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Titlebook: High-Pressure Crystallography; Andrzej Katrusiak,Paul McMillan Conference proceedings 2004 Springer Science+Business Media New York 2004 C

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樓主: 呻吟
51#
發(fā)表于 2025-3-30 10:26:22 | 只看該作者
An Introduction to Diamond Anvil Cells and Loading Techniquesr range, under simultaneous very high- or ultra low-temperature conditions, with implications for fields ranging from Earth and planetary science, to solid state physics and chemistry, and materials science [1–25]. The combination of such high pressure techniques with structure determination of soli
52#
發(fā)表于 2025-3-30 14:23:12 | 只看該作者
53#
發(fā)表于 2025-3-30 18:28:10 | 只看該作者
54#
發(fā)表于 2025-3-31 00:33:28 | 只看該作者
55#
發(fā)表于 2025-3-31 03:19:15 | 只看該作者
56#
發(fā)表于 2025-3-31 06:52:01 | 只看該作者
Computational High Pressure Sciencenment due to increasing electron density often results in structural instability (phase transition) and in unusual electronic properties such as supercoductivity. The task of theoretical calculation is to explain and predict the occurrence of these novel phenomena.
57#
發(fā)表于 2025-3-31 12:26:48 | 只看該作者
Theory of Minerals at High and Ultrahigh Pressures : Structure, Properties, Dynamics, and Phase Tranto ~6000 K). Studying the behaviour, properties, and structure of Earth-forming materials at such conditions allows one to understand better the properties of the Earth’s interior and provides clues to important geological problems. Experimental studies are often problematic at such conditions, and
58#
發(fā)表于 2025-3-31 13:46:35 | 只看該作者
59#
發(fā)表于 2025-3-31 19:45:14 | 只看該作者
Reverse Monte Carlo Modelling of Diffraction Data : Structural Studies of Amorphous Icesuced. Generalities concerning the application of RMC for molecular systems are discussed and then, the use of RMC for modelling structural disorder in crystals is mentioned. The second lecture will be devoted to the analyses of the structure of amorphous ices: the application of the Reverse Monte Ca
60#
發(fā)表于 2025-3-31 22:54:55 | 只看該作者
X-Ray Absorption Spectroscopy under Extreme Conditionse absorption edge that give rise to modern X-ray absorption spectroscopy (XAS) were already recorded; however, their analysis had to await a theoretical interpretation. This was finally achieved in the 1970’s, primarily through the work of E. Stern, D. Sayers and F. Lytle in Seattle [1], and it prov
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