• International Union of Geodesy and Geophysics Korean Journal of Geophysical Research
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• 제25권1호
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• pp.57-81
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• 1997

Numerical prediction of nocturnal thermal high in summer of the 1995 near Taegu city located in a basin has been carried out by a non-hydrostatic numerical model over complex terrain through one-way double nesting technique in the Z following coordinate system. Under the prevailing westerly winds, vertical turbulent fluxes of momentum and heat over mountains for daytime hours are quite strong with a large magnitude of more than $120W/\textrm{m}^2$, but a small one of $5W/\textrm{m}^2$ at the surface of the basin. Convective boundary layer (CBL) is developed with a thickness of about 600m over the ground in the lee side of Mt. Hyungje, and extends to the edge of inland at the interface of land sea in the east. Sensible heat flux near the surface of the top of the mountain is $50W/\textrm{m}^2$, but its flux in the basin is almost zero. Convergence of sensible heat flux occurs from the ground surface toward the atmosphere in the lower layer, causing the layer over the mountain to be warmed up, but no convergance of the flux over the basin results from the significant mixing of air within the CBL. As horizontal transport of sensible heat flux from the top of the mountain toward over the basin results in the continuous accumulation of heat with time, enhancing air temperature at the surface of the basin, especially Taegu city to be higher than $39.3^{\circ}C$. Since latent heat fluxes are $270W/\textrm{m}^2$ near the top of the mountain and $300W/\textrm{m}^2$ along the slope of the mountain and the basin, evaporation of water vapor from the surface of the basin is much higher than one from the mountain and then, horizontal transport of latent heat flux is from the basin toward the mountain, showing relative humidity of 65 to 75% over the mountain to be much greater than 50% to 55% in the basin. At night, sensible heat fluxes have negative values of $-120W/\textrm{m}^2$ along the slope near the top of the mountain and $-50W/\textrm{m}^2$ at the surface of the basin, which indicate gain of heat from the lower atmosphere. Nighttime radiative cooling produces a shallow nocturnal surface inversion layer with a thickness of about 100m, which is much lower than common surface inversion layer, and lifts extremely heated air masses for daytime hours, namely, a warm pool of $34^{\circ}C$ to be isolated over the ground surface in the basin. As heat transfer from the warm pool in the lower atmosphere toward the ground of the basin occurs, the air near the surface of the basin does not much cool down, resulting in the persistence of high temperature at night, called nocturnal thermal high or tropical night. High relative humidity of 75% is found at the surface of the basin under the moderate wind, while slightly low relative humidity of 60% is along the eastern slope of the high mountain, due to adiabatic heating by the srong downslope wind. Air temperature near the surface of the basin with high moisture in the evening does not get lower than that during the day and the high temperature produces nocturnal warming situation.

• 한국응용과학기술학회지
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• 제17권3호
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• pp.158-166
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• 2000

A conductimetric study of foam formed from mixture of the protein, ${\beta}-lactoglobulin$, and the nonioinc surfactant, SML, revealed that their stability was reduced at concentrations of SML in the range $3{\sim}10mM$. The interaction of SML with ${\beta}-lactoglobulin$ was investigated by fluorimetry and a dissociation constant of $0.2{\mu}M$ was calculated for the complex. Surface tension studies confirmed the presence of interaction between the two components and provided evidence for the progressive displacement of ${\beta}-lactogloblin$ from the air/water interface with increasing SML concentration. Experiments using air-suspended microscopic thin liquid films revealed transitions in the chainage characteristics and thickness of the film at SML concentrations below that which resulted in destabilization of the foam. However, measurements of surface mobility of fluorescent-labeled ${\beta}-lactoglobulin$ by a photobleaching method identified that a transition to a mobile system occurred at a SML concentration which correlated with the onset of instability in the disperse phase. The results would indicate that maintenance of the viscoelastic properties of the surface is paramount importance in determining the stability of interfaces comprising mixtures of protein and surfactant.

