• Journal of the Korean Wood Science and Technology
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• 제26권4호
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• pp.1-5
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• 1998

In this study, it was examined the method to estimate equilibrium moisture content(EMC) at high vapor pressures and high temperatures above $100^{\circ}C$. The material used for the experiment was Sugi(Cryptomeria japonica). EMC was investigated at temperatures ranging from $100^{\circ}C$ to $160^{\circ}C$ and under saturated vapor pressures above 1 atm. The correlation between temperatures and vapor pressures have a good agreement with those observed by thermocouple and pressure gauge in the air state of autoclave, respectively. A sensitivity of quartz spring was 65mm/g. Moisture content(MC)s calculated from the quartz spring elongation by vapor sorption showed a good agreement with MCs by oven-dried method. Using this system, it was found that EMC at high vapor pressures and high temperatures above $100^{\circ}C$ were higher than EMC of wood in 1 atm pressure conditions. With this system, therefore, it was concluded that the EMCs of wood and wood-based materials at high temperatures were able to be evaluated.

• 한국지구과학회지
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• 제23권1호
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• pp.38-51
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• 2002

Mantle xenoliths in alkali basalt at Boun, the Gansung area and Baegryung Island in South Korea are spinel lherzolites composed of olivine, orthopyroxene, clinopyroxene, and spinel. Minerals show homogeneous compositions. Olivine compositions have Fo$_{89.0}$ to Fo$_{90.2}$, low CaO (0.03 to 0.12 wt%), and NiO of 0.34 to 0.40 wt%; the orthopyroxene is enstatite with En$_{89.0}$ to En$_{90.0}$ and Al$_{2}$O$_{3}$ of 4 to 5 wt%; the clinopyroxene is diopside with En$_{47.2}$ to En$_{49.1}$ and Al$_{2}$O$_{3}$ of 7.42 to 7.64 wt% from Boun and 4.70 to 4.91 wt% from Baegryung. Spinel chemistry shows a distinct negative trend, with increaeing Al corresponding with decreasing Cr, and Mg$^{#}$ (100Mg/Mg+Fe) and Cr$^{#}$ (100Cr/Cr+Al) of 75.1 to 81.9 and 8.5 to 12.6, respectively. The equilibrium temperatures of these xenoliths, taken as the average obtained from those of Mercier (1980) and Sachtleben and Seck (1981), lie between 970 and 1020$^{\circ}$C, and equilibrium pressures derived from Mercier (1980) fall within the range of 12 to 19 kbar (i.e., 42 to 63 km). These temperatures and pressures are reinforced by considerations of the Al-isopleths in the MAS system (Lane and Ganguly, 1980), as adjusted for the Fe effect on Al solubility in orthopyroxene (Lee and Ganguly, 1988). The equilibrium temperatures and pressures of xenoliths, as considered in P/T space, belong to the oceanic geotherm, based upon the various mantle geotherms presented by Mercier (1980). This geotherm is completely different from continental geotherms, e.g., from South Africa (Lesotho) and southern India. Mineral compositions of spinel-lherzolites in South Korea and eastern China are primitive; paleo-geotherms of both are quite similar, but degrees of depletion of the upper mantle could vary locally. This is demonstrated by eastern China, which has various depleted xenoliths caused by different degrees of partial melting.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2003년도 추계학술대회
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• pp.127-132
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• 2003

A study of high-pressure n-heptane droplet vaporization is conducted with emphasis placed on equilibrium at vapor-liquid interface. General frame of previous rigorous model[1] is retained but tailored for flash equilibrium calculation of vapor-liquid interfacial thermodynamics. The model is based on complete time-dependent conservation equations with a full account of variable properties and vapor-liquid interfacial thermodynamics. The influences of high-pressure phenomena, including ambient gas solubility, thermodynamic non-ideality, and property variation on the droplet evaporation are investigated. The governing equations and associated moving interfacial boundary conditions are solved numerically using a implicit scheme with the preconditioning method and the dual time integration technique. And a parametric study of entire droplet vaporization history as a function of ambient pressure, temperature has been conducted. Some computational results are compared with Sato's experimental data for the validation of calculations. For low ambient temperatures, the droplet lifetime first increases with pressures, then decreases for high pressures. For higher ambient temperatures, the droplet lifetime increase with less amplitude than that of low ambient temperatures, which then decreases with more amplitude than that of low temperatures. The solubility of nitrogen can not be neglected in the high pressure and it becomes higher as the pressure goes up.

