Analysis of uranium distribution in rocks by μ-PIXE

被引:15
作者
Ohnuki, T
Kozai, N
Samadfam, M
Yasuda, R
Kamiya, T
Sakai, T
Murakami, T
机构
[1] Japan Atom Energy Res Inst, Dept Environm Sci, Terr Environm Res Grp, Tokai, Ibaraki 3191195, Japan
[2] Japan Atom Energy Res Inst, Dept Hot Labs, Tokai, Ibaraki 3191195, Japan
[3] Japan Atom Energy Res Inst, Adv Radiat Technol Ctr, Takatsuki, Osaka 3701292, Japan
[4] Univ Tokyo, Inst Mineral, Bunkyo Ku, Tokyo 1130033, Japan
关键词
PIXE; uranium; migration; weathering; mineralization;
D O I
10.1016/S0168-583X(01)00381-0
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
We examined distributions of U as well as P, Ca, Fe and Ti in rock samples collected at the Koongarra uranium deposit, Australia, using a micro-proton-induced X-ray emission (mu -PIXE) analyzing system developed in the TIARA facility of Japan Atomic Energy Research Institute (JAERI). The conventional scanning electron microscopy-energy dispersive X-ray specrometry (SEM-EDS) was also applied to identify a U-bearing phosphate as saleeite, and to examine the distributions of the above elements to clarify relative advantages of mu -PIXE. The advantages of mu -PIXE are as follows: (1) the spatial resolution of mu -PIXE, about 0.8 mum(2) is higher than that of SEM-EDS, about 7 mum(2) (2) the contrast of elemental maps by mu -PIXE is better than that by SEM-EDS, (3) mu -PIXE detection of U using its L-line gives more reliable U distribution when clay minerals containing potassium are present. It is concluded that mu -PIXE is one of the best techniques that allows U to be accurately analyzed and mapped in K-bearing minerals, using its L-line. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:586 / 592
页数:7
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