The neocupferron titration curve illustrates the same mode of behavior, although somewhat less clearly. High-frequency titration of praseodymium chloride verifies the intermediate formation of the 1 to 1 complexes, MCup + + and M(NeoCup) + t.
CONCLUSIONSCupferron and neocupferron seem to be excellent precipitating agents for the rare earth ions, provided that no interfeiing substances are present in the solution. Since cupferron and neocupferron are fairly general precipitating agents for many metal ions, it is obvious that they cannot compete with oxalic acid when the rare earth ions are to be separated from other impurities. However, in the absence of impurities and when only a small amount of rare earth is present in solution (2 to 50 mg.), the relatively large volume of precipitate and the ease with which it can be washed and filtered make the determination somewhat more accurate than the oxalate precipitation.Apparently, under precipitation conditions describe here, considerable amount of coprecipitation makes it impossible to determine accurately the amount of the rare earth present from the weight of the dried precipitate. However, ignition to the oxide is rapid and yields very satisfactory results.
ACKNOWLEDGMENTThe assistance of George E. Knudson in obtaining the absorption spectra of the rare earth solutions is gratefully acknowledged.