• Title/Summary/Keyword: 유체화

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An Experimental Study on the Thermal Characteristics of Direct Contact Liquid-Ice Heat Exchanger (직접접촉식 액-빙 열교환기의 전열특성에 관한 실험적 연구)

  • Lee, Chae-Moon;Park, Jung-Won;Kim, Dong-Hun
    • Solar Energy
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    • v.16 no.2
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    • pp.65-77
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    • 1996
  • The operating thermal chracteristics of direct contact liquid-ice heat exchanger was experimentally investigated. In this paper, The effects of Ice Packing Factor(IPF), the inlet temperature and the flow rate of Heat Transfer Fluid(HTF) were stuided in the liquid-ice heat exchanger. Thermal stratification in liquid-ice heat exchanger was established clearly and faster at the higher inlet temperature and flow rate of HTF. At the end of melting of the lower flow rate is cleared the thermal stratification in liquid-ice heat exchanger. The temperature stratification is long with higher value of IPF of liquid-ice heat exchanger. The mean temperature of liquid-ice storage was changed rapidly with increasing flow rate and inlet temperature of HTF. The gradiant of ratio of total energy to latent energy was found higher with increasing inlet temperature and flow rate.

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Geological Significance of Liquefaction and Soft-sediment Deformation Structures (액상화와 연질퇴적변형구조의 지질학적 의미)

  • Ghim, Yong Sik;Ko, Kyoungtae
    • Economic and Environmental Geology
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    • v.52 no.5
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    • pp.471-484
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    • 2019
  • Liquefaction occurs by a temporal loss of sediment strength as a consequence of increased pore water pressure during the re-arrangement of unconsolidated, granular sediments. Liquefaction is dependent on the physical properties of the sediments and cause surface cracks, landslide, and the formation of soft-sediment deformation structures(SSDS). SSDS is formed by the combined action of the driving force and deformation mechanism(liquefaction, thixotropy, and fluidization) that is triggered by endogenic or exogenic triggers. So research on the SSDS can unravel syndepositional geological events. If detailed sedimentologic analysis together with surrounding geological context suggest SSDS formed by earthquakes, the SSDS provide a clue to unravel syndepositional tectonic activities and detailed paleoseismological information(> Mw 5) including earthquakes that leave no surface expression.

2유체 전단 동축형 인젝터의 미립화 및 분무특성에 관한 실험적 연구

  • Jeon, Chang-Hwan;Han, Jae-Seob;Kim, Yoo;Kim, Sun-Jin
    • Proceedings of the Korean Society of Propulsion Engineers Conference
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    • 1999.10a
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    • pp.1-1
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    • 1999
  • 2유체 동축인젝터(coaxial twin fluid injector)는 액체산소와 액체수소를 추진제로 사용하는 SSME(Space Shuttle Main Engine)이나 유럽의 Arian 5 Vulcain 엔진과 같은 저온추진제 엔진에 널리 사용되고 있다. 추진제를 미립화 시키는 장치로서 사용하는 다른 여러 형태의 인젝터에 비교할 때 저속의 액체산화제 주위에 고속의 가스연료가 분사됨으로서 발생되는 전단력에 의해 추진제가 미립화되는 특징을 가지며, 이러한 메카니즘은 매우 복잡하여 아직까지 정확히 규명되지 못하고 있는 실정이다.

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Well Log Analysis using Intelligent Reservoir Characterization (지능형 저류층 특성화 기법을 이용한 물리검층 자료 해석)

  • Lim Song-Se
    • Geophysics and Geophysical Exploration
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    • v.7 no.2
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    • pp.109-116
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    • 2004
  • Petroleum reservoir characterization is a process for quantitatively describing various reservoir properties in spatial variability using all the available field data. Porosity and permeability are the two fundamental reservoir properties which relate to the amount of fluid contained in a reservoir and its ability to flow. These properties have a significant impact on petroleum fields operations and reservoir management. In un-cored intervals and well of heterogeneous formation, porosity and permeability estimation from conventional well logs has a difficult and complex problem to solve by conventional statistical methods. This paper suggests an intelligent technique using fuzzy logic and neural network to determine reservoir properties from well logs. Fuzzy curve analysis based on fuzzy logics is used for selecting the best related well logs with core porosity and permeability data. Neural network is used as a nonlinear regression method to develop transformation between the selected well logs and core analysis data. The intelligent technique is demonstrated with an application to the well data in offshore Korea. The results show that this technique can make more accurate and reliable properties estimation compared with previously used methods. The intelligent technique can be utilized a powerful tool for reservoir characterization from well logs in oil and natural gas development projects.

