Plaque mineralisation in vitro

Abstract

Dental calculus is plaque mineralised by deposition of calcium and phosphate resulting from interactions between the oral microbial plaque flora and components of oral fluids. An artificial-mouth microcosm dental plaque culture system has been developed to study aspects of plaque mineralisation, including pH control. Five plaques were grown from saliva under simulated oral conditions in a mucin-containing medium, and sucrose was applied to mimic meals. The plaques were mineralised with a urea-based, calcium-phosphate-monofluorophosphate-urea (CPMU) mineralising solution. Alkaline pH oscillations were generated by the plaques in response to CPMU applications, and an acidic oscillation followed sucrose applications. Plaque mineralisation by the CPMU procedure was almost totally dependent on the urea present in the mineralising solution, but total mineralisation also increased as the resting pH increased as a result of urea in the medium. Following four CPMU applications with a sucrose application every 12 hours improved plaque viability and mineralisation. The plaque mineral formed resembled a carbonated hydroxyapatite; other potential calcium phosphate minerals were undetectable except for calcium carbonate. A wide range of mineral deposition patterns in plaque were seen by electron microscopy.