATE CONSTRUCTION OF THE REAL LATTICE Reciprocal lattice point represents the orientation and spacing of a set of planes
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Reciprocal Lattice The reciprocal lattice has an origin!
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Note perpendicularity of various vectors
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Physics comes in from the following:
Reciprocal lattice is the reciprocal of a primitive lattice and is purely geometrical does not deal with the intensities of the points Physics comes in from the following: For non-primitive cells ( lattices with additional points) and for crystals decorated with motifs ( crystal = lattice + motif) the Reciprocal lattice points have to be weighed in with the corresponding scattering power (|Fhkl|2) Some of the Reciprocal lattice points go missing (or may be scaled up or down in intensity) Making of Reciprocal Crystal (Reciprocal lattice decorated with a motif of scattering power) The Ewald sphere construction further can select those points which are actually observed in a diffraction experiment
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Crystal = Lattice + Motif
In crystals based on a particular lattice the intensities of particular reflections are modified they may even go missing Diffraction Pattern Position of the Lattice points LATTICE Intensity of the diffraction spots ‘MOTIF’ There are two ways of constructing the Reciprocal Crystal: 1) Construct the lattice and decorate each lattice point with appropriate intensity 2) Use the concept as that for the real crystal
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SC Lattice = SC Reciprocal Crystal = SC
Examples of 3D Reciprocal Lattices weighed in with scattering power (|F|2) SC 001 011 101 111 Lattice = SC 000 010 100 110 No missing reflections Reciprocal Crystal = SC Figures NOT to Scale
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BCC Lattice = BCC Reciprocal Crystal = FCC 002 022 202 222 011 101 020
000 Lattice = BCC 110 200 100 missing reflection (F = 0) 220 Reciprocal Crystal = FCC Weighing factor for each point “motif” Figures NOT to Scale
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FCC Lattice = FCC Reciprocal Crystal = BCC 002 022 202 222 111 020 000
200 220 100 missing reflection (F = 0) 110 missing reflection (F = 0) Weighing factor for each point “motif” Reciprocal Crystal = BCC Figures NOT to Scale
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Ordered Solid solution
In a strict sense this is not a crystal !! Ordered Solid solution High T disordered BCC 470ºC G = H TS Sublattice-1 Sublattice-2 SC Low T ordered
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SC Ordered BCC Disordered Ordered - NiAl, BCC B2 (CsCl type) - Ni3Al, FCC L12 (AuCu3-I type) FCC SC Ordered FCC BCC
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1) SC + two kinds of Intensities decorating the lattice
There are two ways of constructing the Reciprocal Crystal: 1) Construct the lattice and decorate each lattice point with appropriate intensity 2) Use the concept as that for the real crystal 1) SC + two kinds of Intensities decorating the lattice 2) (FCC) + (Motif = 1FR + 1SLR) FR Fundamental Reflection SLR Superlattice Reflection 1) SC + two kinds of Intensities decorating the lattice 2) (BCC) + (Motif = 1FR + 3SLR)
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The Ewald Sphere * Paul Peter Ewald (German physicist and crystallographer; )
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7. Paul-Peter-Ewald-Kolloquium
Freitag, 17. Juli 2008 organisiert von: Max-Planck-Institut für Metallforschung Institut für Theoretische und Angewandte Physik, Institut für Metallkunde, Institut für Nichtmetallische Anorganische Materialien der Universität Stuttgart Programm 13:30 Joachim Spatz (Max-Planck-Institut für Metallforschung) Begrüßung 13:45 Heribert Knorr (Ministerium für Wissenschaft, Forschung und Kunst Baden-Württemberg Begrüßung 14:00 Stefan Hell (Max-Planck-Institut für Biophysikalische Chemie) Nano-Auflösung mit fokussiertem Licht 14:30 Antoni Tomsia (Lawrence Berkeley National Laboratory) Using Ice to Mimic Nacre: From Structural Materials to Artificial Bone 15:00 Pause Kaffee und Getränke 15:30 Frank Gießelmann(Universität Stuttgart) Von ferroelektrischen Fluiden zu geordneten Dispersionen von Nanoröhren: Aktuelle Themen der Flüssigkristallforschung 16:00 Verleihung des Günter-Petzow-Preises 2008 16:15 Udo Welzel (Max-Planck-Institut für Metallforschung) Materialien unter Spannung: Ursachen, Messung und Auswirkungen- Freund und Feind ab 17:00 Sommerfest des Max-Planck-Instituts für Metallforschung
