Abstract
The ultrastructural characteristics of bone mineral composition during vertebral development remain incompletely understood. This study investigated the crystallographic parameters of hydroxyapatite in L3 vertebrae, comparing samples from newborn (n = 12) and adult (n = 12) specimens. X-ray diffraction analysis was performed using a DRON-3 diffractometer with copper Kα radiation (λ = 0.15433 nm) operating at 30 kV and 20 mA. Diffraction patterns were recorded from 2° to 37° at 1°/min, focusing on the characteristic hydroxyapatite peaks in the 30-34° range. Unit cell parameters were calculated using the (211), (112), and (300) reflections, while crystallite sizes were determined using the Scherrer method. Results revealed significant differences in crystallographic parameters between age groups, with adult samples showing larger crystallite sizes (18.12 ± 0.87 nm vs. 8.92 ± 0.25 nm, p < 0.001) and more defined diffraction peaks. The hexagonal unit cell parameters also differed significantly, with mature bone exhibiting increased lattice parameters in both the a-axis (9.451 ± 0.014 Å vs. 9.391 ± 0.014 Å, p < 0.001) and c-axis length (6.891 ± 0.010 Å vs. 6.860 ± 0.017 Å, p < 0.001) compared to developing bone. While adult specimens showed trends toward greater crystallinity with lower amorphous calcium (-10.76 wt%) and higher crystalline calcium (+2.60 wt%), these differences did not reach statistical significance. These findings provide new insights into the maturation process of bone mineral structure and may contribute to understanding age-related changes in bone mechanical properties.