The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.
The fractionation between Y and Ho in the marine environment
Abstract
Abstract New measurements of Y and Ho in seawater, rivers and rain are presented. Based on the data and a two-box model calculation, we suggest that fractionation between Y and Ho takes place during their removal by particulate matter from the surface ocean to the deep sea. The fractionation factor, K D is calculated to be 0.50, implying that Ho is scavenged two times faster than Y. This presumably occurs due to differences between Y and Ho complexation behavior with respect to seawater inorganic ligands (mainly carbonate ions) and soft organic ligands (though unspecified) of the surface of particulate matter. Fractionation of Y and Ho during weathering and fluvial transport to the ocean appears to have minor influence on the relative abundance of Y and Ho in seawater. We also estimated the mean oceanic residence time to be 5100 years for Y and 2700 years for Ho. Y is less effectively scavenged from seawater than any of the trivalent rare earth elements and theY/Ho ratio in seawater is higher than those in rain, rivers and estuarine waters.
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Citations
Cites
The comparative behaviors of yttrium and lanthanides in the seawater of the North Pacific
Zhang, J., Amakawa, H., & Nozaki, Y. (1994) · Geophysical Research Letters · doi:10.1029/94gl02404 · Cited by 161
Precise determination of variations in the ratios of marine ferromanganese nodules
Amakawa, H., Nozaki, Y., & Masuda, A. (1996) · Chemical Geology · doi:10.1016/0009-2541(96)00066-6 · Cited by 22
Self-citation
Cited by
Characterisation of early Archaean chemical sediments by trace element signatures
Bolhar, R., Kamber, B. S., Moorbath, S., Fedo, C. M., & Whitehouse, M. J. (2004) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2004.02.016 · Cited by 763
Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history
Konhauser, K. O., Planavsky, N. J., Hardisty, D. S., Robbins, L. J., Warchola, T. J., Haugaard, R., Lalonde, S. V., Partin, C. A., Oonk, P. B. H., Tsikos, H., et al. (2017) · Earth-Science Reviews · doi:10.1016/j.earscirev.2017.06.012 · Cited by 537
Kamber, B. S., & Webb, G. E. (2001) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(01)00613-5 · Cited by 488
Slack, J. F., Grenne, T., Bekker, A., Rouxel, O. J., & Lindberg, P. A. (2007) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2006.12.018 · Cited by 277
Extremely low oxygen concentration in mid-Proterozoic shallow seawaters
Tang, D., Shi, X., Wang, X., & Jiang, G. (2016) · Precambrian Research · doi:10.1016/j.precamres.2016.02.005 · Cited by 160
Metadata
- Authors
- Nozaki, Y., Zhang, J., & Amakawa, H.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 1997-04
- Volume
- 148
- Issue
- 1-2
- Pages
- 329-340
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2077125391
- Cited by
- 606
- References
- 2
- FWCI
- 8.06
- Type
- journal article
- Language
- en
- Open access
- closed
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- Nozaki, Y., Zhang, J., & Amakawa, H. (1997). The fractionation between Y and Ho in the marine environment. Earth and Planetary Science Letters. https://doi.org/10.1016/s0012-821x(97)00034-4
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