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Introduction

Neutrons are often pictured as tiny sub-atomic particles that make up approximately 50% of the mass of most atoms. However, due to the principle of wave-particle duality, neutrons also have a wavelength. The momentum, energy, spin, and lack of charge of the neutron makes it an ideal probe of the structure of matter. Neutrons were discovered many years after X-rays, and it was only after the development of nuclear reactors that intense beams of neutrons became viable for research use. The environmentally-friendly alternative to nuclear reactors for the production of intense beams of neutrons is the pulsed spallation source.

Crystal structure refinement from powder data was first developed for the case of neutron diffraction, resulting in the Rietveld method, which is still in use today. This section of the course explains why neutrons are used, together with powder neutron diffractometer design and function.

Neutron versus X-ray powder diffraction

Before discussing powder neutron diffraction in detail, a quick comparison with X-rays may be useful for those less familiar with the use of neutrons for powder diffraction studies. The figure below shows a typical laboratory data set of the mineral anglesite, PbSO4, collected with Cu Kα1 radiation in Bragg-Brentano geometry (to avoid absorption problems due to the lead atoms).

For comparison, a neutron diffraction pattern is shown of the same material collected on a constant wavelength medium-resolution powder diffractometer (D1A at the ILL, Grenoble) with a neutron wavelength equal to 1.909 Å.

There are several obvious differences: The remainder of this section will attempt to explain why some of these differences occur and how powder neutron diffraction experiments exploit them.


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© Copyright 1997-2006.  Birkbeck College, University of London. Author(s): Jeremy Karl Cockcroft