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Euo Chang Jung,Hye-Ryun Cho,Kyoung Kyun Park 한국방사성폐기물학회 2009 방사성폐기물학회지 Vol.7 No.3
시간분해 레이저 유도 형광 분광학을 이용하여 UO22+, UO2(OH)+, (UO2)2(OH)22+, (UO2)3(OH)5+와 같은 우라늄(VI) 화학종 규명 연구를 수행하였다. 들뜸 파장의 변화에 따른 화학종 규명 감도를 조사하였다. 266 nm의 들뜸 파장을 이용할 경우, 나노 몰 농도의 U(VI) 화합물을 구분할 수 있는 화학종 규명 감도를 얻었다. 이온 세기가 0.1 M, pH가 1인 조건에서 UO22+ 이온의 형광 스펙트럼과 형광 수명을 측정하였다. 488, 509, 533, 559 nm 파장의 특징적인 형광 봉우리를 관측하였고, 측정한 형광 수명은 1.92±0.17 ㎲ 이었다. U(VI) 가수분해 화합물의 형광 스펙트럼과 형광 수명의 변화를 이 값을 기준으로 비교하였다. 장파장 방향으로 이동한 형광 봉우리와 길어진 형광 수명을 가진 가수분해 화합물의 특징적인 양상을 보고한다.
Euo Chang Jung,Hee-Kyung Kim,YeoJin Ju,Dawoon Jeong,Min-Hoon Baik,Ji-Hun Ryu,Jang-Soon Kwon 한국방사성폐기물학회 2023 한국방사성폐기물학회 학술논문요약집 Vol.21 No.2
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.
Euo Sik Cho,박병국,Hyung Soo Uh,권상직 한국물리학회 2004 THE JOURNAL OF THE KOREAN PHYSICAL SOCIETY Vol.44 No.1
For the enhancement of the structural and the electrical characteristics of diamond, phosphorus implantation was applied to the growth of diamond films. The implanted diamond films were subsequently grown again by using microwave plasma chemical vapor deposition. The fabricated diamond films were structurally and electrically characterized. From the results of field emission scanning electron microscopy and atomic force microscopy, the implanted diamond samples showed smoother surfaces and new smaller grains on diamond grains as a result of subsequent growth after implantation. The small grains are thought to pile up among the large grains and to compensate for the rough surfaces of diamond which are caused by the large grain size of diamond. The size of the small grains was related to the dose of implanted phosphorus ions. Better field emission characteristics were obtained at higher ion doses. This is considered to be due to the increased emission area from the small grains and to more defects being formed in diamond.
Euo Chang Jung,Hye-Ryun Cho,Mi Ri Park,Min Hoon Baik 한국방사성폐기물학회 2011 방사성폐기물학회지 Vol.9 No.1
한국원자력연구원 내 지하 처분 연구시설(KURT)에서 채취한 지하수에 존재하는 나노 콜로이드 입자의 크기 및 농도를 현장에서 조사하기 위해 이동식 레이저 유도 파열 검출 장치를 개발하였다. 제작한 장치는 CCD 카메라를 이용하여 레이저 유도 플라즈마가 발생한 위치를 2-차원 영상으로 기록함으로써 광학적으로 입자의 크기를 결정할 수 있다. 크기가 정확히 알려진 폴리스틸렌 표준 입자를 이용하여 입자 크기 측정용 검정 곡선(calibration curve)을 구했고, 이를 이용하여 지하 처분 연구시설에서 채취한 지하수내 콜로이드 입자의 크기를 측정하였다. 지하수 내 존재하는 콜로이드 입자의 평균 크기는 108±26 nm임을 보였고, 농도는 50 ppb 이하인 것으로 추정하였다.
Spectroscopic Study of Interaction Between U(VI) and Natural Organic Matters in Domestic Groundwater
Euo Chang Jung,Min-Hoon Baik,Dawoon Jeong,Ji-Hun Ryu 한국방사성폐기물학회 2022 한국방사성폐기물학회 학술논문요약집 Vol.20 No.2
Time-resolved laser fluorescence spectroscopy (TRLFS) and excitation-emission matrix (EEM) spectroscopy were used to study the interaction of U(VI) and natural organic matters (NOMs) in groundwater. Various types of groundwaters (DB-1, DB-3 from KURT site and OB-1, OB-3 from a U deposit in Ogcheon metamorphic belt) were used as samples. Pulsed Nd-YAG laser at 266 nm (Continuum Minilite) was used as the light source of TRLFS. The laser pulse energy of 1.0 mJ was fixed for all measurements. The luminescence spectrum was recorded using a gated intensified chargecoupled device (Andor, DH-720/18U03 iStar 720D) attached to the spectrograph (Andor, SR-303i). EEM spectra were measured using a spectrofluorometer (Horiba Scientific, Aqualog) equipped with a 150 W ozone-free xenon arc lamp. Excitation spectra were recorded by scanning the excitation wavelength from 200 to 500 nm. Emission spectra were measured using a CCD in the wavelength range of 242–823 nm. In the case of the recently collected DB-1 samples, it was observed that the U and NOM quantities decreased compared to the samples collected before 2016. For some DB-1 samples, the amount of dissolved organic carbon indicating the presence of NOM was significantly reduced, and changes consistent with this phenomenon were observed in the EEM spectrum. The time-resolved luminescence characteristics (peak wavelengths and lifetime) of U(VI) in the DB-1 samples agree well with those of Ca2UO2(CO3)3(aq). This U(VI) species remains stable, even in samples taken five years ago. The estimated amounts of U and NOM from the spectroscopic data of DB-3, OB-1, and OB-3 samples are relatively low compared to DB-1 samples. When a known amount of U(VI) was mixed in each groundwater, the time-resolved luminescence spectrum exhibited a characteristic spectral shape different from the expected luminescence intensity. This phenomenon is presumed to be due to the interaction between U(VI) and NOM in groundwater. The results of this study suggest that the chemical speciation of NOM as well as U(VI) is required to understand U behavior in groundwater.