Collaborative Research: Experimental determination of trace element diffusion rates in tooth enamel

合作研究：牙釉质中微量元素扩散速率的实验测定

• 批准号: 1561027
• 负责人: Matthew Kohn
• 金额: $ 17.07万
• 依托单位: Boise State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2016
• 资助国家: 美国
• 起止时间: 2016-05-01 至 2019-04-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1561027&HistoricalAwards=false
• 关键词: Collaborative; Research; Experimental; determination; trace

This project will investigate the rate of uptake of trace elements like barium, strontium, lead and the rare-earth elements (selected elements from lanthanum to lutetium) into tooth enamel. This project requires a key analytical technique "Secondary Ion Mass Spectrometry (SIMS)" because the spatial scale of measurement is so small. This research is important for understanding how trace elements are taken up in the human body and their fidelity in distinguishing individuals on timescales ranging from years to millions of years. The work will have implications for paleontology, archeology, toxicology and forensics, including the litigation of fossil theft. This funding will support the research and training of a PhD student. This research will be used to leverage educational opportunities for non-scientists in the Boise region and connect researchers unaware of how all areas of microchemical research can benefit from SIMS, a tool that is most commonly applied to semiconductors.The central focus of this project is to critically evaluate rates of diffusion of numerous trace elements in natural dental enamel. The research has been formulated to answer three main questions: How do diffusivities (D's) of trace elements in enamel depend on 1) charge vs. ionic radius and partitioning? 2) enamel orientation and enamel type? 3) fossilization state? To address these questions, uptake experiments will be conducted over a range of temperatures (4°, 20° and 37 °C) for a range of ions and ionic radii. D's will be measured in different directions for the two main enamel types in mammals - radial and decussate. Measurements in fossil enamel will be compared with similar measurements we make in modern enamel. The data will be inverted using standard diffusion equations, and natural datasets will be evaluated for their consistency (or not) with diffusion-limited uptake. The results will broadly constrain REE, uranium and alkaline element partition coefficients, which will improve models of diffusion rate and uptake of these geochemically- and toxicologically important elements. All data will be published rapidly in accessible international journals and/or archived in on-line geochemical databases. A PhD student will participate in a SIMS workshop, helping develop a community of SIMS users and present her work on fossils and fossilization to elementary school children and the public through established outreach programs.

该项目将调查微量元素如钡、锶、铅和稀土元素（从镧到镥的选定元素）进入牙釉质的吸收率。由于测量的空间尺度非常小，因此该项目需要一种关键的分析技术“二次离子质谱法”。这项研究对于了解微量元素如何在人体中吸收以及它们在从几年到数百万年的时间尺度上区分个体的保真度非常重要。这项工作将对古生物学、考古学、毒理学和法医学产生影响，包括化石盗窃诉讼。这笔资金将用于支持博士生的研究和培训。这项研究将被用来利用教育机会，为非科学家在博伊西地区和连接研究人员不知道如何所有领域的微量化学研究可以受益于西姆斯，一个工具，是最常用的半导体。该项目的中心重点是严格评估扩散率的许多微量元素在天然牙釉质。这项研究已经制定了回答三个主要问题：如何在搪瓷微量元素的扩散系数（D的）取决于1）电荷与离子半径和分区？2)牙釉质取向和牙釉质类型 3)石化状态？为了解决这些问题，将在一系列温度（4° C、20° C和37 °C）下对一系列离子和离子半径进行吸收实验。将在不同方向上测量哺乳动物中两种主要釉质类型的D-放射状和交叉状。我们将对化石釉质的测量结果与我们在现代釉质中所做的类似测量结果进行比较。将使用标准扩散方程对数据进行反演，并评价自然数据集与扩散限制摄取的一致性（或不一致性）。结果将广泛限制稀土元素，铀和碱性元素的分配系数，这将改善这些地球化学和毒理学重要元素的扩散速率和吸收模型。所有数据将迅速在可查阅的国际期刊上发表和/或在联机地球化学数据库中存档。一名博士生将参加一个西姆斯研讨会，帮助发展一个西姆斯用户社区，并通过既定的推广计划向小学生和公众展示她在化石和化石化方面的工作。