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School of Engineering and Science - Jacobs University

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feature was not recognized in early studies due to the negative anomaly present for<br />

neighboring Ce (e.g., de Baar et al., 1983). Positive Gd <strong>and</strong> Lu anomalies are also<br />

present in seawater REY patterns, though the magnitude <strong>of</strong> these anomalies are<br />

significantly smaller (see Fig. 6). The presence <strong>of</strong> positive La, Gd, <strong>and</strong> Lu anomalies<br />

was originally postulated to arise from a greater stability <strong>of</strong> the solution complexes for<br />

these elements, which presumably resulted from the exactly empty, half-filled, <strong>and</strong><br />

completely filled 4f electron shell configurations for La, Gd, <strong>and</strong> Lu, respectively (de<br />

Baar et al., 1985b). Early work by Cantrell <strong>and</strong> Byrne (1987), as shown in Fig. 7,<br />

predicted no anomalous behavior for these elements, though this study reported<br />

experimental data for only a few REY (e.g., Ce, Eu, Tb), which were then extrapolated<br />

across the entire REY series. More recent experimental studies (Luo <strong>and</strong> Byrne, 2004)<br />

determined equilibrium formation constants for carbonate complexes <strong>of</strong> all 15 REY,<br />

<strong>and</strong> these results are shown in Figure 9. Equilibrium constants for the formation <strong>of</strong><br />

monocarbonate REY complexes in high ionic strength solutions mimicking seawater do<br />

not vary smoothly across the REY series, with La, Gd, Y, <strong>and</strong> Lu showing the greatest<br />

deviations. Predominance diagrams for mono- <strong>and</strong> dicarbonate REY complexes in<br />

seawater also predict that La, Gd, Y, <strong>and</strong> Lu should fractionate from their immediate<br />

neighbors (Fig. 9).<br />

It is also likely that the observed positive La <strong>and</strong> Gd anomalies in seawater are to<br />

some degree generated during adsorption/desorption processes on scavenging particle<br />

surfaces. The authors Byrne <strong>and</strong> Kim (1990) <strong>and</strong> Lee <strong>and</strong> Byrne (1993) suggested that<br />

organic lig<strong>and</strong>s on particle surfaces (e.g., carboxylate) should discriminate against La<br />

<strong>and</strong> Gd, producing an enrichment <strong>of</strong> these elements in seawater. This would be<br />

consistent with the conclusions <strong>of</strong> Bau et al. (1999) regarding REY surface<br />

complexation on hydrous Fe-Mn oxides in seawater. It therefore appears that the La,<br />

18

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