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The Ewald Sphere The reciprocal lattice points are the values of momentum transfer for which the Bragg’s equation is satisfied For diffraction to occur the scattering vector must be equal to a reciprocal lattice vector Geometrically if the origin of reciprocal space is placed at the tip of ki then diffraction will occur only for those reciprocal lattice points that lie on the surface of the Ewald sphere See Cullity’s book: A15-4
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Bragg’s equation revisited
Draw a circle with diameter 2/ Construct a triangle with the diameter as the hypotenuse and 1/dhkl as a side (any triangle inscribed in a circle with the diameter as the hypotenuse is a right angle triangle): AOP The angle opposite the 1/d side is hkl (from the rewritten Bragg’s equation)
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The Ewald Sphere construction
Crystal related information is present in the reciprocal crystal The Ewald sphere construction generates the diffraction pattern Radiation related information is present in the Ewald Sphere
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K = K =g = Diffraction Vector
Ewald Sphere The Ewald Sphere touches the reciprocal lattice (for point 41) Bragg’s equation is satisfied for 41 K = K =g = Diffraction Vector
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Ewald sphere X-rays (Cu K) = 1.54 Å, 1/ = 0.65 Å−1 (2/ = 1.3 Å−1), aAl = 4.05 Å, d111 = 2.34 Å, 1/d111 = 0.43 Å−1
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Crystal structure determination
Many s (orientations) Powder specimen POWDER METHOD Monochromatic X-rays Single LAUE TECHNIQUE Panchromatic X-rays ROTATING CRYSTAL METHOD Varied by rotation Monochromatic X-rays
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THE POWDER METHOD Cone of diffracted rays
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POWDER METHOD Diffraction cones and the Debye-Scherrer geometry
Different cones for different reflections Film may be replaced with detector
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The 440 reflection is not observed
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The 331 reflection is not observed
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THE POWDER METHOD Cubic crystal
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Relative Intensity of diffraction lines in a powder pattern
Structure Factor (F) Scattering from UC Multiplicity factor (p) Number of equivalent scattering planes Polarization factor Effect of wave polarization Lorentz factor Combination of 3 geometric factors Absorption factor Specimen absorption Temperature factor Thermal diffuse scattering
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Multiplicity factor * Altered in crystals with lower symmetry Lattice
Index Multiplicity Planes Cubic (with highest symmetry) (100) 6 [(100) (010) (001)] ( 2 for negatives) (110) 12 [(110) (101) (011), (110) (101) (011)] ( 2 for negatives) (111) [(111) (111) (111) (111)] ( 2 for negatives) (210) 24* (210) 3! Ways, (210) 3! Ways, (210) 3! Ways, (210) 3! Ways (211) 24 (211) 3 ways, (211) 3! ways, (211) 3 ways (321) 48* Tetragonal 4 [(100) (010)] ( 2 for negatives) [(110) (110)] ( 2 for negatives) 8 8* (210) = 2 Ways, (210) = 2 Ways, (210) = 2 Ways, (210) = 2 Ways 16 [Same as for (210) = 8] 2 (as l can be +1 or 1) 16* Same as above (as last digit is anyhow not permuted) * Altered in crystals with lower symmetry
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Multiplicity factor Cubic hkl hhl hk0 hh0 hhh h00 48* 24 24* 12 8 6
Hexagonal hk.l hh.l h0.l hk.0 hh.0 h0.0 00.l 12* 2 Tetragonal h0l 00l 16* 8* 4 Orthorhombic 0kl 0k0 Monoclinic Triclinic * Altered in crystals with lower symmetry (of the same crystal class)
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Polarization factor Lorentz factor
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Valid for Debye-Scherrer geometry I → Relative Integrated “Intensity”
Intensity of powder pattern lines (ignoring Temperature & Absorption factors) Valid for Debye-Scherrer geometry I → Relative Integrated “Intensity” F → Structure factor p → Multiplicity factor POINTS As one is interested in relative (integrated) intensities of the lines constant factors are omitted Volume of specimen me , e (1/dectector radius) Random orientation of crystals in a with Texture intensities are modified I is really diffracted energy (as Intensity is Energy/area/time) Ignoring Temperature & Absorption factors valid for lines close-by in pattern
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THE POWDER METHOD Cubic crystal
