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穆斯堡尔效应的应用十分广泛,己应用于物理学、化学、生物和医学,材料科学,环境科学、矿物地质学、考古学以及工业技术等各个研究领域。对于铁来说,已经形成哪里有铁,哪里就有穆斯堡尔谱学的研究局面。1964年Sprenkel—Segel等人使用穆斯堡尔效应首先研究了石陨石,开创了穆斯堡尔谱学在陨石地质学中应用的新局面。陨石是稀有的标本,它对于研究太阳系的形成和演化,生命的起源,空间技术等方面都有重大的科学价值。由于穆斯堡尔谱学具有相当高的能量分辨率,能直接观察和研究超精细结构,因而成为陨石地质学研究中的一种重要的手段。
Mossbauer effect is widely used and has been applied in various fields such as physics, chemistry, biology and medicine, material science, environmental science, mineralogy, archeology and industrial technology. For iron, where iron has been formed, there is a study of Mossbosch. In 1964, Sprenkel-Segel et al. First studied the meteorite using the Mössbauer effect and started the new situation of the application of Mössbauer spectroscopy in meteorite geology. Meteorite is a rare specimen, which is of great scientific value in studying the formation and evolution of the solar system, the origin of life, and space technology. Due to its relatively high energy resolution, Mössbauer spectroscopy can directly observe and study the ultrafine structure, which has become an important method in the research of meteorite geology.