Raman characteristics of various minerals constituting natural rocks collected from uranium deposits in Okcheon metamorphic zone in Korea are presented. Micro-Raman spectra were measured using a confocal Raman microscope (Renishaw in Via Basis). The focal length of the spectrometer was 250 mm, and a 1800 lines/mm grating was installed. The outlet of the spectrometer was equipped with a CCD (1,024256 pixel) operating at -70°C. Three objective lenses were installed, and each magnification was 10, 50, and 100 times. The diameter of the laser beam passing through the objective lens and incident on the sample surface was approximately 2 m. The laser beam power at 532 nm was 1.6 mW on the sample surface. Raman signal scattered backward from the sample surface was transmitted to the spectrometer through the same objective lens. To accurately determine the Raman peak position of the sample, a Raman peak at 520.5 cm-1 measured on a silicon wafer was used as a reference position. Since quartz, calcite, and muscovite minerals are widely distributed throughout the rock, it is easy to observe with an optical microscope, so there is no difficulty in measuring the Raman spectrum. However, it is difficult to identify the uraninite scattered in micrometer sizes only with a Raman microscope. In this case, the location of uraninite was first confirmed using SEM-EDS, and then the sample was transferred to the Raman microscope to measure the Raman spectrum. In particular, a qualitative analysis of the oxidation and lattice conditions of natural uraninite was attempted by comparing the Raman properties of a micrometer-sized natural uraninite and a laboratory-synthesized UO2 pellet. Significantly different T2g/2LO Raman intensity ratio was observed in the two samples, which indicates that there are defects in the lattice structure of natural uraninite. In addition, no uranyl mineral phases were observed due to the deterioration of natural uraninite. This result suggests that the uranium deposit is maintained in a reduced state. Rutile is also scattered in micrometer-sizes, similar to uraninite. The Raman spectrum of rutile is similar in shape to that of uraninite, making them confused. The Raman spectral differences between these two minerals were compared in detail.

In south Korea, most of uranium deposits are distributed in the Ogcheon belt, which is one of two late Precambrian to Paleozoic fold belts (the Imjingang and Ogcheon belts). A study site of the Ogcheon metamorphic belt (OMB) in Hoenam-myun, Boeun-gun was selected for the natural analogue study by preliminary site investigation for several candidate study sites. Three boreholes were drilled in the site and some rock cores and groundwater samples were taken from the boreholes. Various analytical studies for the samples are now being performed. Thus, in this study, various basic characteristics of the study site such as occurrence, geological, mineralogical, and chemical properties were investigated for a future study. Base rocks containing uranium in the OMB are usually black slate and coaly slate. Coaly slate usually shows a higher content of uranium and larger grain size of uranium than black slate. Uranium minerals found in the OMB are uraninite, uranothorite, brannerite, ekanite, coffinite, francevillite, uranophane, autunite, and torbernite depending on the base rock types. Uranothorite is abundant in black slate whereas uraninite is mostly abundant in coaly slate. Chemical compositions of the solid and groundwater samples from the study site were also analyzed by using ICP-MS/OES (Inductively Coupled Plasma Mass Spectrometry) and XRF (X-ray Fluorescence). This will contribute to determine uranium minerals in the solid samples and uranium speciation in the groundwater. The results of this study will contribute to performing future natural analogue studies in domestic uranium deposits and provide basic information and knowledge for understanding long-term geochemical behaviors of radionuclides in a high-level radioactive repository.

전해정련공정을 통해 생산된 우라늄 전착물은 약 30%의 용융염을 포함하고 있으므로, 순수한 우라늄을 회 수하여 금속 잉곳으로 용이하게 제조하기 위해서는 용융염을 먼저 제거하는 공정이 필요하다. 우라늄 전착물의 염증류 거동을 고찰하기 위해서는 염증류의 주요 공정변수인 유지온도와 진공압의 염제거율에 대한 영 향를 고찰해야 한다. 이전 연구에서 우라늄전착물에 대한 염증류 거동에 대해 Hertz-Langmuir 관계식을 적 용하여 각 용융염의 휘발 조건에 대해 염휘발계수를 얻을 수 있었으며 이로부터 우라늄 전착물에 대해 99% 이상의 염제거율을 나타내는 염증류공정의 조업조건을 도출하였다[1]. 한편, 염증류 장치에서 사용되는 재질 인 스테인리스강에 대해 우라늄 전착물에서 염휘발된 우라늄 금속이 스테인리스강의 주성분인 철, 니켈, 크 롬 등과 공정(eutectic melt)을 형성하지 않는 온도에서 염증류공정을 수행해야 하는 제한 조건이 따른다. 이 번 연구에서는 우라늄 금속과 스테인리스강과의 반응성을 검토함으로써 우라늄 전착물의 염을 99% 이상 제 거할 수 있는 조건을 확인하였다. 그리고 염증류 속도를 증진시키며 휘발된 염을 더 효율적으로 회수하기 위 해 공급되는 알곤 흐름에 의한 염증류 장치의 열해석을 수행함으로써 알곤 흐름에 의한 우라늄 전착물에 대 한 염증류 거동을 고찰하였다.