Lightning Impulse Response with Two-Phase Flow in Dielectric Liquid by Using Finite Element Analysis (절연유체 내 2상유동을 고려한 뇌임펄스 응답 유한요소해석)

  • Lee, Ho-Young;Lee, Jong-Chul;Lee, Se-Hee
    • Proceedings of the KIEE Conference
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    • 2011.07a
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    • pp.1521-1522
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    • 2011
  • 뇌임펄스에 의한 절연유체 내 절연파괴 현상은 스트리머 채널에서의 유체유동과 기체유동이 동시에 발생한다. 스트리머 개시와 동시에 발생하는 기포들은 절연파괴에 직접적인 영향을 미치며 이를 모의해석하기위해서 2상유동이 고려되어야한다. 2상유동이 고려된 뇌임펄스 응답 유한요소해석은 전계에 의한 푸아송 방정식과 전자, 양이온, 음이온에 대한 전하연속방정식으로 구성되며 전계 방출과 열전자 방출효과를 경계조건으로 부여하였다. 기체 전리현상은 타운젠트 이론을 도입하였으며, 유체 전리현상은 제너 이온화 모델을 도입하여 수학적 모델링을 통한 2상유동으로 결합하였다. IEC standard #60897의 표준규격에 따라 침-구형 전극을 설계하였고 2차원 축대칭 간략화모델에 적용하여 실험적 결과와 비교분석함으로써 신뢰할 수 있는 수치해석기법이 제시되었다.

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Technology Development for Cavitation Utilization of High viscosity Liquid Fuels (고점도 유체의 캐비테이션 활용 기술 개발)

  • Park, Jun-Sung;Chung, Seok-Woo;Lee, Seoung-Jong
    • 한국신재생에너지학회:학술대회논문집
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    • 2009.06a
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    • pp.884-887
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    • 2009
  • 최근에 경기악화에 따른 석유수요 감소로 우리가 주로 수입하는 두바이유는 배럴당 56 달러선이지만, 유가가 배럴당 100~120 달러로 오를 경우, 원유 대체 및 신규 에너지원 확보를 위해 Bitumen, Oil Shale, 중질잔사유 등 고점도 액상연료를 이용하기 위한 기술개발이 활발히 진행될 것으로 예상된다. 그리고 이에 따라 연소효율이 떨어지는 고점도 저급연료를 이용하여 연소효율을 극대화시키기 위해 계면활성제를 이용하여 화학적으로 유화시키는 기술들이 개발되어 있다. 본 연구에서는 고점도 유체에 대해 계면활성제를 이용하지 않고 캐비테이션 방식을 이용하여 고점도 유체를 에멀젼화 하는 기술을 연구하였다. 에멀젼화 기술은 저급연료유에 물을 혼합하여 안정적으로 장기간 유수분리가 일어나지 않으며, 복합연료로서 반응로에서 연소시킴으로써 연소율을 개선시킬수 있는 기술인데, 발전소의 보일러, 선박, 소각로 등에 적용할 수 있으며 중질잔사유를 사용하는 가스화 발전에도 본 기술이 사용될 수 있을 것으로 기대된다.

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Silk Sensitivity Technology of Nylon Filament Using Fluid System (유체시스템을 이용한 나일론 필라멘트의 실크감성화 기술)

  • Kim, Seung-Jin
    • Science of Emotion and Sensibility
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    • v.10 no.3
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    • pp.367-372
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    • 2007
  • This study surveys the silk sensitivity technology of nylon filament using fluid system. For this purpose, taslan texturing ATY m/c is modified and 4 kinds of nylon filaments with 40d/12f are made using functional chemicals on the modified ATY texturing machine. Using these yarns, 4 kinds of fabrics are woven and processed on the dyeing and finishing. The various physical properties of these fabrics such as water contents, UV-cut, fabric hand are measured and discussed with ATY texturing and functional chemical treatment conditions.

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Evolution of Hydrothermal Fluids at Daehwa Mo-W Deposit (대화 Mo-W 열수 맥상 광상의 유체 진화 특성)

  • Jo, Jin Hee;Choi, Sang Hoon
    • Economic and Environmental Geology
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    • v.46 no.1
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    • pp.11-19
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    • 2013
  • The Daehwa Mo-W deposit is located within the Gyeonggi massif. Quartz and calcite vein mineralization occurred in the Precambrian gneiss and Jurassic granites. Three main types (Type I: liquid-rich $H_2O$ type, Type II: vapor-rich $H_2O$ type, Type III: $CO_2-H_2O$ type) of fluid inclusions were observed and are classified herein based on their phase relations at room temperature. Within ore shoots, type III fluid inclusions have been classified into four subtypes (type IIIa, IIIb, IIIc and IIId) based on their volume percent of aqueous and carbonaceous ($CO_2$) phase at room temperatures combined with their total homogenization behavior and homogenization behavior of $CO_2$ phase. Homogenization temperatures of primary type I fluid inclusions in the quartz range from $374^{\circ}C$ to $161^{\circ}C$ with salinities between 13.6 and 0.5 equiv. wt.% NaCl. Homogenization temperatures of primary type III fluid inclusions in quartz of main generation, are in the range of $303^{\circ}C$ to $251^{\circ}C$. Clathrate melting temperatures of the type III fluid inclusions were 7.3 to $9.5^{\circ}C$, corresponding to salinities of 5.2 to 1.0 equiv. wt. % NaCl. Melting and homogenization temperatures of $CO_2$ phase of type III fluid inclusions were -57.4 to $-56.6^{\circ}C$ and 29.0 to $30.8^{\circ}C$, respectively. Fluid inclusion data indicate a complex geochemical evolution of hydrothermal fluids. The Daehwa early hydrothermal system is characterized by $H_2O-CO_2$-NaCl fluid at about $400^{\circ}C$. The main mineralization occurred by $CO_2$ immiscibility at temperatures of about 300 to $250^{\circ}C$. At the late base-metal mineralization aqueous fluid formed by mixing with cooler and less saline meteoric groundwater.