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A teaching exercise to introduce stable isotope fractionation of metals into geochemistry courses

机译:将金属的稳定同位素分馏引入地球化学课程的教学练习

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Variations in the isotopic composition of elements have been widely used to study earth's climate, biosphere, and interior, and more recently to track the fate of contaminants. Within the broad range of elements that exhibit measureable isotopic variations, metal stable isotopes are increasingly applied across the biological, geological, environmental, and chemical sciences. Mass spectrometry and the isotope (geo-) chemistry of metals, often termed non-traditional stable isotopes, are not yet regularly taught in university courses. However, their growing importance in the natural sciences is reflected in the increasing number of research papers published. We present here a novel teaching exercise that can be incorporated into a curriculum where the stable isotope (geo-) chemistry of more traditional stable isotope systems (e.g., C, H, N, O, S) or inorganic mass spectrometry is taught. The exercise first introduces the basics of metal stable isotope fractionation. Next, the students use scientific papers to develop spreadsheets that enable them to program equations, to test isotope fractionation models, and to interpret environmental processes.
机译:元素同位素组成的变化已广泛用于研究地球的气候,生物圈和内部,最近还用于追踪污染物的归宿。在表现出可测量的同位素变化的多种元素中,金属稳定同位素越来越多地应用于生物学,地质学,环境学和化学科学。质谱和金属的同位素(地球化学),通常被称为非传统稳定同位素,尚未在大学课程中定期教授。然而,它们在自然科学中日益重要的地位反映在越来越多的研究论文上。我们在这里提出一种新颖的教学练习,可以将其纳入课程中,在该课程中教授更传统的稳定同位素系统(例如C,H,N,O,S)或无机质谱法的稳定同位素(地球化学)。本练习首先介绍金属稳定同位素分馏的基础知识。接下来,学生使用科学论文来开发电子表格,使他们能够编程方程式,测试同位素分馏模型以及解释环境过程。

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