Partitioning of rare earth elements between dissolved and colloidal phases

被引:9
|
作者
Verplanck, Philip L. [1 ]
机构
[1] US Geol Survey, MS Denver Fed Ctr 973, Denver, CO 80225 USA
来源
PROCEEDINGS OF THE FOURTEENTH INTERNATIONAL SYMPOSIUM ON WATER-ROCK INTERACTION, WRI 14 | 2013年 / 7卷
关键词
rare earth elements; fractionation; water-rock interaction; ultrafiltration; WATER;
D O I
10.1016/j.proeps.2013.03.149
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
To utilize rare earth elements (REEs) as tracers in the weathering environment, an understanding of how these elements partition between aqueous and solid phases is essential. This study evaluates the partitioning between REEs and colloidal material over a range in pH (3.6-8.0) and solid and aqueous compositions. This paper presents results of filtration studies for REEs in 4 different conditions. Sample aliquots include an unfiltered fraction, a 0.45 mu m filtrate, and an ultrafiltrate (similar to < 0.005 mu m). Results show that the REEs behave conservatively in waters with pH below similar to 5.0. REEs tend to partition onto solid phases in circumneutral waters that have colloidal material, but the nature of the fractionation can vary from light REE enriched, heavy REE enriched, or no fractionation. (C) 2013 The Authors. Published by Elsevier B.V.
引用
收藏
页码:867 / 870
页数:4
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