Thorium and uranium rapid quantification in soil with portable X-ray fluorescence

被引:1
|
作者
Melquiades, Fabio L. [1 ,4 ]
Bastos, Rodrigo O. [2 ]
Rampim, Leandro [3 ]
Sandrino, Israel Isaias [2 ]
Rodriguez, Duvan Gil [2 ]
Parreira, Paulo S. [1 ]
机构
[1] Univ Estadual Londrina, Dept Fis, Lab Fis Nucl Aplicada, Londrina, Brazil
[2] Univ Estadual Centro Oeste, Dept Fis, Lab Aplicacoes Nucl, Guarapuava, Brazil
[3] Univ Estadual Centro Oeste, Dept Agron, Guarapuava, Brazil
[4] Univ Estadual Londrina, Dept Fis, Lab Fis Nucl Aplicada, Campus Univ PR 445 Km 380, BR-86057970 Londrina, PR, Brazil
关键词
FERTILIZERS;
D O I
10.1002/saj2.20639
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
This study aims to evaluate the thorium (Th) and uranium (U) quantification in soil employing a commercial routine in a portable X-ray fluorescence (pXRF) spectrometer. Certified reference materials (CRMs), as well as a soil sample set, were measured by pXRF and gamma-ray spectrometry. The pXRF results showed that the thorium average detection and quantification limits (in mg kg-1) were 3.3 +/- 0.5 and 11.0 +/- 1.7, respectively. The uranium values were 3.0 +/- 0.4 and 9.9 +/- 1.3. Quantitative pXRF results for Th were in accordance with the reference reported for most CRMs analyzed, and the same accordance was obtained in the comparison with gamma-ray spectrometry results for the soil sample set. However, U results were overestimated by pXRF when compared both with the CRM-reported values and the gamma-ray spectrometry results. In conclusion, the tested pXRF commercial routine may be a viable technique to identify variations in natural Th levels in soil but needs to be used with caution to identify and quantify U. Th and U quantification in soil with portable X-ray fluorescence (pXRF) was tested against reference materials and gamma spectrometric analysis. The tested pXRF commercial routine proved to be a viable and rapid technique to quantify Th natural levels in soil. pXRF commercial routine needs to be used with precaution to identify U natural levels in soil.
引用
收藏
页码:557 / 564
页数:8
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