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Journal ArticleDOI

The rare earth elements in rivers, estuaries, and coastal seas and their significance to the composition of ocean waters

TLDR
The concentrations of rare earth elements (REEs) in samples from 15 rivers, from 6 estuarine transects, and of 5 coastal seawaters are reported and have been used with literature data to examine the continuity in average REE pattern between average continental crust and the dissolved input of REE to the oceans via estuaries.
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This article is published in Geochimica et Cosmochimica Acta.The article was published on 1990-04-01. It has received 933 citations till now. The article focuses on the topics: Cerium anomaly.

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Citations
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Journal ArticleDOI

Ocean particle chemistry: The fractionation of rare earth elements between suspended particles and seawater

TL;DR: In this paper, a new method is explored for estimating the residence time of suspended particles by combining the Ce concentration data of dissolved and surface-bound phases with the Ce(III) oxidation rate measurements of MOFFETT (1990).
Book ChapterDOI

Trace Elements in River Waters

TL;DR: In this article, the authors reviewed the recent literature on trace elements in rivers, in particular by incorporating the results derived from recent ICP-MS measurements, and the basic questions which they want to address are the following: What are the trace element levels in river waters? What controls their abundance in rivers and fractionation in the weathering+transport system?
Journal ArticleDOI

Rare earth elements in pore waters of marine sediments

TL;DR: In this paper, the rare earth elements (REEs) were measured in pore waters of the upper ∼25 cm of sediment from one site off Peru and three sites on the California margin.
Journal ArticleDOI

Rare earth element geochemistry of Late Devonian reefal carbonates, Canning Basin, Western Australia : Confirmation of a seawater REE proxy in ancient limestones

TL;DR: In this article, rare earth element and yttrium (REE+Y) concentrations were determined in 49 Late Devonian reefal carbonates from the Lennard Shelf, Canning Basin, Western Australia, and the results suggest that most limestones should record important aspects of the REE geochemistry of the waters in which they precipitated, provided they are relatively free of terrigenous contamination and major diagenetic alteration from fluids with high, non-seawater-like REE contents.
Journal ArticleDOI

Chemical and physical denudation in the Amazon River Basin

TL;DR: In this article, major and trace element data on the suspended and dissolved phases of the Amazon River and its main tributaries are presented, where the proportions derived from different sources are calculated.
References
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Journal ArticleDOI

Ferrozine---a new spectrophotometric reagent for iron

TL;DR: The ferroin group has been known to react as bidentate ligands with certain metal ions such as ferrous, cuprous, and cobaltous, to give colored complex species.
Journal ArticleDOI

The rare earth elements in seawater

TL;DR: In this article, the depth distributions of La, Ce, Nd, Sm, Eu, Gd, Dy, Er and Yb in the oceanic water column are used to evaluate the marine geochemical cycle of the rare earth elements and their application as water-mass tracers.
Journal ArticleDOI

Flocculation of dissolved organic and inorganic matter during the mixing of river water and seawater

TL;DR: In this paper, a new approach to estuarine studies is presented which establishes 1) the extent and salinity dependence of non-conservative behaviour; 2) composition and chemical form of removal products; and 3) abiological removal mechanisms.
Journal ArticleDOI

Mobility and fractionation of rare earth elements during weathering of a granodiorite

TL;DR: The rare earth elements (REE) have been mobilised and fractionated during supracrustal alteration of the Torrongo granodiorite as mentioned in this paper, and the residual products are especially depleted in the heavy REE.
Journal ArticleDOI

The mechanism of iron removal in estuaries

TL;DR: A survey of U.S. east coast estuaries confirms that large-scale rapid removal of iron from river water is a general phenomenon during estuarine mixing as discussed by the authors.
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