Kinetic Consideration of Ca Transport and Associated Crystal Precipitation in an in vitro Precipitation Model Using Dialysis Membranes: Fluoride-dependent Regulation of Ca Concentration in Liquid Environment

M. Hattori, Y. Taya, Kaori Sato, T. Aoba
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引用次数: 1

Abstract

To elucidate how the fluid environment in forming enamel is modified by ion transport through the ameloblasts and associated extracellular events, we studied precipitation reactions in an experimental model utilizing a dialysis chamber. The experimental set-up comprised of upper and lower compartments, which were separated by a dialysis membrane of various cut-off sizes. Synthetic hydroxyapatite and pig enamel proteins were used as seeds and adsorbates, respectively. Seed crystals with or without proteincoating were placed in the lower compartment. Upon feeding the supersaturated solution (containing 1mM or 0.5mM Ca) in the upper compartment, Ca ion was allowed to diffuse into the lower compartment according to the existing concentration gradients. By monitoring time-sequential changes in Ca concentration in the lower solution, we found that Ca supply through the membrane was a rate-determining step, so the Ca concentration in the medium surrounding seed crystals became in proximity to the steady-state condition, under which the Ca concentration ([Ca] s) was maintained at lower levels than that of the supersaturated solution filling the upper compartment. The establishment of [Ca] s in the mineralizing milieu was speculated to be due to the kinetic difference between Ca supply and consumption for precipitation because [Ca] s levels were affected markedly by the presence of regulators (i. e., enamel proteins and fluoride) for precipitation. Notably, fluoride at 1ppm or lower levels exerted decreasing effects on [Ca] s, due to accelerating the precipitation kinetics and lowering the solubility of precipitated fluoridated crystals. The overall results obtained support the importance of the multitudinous physico-chemical processes in determin- ing the fluid composition surrounding forming enamel mineral.
透析膜体外沉淀模型中钙转运和相关晶体沉淀的动力学考虑:液体环境中钙浓度的氟化物依赖性调节
为了阐明形成牙釉质的流体环境是如何通过成釉细胞的离子运输和相关的细胞外事件来改变的,我们在一个利用透析室的实验模型中研究了沉淀反应。实验装置由上下隔间组成,由不同截止尺寸的透析膜分开。合成羟基磷灰石和猪牙釉质蛋白分别作为种子和吸附剂。有或没有蛋白包被的种子晶体放置在下室。将过饱和溶液(含1mM或0.5mM Ca)送入上腔室后,让Ca离子按照已有的浓度梯度向下腔室扩散。通过监测下层溶液中Ca浓度的时间序列变化,我们发现Ca通过膜的供应是一个速率决定步骤,因此种子晶体周围介质中的Ca浓度变得接近稳态条件,在此条件下,Ca浓度([Ca] s)保持在低于填充上层腔室的过饱和溶液的水平。[Ca] s在矿化环境中的形成被推测是由于沉淀中Ca供应和消耗之间的动力学差异,因为沉淀中的调节因子(即牙釉质蛋白和氟化物)的存在显著影响了[Ca] s水平。值得注意的是,1ppm或更低水平的氟化物对[Ca] s的影响越来越小,因为它加速了沉淀动力学,降低了沉淀的氟化晶体的溶解度。所获得的总体结果支持众多物理化学过程在确定形成珐琅质矿物周围流体成分中的重要性。
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