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COPRECIPITATION IN SOME BINARY SYSTEMS OF RARE EARTH OXALATES

Journal Article · · Analytical Chemistry (U.S.) Formerly Ind. Eng. Chem., Anal. Ed.
DOI:https://doi.org/10.1021/ac60142a007· OSTI ID:4286366
On the basis of an equilibrium model, the distribution coefflcient, h, in the Doerner-Hoskine equation should be functionally related to the solubility products of the coprecipitating species. 1n the case of the rare earth oxalates, the coefficient should be equal to the square root of the ratio of the solubility products. The neodymium-cerium, yttrium-cerium, and ytterbiumneodymium systems were studied. These systems obeyed the Doerner- Hoskins relationship in that the distribution coefficient, lambda , was constant over the range 0 to 100% of the host crystal precipitated; when the mole ratio composition of the solid phase of the neodymium-cerium system was varied over a 106 range, lambda also remained constant. However, the equilibrium model does not appear to be valid because there is no correlation between lambda and the solubility product ratio. It appears likely that the value of the distribution coefficient is determined by the kinetics of the precipitation process rather than the solubilities of the substances. (auth)
Research Organization:
Brookhaven National Lab., Upton, N.Y.; Syracuse Univ., N.Y.
Sponsoring Organization:
USDOE
NSA Number:
NSA-13-001139
OSTI ID:
4286366
Journal Information:
Analytical Chemistry (U.S.) Formerly Ind. Eng. Chem., Anal. Ed., Journal Name: Analytical Chemistry (U.S.) Formerly Ind. Eng. Chem., Anal. Ed. Vol. Vol: 30; ISSN ANCHA
Country of Publication:
Country unknown/Code not available
Language:
English

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