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Titlebook: Deuterium and Shift Calculation; U. Fleischer,W. Kutzelnigg,M. Schindler Conference proceedings 1991 Springer-Verlag Berlin Heidelberg 199

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11#
發(fā)表于 2025-3-23 13:25:16 | 只看該作者
12#
發(fā)表于 2025-3-23 16:16:38 | 只看該作者
Smart Mobility and Geodesign in Urban Lifedensity is pointed out. The gauge origin problem and its solution by means of the IGLO method is explained. Various methods for the calculation of chemical shifts are compared and the IGLO method is presented in detail both as far as computations and interpretation of the result are concerned.
13#
發(fā)表于 2025-3-23 20:22:20 | 只看該作者
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發(fā)表于 2025-3-24 00:13:05 | 只看該作者
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發(fā)表于 2025-3-24 10:18:07 | 只看該作者
0170-5989 cts. Because of the unique mass relation between the different hydrogen isotopes hydrogen/deuterium isotope effects are particularly large and have attracted mo978-3-642-75934-5978-3-642-75932-1Series ISSN 0170-5989
17#
發(fā)表于 2025-3-24 11:09:34 | 只看該作者
Shlomit Flint Ashery,Yossi Katzements—the question arises whether this method can also be a useful kinetic tool in the chemistry of hydrogen isotopes. The scope of this review is to show that dynamic NMR spectroscopy can indeed contribute to the development of the field of isotopic reaction kinetics. Certain kinetic isotope effects can even only be observed using this method.
18#
發(fā)表于 2025-3-24 15:49:22 | 只看該作者
Dynamic NMR Spectroscopy in the Presence of Kinetic Hydrogen/Deuterium Isotope Effects,ements—the question arises whether this method can also be a useful kinetic tool in the chemistry of hydrogen isotopes. The scope of this review is to show that dynamic NMR spectroscopy can indeed contribute to the development of the field of isotopic reaction kinetics. Certain kinetic isotope effects can even only be observed using this method.
19#
發(fā)表于 2025-3-24 19:31:24 | 只看該作者
20#
發(fā)表于 2025-3-25 02:08:27 | 只看該作者
0170-5989 t the electrolysis oflight water is faster than of heavy water [1,2]. This success showed that although different isotopes of an element behave identically from a chemical standpoint the different isotopic masses nevertheless lead to both isotope effects on equilibrium as well as on rate constants o
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