Driessens F C, Theuns H M, Heijligers H J, Borggreven J M
Dental Subfaculty, Catholic University, Nijmegen, The Netherlands.
Arch Oral Biol. 1986;31(12):837-40. doi: 10.1016/0003-9969(86)90138-x.
Six lesions were made on the buccal surfaces of premolars. The volume percentage of mineral was determined as a function of depth by microradiography. Using the electron microprobe, the signals for Ca, Na, Mg, P and Cl were recorded as a function of depth both through the lesions and through the adjacent sound enamel. In the demineralized parts, there was a preferential loss of Na and a preferential retention of chloride. In the surface layers, the Na:Ca and Cl:Ca ratios were almost the same as in the adjacent sound enamel, indicating that the surface layers were not formed by gross dissolution of the original mineral followed by gross reprecipitation of another, less-soluble calcium phosphate, but remained probably because their microcrystals were protected by a thin layer of precipitated fluorapatite or fluoridated hydroxyapatite. The same had been found for surface layers in natural caries.
在双尖牙的颊面制作了六个病损。通过显微放射照相术测定矿物质的体积百分比作为深度的函数。使用电子微探针,记录了钙、钠、镁、磷和氯的信号作为穿过病损以及穿过相邻健康釉质的深度的函数。在脱矿部分,钠优先流失,氯优先保留。在表层,钠钙比和氯钙比与相邻健康釉质几乎相同,这表明表层不是由原始矿物质的大量溶解,随后另一种难溶性磷酸钙的大量再沉淀形成的,而是可能由于其微晶受到一层沉淀的氟磷灰石或氟化羟基磷灰石薄层的保护而得以保留。在自然龋的表层也发现了同样的情况。