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XRD (X-Ray Diffractometer)

XRD is an important tool for determining the intercrystalline structures of minerals and chemical compounds. The method is non-destructive and mineral species can be identified (‘fingerprinted’) in bulk samples even if only in very small particles.

Mineralogical make-up of sediments and sedimentary rocks can also be estimated (for species with concentrations in excess of about 5%). An Environmental Chamber is available for running air-sensitive samples.

Make/model Philips Automated Powder Diffractometer (model PW1710)
Details Solid and powdered crystaline materials are identified against a database of more than 70,000 recorded phases. Quantification is possible.
Facility Electron microbeam facility
School School of Earth and Environmental Sciences

  • Solid and powdered samples can be analysed and matched against a database of 70 000 recorded phases, thereby identifying and quantifying unknown phases.
  • Each pure mineral or compound has a specific X-ray diffraction pattern and these are matched against the unknowns.
  • The diffractometer gives compound or mineral names, as opposed to a list of elements as in other analytical methods.

Get in touch

Dr Duncan Muir

Email
muird1@cardiff.ac.uk
Telephone
+44 (0)29 2087 5059

Location

Main Building
Park Place
CF10 3AT