• 제목/요약/키워드: U-Mo/Al

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회남지역(懷南地域)의 옥천누층군(沃川累層群)에 분포(分布)하는 탄질(炭質) 변성이질암(變成泥質岩)의 미량(微量) 및 희토류원소(稀土類元素) 지화학(地化學) (Geochemistry of Trace and Rare Earth Elements from Coal-bearing Metapelites of the Ogcheon Supergroup at the Hoenam Area, Korea)

  • 이현구;이찬희
    • 자원환경지질
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    • 제29권6호
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    • pp.689-698
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    • 1996

  • The coal-bearing metapelites from the Hoenam area are interbedded within the Ogcheon Supergroup, which are composed mainly of graphite, quartz, muscovite and associated with trace amount of biotite, chlorite, pyrite, rutile and barite. Although the formation was mined for coal, and the contents of V, U and Mo are a higher grade in coal formations than the host metapelites. The ratios of Al/Na and K/Na in coal formation are very heterogeneous and wide range from 10.28 to 90.91 and from 3.73 to 36.60, respectively. The V content increase with increasing Al and Ba contents, but the U and Mo are not related with other elements. Those are suggested that controlled of mineral compositions in coaly metapelites due to substitution, migration and reequilibrium of elements by regional metamorphism. These coal formation were deposited in basin of marine environments and the REE of these rocks are not influenced with metamorphism and hydrothermal alterations on the basis of Al content versus La, La against Ce, the ratios of La/Ce (0.23 to 0.73) and Th/U (0.03 to 16.6). These rocks also show much variation in $La_N/Yb_N$ (0.53 to 14.19), Th/Yb (0.51 to 6.00) and La/Th (0.15 to 18.92), and their origin is explained by derivation from a mixture of sedimentary and metasedimentary rocks. The wide range in trace and REE element characteristics as Co/Th (0.07 to 3.00), La/Sc (0.04 to 23.48), Sc/Th (0.06 to 7.57), V/Ni (2 to 3319), Cr/V (0.03 to 1.06) and Ni/Co (1.00 to 79.85) of these coaly metapelites argues for inefficient mixing of the various source lithologies during sedimentation.

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Thermal creep effects of aluminum alloy cladding on the irradiation-induced mechanical behavior in U-10Mo/Al monolithic fuel plates

  • Jian, Xiaobin;Ding, Shurong
    • Nuclear Engineering and Technology
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    • 제52권4호
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    • pp.802-810
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    • 2020

  • Three-dimensional finite element simulations are implemented for the in-pile thermo-mechanical behavior in U-Mo/Al monolithic fuel plates with different thermal creep rates of cladding involved. The numerical results indicate that the thickness increment of fuel foil rises with the thermal creep coefficient of cladding. The maximum Mises stress of cladding is reduced by ~85% from 344 MPa on the 98.0th day when the creep coefficient of cladding increases from 0.01 to 10.0, due to its equivalent thermal creep strain enlarged by 3.5 times. When the thermal creep coefficient of Aluminum cladding increases from 0 to 1.0, the maximum mesoscale stress of fuel foil varies slightly. At the same time, the peak mesoscale normal stress of fuel foil can reach 51 MPa on the 98.0th day for the thermal creep coefficient of 10, which increases by 60.3% of that with the thermal creep un-occurred in the cladding. The maximum through-thickness creep strain components of fuel foil differ slightly for different thermal creep coefficients of cladding. The dangerous region of fuel foil becomes much closer to the heavily irradiated side when the creep coefficient of cladding becomes 10.0. The creep performance of Aluminum cladding should be optimized for the integrity of monolithic fuel plates.

  • https://doi.org/10.1016/j.net.2019.09.008 인용 PDF KSCI

덕평리 지역 우라늄광상의 흑색점판암과 탄질점판암의 지구화학적 특성 (Geochemical Characteristics of Black Slate and Coaly Slate from the Uranium Deposit in Deokpyeong Area)

  • 신동복;김수정
    • 자원환경지질
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    • 제44권5호
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    • pp.373-386
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    • 2011

