Surface chemistry of weathered zircons

被引:48
作者
Balan, E
Trocellier, P
Jupille, J
Fritsch, E
Muller, JP
Calas, G
机构
[1] Univ Paris 06, Lab Mineral Cristallog, CNRS, UMR 7590,IPGP, F-75252 Paris 05, France
[2] Univ Paris 07, Lab Mineral Cristallog, CNRS, UMR 7590,IPGP, F-75252 Paris, France
[3] Ctr Etud Saclay, CEA, CNRS, Lab Pierre Sue, F-91191 Gif Sur Yvette, France
[4] Lab CNRS St Gobain Surface Verre & Interfaces, F-93303 Aubervilliers, France
[5] IRD, F-75480 Paris 10, France
关键词
zircon; zirconium; surface chemistry; weathering;
D O I
10.1016/S0009-2541(01)00271-6
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We have investigated the surface morphology and chemistry of zircon in sediments and soils of the Amazon basin (Brazil). The extent of metamictization in the near-surface region of these zircons was previously determined by Raman micro-probe. Scanning electron microscopy (SEM) reveals scarce dissolution features and numerous marks related to the sedimentary transport of the zircon grains, which attest to the high resistance of these zircons to tropical weathering. Rutherford backscattering (RBS) micro-analysis and X-ray photoelectron spectroscopy (XPS) failed to reveal any strong chemical change at the surface of the zircon grains. In particular no Zr enrichment was detected, which excludes the occurrence of a protecting layer of Zr oxide or hydroxide at the zircon surface. This result suggests that the slow weathering rate of zircon could be the principal factor limiting the Zr mobility in the investigated weathering environments. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:13 / 22
页数:10
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