• 제목/요약/키워드: Deep water formation

검색결과 99건 처리시간 0.029초

김원치과의원 실내디자인 (Kim-Won Dental Clinic Interior Design)

  • 최선희
    • 한국실내디자인학회:학술대회논문집
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    • 한국실내디자인학회 2006년도 춘계학술발표대회 논문집
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    • pp.99-100
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    • 2006
  • The concept of dental clinic have been changed along the advanced dental science to meet the need of setting up high-technology-digital appliances. As the general idea about the dental clinic has been changed from systematic connection, the expansion of zoning needs to become more accurate and mote detailed. In the spacious waiting room. the interment cafe has been established to supply the information services, and the various multi-imaged channels, which were built in, will relieve the boredom of the waiting time. The formation of water space leads to the effect of humidification and makes parents share visual and auditory sympathy All of the unit-chairs attached cameras in the consultation room enables people to diagnose more quickly and precisely through the computerized system. Partitions have been set of to put it in and to help diagnosis process to be done smoothly in the formational space. The whole atmosphere is intended to be harmony with the natural surroundings in Je-Ju. It will inspire people visiting this clinic to image the deep blue sea in Je-Ju. By using projective non-material a lot, especially material wooden windows and doors, it is believed to create the bright and stable atmosphere. It will lead patients feel comfortable.

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무극 금은 광상에 대한 유체포유물 및 안정동위원소 분석연구 (Stable Isotope and Fluid Inclusion Studies of the Mugug Au-Ag Mineral Deposits)

  • 김규한;김옥준;장원선
    • 자원환경지질
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    • 제23권1호
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    • pp.1-9
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    • 1990
  • A couple of Au-Ag-bearing epithermal quartz veins of Cretaceous(87.9Ma) in age are developed in the Cretaceous(112Ma) granodiorite batholith which was emplaced in Mesozoic Baegyari sedimentary formation. Au minerals consist mostly of electrum with a 54.2-61.9 wt% Au and are closely associated with sulfide minerals including pyrite, chalcopyrite, pyrrhotite, galena and sphalerite. Homogenization temperatures of fluid inclusions in quartz, fluorite and calcite are $196-368^{\circ}C$ (avg. $240^{\circ}C$), $74-176^{\circ}C$ (avg. $115^{\circ}C$) and $75-200^{\circ}C$ (avg. $119^{\circ}C$) respectively. Sulfur isotopic compositions( +5- +8‰) of ore sulfides indicate a deep-seated sulfur origin. Oxygen isotope compositions of different stages of quartz vary from +5.6 to +9.3‰ and calculated ${\delta}^{18}O$ values of ore fluid at $250^{\circ}C$ range from -3.2 to +0.4‰, reflecting an isotopically evolved ore fluid mixed with a $^{18}O$ depleted meteoric water under the variable mixing ratios between hydrothermal and meteoric waters. Isotopic data of calcite minerals support the above conclusions.

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Hydrodynamic performance of a pump-turbine model in the "S" characteristic region by CFD analysis

  • Singh, Patrick Mark;Chen, Chengcheng;Choi, Young-Do
    • Journal of Advanced Marine Engineering and Technology
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    • 제39권10호
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    • pp.1017-1022
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    • 2015
  • Specific hydrodynamic characteristic of pump-turbine during the start and load rejection process of generating mode causes anomalous increase of water pressure, along with large machine vibration, called "S" characteristic. The aim of this study is to understand and explain the hydrodynamic performance of pump-turbine at "S" characteristic region by using a model of pump-turbine system. The operation in the condition of runway and low discharge in a typical "S" characteristic curve may become unstable and complex flow appears at the passage of guide vane and impeller. Therefore, velocity and pressure distribution are investigated to give an all-sided explanation of the formation and phenomenon of this characteristic, with the assistance of velocity triangle analysis at the impeller inlet. From this study, the internal flow and pressure fluctuation at the normal, runway and low discharge points are explored, giving a deep description of hydrodynamic characteristic when the pump-turbine system operates with "S" characteristic.

