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通过时间分辨激光荧光显微镜(TRLFM)研究铕(III)在异质表面上的吸附。

Adsorption of Eu(III) on a heterogeneous surface studied by time-resolved laser fluorescence microscopy (TRLFM).

作者信息

Ishida Keisuke, Kimura Takaumi, Saito Takumi, Tanaka Satoru

机构信息

Department of Quantum and Systems Science, School of Engineering, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-8656, Japan.

出版信息

Environ Sci Technol. 2009 Mar 15;43(6):1744-9. doi: 10.1021/es8024287.

Abstract

Time-resolved laser fluorescence microscopy (TRLFM) is a useful tool to simultaneously investigate the intensity, location, type, and surrounding chemical environment of a fluorophore. In this study, we demonstrated the applicability of TRLFM for the adsorption of Eu(III) on a natural heterogeneous surface. Different adsorption species of Eu(III) were observed on the Makabe granite surface and its constituents (biotite, plagioclase, potassium feldspar, and quartz). Eu(III) heterogeneously adsorbed on biotite, plagioclase, and quartz and homogeneously on potassium feldspar. The histograms of the fluorescence decay rates of adsorbed Eu(III) indicated efficient quenching of Eu(III) fluorescence probably due to Eu(III)-surface interaction or the formation polynuclear hydoxo Eu(III) species on the surfaces. It was also revealed that single species of Eu(III) was observed on biotite and two species on plagioclase and potassium feldspar. The adsorption of Eu(III) on the granite surface was highly heterogeneous. The TRLFM measurements of different regions of the granite surface turned into the finding of Eu(III) with different fluorescence decay rates. Comparing with the fluorescence decay histograms of the mineral constituents, Eu(III) clearly adsorbed on the feldspar family. It was also found that Eu(III) adsorbed as an outer-sphere complex and on an altered mineral of the granite.

摘要

时间分辨激光荧光显微镜(TRLFM)是一种用于同时研究荧光团的强度、位置、类型及其周围化学环境的有用工具。在本研究中,我们证明了TRLFM在研究Eu(III)在天然异质表面上的吸附情况方面的适用性。在真壁花岗岩表面及其成分(黑云母、斜长石、钾长石和石英)上观察到了Eu(III)的不同吸附形态。Eu(III)在黑云母、斜长石和石英上非均相吸附,而在钾长石上均匀吸附。吸附的Eu(III)荧光衰减率直方图表明,Eu(III)荧光可能由于Eu(III)与表面的相互作用或表面多核羟基Eu(III)物种的形成而有效猝灭。研究还发现,在黑云母上观察到单一形态的Eu(III),而在斜长石和钾长石上观察到两种形态。Eu(III)在花岗岩表面的吸附具有高度的非均质性。花岗岩表面不同区域的TRLFM测量结果显示出具有不同荧光衰减率的Eu(III)。与矿物成分的荧光衰减直方图相比,Eu(III)明显吸附在长石族上。研究还发现,Eu(III)以外部络合物的形式吸附在花岗岩的蚀变矿物上。

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