Néri G A
SSO Schweiz Monatsschr Zahnheilkd. 1978 May;88(5):469-85.
A study of the mineral substance of human dental cementum was made by various biophysical methods. In healthy teeth, average degree of mineralization of the cementum as well as crystallinity and fluoride content of its mineral substance, were found to increase as a function of age. This evolution, typical of the physiological ageing process of calcified tissues, is especially pronounced for the cementum, because of the absence of remodeling activity such as that occuring in bone tissue. Cementum of impacted or semi-impacted teeth was found to have a significantly lower degree of mineralization than that of sound teeth in occlusion. In periodontally diseased teeth, the increase in crystallinity and degree of mineralization of the cementum as a function of age is considerably greater than that observed in healthy teeth. These changes were found to affect the cervical cement first of all, and progressively, the entire tissue. No difference was observed, however, in the fluoride content of the cement of periodontally diseased teeth and healthy teeth of the same age.
采用多种生物物理方法对人牙骨质的矿物质进行了研究。在健康牙齿中,发现牙骨质的平均矿化程度及其矿物质的结晶度和氟含量随年龄增长而增加。这种演变是钙化组织生理老化过程的典型特征,对于牙骨质尤为明显,因为它缺乏像骨组织中发生的那种重塑活动。发现阻生或半阻生牙的牙骨质矿化程度明显低于正常咬合的健康牙齿。在牙周病牙齿中,牙骨质的结晶度和矿化程度随年龄的增加比在健康牙齿中观察到的要大得多。这些变化首先影响颈部牙骨质,并逐渐影响整个组织。然而,在相同年龄的牙周病牙齿和健康牙齿的牙骨质氟含量方面未观察到差异。