Abstract:20) Reference 18 shows that the first process is slow. The fraction of the enol isomer of 0-diketones is often measured by bromine titration; consequently, the isomerization must be slow.
“…In the case of fluorine or chlorine substitution, air stability is also enhanced, but not as greatly.3•14 Also, in monofluoro and polyfluoro cases explosive character has been encountered.9 •14 In fact, when more than two fluorines are attached to the arene ligand, only unstable, very explosive chromium complexes are obtained. 14 Apparently the aryl fluorines are quite labile, and on decomposition Cr-F (or V-F) bonds are formed in a very exotherriiic process. (Workers should be wary of this possible behavior in any organohalogenated complexes of this type.)…”
“…In the case of fluorine or chlorine substitution, air stability is also enhanced, but not as greatly.3•14 Also, in monofluoro and polyfluoro cases explosive character has been encountered.9 •14 In fact, when more than two fluorines are attached to the arene ligand, only unstable, very explosive chromium complexes are obtained. 14 Apparently the aryl fluorines are quite labile, and on decomposition Cr-F (or V-F) bonds are formed in a very exotherriiic process. (Workers should be wary of this possible behavior in any organohalogenated complexes of this type.)…”
“…La plupart des monocarboxylates des terres rares 6tudiCs 8. ce jour sont des hydroxy-1-carboxylates [2]. I1 a CtC montrk qu'en solution aqueuse ces complexes sont des chClates [3]. Par contre, il n'existe @re d'informations sur les hydroxy-2carboxylates.…”
Section: Stabilitc Des Carboxylates De Terres Rares 111)unclassified
1873thermostatted chromium trioxide solution was added and the mixture stirred with a glass rod. Liquid samples were added directly by means of a syringe to the chromium trioxide solution in the cell. The concentration of chromium (VI) at the beginning of all kinetic runs was ca. 5 x 1 0 -4~. A t least a ten-fold excess of organic substrate was used for the determination of first-order rate constants.Under the conditions employed solvent oxidation was found to be negligible. The disappearance of chromium (VI) was followed by continuously measuring the absorbance at 350 nm. Good straight lines were obtained, plotting log ( A -A m ) against time. The second-order rate constants were calculated by division of the pseudo-first-order rate constants with the initial concentration of organic substrate. The values given are averages from 3 to 6 runs and were reproducible to 5%.Summary. The stability constants of 2,2-bis-hydroxymethyl-propionates of rare earths have been determined a t ionic strength 0,100 (NaC10,) at 25.0" C by a potentiometric method. The ligand forms 1 : 1 and 1 : 2 complexes with all the rare earths and weak 1 : 3 complexes with light rare earths only. In these last complexes, it binds in a unidentate way. The dissociation constant of the acid has also been measured.
“…- (4,30 . 10-3[I.-]), pK,, = 2,98 (p = 0,100, NaC10,) ; en corrigeant cette valeur B l'aide cle la relation de DAVXES r61, on obtient la constante thermodynamique (p + 0) : p t I<" = 3,198 (3,164 selon LUMNE 171).…”
Section: Stabilitk Des Carboxylates De Terres Rares I Furanne-unclassified
The stability constants of 2‐furanecarboxylates and 2‐thiophencarboxylates of some rare earths have been determined at ionic strength 0.100 (NaClO4) at 25.0°C by a potentiometric method. The ligands form 1 : 1 complexes similar to the rare earths propionates.
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