1950
DOI: 10.1016/0371-1951(50)80017-6
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Die fluoreszenzspektren von uranmineralien im filtrierten ultravioletten licht

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Cited by 24 publications
(10 citation statements)
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“…[45] The information in this spectral region reveals the oxidation states of uranium and can fundamentally be used to fingerprint minerals containing uranium. [46,47] The absorption properties of U 4+ and U 6+ are well known. [45] The principal absorption bands of U 4+ are in the 22 000-8000 cm −1 region.…”
Section: Resultsmentioning
confidence: 99%
“…[45] The information in this spectral region reveals the oxidation states of uranium and can fundamentally be used to fingerprint minerals containing uranium. [46,47] The absorption properties of U 4+ and U 6+ are well known. [45] The principal absorption bands of U 4+ are in the 22 000-8000 cm −1 region.…”
Section: Resultsmentioning
confidence: 99%
“…It has been long known that some uranyl salts exhibit emission with distinctive spectral characteristics. [1][2][3][4][5][6][7][8][9][10][11][12] The literature reports that the emission wavelength and intensity are different for different uranyl compounds. 5,8,24,25,38,[45][46][47] The wavelength variability of different uranyl compounds has been attributed to the effect of ligands and of the media.…”
Section: Results and Discusssionmentioning
confidence: 99%
“…No interference was encountered from chloride, nitrate, or sulfate at 50-1 ratios. Because salicylidene-o-aminophenol had previously been prepared in this laboratory and formed a fluorescent chelate with aluminum (6), this type of ligand was chosen for the present series of experiments. Holzbecker (7,8) has also studied the 2,2'-dihydroxyazomethines and recommends salicylidene-oaminophenol as a reagent for aluminum.…”
Section: Resultsmentioning
confidence: 99%
“…Other fluorometric methods for the determination of uranium have employed silica gel (18), uranium-HCl complexes (8), changes in fluorescence intensity as a function of calcium (16) and chromium (17) concentration, UCI3 in LaCl3 (3), and direct measurements of the fluorescence of minerals (4,6). However, these determinations are no more desirable than the sodium fluoride method because of experimental complexities or, for silica gel (18), because it is only semiquantitative.…”
mentioning
confidence: 99%