MATE50005 Diffraction

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95 Terms

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Lattice
An infinite periodic array of identical lattice points generated by integer combinations of basis vectors a, b, c.
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Motif
The group of atoms attached to each lattice point; repeating the motif over the lattice yields the crystal.
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Crystal structure
C = L ∗ M — convolution of lattice (L) and motif (M) so the motif repeats at every lattice point.
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Unit cell volume

V = a · (b × c)

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Primitive unit cell
Contains exactly one lattice point; any lattice point can be formed from integer linear combinations of a, b, c.
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Non-primitive unit cell
Contains more than one lattice point; requires fractional u, v, w in t = ua + vb + wc.
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Wigner–Seitz cell
Primitive cell formed by bisecting lines from a lattice point to neighbours; region closer to that point than any other.
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Lattice vector
t = ua + vb + wc, translation connecting any two lattice points.
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Miller indices (h k l)
Reciprocals of intercepts of a plane with the axes, then cleared of fractions to integers h,k,l.
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Direction [u v w]
Vector parallel to ua + vb + wc, reduced to smallest integer ratio; overbar for negative.
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Family of directions ⟨u v w⟩
All symmetry-equivalent directions in lattice.
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Family of planes {h k l}

All symmetry equivalent planes in a crystal

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Interplanar spacing (cubic)
d = a / √(h² + k² + l²).
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Interplanar spacing (orthorhombic)
1/d² = (h²/a²) + (k²/b²) + (l²/c²).
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Interplanar spacing (hexagonal)
1/d² = (4/3)((h² + hk + k²)/a²) + (l²/c²).
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Reciprocal lattice & diffraction

A lattice of vectors normal to real-space planes with magnitude 2π/dhkl

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Reciprocal basis vectors
a* = (2π/V)(b × c), b* = (2π/V)(c × a), c* = (2π/V)(a × b).
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Magnitude of reciprocal vector
|G_hkl| = 2π/d_hkl.
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Laue condition
Diffraction occurs when scattering vector Q equals reciprocal lattice vector G.
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Wavevector magnitude
|k| = 2π/λ; direction is normal to wavefronts.
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Huygens–Fresnel principle
Each point on a wavefront acts as a secondary wave source; explains diffraction & interference.
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Fourier transform of lattice
Perfect infinite lattice of Dirac deltas produces reciprocal lattice points.
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Crystal FT
C̃(Q) = L̃(Q) × M̃(Q) → diffraction pattern = reciprocal lattice modulated by structure factor.
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Convolution theorem
FT(f ∗ g) = FT(f) × FT(g); used to relate crystal structure and diffraction pattern.
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Dirac delta
Zero everywhere except one point; integrates to 1; represents an ideal lattice point.
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Dirac comb
Infinite series of delta functions spaced periodically; its FT is another comb with reciprocal spacing.
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Structure factor definition
F_hkl = Σ_j f_j exp[2πi(hx_j + ky_j + lz_j)], summing over atoms at fractional coordinates (x_j,y_j,z_j).
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Systematic absences
Reflections where structure factor sums to zero due to destructive interference; peaks that physically cannot appear.
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BCC structure factor rule
Two atoms (0,0,0) and (½,½,½): F = f[1 + exp(iπ(h+k+l))] → reflections allowed only when (h+k+l) even; odd ⇒ absent.
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FCC structure factor rule
Atoms at (0,0,0), (0,½,½), (½,0,½), (½,½,0); allowed only when h,k,l are all even or all odd; mixed parity forbidden.
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NaCl structure factor
FCC lattice + Na at (0,0,0), Cl at (½,½,½). F = f_Na + f_Cl exp[iπ(h+k+l)]. Even sum ⇒ constructive; odd sum ⇒ partial cancellation → weak or absent peaks.
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Glide plane definition
Mirror reflection + fractional translation in the plane; produces destructive interference giving systematic absences.
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Glide plane absence rule
If glide translation = ½ along a direction, reflections with odd index in that direction vanish (e.g., h odd ⇒ absent for (h0l)).
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Screw axis definition
Rotation + translation along the axis (e.g., 2₁ screw = 180° rotation + ½ translation).
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2₁ screw systematic rule
(h00) reflections only allowed when h even, because translation gives exp(iπ h).
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Single slit diffraction

Minima occur at θ ≈ (1 +2n)λ/W

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Double slit diffraction

Constructive intereference (bright fringes) occurs when dsinθ = nλ

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Diffraction grating

Evenly spaced slits, peaks become narrower and more intense due to path interference sinθ = nλ/S

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Diffuse vs sharp diffraction

Sharp is in a perfectly infinite crystal lattice, diffuse is in finite crystal (FT of a finite shape)

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How does diffraction measure strucutre?

Diffraction pattern is the FT of the electron density (finding F(Q) gives back atomic positions)

