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- W2085281350 abstract "Ten trisdithiocarbamate compounds of arsenic, antimony and bismuth are studied by mass spectrometry. Their fragmentation modes and the fragment ions with common structures are discussed. The molecular ion peaks were not observed in all compounds. The highest mass number fragment ions, which might be generated directly from the molecular ions, are those with less mass units, equal to a dithiocarbamate group; signifing a facile detaching of one of the dithiocarbamato groups. The observed peaks are attributed, either to electron impact or to pyrolytic decomposition. The most prominent peaks, in the higher mass number region of all the spectra, correspond to polynuclear compounds of the general formula MnSm, where M = As, Sb, Bi; S = sulfur; n = 1, 2, 3, 4 and m = 0, 1, 2, 3, 4, 5. Massenspektren von Trisdithiocarbamaten. Massenspektroskopische Untersuchung von Trisdithiocarbamat-Komplexen des Arsens, Antomons und Wismuts Zehn Trisdithiocarbamat-Verbindungen von Arsen, Antimon und Wismut wurden massenspektrometrisch untersucht. Ihre Fragmentationsweise und die Fragment-Ionen mit gleichen Strukturen werden diskutiert. Die Peaks der Molekül-Ionen wurden von allen Verbindungen nicht beobachtet. Die Fragment-Ionen mit der größten Massen-Zahl, die direkt aus den Molekül-Ionen hervorgehen, sind diejenigen mit einer um eine Dithiocarbamat-Gruppe kleineren Masseneinheit, was eine leichte Abspaltung einer Dithiocarbamat-Gruppe andeutet. Die beobachteten Peaks sind auf Elektronenstoß oder auf pyrolytische Zersetzung zurückzuführen. Die stärksten Peaks im oberen Massenzahl-Bereich aller Spektren entsprachen Polynuklear-Verbindungen der allgemeinen Formel MnSm, wobei M = As, Sb, Bi; S = Schwefel; n = 1, 2, 3, 4 und m = 0, 1, 2, 3, 4, 5 sind." @default.
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- W2085281350 date "1974-01-01" @default.
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- W2085281350 title "Trisdithiocarbamates mass spectra mass spectra. Study of arsenic, antimony and bismuth Trisdithiocarbamate Complexes" @default.
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- W2085281350 doi "https://doi.org/10.1002/zaac.19744030111" @default.
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