Bragg's Law & Finite Crystal Thickness ($N$ Planes)
Constructive interference occurs when path difference equals integer wavelengths $\lambda$. Adjust the number of atomic planes $N$ (thickness $t = N \cdot d$) to see how thin crystal plates cause diffraction peak broadening via the Laue interference function.
Experimental Parameters
Interference Function $I(\theta)$ vs $\theta$
Current θ markerThickness Effect: Increasing $N$ concentrates intensity into sharper peaks whose width is inversely proportional to $t = N \cdot d$. As $N \to \infty$, the function converges to the delta-function of ideal infinite Bragg reflection.
Reciprocal Lattice, Ewald Sphere & 2D Area Detector
Because a single crystal has one unique orientation in 3D, constructive interference occurs only when a reciprocal lattice point intersects the Ewald sphere of radius $1/\lambda$, projecting sharp, discrete diffraction spots onto the detector.
2D Area Detector Frame
Sharply localized diffraction spots
In a single crystal, all unit cells have parallel lattice orientations. The condition $\mathbf{k}_{\text{diff}} - \mathbf{k}_{\text{in}} = \mathbf{G}_{hkl}$ is satisfied only at discrete rotational angles $\omega$. This produces isolated spots rather than continuous rings!
Debye-Scherrer Cones & 1D Diffractogram: $I$ vs $2\theta$
Billions of randomly oriented crystallites project concentric Debye-Scherrer cones of aperture angle $4\theta$. Radially integrating these rings yields the 1D powder pattern plotted directly as Diffraction Intensity versus $2\theta$.
Debye Rings on 2D Detector
$R = D \tan(2\theta)$Cutting the cones with a flat camera produces concentric circular rings.
Powder Diffractogram: Intensity vs $2\theta$ (Bragg-Brentano Geometry)
Horizontal axis is $2\theta$ (two times the Bragg angle) from $10^\circ$ to $90^\circ$. Broadening and shifts reflect both crystallite thickness and lattice strain parameters.
Microstrain, Macrostrain & Williamson-Hall Separation
Crystal thickness causes $1/\cos\theta$ broadening, microstrain causes $\tan\theta$ broadening, and macrostrain shifts peaks ($\Delta 2\theta = -2\varepsilon_{\text{macro}}\tan\theta$). The Williamson-Hall Plot ($\beta\cos\theta$ vs $4\sin\theta$) separates size (y-intercept) from strain (slope).
Williamson-Hall Plot ($\beta \cos\theta$ vs $4 \sin\theta$)
Separates size from microstrain by linear regression
Extracted $\varepsilon$: 0.200 %
Microscopic Lattice State
Distortion of atomic lattice planes under chosen parameters
Physical Principles of X-Ray Diffraction, Size & Strain
Review the geometrical derivation of Bragg's Law, crystal thickness effects (Laue interference function and Scherrer broadening), lattice strain effects (microstrain vs macrostrain), and the Williamson-Hall deconvolution.
1. Bragg's Law & Geometric Path Difference
Parallel monochromatic X-ray beams striking adjacent planes separated by distance $d$ at grazing incident angle $\theta$ have an optical path difference equal to:
Because $\sin\theta \le 1$, observable diffraction demands that $\lambda \le 2d$. X-rays possess wavelengths of $\approx 0.5 - 2.5\text{ \AA}$, making them ideally suited to probe crystal lattices.
2. Crystal Thickness & Scherrer Equation
For a finite crystal of $N$ planes (thickness $t = N \cdot d$), summing the electric fields yields the Laue interference function:
Here, $\beta$ is the full width at half-maximum (FWHM) in radians, $K \approx 0.9$ is the Scherrer shape constant, and $L$ is the crystallite thickness. As $L \to \infty$, the function converges to an infinitely sharp delta-function.
3. Microstrain vs Macrostrain
Lattice strain exerts two distinctly different physical consequences on the diffraction pattern:
Tensile macrostrain increases $d$, shifting peaks to lower $2\theta$. Compressive macrostrain decreases $d$, shifting peaks to higher $2\theta$. Microstrain represents crystal defect fields (dislocations, vacancies) with distributed $\Delta d/d$.
4. Williamson-Hall Method
Assuming Lorentzian or Voigt sum of the size and strain contributions to the total peak integral breadth $\beta_{\text{total}}$:
Plotting $\beta_{\text{total}}\cos\theta$ on the y-axis against $4\sin\theta$ on the x-axis yields a straight line with:
• Y-intercept: $K\lambda / L$ (inversely proportional to crystallite size)
• Slope: $\varepsilon$ (equal to the microstrain)
Comparison: Single Crystal XRD vs Powder XRD
| Property | Single Crystal XRD (SC-XRD) | Powder XRD (PXRD) |
|---|---|---|
| Sample Form | One discrete, uniform crystal (~50–300 μm) | Ensemble of $10^7$ to $10^{10}$ microcrystallites |
| Diffraction Pattern | Discrete 3D spots in reciprocal space | Debye-Scherrer concentric rings $\to$ 1D trace ($I$ vs $2\theta$) |
| Strain Measurement | 3D spot shape profile tensor & orientation matrix distortion | Peak broadening ($\tan\theta$ dependence) & position shifts |
| Thickness Effect | Reciprocal lattice nodes elongate into reciprocal rods ("rel-rods") | Diffraction peaks broaden into Cauchy/Voigt profiles (Scherrer effect) |