4.4 Article

Preparation of bone powder for FTIR-ATR analysis: The particle size effect

Journal

VIBRATIONAL SPECTROSCOPY
Volume 99, Issue -, Pages 167-177

Publisher

ELSEVIER
DOI: 10.1016/j.vibspec.2018.09.004

Keywords

Bone; FTIR-ATR; Sample preparation; Particle size; Bioapatite; Crystal order/disorder

Funding

  1. Onassis Foundation [F ZL 047-1/2015-2016]
  2. Leventis Foundation
  3. Greek Archaeological Committee UK (GACUK)
  4. Leverhulme Trust [PLP-2012-116]
  5. DNRF
  6. Laboratory of Mass Spectrometry and Gaseous Ion Chemistry (Rockefeller University)
  7. Brian Chait

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Fourier transform infrared (FTIR) spectroscopy using attenuated total reflection (ATR) is commonly used for the examination of bone. During sample preparation bone is commonly ground, changing the particle size distribution. Although previous studies have examined changes in crystallinity caused by the intensity of grinding using FTIR, the effect of sample preparation (i.e. particle size and bone tissue type) on the FTIR data is still unknown. This study reports on the bone powder particle size effects on mid-IR spectra and within sample variation (i.e. periosteal, mesosteal, trabecular) using FTIR-ATR. Twenty-four archaeological human and faunal bone samples (5 heated and 19 unheated) of different chronological age (Neolithic to post-Medieval) and origin (Belgium, Britain, Denmark, Greece) were ground using either (1) a ball-mill grinder, or (2) an agate pestle and mortar, and split into grain fractions ( > 500 mu m, 250-500 mu m, 125-250 mu m, 63-125 mu m, and 20-63 mu m). Bone powder particle size has a strong but predictable effect on the infrared splitting factor (IRSF), carbonate/phosphate (C/P) ratio, and amide/phosphate (Am/P) values. The absorbance and positions of the main peaks, the 2nd derivative components of the phosphate and carbonate bands, as well as the full width at half maximum (FWHM) of the 1010 cm(-1) phosphate peak are particle size dependent. This is likely to be because of the impact of the particle size on the short- and long-range crystal order, as well as the contact between the sample and the prism, and hence the penetration depth of the IR light. Variations can be also observed between periosteal, cortical and trabecular areas of bone. We therefore propose a standard preparation method for bone powder for FTIR-ATR analysis that significantly improves accuracy, consistency, reliability, replicability and comparability of the data, enabling systematic evaluation of bone in archaeological, anthropological, paleontological, forensic and biomedical studies.

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