X-ray Powder Diffraction (XRD)

If you have used these instruments please cite using the following:

Siemens D5000 Diffractomer

Siemens. (2025). X-Ray Powder Diffracrometer (XRD) (Siemens D5000). James Cook University, Advanced Analytical Centre. https://doi.org/10.25903/WJVB-XS57

Bruker D2 Phaser

Bruker. (2025). X-Ray Powder Diffractometer (Bruker D2 Phaser). James Cook University, Advanced Analytical Centre. https://doi.org/10.25903/DS5E-XQ16

About the Technique

X-ray powder Diffraction is a technique used to determine the crystallographic structure of natural and synthetic materials.

A beam of monochromatic (single wavelength) X-rays are focused on to the surface of a finely powdered sample.

The X-rays are scattered (diffracted) as they interact with the sample material, the angle of which is characteristic of the crystal lattice of the material analysed.

By rotating an  X-ray detector around the sample the angle and intensity of the resultant diffracted X-rays can be measured allowing for the identification of the mineral(s) present.

Current instrumentation

The Siemens D5000 Diffractometer (XRD) theta-2 theta goniometer with a copper anode x-ray tube, fixed slits , monochromator and a forty position sample changer which allows phase & mineral identification. DiffracPlus with the search/match option is used to collect and analyse the diffraction data.

The D2 Phaser is a compact, bench-top XRD.  It is fitted with a copper anode X-ray tube and a lynxeye detector, which simultaneously captures a large angual range, reducing measurement time and increasing sensitivity.

Applications

Powder XRD is used in many areas where the identification of unknown materials is required; these include geological, environmental, material science, biological and industrial applications.

Identification of mineral phases is made by comparison to extensive collections of reference data. For the interpretation of single phase material this process can be relatively simple. However, with increasing phases present this can become more complex, particularly with the overlay of one set of crystal peaks on another. It is often necessary to have element chemistry of the sample in order to refine search patterns (typically at the AAC we will suggest that if the chemistry cannot be supplied that we also perform a semi-quantitative XRF analysis.

Sample requirements

Samples must be crushed to a fine powder.

For further information contact Shane Askew