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Determination of Crystal Structure from 2 versus Intensity Data
2→ Intensity Sin Sin2 ratio
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FCC 2→ Intensity Sin Sin2 ratio 1 21.5 0.366 0.134 3 2 25 0.422
0.178 4 37 0.60 0.362 8 45 0.707 0.500 11 5 47 0.731 0.535 12 6 58 0.848 0.719 16 7 68 0.927 0.859 19 FCC
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h2 + k2 + l2 SC FCC BCC DC 1 100 2 110 3 111 4 200 5 210 6 211 7 8 220 9 300, 221 10 310 11 311 12 222 13 320 14 321 15 16 400 17 410, 322 18 411, 330 19 331
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The ratio of (h2 + K2 + l2) derived from extinction rules
SC 1 2 3 4 5 6 8 … BCC 7 FCC 11 12 DC 16
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Peaks or not idealized peaks broadened
Powder diffraction pattern from Al Radiation: Cu K, = Å 111 Note: Peaks or not idealized peaks broadened Increasing splitting of peaks with g Peaks are all not of same intensity 220 311 200 420 331 422 222 400 1 & 2 peaks resolved X-Ray Diffraction: A Practical Approach, C. Suryanarayana & M. Grant Norton, Plenum Press, New York (1998)
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Actually, the variation in 2 is to be seen
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Determination of Crystal Structure from 2 versus Intensity Data
ratio Index a (nm) 1 38.52 19.26 0.33 0.11 3 111 2 44.76 22.38 0.38 0.14 4 200 65.14 32.57 0.54 0.29 8 220 78.26 39.13 0.63 0.40 11 311 5* 82.47 41.235 0.66 0.43 12 222 6* 99.11 49.555 0.76 0.58 16 400 7* 112.03 56.015 0.83 0.69 19 331 8* 116.60 58.3 0.85 0.72 20 420 9* 137.47 68.735 0.93 0.87 24 422 * 1 , 2 peaks are resolved (1 peaks are listed)
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Error in d spacing For the same the error in Sin with
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Error in d spacing Error in d spacing decreases with
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Applications of XRD Bravais lattice determination
Lattice parameter determination Determination of solvus line in phase diagrams Long range order Crystallite size and Strain More
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Crystal Intensity → Diffraction angle (2) → Intensity →
90 180 Crystal Schematic of difference between the diffraction patterns of various phases 90 180 Diffraction angle (2) → Intensity → Monoatomic gas 90 180 Diffraction angle (2) → Intensity → Liquid / Amorphous solid
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Crystallite size and Strain
Bragg’s equation assumes: Crystal is perfect and infinite Incident beam is perfectly parallel and monochromatic Actual experimental conditions are different from these leading various kinds of deviations from Bragg’s condition Peaks are not ‘’ curves Peaks are broadened There are also deviations from the assumptions involved in the generating powder patterns Crystals may not be randomly oriented (textured sample) Peak intensities are altered In a powder sample if the crystallite size < 0.5 m there are insufficient number of planes to build up a sharp diffraction pattern peaks are broadened
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XRD Line Broadening
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XRD Line Broadening Instrumental Crystallite size Strain
Unresolved 1 , 2 peaks Non-monochromaticity of the source (finite width of peak) Imperfect focusing Bi Crystallite size In the vicinity of B the −ve of Bragg’s equation not being satisfied Bc Strain ‘Residual Strain’ arising from dislocations, coherent precipitates etc. leading to broadening Bs Stacking fault In principle every defect contributes to some broadening Other defects
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Size (10, 0.5) Smooth continuous ring pattern
Crystallite size Size > 10 m Spotty ring (no. of grains in the irradiated portion insufficient to produce a ring) Size (10, 0.5) Smooth continuous ring pattern Size (0.5, 0.1) Rings are broadened Size < 0.1 No ring pattern (irradiated volume too small to produce a diffraction ring pattern & diffraction occurs only at low angles) Spotty ring Rings Diffuse Broadened Rings
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Effect of crystallite size on SAD patterns
Single crystal “Spotty” pattern Few crystals in the selected region
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Effect of crystallite size on SAD patterns
Ring pattern Broadened Rings
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Subtracting Instrumental Broadening