• 한국대기환경학회지
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• 제4권1호
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• pp.13-22
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• 1988

Interactions between hydrodesulfurization of thiophene and hydrodenitrogenation of pyridine and the kinetic analysis were studied over $Ni-W/\gamma-Al_2O_3$ catalysts and this study was made at temperatures ranging from 473-673 K and at total pressures ranging from 10-25 $\times 10^5$ Pa. Hydrodesulfurization of thiophene was inhibited by presence of pyridine at all temperatures studied, and the rate of pyridine hydrodenitrogenation was slower than that of thiophene hydrodesulfurization in the operating conditions. Pyridine hydrodenitrogenation was also inhibited by the presence of thiophene at low temperatures but was enhanced by the thiophene at temperatures higher than 613K. Thiophene reaction rate was determined by multiple linear regression analysis using Langmuir-Hinshelwood-Hougen-Watson model and the result was given to be $r = kP_T^p_H/(1+K_Tp_T+K_Pp_P)^2$. At each temperature, reaction rate constants and absorption equilibrium equilibrium constants were determined and the activation energy was 12.98 kcal/gmol from Arrhenius plot.

• 청정기술
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• 제19권1호
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• pp.8-12
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• 2013

가변부피 투시셀이 장착된 고압 상평형 장치를 사용하여 이산화탄소 + 계면활성제 이성분계와 이산화탄소 + 계면활성제 + 물 삼성분계의 상평형 거동을 318 K부터 348 K의 온도범위에서 관찰하였다. 계면활성제로는 소르비탄 모노팔미테이트를 사용하였다. 이산화탄소 + 소르비탄 모노팔미테이트 이성분계에서 관측된 운점압력은 온도가 상승함에 따라 증가하며, 소르비탄 모노팔미테이트의 조성이 0.226 wt%에서 최대 운점압력이 측정되었다. 반면에 계면활성제의 농도를 0.1 wt%로 고정한 삼성분계에서 관측된 운점압력은 온도와 물의 조성이 증가함에 따라 커지는 것을 확인할 수 있었다. 물의 농도를 0.2 wt%로 고정한 삼성분계에서의 압력-조성의 곡선은 상대적으로 수평의 형태를 나타냈다. 이 때, 운점압력은 온도와 계면활성제의 조성이 증가함에 따라 상승함을 확인할 수 있다.

• 대한화학회지
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• 제19권2호
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• pp.73-84
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• 1975

톨루엔과 요오드 사이의 전하이동착물의 안정도에 미치는 압력과 온도의 영향을 n-헥산용액에서 자외선 분광광도법으로 연구하였다. 압력은 1에서 1,200bar, 온도는 $25^{\circ}C$에서 $60^{\circ}C 사이에서 측정하였다. 착물의 평형상수는 압력 및 온도의 증가와 더불어 증가 및 감소하고 흡수계는 대체로 증가함을 알았다. 이들 각 평형정수로부터 착물 형성에 따른 부피, 엔탈피, 자유에너지 및 엔트로피 변화 양을 구하였다. 또한 압력의 증가에 의한 blue-shift현상 및 압력 변화에 의한 진동자 세기와의 관계를 열역학적 함수와 관계지워 설명하였다

• 암석학회지
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• 제5권1호
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• pp.1-9
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• 1996

