• Title/Summary/Keyword: 수연

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Leaching behavior of rhenium and molybdenum from molybdenite roasting dust in NaOH solutions (휘수연석(輝水鉛石)의 배소(焙燒) 중 발생한 분경(粉慶)으로부터 NaOH에 의한 Rhenium과 Molybdenum의 침출(浸出))

  • Kim, Young-Uk;Kang, Jin-Gu;Sohn, Jeong-Soo;Cho, Bong-Gyu;Shin, Shun-Myung
    • Resources Recycling
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    • v.18 no.5
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    • pp.37-43
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    • 2009
  • The demand for rhenium has considerably increased recently owing to the large-scale consumption in industries and the price of rhenium has increased owing to the lack of supply and its availability. The dust from the roasting of molybdenite was employed to investigate the leaching behavior of rhenium and molybdenum. Leaching experiments were done by varying optimum parameters, such as reaction time, NaOH concentration and leaching temperature. The optimum leaching condition was found to be $4\;mol{\cdot}L^{-1}$ NaOH, 2 hours leaching time, $100\;g{\cdot}L^{-1}$ solid/liquid ratio, $80^{\circ}C$ temperature, and 250 rpm. At this condition, leaching percentage of rhenium and molybdenum was 86.1% and 88.6%, respectively.

Geochemistry and Molybdenum Mineralisation of the Shap Granite, Westmorland, Northern England (영국(英國)의 북부(北部) Westmorland 지역(地域)에 분포(分布)한 Snap 화강암(花崗岩)의 지화학적(地火學的) 연구(硏究)와 휘수연석(輝水鉛石)의 광화작용(鑛化作用)에 관(關)한 연구(硏究))

  • Kim, Sahng Yup
    • Economic and Environmental Geology
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    • v.9 no.4
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    • pp.177-212
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    • 1976
  • The Shap granite encloses well developed quartz veins and veinlets containing molybdenite in association with other ore sulphide minerals. The preliminary study of the geochemical aspects of the granite stock and mineralisation of molybdenite in comparison with the porphyry deposits is carried out; the distribution of major, minor and ore metal elements in wall rocks, altered envelope and veins, and the molybdenum mineralisation, mainly in connexion with hydrothermal alteration are discussed. The molybdenite and other ore mineralisation, especially bismuthinite and chalcopyrite, are spatially closely related to the hydrothermal alteration adjacent to the veinings, and are dominant where the strong orthoclase alteration has taken place. A pattern of alteration and mineralisation can be recognised and forms the basic for the subdivision of the quarry into several distinct zones, which correspond with the sequence of alteration and mineralisation. The veins, veinlets and their alteration haloes can be further subdivided into a series of concentric zones.

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Significance of Ages of Tungsten Mineralization (중석(重石) 광화작용(鑛化作用) 시기(時期)의 의의(意義))

  • Moon, Kun Joo
    • Economic and Environmental Geology
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    • v.28 no.6
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    • pp.613-621
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    • 1995
  • It is understood that many big tungsten deposits such as the Sangdong in Korea, Fugigatami in Japan, Yukon in Canada, Pine Creek in U.S.A and Vostok in Russia were formed at late Cretaceous ages. However, most of tungsten mineralization in China where half the total world tungsten ores is reserved took place in late Jurassic to early Cretaceous ages. While the close association of molybdenum with tungsten mineralization is observed in the deposits related with Cretaceous magma, tungsten deposits in China related with late Jurassic to early Cretaceous show a close association of tin as well as molybdenum mineralization. It is characteristic that tungsten mineralization in China was followed by tin mineralization. The mode of occurrence of tungsten ore deposits in China is various and may represent the origin of tungsten in general, since the larger half of total amount of tungsten ores in the world are reserved in China. In case of Korea, more than 90% of total production of tungsten was occupied by the Sangdong tungsten deposit, which produced molybdenite as a byproduct Even if tin is detected in ppm unit content, no cassiterite is found in the Sangdong tungsten orebody. A similar type of two tungsten deposits is comparatively studied in order to confirm the published data; one is the Moping tungsten deposit in China and the other is the Dehwa tungsten deposit in Korea. Mineral assemblages occurring in quartz veins of both deposits are more or less same except that zinnwaldite and cassiterite occur only in the former deposit Ages of zinnwaldite and muscovite closely with molybdenite in the former deposit are 181.1 Ma and 167.8 Ma respectively, while muscovites associated with molybdenite in the latter deposit show ages of 80.9 Ma and 80.2 Ma. These results may represent deficient supply of tin from the source granitoid from which tungsten was derived in Korean peninsula during Cretaceous period, while tin supplied during tungsten mineralization tended to increase and the active tin mineralization followed the Jurassic tungsten mineralization in China.

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The Movie 's Symbol, Imagination, Real Image and Meaning (영화<장화, 홍련>의 상징, 가상, 실재 이미지와 의미)

Development of Marine Virus-like Particles Live/Dead Determination Method for the Performance Evaluation of Ballast Water Treatment System (선박평형수처리장치 성능 평가를 위한 해양 바이러스 생사판별 방법 개발)

  • Hyun, Bonggil;Woo, Joo-Eun;Jang, Pung-Guk;Jang, Min-Chul;Lee, Woo-Jin;Bae, Mi-Kyung;Shin, Kyoungsoon
    • Journal of the Korea Academia-Industrial cooperation Society
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    • v.22 no.1
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    • pp.431-438
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    • 2021
  • To prepare more stringent regulations for USCG Phase II ballast water management, this study investigated the staining efficiency of SYBR Green I(SGI) and SYBR Gold(SG) on the virus-like particle (VLP). A dye with high staining efficiency was applied to the treated water that was passed through the ballast water treatment system (BWTS). VLP staining was observed most clearly under the 100-fold and 200-fold dilution of the stock solution when the volume of filtered samples was 0.5 mL to 2 mL. The staining efficiency of SGI and SG did not show a significant difference. On the other hand, the green fluorescence of viruses in the sample stained with SGI was more pronounced than in the samples stained with SG (expressed yellow fluorescence), making it easier to observe. The abundance of VLP in the test water and control water treatments that did not pass through the two types of BWTS (electrolysis type, UV + electrolysis type) was approximately 109 - 1010 VLP 100 mL-1. In contrast, no stained VLP was observed in the treated water treatments. Moreover, SGI was confirmed to be effectively stained under various salinity conditions, including seawater, brackish water, and freshwater. Further verification tests and development of staining methods under various BWTS are required, but the SGI staining method is believed to be a good alternative to the VLP live/dead determination of the USCG Phase II type approval test.