Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed Oxalate

Thermodynamic modelling of a leaching system that involves concurrent precipitation depends on an understanding of how the metals distribute into the precipitate before an assessment of solubility can be made. It has been suggested in the past that a pair of rare earths (A and B) in solution will se...

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Main Authors: Harry Watts, Yee-Kwong Leong
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/10/8/712
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author Harry Watts
Yee-Kwong Leong
author_facet Harry Watts
Yee-Kwong Leong
author_sort Harry Watts
collection DOAJ
description Thermodynamic modelling of a leaching system that involves concurrent precipitation depends on an understanding of how the metals distribute into the precipitate before an assessment of solubility can be made. It has been suggested in the past that a pair of rare earths (A and B) in solution will separate from each other by oxalate precipitation according to a logarithmic distribution coefficient (<inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula>), determined by the kinetics of the precipitation. By contrast, the present study hypothesises that <inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula> may be approximated from thermodynamic terms, including the solubility product (K<sub>Sp</sub>) of each rare earth oxalate and the stability constant (<inline-formula><math display="inline"><semantics><mrow><msub><mi mathvariant="sans-serif">β</mi><mn>1</mn></msub><mo stretchy="false">)</mo></mrow></semantics></math></inline-formula> for the mono-oxalato complex of each rare earth. The proposed model was used to calculate <inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula> between pairs of rare earths. An experimental study was conducted to determine <inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula> between selected pairs using homogenous precipitation through the hydrolysis of an oxalic acid ester, with fairly close agreement to the values under the proposed model. Though this model requires more thorough testing, as well as application to other organic salts, it may provide insight into distribution factors of a precipitate formed by a sequence of organic complexes.
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spelling doaj.art-33051a7d7bf442a6bfa833a0b7e07a372023-11-20T09:51:42ZengMDPI AGMinerals2075-163X2020-08-0110871210.3390/min10080712Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed OxalateHarry Watts0Yee-Kwong Leong1Department of Chemical Engineering, University of Western Australia, Crawley, WA 6009, AustraliaDepartment of Chemical Engineering, University of Western Australia, Crawley, WA 6009, AustraliaThermodynamic modelling of a leaching system that involves concurrent precipitation depends on an understanding of how the metals distribute into the precipitate before an assessment of solubility can be made. It has been suggested in the past that a pair of rare earths (A and B) in solution will separate from each other by oxalate precipitation according to a logarithmic distribution coefficient (<inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula>), determined by the kinetics of the precipitation. By contrast, the present study hypothesises that <inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula> may be approximated from thermodynamic terms, including the solubility product (K<sub>Sp</sub>) of each rare earth oxalate and the stability constant (<inline-formula><math display="inline"><semantics><mrow><msub><mi mathvariant="sans-serif">β</mi><mn>1</mn></msub><mo stretchy="false">)</mo></mrow></semantics></math></inline-formula> for the mono-oxalato complex of each rare earth. The proposed model was used to calculate <inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula> between pairs of rare earths. An experimental study was conducted to determine <inline-formula><math display="inline"><semantics><mi mathvariant="sans-serif">λ</mi></semantics></math></inline-formula> between selected pairs using homogenous precipitation through the hydrolysis of an oxalic acid ester, with fairly close agreement to the values under the proposed model. Though this model requires more thorough testing, as well as application to other organic salts, it may provide insight into distribution factors of a precipitate formed by a sequence of organic complexes.https://www.mdpi.com/2075-163X/10/8/712rare earthsdistribution factorselective precipitationoxalatesorganic complexes
spellingShingle Harry Watts
Yee-Kwong Leong
Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed Oxalate
Minerals
rare earths
distribution factor
selective precipitation
oxalates
organic complexes
title Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed Oxalate
title_full Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed Oxalate
title_fullStr Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed Oxalate
title_full_unstemmed Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed Oxalate
title_short Predicting the Logarithmic Distribution Factors for Coprecipitation into an Organic Salt: Selection of Rare Earths into a Mixed Oxalate
title_sort predicting the logarithmic distribution factors for coprecipitation into an organic salt selection of rare earths into a mixed oxalate
topic rare earths
distribution factor
selective precipitation
oxalates
organic complexes
url https://www.mdpi.com/2075-163X/10/8/712
work_keys_str_mv AT harrywatts predictingthelogarithmicdistributionfactorsforcoprecipitationintoanorganicsaltselectionofrareearthsintoamixedoxalate
AT yeekwongleong predictingthelogarithmicdistributionfactorsforcoprecipitationintoanorganicsaltselectionofrareearthsintoamixedoxalate