미역과 다시마 가루를 첨가한 케이크의 물리화학적 및 관능적 특성 (Physico-chemical and Sensory Characteristics of Cakes Added Sea Mustard and Sea Tangle Powder)

  • 송영선;안정미
    • 한국식품영양과학회지
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    • 제28권3호
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    • pp.534-541
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    • 1999
  • This study was undertaken to examine the effect of sea tangle and sea mustard on physiochemical and sensory characteristics of cakes and the possibility commercialization of these functional cakes. The moisture contents of cakes prepared with sea tangle and sea mustard were higher than those of control, and a positive correlation between water holding capacity(WHC) and moisture contents was observed(r=0.836). As addition level of sea tangle and sea mustard was increased, volume of cakes were decreased, whereas hardness was increased slightly and color became deep. Hardness was strongly correlated to the volume of cakes(r= 0.914). Visual observation by photomicrography showed that, as addition level of sea mustard and sea tangle was increased, formation of air cells were prohibited and thus volume of cakes was decreased. The microstructural observation by scanning electron microscopy(SEM) showed that air cells of cakes were well developed up to 5% addition of sea tangle powder. As a result of the sensory evaluation for the cakes prepared with sea tangle and sea mustard, no significant difference was observed between control and those addition levels up to 5%. Flavor was proved to be the most important factor in determining overall acceptability and hedonic hardness score was inversely correlated to the objective hardness value(r= 0.853).

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동해 울릉분지 남서부 천부 퇴적층에서의 가스 생성 및 천연가스 하이드레이트 형성 잠재력과 이들의 부존 증거 (Potential of gas generation and/or natural gas hydrate formation, and evidences of their presence in near seafloor sediments of the southwestern Ulleung Basin, East Sea)

  • 류병재;이영주;김지훈;;;김일수
    • 한국신재생에너지학회:학술대회논문집
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    • 한국신재생에너지학회 2006년도 추계학술대회
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    • pp.50-53
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    • 2006
  • Regional geophysical surveys and geological cal studies on natural gas hydrate (NGH) in the East Sea were carried out by the Korea Institute of Geoscience and Mineral Resources (KIGAM) from 2000 to 2004. 16 piston cores, 2270 L-km of multi-channel reflection seismic (MCRS) data and 730 L-km of 3.5kHz Chirp data obtained from the southwestern part of the deep-water Ulleung Basin were analyzed in this study. In piston cores, cracks generally developed parallel to bedding suggest significant gas content. The core analyses showed high total organic carbon (TOC) content, sedimentation rate and heat flow of sediments. These are in favor of the general ion of substantial biogenic methane, which can form the NGH within the stability zone of the near seafloor sediments in the study area. The cores generally show also high residual hydrocarbon gas concentrations for the formation of natural gas hydrates The geophysical indicators of the presence of gas and/or NGH such as bottom simulating reflectors (BSRs), seismic blank Bones, pockmarks and gas seeping features were well defined on the MCRS and Chirp data.

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The preparation of skin analogue composition having the liquid crystalline structure and its cosmetic applications

  • Lee, Dong-Kyu;Jeong, Kwan-Young
    • 한국응용과학기술학회지
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    • 제30권2호
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    • pp.215-224
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    • 2013
  • Recently, many cosmetic researchers have been focused on the development of high functional cosmetics including anti-wrinkle and whitening. In these studies, they couldn't afford to pay a deep attention to stable encapsulations for unstable materials and efficient drug deliveries for them. Particularly, in order to show a degree of instant effects as cosmetics, they can't also ignore moisturizing effect enough to satisfy customers just after applying and its maintenance by improving the function of skin barrier as well as above two effects. Therefore, skin analogue systems have attracted considerable attention in the view of structural and compositional similarity to intercellular membrane in stratum corneum. And, some models for skin analogue composition were developed to improve the function of skin barrier, stably encapsulate unstable materials such as retinol, vitamin B, C, E, etc., and control their skin penetration in order to show good effects as cosmetics. In this study, we suggest the new skin analogue model having the compositional similarity as well as conventional structural ones. Our skin analogue membrane(SAM) is mainly composed of ceramide/ cholesterol/phosphatidylcholin/fatty acids and its structural defects are compensated by including cholesterol amphiphile and controlling the ratio of ceramide/cholesterol. It was possible to confirm the formation of skin analogue membrane having highly-densed multilamella structure and compare them according to the change of each ratio with a polarized microscope, X-ray diffraction. More detaily, we observed their structures with a electron microscope(TEM). Finally, we dispersed them in excess of continuous water phase, observed the formation of maltese-cross liquid crystalline and measured the efficiency of drug deliveries and moisturizing effects.