• The Journal of Advanced Prosthodontics
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• 제3권3호
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• pp.119-125
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• 2011

PURPOSE. The aim of this study was to evaluate the influence of resin cement thickness on the microtensile bond strength between zirconium-oxide ceramic and resin cement. MATERIALS AND METHODS. Thirty-two freshly extracted molars were transversely sectioned at the deep dentin level and bonded to air-abraded zirconium oxide ceramic disks. The specimens were divided into 8 groups based on the experimental conditions (cement type: Rely X UniCem or Panavia F 2.0, cement thickness: 40 or 160 ${\mu}m$, storage: thermocycled or not). They were cut into microbeams and stored in $37^{\circ}C$ distilled water for 24 h. Microbeams of non-thermocycled specimens were submitted to a microtensile test, whereas those of thermocycled groups were thermally cycled for 18,000 times immediately before the microtensile test. Three-way ANOVA and Sheffe's post hoc tests were used for statistical analysis (${\alpha}$=95%). RESULTS. All failures occurred at the resin-zirconia interface. Thermocycled groups showed lower microtensile bond strength than non-thermocycled groups (P<.001). Differences in cement thickness did not influence the resin-zirconia microtensile bond strength given the same resin cement or storage conditions (P>.05). The number of adhesive failures increased after thermocycling in all experimental conditions. No cohesive failure was observed in any experimental group. CONCLUSION. When resin cements of adhesive monomers are applied over air-abraded zirconia restorations, the degree of fit does not influence the resin-zirconia microtensile bond strength.

• 한국진공학회:학술대회논문집
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• 한국진공학회 2012년도 제42회 동계 정기 학술대회 초록집
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• pp.217-217
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• 2012

Solution-processed tungsten oxide thin film with thickness of about 30 nm is prepared from ammonium tungstate. This layer is introduced into the interface between the poly(3-hexylthiophene):[6,6]-phenyl-C61-butyric acid methyl ester (P3HT:PCBM) layer and the ITO electrode to be used as an electron blocking layer. The annealed tungsten oxide thin films at $150^{\circ}C$ and $300^{\circ}C$ show amorphous phase, while the $400^{\circ}C$ -annealed tungsten oxide film shows crystalline phase. At $150^{\circ}C$ annealing temperature, the conversion efficiency is significantly improved from 0.71% to 1.42% as the condition is changed from vacuum to air atmosphere, which is related to oxidation state of tungsten in amorphous phase. For the air annealing condition, the conversion efficiency is further increased from 1.42% to 2.01% as the temperature is increased from $150^{\circ}C$ to $300^{\circ}C$, which is mainly due to the removal of the chemisorbed water. However, a slight deterioration in photovoltaic performance is observed when the temperature is increased to $400^{\circ}C$, which is ascribed to poor electron blocking ability due to the formation of crystalline phase. It is concluded that $W^{6+}$ oxidation state and amorphous nature in tungsten oxide interlayer is essential for blocking electron effectively from the active layer to the ITO electrode.

• 한국구조물진단유지관리공학회 논문집
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• 제18권2호
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• pp.126-133
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• 2014

유체의 흐름에 의해 교량의 교각 및 교대 주변의 하상재료가 유실되는 현상을 말하는 교량 세굴은 교량 파괴의 주요원인이다. 그리고 홍수시 교량의 수위는 교량자체 안전뿐만 아니라 교량을 이용하는 사용자의 안전을 위해도 반드시 확인해야 한다. 따라서 교량의 안전관리를 위해 세굴과 수위계측은 필수적이라 할 수 있다. 본 연구는 기존의 세굴계측의 한계를 극복할 수 있는 새로운 교량세굴 측정방법을 개발하고 현장 검증을 통해 개발 기술의 우수성과 타당성을 확인하였다. 새롭게 개발된 세굴 및 수위 측정방법은 교각에 수직으로 계측장치를 설치하고 일정간격으로 설치된 온도 센서의 온도를 측정하여 수면 위치와 수중 지면의 위치를 추정하는 방법으로 대기온도와 수온, 수온과 수중 지온의 차이를 분석하여 수면 및 수중 지면의 위치를 추정하는 방법이다. 개발 기술은 절대적인 온도 차이뿐만 아니라 대기와 수중 그리고 지중의 일변화량이 서로 다르다는 점을 이용하여 수면의 위치와 수중 지면 위치를 보다 정확하게 추정할 수 있다. 개발 기술의 검증을 위해 소하천 및 실험실, 그리고 교량 교각에서 개발기술을 시범 적용하고, 매질별 온도분포 특성, 시간에 따른 온도변화 추이 등을 분석하여 개발기술이 효과적으로 교량 세굴과 수위를 계측할 수 있는 방법임을 확인하였다.

