Aoba T, Shimoda S, Moreno E C
Forsyth Dental Center, Boston, Massachusetts 02115.
J Dent Res. 1992 Nov;71(11):1826-31. doi: 10.1177/00220345920710111201.
The present study was undertaken to assess the labile or surface pools of Mg, Na, and K ions in porcine enamel tissues at various developmental stages. The enamel samples, corresponding to the outer and the inner secretory, the early maturing, and the mature hard enamel, were dissected from the labial sides of permanent incisors of 6- to 8-month-old piglets. Each enamel sample was extracted successively with solutions of de-ionized water and 50 mmol/L Tris-4 mol/L guanidine buffer (for removal of organic matrix proteins, mainly amelogenins). The labile (free or organically bound) pools of Mg, Na, and K were assessed by the total amounts of these ionic species extracted by the water and Tris-guanidine buffer. The surface (adsorbed onto enamel mineral) pool of Mg was assessed directly by determination of the adsorption of Mg onto enamel mineral at various developmental stages. The results showed that: (i) 30-40% of the Mg in the secretory and early maturation enamel was in the surface pool (adsorbed onto the enamel mineral); (ii) 25 to 40% of the total sodium in the enamel samples was in labile forms; and (iii) most (around 70-80%) of the total potassium was readily extracted in water and appeared to originate from the enamel fluid; only marginal portions remained in the solids. The present adsorption studies also indicated that the maximum uptake of magnesium in the early maturation enamel was due mostly to an increase of the occupancy by Mg ions of adsorption sites on the crystal surfaces, which become accessible with a massive removal of enamel matrix proteins.(ABSTRACT TRUNCATED AT 250 WORDS)
本研究旨在评估猪牙釉质组织在不同发育阶段中镁、钠和钾离子的不稳定或表面池。从6至8月龄仔猪的恒切牙唇侧切取对应于外分泌和内分泌、早期成熟和成熟硬牙釉质的牙釉质样本。每个牙釉质样本依次用去离子水和50 mmol/L Tris - 4 mol/L胍缓冲液(用于去除有机基质蛋白,主要是釉原蛋白)进行提取。通过水和Tris - 胍缓冲液提取的这些离子种类的总量来评估镁、钠和钾的不稳定(游离或有机结合)池。通过测定不同发育阶段镁在牙釉质矿物质上的吸附量直接评估镁的表面(吸附在牙釉质矿物质上)池。结果表明:(i)分泌期和早期成熟牙釉质中30 - 40%的镁存在于表面池(吸附在牙釉质矿物质上);(ii)牙釉质样本中25%至40%的总钠呈不稳定形式;(iii)大部分(约70 - 80%)的总钾易于在水中提取,似乎源自牙釉质液;只有少量部分保留在固体中。目前的吸附研究还表明,早期成熟牙釉质中镁的最大吸收量主要是由于晶体表面吸附位点上镁离子占据率的增加,随着牙釉质基质蛋白的大量去除,这些位点变得可及。(摘要截短于250字)