Comunicato stampa

Learning from meteorites to improve bone replacements

08/04/2021

Whitlockite structure: view of the (T(1)O3OH) group split along c axis; details of O10-H10...O1 hydrogen bond; coordination of O1 atom.
Whitlockite structure: view of the (T(1)O3OH) group split along c axis; details of O10-H10...O1 hydrogen bond; coordination of O1 atom.

Whitlockite, which has the ideal formula Ca9Mg(PO4)6[PO3(OH)], is a rare natural calcium phosphate found in granite rocks. It is retrieved also in chondritic meteorites, along with its de-hydrogenated analogue, the mineral merrillite (the most important reservoir of phosphate phosphorous in the Solar System), making it a natural phase largely studied in planetary science.

However, it’s not just space scientists that find whitlockite interesting; this mineral, is the natural counterpart of the synthetic biomaterial tricalcium phosphate (TCP), chemically Ca3(PO4)2, largely employed in dentistry and orthopaedics such as cements, scaffolds and coatings. 

By studying the structure of these natural materials, scientists can improve the synthetic versions to better adapt to the expected function in medical applications. In particular, TCP is an alternative to the synthetic hydroxyapatite Ca5(PO4)3OH, which is very similar to the mineral part of human teeth and bones, but is too brittle to be used for some biomedical applications, on all within prosthetic implants.

 Any synthetic implants are also at risk from rejection from the body. The information gathered by studing the natural material can be used to modify the synthetic materials in order to reduce both brittleness and rejection rates, therefore improving their overall performance. 

When whitlockite was originally characterised in 1972, the technical equipment was not of high enough standard to get extremely accurate data. This study, published in Crystals, is the first to measure the structure with higher accuracy, using the unique capability of neutron diffraction to locate the hydrogen atoms within the mineral. 

A sample of the mineral from the Palermo mine in the USA was sent to the SXD instrument at ISIS, after preliminary investigations using X-ray diffraction, where it underwent neutron diffraction measurements. These measurements allowed the completion of the structural investigation by establishing the hydrogen bonding network within the mineral. The sample was also studied by electron microprobe analysis to confirm the chemical content, and for the first time on this mineral, by infrared spectroscopy to complement the diffraction results.

Rome 8 April 2021

In brief

Who: Istituto di cristallografia (Cnr-Ic), Sapienza Università di Roma, Università Roma Tre, ISIS Neutron and Muon Source (Didcot, U.K.)
What: Neutron and XRD single-crystal diffraction study and vibrational properties of whitlockite, the natural counterpart of synthetic tricalcium phosphate, Crystals 2021, 11(3), 225; https://doi.org/10.3390/cryst11030225
For information: Francesco Capitelli, Cnr-Ic, francesco.capitelli@ic.cnr.it

Per informazioni:
Francesco Capitelli
CNR - Istituto di cristallografia
francesco.capitelli@ic.cnr.it
0690672616

Ufficio stampa:
Alessia Cosseddu
Cnr - Ufficio stampa
alessia.cosseddu@cnr.it

Capo ufficio stampa:
Marco Ferrazzoli
marco.ferrazzoli@cnr.it
ufficiostampa@cnr.it
06 4993 3383

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