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Updated: May 30, 2025

Synchrotron X-ray Microdiffraction and Fluorescence Imaging of Mineral and Rock Samples
Published on: June 19, 2018
Quantifying structural changes in organised biomineralized surfaces using synchrotron Polarisation-Induced Contrast
Hui Lynn Ooi1, Alexander Morrell1, Aaron LeBlanc1
1Faculty of Dentistry, Oral & Craniofacial Sciences, King's College London, United Kingdom.
We developed Calcium (Ca) K-edge Polarisation Induced Contrast X-ray Fluorescence (PIC-XRF) to quantify biomineral surface structure. This method enables repeated, minimally invasive analysis of hydroxyapatite (HAp) crystallite orientation and texture, crucial for regenerative strategies.
Area of Science:
- Biomineralization research
- Materials science
- Biophysics
Background:
- Quantitative characterization of biomineral surfaces is vital for regenerative medicine.
- Existing techniques for surface analysis have limitations, including extensive sample preparation, limited scale, and inability for repeated measurements.
Purpose of the Study:
- To develop Calcium (Ca) K-edge Polarisation Induced Contrast X-ray Fluorescence (PIC-XRF) for quantifying hydroxyapatite (HAp) crystallite structural arrangements.
- To address limitations of current techniques by enabling minimally prepared, repeated surface measurements.
- To analyze structural changes in biomineral surfaces, exemplified by human dental enamel.
Main Methods:
- Utilized Calcium (Ca) K-edge Polarisation Induced Contrast X-ray Fluorescence (PIC-XRF) with a focused monochromatic X-ray source.
- Measured minimally prepared human dental enamel at different rotational angles.
- Quantified crystallite orientations (principal and secondary) and texture in low and high textured surfaces.
Main Results:
- PIC-XRF successfully quantified HAp crystallite orientations and texture in human dental enamel.
- The technique identified crystallites oriented perpendicular to the surface, a challenge for other synchrotron methods.
- Detected significant structural modifications following short-term acid erosion, including shifts in crystallite orientation and reduced surface texture (p < 0.001).
Conclusions:
- PIC-XRF is a powerful tool for quantifying biomineral surface structure with minimal sample preparation.
- The method allows for monitoring of surface structural changes through repeated measurements.
- Findings suggest preferential dissolution of HAp based on crystallite orientation, offering insights for regenerative strategies.
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