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Micro spatial distributions of lead andzinc in human deciduous tooth enamel

机译:人落叶牙釉质中铅锌的微空间分布

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Enamel is the hard crystalline external covering of teeth, and has a mineralcomponent that closely resembles hydroxyapatite (Boyde, 1989; Brudevoldand Soremark, 1967). The chemical constituents of hydroxyapatite are toler-ant to substitution by a range of trace elements, and are readily incorporatedinto enamel formation at the time of environmental exposure. The composi-tion of sub-surface enamel is fixed before tooth emergence, and is thereforeable to provide a retrospective and relatively permanent record of the traceelements absorbed during the period of enamel formation. The informationlocked within this deep enamel can provide evidence of early nutrition, res-idential mobility, and exposure to toxic metals. The incorporation of sometrace elements into enamel hydroxyapatite also has the potential to affect sus-ceptibility to caries. The trace element composition of enamel has a broadrelevance in disciplines ranging from dentistry and child health (Brown et al.,2004; Dolphin et al., 2005) to forensics (Gulson et al., 1997a) and archaeology(Budd et al., 2000). Two trace elements of particular interest are lead (Pb) andzinc (Zn).
机译:牙釉质是牙齿的硬结晶外部覆盖物,并且具有与羟基磷灰石密切类似的无机组成(Boyde,1989; Brudevoldand Soremark,1967)。羟基磷灰石的化学成分是耐于含量的耐受一系列痕量元素,并且在环境暴露时容易掺入丁香烯烃形成。在牙齿出现之前固定亚表面釉质的组合物,并且不必提供在牙釉质期间吸收的排列的回顾性和相对永久的记录。这种深层搪瓷内的综合锁定可以提供早期营养,res-entivion的流动性和暴露于有毒金属的证据。将有些元素掺入搪瓷羟基磷灰石中也有可能影响龋齿的粘连。搪瓷的痕量元素组成在牙科和儿童健康范围内具有广泛的学科(Brown等,2004; Dolphin等,2005)到法医(Gulson等,1997a)和考古学(Budd等, 2000)。特别兴趣的两种微量元素是铅(Pb)znzinc(Zn)。

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