Instrumental broadening has to be subtracted to get the broadening effects due to the sample 1 Mix specimen with known coarse-grained (~ 10m), well annealed (strain free) does not give any broadening due to strain or crystallite size (the only broadening is instrumental). A brittle material which can be ground into powder form without leading to much stored strain is good. If the pattern of the test sample (standard) is recorded separately then the experimental conditions should be identical (it is preferable that one or more peaks of the standard lies close to the specimen’s peaks) 2 Use the same material as the standard as the specimen to be X-rayed but with large grain size and well annealed
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For a peak with a Lorentzian profile
Hendrik Antoon Lorentz Longer tail On the theory of reflection and refraction of light For a peak with a Gaussian profile A geometric mean can also used Johann Carl Friedrich Gauss ( ), painted by Christian Albrecht Jensen University of Göttingen
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Scherrer’s formula → Wavelength
For Gaussian line profiles and cubic crystals → Wavelength L → Average crystallite size ( to surface of specimen) k → 0.94 [k (0.89, 1.39)] ~ 1 (the accuracy of the method is only 10%)
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Smaller angle peaks should be used to separate Bs and Bc
Strain broadening → Strain in the material Smaller angle peaks should be used to separate Bs and Bc
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Separating crystallite size broadening and strain broadening
Plot of [Br Cos] vs [Sin]
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Example of a calculation
Sample: Annealed Al Radiation: Cu k ( = 1.54 Å) Intensity → Sample: Cold-worked Al Radiation: Cu k ( = 1.54 Å) 2 → 40 60 Intensity → 2 → 40 60 X-Ray Diffraction: A Practical Approach, C. Suryanarayana & M. Grant Norton, Plenum Press, New York (1998)
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Annealed Al Peak No. 2 () hkl Bi = FWHM () Bi = FWHM (rad) 1 38.52 111 0.103 1.8 10−3 2 44.76 200 0.066 1.2 10−3 3 65.13 220 0.089 1.6 10−3 Cold-worked Al 2 () Sin() hkl B () B (rad) Br Cos (rad) 1 38.51 0.3298 111 0.187 3.3 10−3 2.8 10−3 2.6 10−3 2 44.77 0.3808 200 0.206 3.6 10−3 3.4 10−3 3.1 10−3 3 65.15 0.5384 220 0.271 4.7 10−3 4.4 10−3 3.7 10−3
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end
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Iso-intensity circle
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Extinction Rules Structure Factor (F): The resultant wave scattered by all atoms of the unit cell The Structure Factor is independent of the shape and size of the unit cell; but is dependent on the position of the atoms within the cell
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Consider the compound ZnS (sphalerite)
Consider the compound ZnS (sphalerite). Sulphur atoms occupy fcc sites with zinc atoms displaced by ¼ ¼ ¼ from these sites. Click on the animation opposite to show this structure. The unit cell can be reduced to four atoms of sulphur and 4 atoms of zinc. Many important compounds adopt this structure. Examples include ZnS, GaAs, InSb, InP and (AlGa)As. Diamond also has this structure, with C atoms replacing all the Zn and S atoms. Important semiconductor materials silicon and germanium have the same structure as diamond. Structure factor calculation Consider a general unit cell for this type of structure. It can be reduced to 4 atoms of type A at 000, 0 ½ ½, ½ 0 ½, ½ ½ 0 i.e. in the fcc position and 4 atoms of type B at the sites ¼ ¼ ¼ from the A sites. This can be expressed as: The structure factors for this structure are: F = 0 if h, k, l mixed (just like fcc) F = 4(fA ± ifB) if h, k, l all odd F = 4(fA - fB) if h, k, l all even and h+ k+ l = 2n where n=odd (e.g. 200) F = 4(fA + fB) if h, k, l all even and h+ k+ l = 2n where n=even (e.g. 400)
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421 missing
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(Cu K) = 1.54 Å, 1/ = 0.65 Å−1, aCu = 3.61 Å, 1/aCu = 0.28 Å−1
Ewald sphere X-rays (Cu K) = 1.54 Å, 1/ = 0.65 Å−1, aCu = 3.61 Å, 1/aCu = 0.28 Å−1
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Multiplicity factor Lattice Index Planes Cubic with highest symmetry
(100) 6 [(100) (010) (001)] ( 2 for negatives) (110) 12 [(110) (101) (011), (110) (101) (011)] ( 2 for negatives) (111) 8 [(111) (111) (111) (111)] ( 2 for negatives) (210) 24 (210) = 3! Ways, (210) = 3! Ways, (210) = 3! Ways, (210) = 3! Ways, (211) (321) 48 Tetragonal 4 [(100) (010)] [(110) (110)]
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