Eonyang amethyst deposits are thought to be spatially and temporally associated with the biotite granite of the Kyeongsang Basin. The examined euhedral quartz crystals in cavities in the aplite intruded biotite granite are colored-zoned from white at the base to amethystine at the tops. Three types of primary Inclusions were observed and three is representing each types are constructed to constrain the trapping conditions and fluid evolution involved during the formation of the amethyst. The intersection of the isochore representing the early fluid inclusions with solidus temperature of the host granite indicates initial quartz formation at about $600^{\circ}C$ and 1.0-1.5 kbars . Intermediate quartz formation, associated with the high-salinity inclusions, occurred at somewhat lower temperatures ($400^{circ}c$) and pressures of about 1 kbar. The amethystine quartz formed from $H_2O$-$CO_2$-NaCl fluids at temperatures between 280-$400^{circ}c$ and pressures of about 1 kbar. Early quartz is interpreted to have formed from fluids that either exsolved from or were in equilibrium with the granite at near solidus conditions, whereas the amethystine quartz apparently grew from fluids of at least partial sedimentary origin.

• 설비공학논문집
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• 제8권2호
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• pp.177-186
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• 1996

The characteristics of the flow of pure HFC refrigerants(R32, R125, and R134a) and their mixtures through capillary tubes were investigated experimentally. Two capillary tubes with 1.2mm and 1.6mm inner diameter and 1.5m length were adopted as test sections. Mass flow rates and temperatures and pressures were measured for several condensing temperatures and degrees of subcooling at capillary tube inlet. The effects of the condensing temperature, inner diameter of capillary tube, and subcooling on the mass flow rate of refrigerants were discussed, and the mass flow rates of HFC refrigerants were compared with that of R22. The pressure and temperature distributions along the capillary tube compared with that of R22. The pressure and temperature distributions along the capillary tube show that there is a metastable equilibrium state in the flow through the tube. Underpressure for vaporization increases as refrigerant mass flux increases and inlet subcooling decreases. Empirical correlation was suggested to predict underpressure for vaporization of the HFC refrigerants.

• 분석과학
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• 제24권6호
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• pp.467-476
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• 2011

Methylsulfate 음이온을 갖는 이미다졸리움계 이온성 액체들을 대상으로 이온성 액체에 녹는 이산화탄소의 용해도를 측정하고, 이온성 액체가 가지고 있는 양이온의 변화에 따른 용해도의 차이를 비교하였다. 본 연구에서 사용한 methylsulfate 음이온을 가진 이온성 액체는 1-ethyl-3-methylimidazolium methylsulfate ([emim][$mSO_4$])와 1-butyl-3-methylimidazolium methylsulfate ([bmim][$mSO_4$])였다. 가변부피투시창(variable-volume view cell)이 장착된 고압용 상평형 장치를 사용하여 303.15 K에서 343.15 K까지 온도를 변화시키면서 여러 가지 조성을 갖는 이온성 액체와 이산화탄소의 혼합물의 기포점 압력을 측정함으로써 이온성 액체에서의 고압 이산화탄소의 용해도를 측정하였다. 이온성 액체에서 이산화탄소의 농도가 증가함에 따라 압력이 급격히 증가하였으며, 온도가 증가함에 따라 용해도는 감소하였다. 또한 이미다졸리움 양이온에 붙어 있는 알킬 체인의 길이가 길수록 높은 용해도를 가지는 것으로 나타났다. Peng-Robinson 상태방정식을 사용하여 이온성 액체와 이산화탄소 혼합물 시스템에 대한 상평형 모델링을 수행하였다.

• 설비공학논문집
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• 제19권3호
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• pp.213-219
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• 2007

An experimental apparatus was constructed to obtain vapor-liquid equilibrium data for $CO_2/oil$ mixtures using mass analysis method with sample cylinder. Lubricants employed were POE (poly-ol ester) and PAG (poly alkylene glycol). The phase equilibria of $CO_2/oil$ mixtures prevailed in an equilibrium cell were observed through a couple of sight glasses at the opposite ends. Data were obtained over the temperatures $-10^{\circ}C,\;-5^{\circ}C,\;0^{\circ}C,\;5^{\circ}C,\;10^{\circ}C,\;25^{\circ}C,\;40^{\circ}C,\;60^{\circ}C,\;and\;80^{\circ}C$ under pressures up to 14 MPa and then mole fractions were calculated, respectively In general, more solubility of $CO_2$ is observed in POE than in PAG. Miscibility gap is closed for $CO_2/POE$ mixture but not for $CO_2/PAG$.