  • 옥천변성대의 대표적인 우라늄 광화대인 괴산군 덕평리 일대의 흑색점판암과 이에 협재하는 함우라늄 탄질점판암을 상호 구분하여 이들에 대한 지구화학적 연구를 수행함으로써 우라늄 광상의 생성환경에 대해 고찰하였다. 희토류원소 함량은 탄칠점판암이 평균 254 ppm로서 혹색점판암(169 ppm) 보다 높고, 표준시료로 표준화한 결과 탄질시료의 Eu이 현저히 부화되어 나타난다. 산화환원지시원소에 해당하는 원소들의 경우 V, Cr, Co, Ni, Mo, 및 U 등이 흑색점판암에 비해 탄질점판암에서 현저히 부화되어 있는데, 특히, V은 흑색점판암에 비해 24배, Mo은 62배, U은 60배 가량 높게 산출된다. 이 밖에 백금족원소의 경우 Pd와 Pt가 탄질점판암에서 높은 함량을 나타낸다. 정의 Eu 이상을 비롯해 표준 해수기원 셰일에 비해 현저히 부화된 상기 원소들의 산출은 이들이 단순한 해수로부터 침전된 것이 아닌 고온의 환원환경인 해저열수활동과 관련된 퇴적환경에서 생성되었음을 시사한다. 넓은 조성변화를 나타내는 주성분 원소비 ($SiO_2/Al_2O_3$: 3.98~11.88, $Al_2O_3/Na_2O$: 25.6~139.06, $K_2O/Na_2O$: 6.80~46.85)도 퇴적물의 근원암이 퇴적암과 화성암이 혼재되었을 가능성을 나타내며, 또한 황의 함량이 흑색점판암에서 평균 0.6 wt.%인 반면, 탄질점판 암에서는 2.6 wt.%로 높게 나타나는 것은 탄질점판암이 황을 다량 포함하는 열수환경의 영향을 받았음을 보여준다. 이와 같은 지화학적 특징은 옥천변성대와 지구조적으로 대비되며 퇴적분기성 기원으로 알려진 남중국형 백금족광상(Mo-Ni-Zn-PGE)의 생성환경과도 유사한 특징이다. 이상으로 보아 덕평려 일대 우라늄광화작용은 해저열수활동의 영향을 받고 산소가 결핍된 유기물이 풍부한 퇴적분지에서 형성된 것으로 해석된다.

  • https://doi.org/10.9719/EEG.2011.44.5.373 인용 PDF KSCI

아크롤레인 선택 산화반응에서 Mo-V-O와 금속산화물의 상간협동 (Phase Cooperation Between Mo-V-O and Metal Oxide in Selective Oxidation of Acrolein)

  • 박대원;나석은;김경훈;이원호;정종식
    • 공업화학
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    • 제5권2호
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    • pp.327-336
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    • 1994

  • 본 연구는 아크롤레인의 선택산화반응에서 Mo-V-O와 금속산화물의 기계적 혼합촉매에 대한 synergy 효과를 고찰한 것으로 금속산화물로는 $SnO_2$, ${\alpha}-Sb_2O_4$, $WO_3$, ${\alpha}-Al_2O_3$, CuO, $MnO_2$, $Cu_2O$, MgO, CoO 그리고 ZnO 등을 사용하였다. $SnO_2$나 ${\alpha}-Sb_2O_4$와 Mo-V-O의 혼합물 촉매는 Mo-V-O보다 높은 전화율과 수율을 나타내었는데 이것은 이들이 산소 빈자리에 해리 홉착된 산소를 형성하여 Mo-V-O에 전달하는 상간협동에 의한 것으로 판단된다 그러나 $Cu_2O$, MgO, CuO, $MnO_2$와 Mo-V-O의 혼합물 촉매의 경우 전화율은 증가하였으나 수율은 감소하였고, CoO와 ZnO는 Mo-V-O의 촉매성능을 억제하였다. 각 금속산화물의 역할이 서로 다른 점을 그들의 산화-환원 특성으로 설명하였다.

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추부지역 흑색셰일 및 점판암 분포지역에서의 잠재적 독성원소들의 분산과 부화 (Dispersion and Enrichment of Potentially Toxic Elements in Chubu Area Covered with Black Shales and Slates in Korea)

  • 김종신;전효택
    • 자원환경지질
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    • 제30권2호
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    • pp.89-103
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    • 1997

  • The purpose of this research is to investigate the enrichment and distribution patterns of naturally occurring potentially toxic elements in soils derived from black shales and slates. Soil samples were collected from the Chubu area covered with uranium-enriched black shales and slates of the Changri Formation of the Okchon Super Group, and analysed for multiple-elements using INAA, ICP-AES and AAS. Soil pH and loss-an-ignition were also measured. Trace element contents in black shale and slate of the Chubu area are relatively lower than those in black shales, and higher than those in black slates reported elsewhere (Chon, Jung, 1991; Chon et al., 1996). Soil pH values range from 3.5 to 6.5, and loss-an-ignition values are in the range from 3 to 10%. Potentially toxic elements including As, Ba, Cr, Cu, Mo and U are highly enriched in residual soils with maximum content of $540{\mu}g/g$, $35,000{\mu}g/g$, $280{\mu}g/g$, $300{\mu}g/g$, $240{\mu}g/g$ and $860{\mu}g/g$, respectively. Significant concentrations of those elements were found in soils taken from the Tojangkol, the Chubu tunnel and the Meokti areas. Soils derived from black shales and slates, calcareous and phyllitic rocks, and intrusions were discriminated in terms of As, Ba, Co, Cr, Cu, Mo, Sc and U contents. Enrichment index was calculated using the concentrations of As, Ba, Cr and Mo, and enrichment index map shows very similar trend with U distribution in soils.

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