Late stages of mineralisation and their signature on the bone mineral density distribution

TL;DR

This study uses computational models to investigate late-stage bone mineralisation, revealing that mineralisation continues gradually beyond previously assumed limits and highlighting differences between bone types.

Contribution

It introduces an extended BMDD model accounting for variable maximum calcium capacities to better understand late mineralisation stages in bone.

Findings

Mineralisation does not stop abruptly but continues slowly beyond 30 wt% Ca.

Tuning maximum calcium capacity alone cannot explain differences between trabecular and cortical bone BMDDs.

Smooth decrease in mineralisation rate better matches experimental data than abrupt stopping.

Abstract

Purpose: Experimental measurements of bone mineral density distributions (BMDDs) enable a determination of secondary mineralisation kinetics in bone, but the maximum degree of mineralisation and how this maximum is approached remain uncertain. We thus test computationally different hypotheses on late stages of bone mineralisation by simulating BMDDs in low turnover conditions. Materials and Methods: An established computational model of the BMDD that accounts for mineralisation and remodelling processes was extended to limit mineralisation to various maximum calcium capacities of bone. Simulated BMDDs obtained by reducing turnover rate from the reference trabecular BMDD under different assumptions on late stage mineralisation kinetics were compared with experimental BMDDs of low-turnover bone. Results: Simulations show that an abrupt stopping of mineralisation near a maximum calcium capacity induces a pile-up of minerals in the BMDD statistics that is not observed experimentally. With a smooth decrease of mineralisation rate, imposing low maximum calcium capacities helps to match peak location and width of simulated low turnover BMDDs with peak location and width of experimental BMDDs, but results in a distinctive asymmetric peak shape. No tuning of turnover rate and maximum calcium capacity was able to explain the differences found in experimental BMDDs between trabecular bone (high turnover) and femoral cortical bone (low turnover). Conclusions: Secondary mineralisation in human bone does not stop abruptly, but continues slowly up to a calcium content greater than 30 wt% Ca. The similar mineral heterogeneity seen in trabecular and femoral cortical bones at different peak locations was unexplained by turnover differences tested.