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首页> 外文期刊>Nuclear Instruments & Methods in Physics Research >Spectroscopic characterization of Greek dolomitic marble surface interacted with uranium and thorium in aqueous solutions
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Spectroscopic characterization of Greek dolomitic marble surface interacted with uranium and thorium in aqueous solutions

机译:水溶液中铀和or相互作用的希腊白云岩大理石表面的光谱表征

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摘要

The surface of a typical Greek (Thassian) dolomitic marble was studied after interaction with U- and Th-containing aqueous solutions (1000 mg/L, free-drift experiments for 1 week at atmospheric P_(co2))> using ~(12)C-RBS and Laser μ-Raman spectroscopy. Powder-XRD and SEM-EDS were also applied to investigate the phases deposited on the surface of the interacted samples. The obtained results indicated a considerable removal of U from the aqueous medium mainly due to massive surface precipitation of amorphous UO_2-hydroxide phases forming a relatively thick (nm-sized) coating on the carbonate substrate. The interaction of Th with dolomitic marble surface is also intense leading to a formation of an amorphous Th-hydroxide layer of similar thickness but of significantly lower elemental atomic proportion.
机译:在与含U和Th的水溶液(1000 mg / L,在大气P_(co2)下进行1周的自由漂流实验)相互作用后,使用〜(12)研究了典型的希腊(Thassian)白云岩大理石的表面。 C-RBS和激光μ拉曼光谱。 Powder-XRD和SEM-EDS还用于研究沉积在相互作用样品表面的相。所获得的结果表明,从水性介质中大量去除了U,这主要是由于无定形UO_2-氢氧化物相的大量表面沉淀在碳酸盐基材上形成了相对较厚(纳米尺寸)的涂层。 Th与白云石大理石表面的相互作用也很强烈,导致形成了类似厚度但元素原子比例明显较低的无定形Th-氢氧化物层。

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