용화광산(龍化鑛山)의 금은광화작용(金銀鑛化作用) (Gold and Silver Mineralization in the Yonghwa Mine)

  • 윤석태;박희인
    • 자원환경지질
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    • 제24권2호
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    • pp.107-129
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    • 1991
  • The Yonghwa gold-silver deposits are emplaced along $N15^{\circ}{\sim}25^{\circ}W$ trending fissures in middle Cretaceous porphyritic granite or Precambrian Sobaegsan gneiss complex. The results of paragenetic studies suggest that vein filling can be subdivided into four identifiable stages; state I: the main sulfide stage, characterized by base-metal sulfide minerals, iron oxides and minor electrum, stage II: electrum stage, stage III: electrum and silver-bearing sulfosalts stage, stage IV: post ore stage of carbonates and quartz. The ore mineralogy suggests that depositional temperature of the formation of the gold and silver minerals are estimated as 200 to $250^{\circ}C$ and 140 to $180^{\circ}C$, respectively. Sulfur fugacity of the formation of the gold and silver minerals are estimated as $10^{-14.0}$ to $10^{-12.2}$ atm and $10^{-18.5}$ to $10^{-17.2}$ atm, respectively. A consideration of the pressure regime during ore deposition bases on the fluid inclusion evidence of boiling suggests lithostatic pressure of less than 180 bars. This range of pressure indicate that vein system lay at depth of 700m below the surface at the time during mineralization. Salinities of ore-bearing fluids range from 0.4 to 6.9 wt.% equivalent NaCl. The sulfur and carbon isotopic data reveal that these elements were probably derived from a deep-seated source. The ${\delta}^{18}O$ of the hydrothermal fluid was determined from ${\delta}^{18}O$ values of quartz and calcite. Oxygen and hydrogen isotopic studies reveal that meteoric water dominate over ore-bearing fluid.

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천연해수 중 온도 변화에 따라 전착한 환경친화적인 석회질 피막의 특성 분석 (Properties analysis of environment friendly calcareous deposit films electrodeposited at various temperature conditions in natural seawater)

  • 이찬식;강준;이명훈
    • Journal of Advanced Marine Engineering and Technology
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    • 제39권7호
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    • pp.779-785
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    • 2015
  • 일반적으로 선박 및 해양구조물, 그리고 심해 설비의 가장 적절한 부식 방지법으로는 음극방식법이 널리 사용되고 있다. 해수 중에 이러한 음극방식법이 적용될 경우, 음극전류가 용존 해 있는 산소를 환원시킴으로써 음극분극 된 설비 표면에 수산화 이온을 다량 발생시키게 되고, 이로 인하여 계면에서의 pH는 증가하게 된다. 또한 탄산이온의 농도 역시 증가하게 되어, 바닷물 속에 용해되어 있는 마그네슘과 칼슘 이온들이 이들 수산화 이온 및 탄산 이온과 결합함으로써, 수산화마그네슘 및 탄산칼슘을 주성분으로 하는 무기물 층이 설비 표면에 석출하게 되는데 이렇게 형성된 피막을 일반적으로 "석회질 피막"이라고 한다. 이러한 무기물 층은 해수라는 부식환경에서 모재를 보호하는 물리적 장벽으로서의 역할을 함은 물론 음극방식을 할 때 요구되는 전류밀도를 감소시키는 역할을 하게 된다. 한편 이러한 해수 중에서의 석회질 피막의 형성은 전위, 전류, pH, 온도, 시간 등을 포함한 많은 변수들에 의해 변화하게 되는데, 이에 본 연구에서는 여러 가지 변수들 중 특히나 해수의 온도 및 시험편 표면 조건에 따른 무기물 층의 피막구조변화 및 특성변화를 살펴봄으로서 환경친화적인 코팅막의 개발에 대한 설계지침을 제공 할 수 있었다.

