How does XRF work ?
X-ray Fluorescence (XRF) is based on the interaction between high-energy radiation and atoms within a material. When a sample is irradiated, inner-shell electrons are ejected from their orbitals. As the atom returns to a stable state, electrons from higher energy levels move down to fill these vacancies. During this relaxation process, characteristic X-ray fluorescence is emitted. Importantly, this entire mechanism occurs without physically altering or damaging the sample.
The emitted fluorescent X-rays are unique to each element—much like an atomic fingerprint. For example, the fluorescence signature of copper is distinctly different from that of zinc or any other element in the periodic table. This uniqueness makes XRF one of the most direct, reliable, and user-friendly techniques for elemental analysis. It has therefore become widely adopted across industrial, research, and educational environments.
XRF data can provide qualitative identification, semi-quantitative estimation, or fully quantitative determination of elemental composition. It is capable of analyzing major constituents, minor components, and even trace-level elements within a wide range of materials.