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Determining lattice parameter (cubic)
a = λ √(h²+k²+l²)/(2 sinθ) from each peak.
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Indexing powder patterns
Compute sin²θ or d; match with allowed h²+k²+l² for cubic; first peak identifies lattice type (FCC starts at 111, BCC at 110).
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Preferred orientation effect
Certain planes show enhanced intensity if platelets or grains align; peaks differ from ideal powder pattern.
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Anisotropic broadening
Peak widths change with hkl due to directional strain or different coherence lengths.
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Peak splitting
Occurs when symmetry is lowered (e.g., cubic → tetragonal); previously equivalent reflections separate.
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Scherrer equation
D = (K λ)/(β cosθ), K ~ 0.9, β = FWHM (radians). Estimates crystallite size from peak broadening.
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Williamson–Hall method
Plot β cosθ vs 4 sinθ/λ → intercept gives size (Scherrer-like), slope gives microstrain.
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Is K = 0.9 always correct?
No. Depends on crystallite shape; spherical≈0.89, plates, needles differ; using 0.9 is an approximation.
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BCC vs FCC diffraction
BCC first peak = 110; FCC first peak = 111. Allowed/absent rule identifies structure.
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Gold vs Ir FCC alloy test
If alloy: single FCC pattern with peaks shifted between pure Au and pure Ir. If separate phases: two FCC patterns with different a.
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X-ray vs neutron scattering
X-rays scatter from electrons, so heavy atoms dominate. Neutrons scatter from nuclei, so light atoms can give strong peaks; intensities differ.
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Background noise in XRD
Comes from incoherent scattering, fluorescence, Compton scattering, air scatter, detector noise, and imperfect sample packing; adds broad, low-intensity signal underneath peaks.
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Air scatter background
X-rays scatter elastically from air atoms, creating a smooth low-angle background; minimised by shielding, helium purge, or vacuum paths.
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Fluorescence background
When incident X-ray energy exceeds absorption edge of the sample, atoms fluoresce and emit broad X-rays, raising background; especially strong for Fe when using Cu sources.
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Compton scattering
Inelastic scattering of X-rays causes loss of energy and a broad background hump at low and mid 2θ.
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Instrument noise
Electronic noise from detector and readout system contributes random background counts.
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Doublet peaks
Cu tube emits Kα1 and Kα2 wavelengths; each reflection produces two slightly separated peaks at predictable spacing, forming a doublet.
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Why use a Ni filter with Cu radiation
Ni absorbs Kβ wavelengths, producing a cleaner spectrum with mainly Cu Kα1 and Kα2, reducing extra unwanted peaks.
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Why Kα1 and Kα2 are resolved more at high angles
Peak separation in 2θ increases with angle; doublets merge at low angles but split at high angles.
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Peak broadening from small crystallites
Finite grain size reduces coherence length; Scherrer broadening produces wide peaks inversely proportional to crystallite size.
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Peak broadening from microstrain
Variation of lattice spacings causes angular spread in Bragg condition, giving broad peaks that increase with 2θ.
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Instrumental broadening
Finite slit widths, detector resolution and monochromator imperfections produce a baseline broadening added to sample broadening.
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Preferred orientation
If grains align, certain hkl planes scatter more strongly, distorting intensities compared to reference powder pattern.
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Zero-shift error
If sample is above or below the diffractometer axis, all peaks shift slightly in 2θ; corrected by internal standard or fitting.
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Peak asymmetry at low angles
Caused by axial divergence of incident beam; peaks tail toward lower 2θ.
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Sample transparency effect
X-rays penetrate substrate causing absorption and refraction, modifying peak shape and positions.
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Sample displacement error
If sample surface is not exactly at diffractometer centre, Bragg angles shift by a small constant amount.
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Why use monochromators
Reduce Kβ and white radiation; sharpen peaks; reduce fluorescence; improve signal-to-noise ratio.
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Why powder samples are rotated during measurement
Ensures random grain orientation, improves statistical averaging, reduces preferred orientation effects.
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Why we grind samples to fine powders
Reduces grain size so many crystallites contribute; ensures random orientation; avoids spotty diffraction.
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Particle size too large problem
Coarse grains produce spotty (not smooth) powder rings; missing reflections or erratic intensities.
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Why peaks get weaker at high 2θ
Atomic form factor decreases with scattering angle, reducing intensity of high-angle reflections.
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Scattering from sample holder
If holder is amorphous (glass/plastic), broad humps appear; low-background holders minimise this.
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Spurious peaks from Cu anode
Cu Kβ and white radiation produce unwanted extra peaks; removed using Ni filters or monochromators.
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Preferred orientation in plate-like samples (e.g. alumina)
Basal planes align, enhancing low-angle reflections like (00l), causing intensity mismatch.
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Preferred orientation in needle-like crystals
Preferred alignment enhances certain (h00)/(0k0) peaks depending on habit.
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Why peak intensities differ between X-ray and neutron diffraction
X-rays scatter from electron density; neutrons scatter from nuclei with different scattering lengths, so heavy atoms weaken and light atoms strengthen relatively.
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Kβ leakage and unwanted peaks
If filter is imperfect, small Kβ intensity remains, causing small peaks at slightly different angles.
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Why use internal standards
Correct for zero-shift, lattice parameter accuracy, and instrument drift by comparing known and unknown peaks.
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Instrumental drift
X-ray intensity varies over time due to tube ageing or temperature shifts; corrected by normalisation or standards.
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Absorption correction
Heavy elements absorb X-rays strongly, changing relative intensities; absorption correction normalises true structure factor intensities.
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Why we see noise at low counts
Diffraction follows Poisson statistics; low counts give higher relative statistical scatter.
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Lorentz–polarisation factor
Intensity must be corrected for geometric factors of diffractometer and polarisation of X-ray beam.
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Wavelength and frequency equation

c = vλ

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de Broglie Wavelength

λ = h/p

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Bragg’s law

nλ = 2dsinθ

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|Ghkl|

2π/dhkl

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Wavevector equation

|k| = 2π/λ

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Q

kf - ki

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Crystal lattice with motif convolution

C = (L * M) x S

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Fourier transform formula

FT[ f( r ) x g( r )] = ( r* ) * g̃( r* )

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What does FT do to the points?

Small features spread out (smear), large features become narrow

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Cubic crystal system

a = b = c, α = β = γ = 90°, (h² + k² + l²)/a²

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Tetragonal

a = b ≠ c , α = β = γ = 90°, (h² + k²)/a² + l²/c²

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Orthorhombic

a ≠ b ≠ c, α = β = γ = 90°, h²/a² + k²/b² + l²/c²