가축 수정란 동결보존의 최근 이용방법 (Current Application of Embryo Cryopreservation for Farm Animals)

  • 석호봉
    • 한국수정란이식학회지
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    • 제4권1호
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    • pp.1-13
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    • 1989
  • This paper reviews the most important steps that have generated consistent progress in principles and developmental progress of embryo cryopreservation, and also study on freezing procedure and its application by conventional method and current improved method for freezing procedure and its appilcation of embryo cryopreservation in farm animals. Four were of particular interest: 1.The transport of water across the ccli membrane (zona pellucida) during freezing and thawing accordinglyplays a role in determing whether the celi survives. This movement of water is controlied mainly by extracellular phase changes and by the nature and concentration of any cryoprotective agent present. Therates of cooling, freezing and warming, and the intervals over which they are applied are further decisi've factors in determining whether a cryopreservation procedure allows survival after thawing. 2.The first successful deep freezing experiments with sheep morula and blastocysts during the seventies were based on the early procedures used for mouse embryos.Current research during the eighties is developed with the aim of simplifying and improving current procedures such as one-step dilution and rapid or ultra-rapid cooling by using the model of laboratory animals. 3.The conventional method for the embryo cryopreservation is described. An alternative to this method which may result in high survival and also in reducing of the freezing and thawing time is done by combing a permeable cryoprotectant such as glycerol, DMSO or propanediol and a non-permeable compound such as sucrose, trehalose, raffinose or lactose. 4.Finally a different approach to the preservation of embryos, named vitrification, is introduced. This procedure depends upon the ability of concentrated solutions of cryoprotective agents such as glycerol and propanediol to supercool to very low temperature (-196$^{\circ}C$) during rapid cooling before solidifying without formation of ice. However, more complete data are necessary for successful vitrification of blastocysts.

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울릉분지 남서부 심해저 퇴적층에 분포하는 천부 가스의 지화학 및 지구물리 특성 (Geochemical and Geophysical Characteristics of Shallow Gases in the Deep Sea Sediments, Southwestern Ulleung Basin)

  • 김일수;이영주;유동근;류병재
    • 자원환경지질
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    • 제36권3호
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    • pp.149-157
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    • 2003
  • 울릉분지 남서부 심해저 퇴적층에 분포하는 천부 가스의 특성을 파악하기 위해서 피스톤 코아시료를 채취하고 공기층 가스 기법으로 퇴적물 내에 함유된 가스를 포집하여 탄화수소 가스의 함량, 성분 및 탄소 동위원소 분석을 실시하였다. 또한 가스의 함량과 시추 코아 퇴적물의 연관성 및 특성을 파악하기 위해서 가스를 함유하는 퇴적물에 대해서 유기 지화학 분석을 실시하였다. 그리고 가스를 함유하는 퇴적물의 탄성파 특성을 살펴보았다. 퇴적물에서는 탄화수소 가스가 0.01%에서 11.25%까지 검출되었다. 단위 퇴적물내의 탄화수소 가스의 양을 젖은 퇴적물의 부피를 기준으로 정량적으로 계산하면 0.1에서 87.4ml/L wet sediment를 나타냈다. 분석된 탄화수소 가스의 성분은 주로 메탄으로 분석 시료에서 2개 시료를 제외하고는 메탄의 함유비가 98%이상을 나타냈으며 32개 분석 시료 중에서 15개 구간에서는 메탄만이 검출되었다. 채취된 시료의 메탄 가스의 탄소 동위원소 비$(\delta^{13}c)$는 -94.31$extperthousand$에서 -55.50$\textperthousand$까지의 범위를 나타내서 분석된 가스의 기원은 메탄 생성 박테리아에 의한 생물 기원 가스인 것으로 판명된다. 연구 지역의 퇴적물내의 탄화수소 가스의 함량은 지역에 따라서 차이를 보인다. 퇴적물내의 가스의 함량은 퇴적물의 지화학적 특성과 퇴적물의 입도와는 뚜렷한 상관 관계를 보이지 않았다. 단지 탄성파 단면상에서 이상대를 나타내는 곳에서는 가스의 함량이 많은 것으로 나타났다. 탄성파 단면상에 보이는 이상대는 현장의 온도 압력 조건에서 공극수에 탄화수소 가스가 과포화 된 곳으로 다른 조건이 만족된다면 가스 하이드레이트를 형성하기에 적합한 것으로 해석한다.