X-ray diffraction (XRD) analysis
What does X-ray diffraction do?
- XRD is the primary, non-destructive tool for identifying and quantifying
the mineralogy of crystalline compounds in rocks, soils and particulates.
- Every mineral or compound has a characteristic X-ray diffraction
pattern whose ‘fingerprint’ can be matched against a database of
over 250,000 recorded phases.
- Modern computer-controlled diffraction systems can interpret the
diffraction traces produced by individual constituents and highly
complex mixtures.
- XRD is an essential technique for identifying and characterising
the nature of clay minerals, providing information which cannot be
determined by any other method (link to
Clay mineralogy page).
MPANalytical X'Pert Pro diffractometer, loading sample.
How does X-ray diffraction work?
- When monochromatic X-rays are projected onto a crystalline material
at an angle θ, diffraction occurs when the distance traveled
by the rays reflected from successive planes differs by an integer (n) of
wavelengths (λ).
- By varying the angle θ, the Bragg's Law conditions [nθ =
2d sinΘ] are satisfied by different d-spacings.
- Plotting the angular positions and intensities of the resultant
diffracted peaks produces a characteristic pattern. Where different
phases are present, the diffraction trace represents the sum of the
individual patterns.
PANalytical X'Pert Pro diffractometer.
PANalytical X'Pert Pro diffractometer, capillary stage and divergence
slits.
Equipment?
- State-of-the-art PANalytical X’Pert Pro diffractometer which can
be flexibly configured with flat spinning or capillary stages, 45-position
sample changer, temperature/humidity chamber for either routine or
research analyses.
- Backup Philips PW1700 series diffractometer.
- Latest versions of the internationally-recognised ICDD and ICSD
databases
- PANalytical HighScore Plus analytical software including Rietveld
refinement for quantification.
Applications?
The XRD laboratories at Keyworth play a key role in projects that
span the BGS science programme, for example:
- characterisation of lithologies intended for radioactive waste
disposal and CO2 capture/storage
- researching changes in soil clay mineralogy with different land
management practices
- determining the contribution of clay minerals to the engineering
behaviour of rocks and soils
- distinguishing natural and anthropogenic sources of toxic elements
in brown field sites
- providing forensic evidence
- providing indicators of geological history, basin maturity and
low grade metamorphism
Staff and facilities are also in constant demand for direct consultancy
analysis and interpretation by external clients including: oil, mineral
and mining companies, engineering and utility companies, consultancies,
university departments and local authorities.