Relationship between micrometer to submicrometer surface roughness and topography variations of natural iron oxides and trace element concentrations

被引:15
作者
Fischer, Cornelius [1 ,3 ]
Karius, Volker [3 ]
Weidler, Peter G. [4 ]
Luettge, Andreas [1 ,2 ]
机构
[1] Rice Univ, Dept Earth Sci, Houston, TX 77251 USA
[2] Rice Univ, Dept Chem, Houston, TX 77251 USA
[3] Univ Gottingen, Geowissensch Zentrum, Abt Sedimentol & Umweltgeol, D-37077 Gottingen, Germany
[4] Forschungszentrum Karlsruhe, Abt Nanomineral, ITC WGT, D-76021 Karlsruhe, Germany
关键词
D O I
10.1021/la703221k
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The surface area and roughness of natural iron oxide precipitations were quantified by 3D optical microscopy in order to get information about fluid-rock interface topography in high-permeability zones. Converged surface roughness data of microscale to submicroscale topography show the predominance of macroporous half-pores (> 500 nm) and the occurrence of smaller half-pores (<500 nm) that dominate the BET surface area of iron oxides. A relationship was found between the occurrence of macroporous surface structures (micrometer range) and the uranium content of iron oxide encrustations. Iron-normalized uranium concentrations of an X-ray amorphous iron oxide encrustation correlate linearly with maximum topography heights of 1 to 2 mu m on hand specimen subsamples. Our study shows the potential importance of micrometer- to submicrometer-size surface features, whose environmental impact is often ignored.
引用
收藏
页码:3250 / 3266
页数:17
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