REE partitioning between Fe-Mn oxyhydroxide precipitates and weakly acid NaCl solutions: Convex tetrad effect and fractionation of Y and Sc from heavy lanthanides
Iwao Kawabe, Atsuyuki Ohta, Satoru Ishii, Maki Tokumura, Kazue Miyauchi
Geochemical Journal, Vol. 33, No. 3, P. 167-179, 1999
ABSTRACT
Distribution coefficients of Kd (REE: ppt./sol.) with REE = lanthanides (Ln), Y, and Sc between Fe-Mn oxyhydroxide precipitates and NaCl solutions have been determined in pH = 5.4-6.4 at room temperature and atmospheric pressure. The logKd(Ln) values show convex tetrad effect variations across the series and positive Ce anomalies. Kd(Y) values are significantly lower than those for Ho and Er, whereas Kd(Sc) values are higher than those for Lu. Behaviors of Y3+ and Sc3+ are distinct from heavy Ln3+ when REE coprecipitate with Fe-Mn oxyhydroxides in weakly acid solutions. The observed convex tetrad effect variations of logKd(Ln) are commonly modified from theoretically expected ones in light Ln and heavier Ln. The variations of logKd(Ln) across the series are related to {ΔGof(Ln3+, aq)-ΔGof(Ln(OH)3.nH2O) } for the following reactions between Ln3+(aq) and Ln(OH)3.nH2O as precipitate: Ln(OH)3.nH2O(ss) + 3H+(aq) = Ln3+(aq) + (3 + n)H2O(l). Hence, the variations of logKd(Ln) reflect (i) the tetrad effect originating from differences in Racah E1 and E3 parameters for 4f electron repulsion in Ln3+ ions between the two Ln(III) series, and (ii) the changes of coordination states of Ln3+ ions in the respective Ln(III) complex series. The structural changes of the first-coordination spheres of Ln3+ ions in light Ln3+(aq) and heavy Ln(OH)3.nH2O series make the series variation of logKd(Ln) irregular. When we correct the logKd(Ln) values for the structural changes, they become regular tetrad effect variations compatible with the refined spin-pairing energy theory. Racah parameters for 4f electron repulsion in Ln3+ ions of octahydrate Ln3+(aq) series are inferred to be larger than those of Ln(OH)3.nH2O.
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