• 대한방사선치료학회지
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• 제19권2호
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• pp.107-112
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• 2007

목 적: 본원에서 시행하고 있는 전립선암의 세기조절 방사선치료시 직장 내에 존재하는 불균질부에 의한 선량변화를 전산화 치료계획 선량과 자체 제작한 전립선암 환자형 골반 팬톰을 이용하여 측정한 선량을 비교하고자 한다. 대상 및 방법: 전립선암 환자형 골반 팬톰(타원형의 물 팬톰: $30\times20\times20cm^3$, 방광, 직장, 정낭을 묘사하는 팬톰)을 제작하였으며, 전산화단층촬영으로 3차원 영상을 획득하였다. 전산화치료계획장치(ECLIPSE, Varian, USA), 6 MV X선(Clinac 6EX, Varian, USA)을 이용하여 세기조절 방사선치료계획을 수립한 후, 전립선암 환자형 골반 팬톰을 이용하여 직장벽, 방광벽, 정낭 부위에 TLD를 삽입하고, 전산화치료계획 선량과 비교하였다. 결 과: 전산화치료계획에 의한 선량은 직장벽 100%, 방광벽 52%, 우측 정낭 86%, 좌측 정낭 87%, 표면 18%였으나, TLD로 측정 한 선량은 직장벽 89%, 방광벽 54%, 우측 정낭 85%, 좌측 정낭 84%, 표면 17%로 측정되었다. 직장벽은 11%, 방광벽은 2%, 우측 정낭은 1%, 좌측 정낭 3%, 표면 1%의 선량차이를 확인하였다. 결 론: 본원에서 개발한 전립선암 환자형 골반 팬톰으로 전산화치료계획에서 구현하는 불균질부 선량계산의 오차를 확인할 수 있었으며, 다양한 선량 측정 장치(TLD, film)를 이용하여 쉽고 간편하게 선량 검증을 할 수 있을 것으로 사료된다.

• 멤브레인
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• 제5권2호
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• pp.89-96
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• 1995

Azobenzene기를 가지는 인산형 양친매성 화합물의 기/액 계면에 있어서으 단분자막 거동이 $\pi-A$ 곡선 및 표면흡수스펙트라로 검토되었다. 분자간의 강한 수소결합력을 가지는 이 화합물들은 수면에 전개 후 즉시 결정화하여 단분자막 domain들을 형성한 회합체 흡수스펙트라를 나타내었다. 그러나 subphase의 조건(분자량이 큰 유가염의 첨가 및 pH의 상승)을 변화시킴에 의해 결정 domain 형성을 제어하는 것이 가능하였다. 한편, 금속이온 첨가는 인산령 양친매성 단분자막의 분재배향상태를 변화시켰다. 금속이온의 전하가 높을수록 ($1\leq2$ < 3 < 4 가), azobenzene기를 가지는 양친매성 화합물의 분자상태가 tilt된 배향성에 기인하는 장파장으로 이동한 흡수극대를 나타내었다. 이것은 서로 다른 전하를 가진 금속이온을 흡착시킴에 의해 단분자막의 분자배향성을 변화시켜, 단분자막의 집합상태 제어 가능성을 시사한다.

• Journal of the korean society of oceanography
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• 제36권1호
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• pp.19-26
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• 2001

The biological pump is one of the important pumping mechanisms absorbing CO$_2$ from the atmosphere into the ocean and can be quantified by estimating new production. New production in the open ocean mostly depends on the supply of nitrate from the water below the mixed layer. While nitrate is affected by many biological processes, the helium isotope ($^3$He) is inert and has very simple physical properties. Using the $^3$He flux and the relation between $^3$He and NO${_3}\;{^-}$- within the thermocline, the nitrate flux supporting new production was estimated in the southern East Sea. The average ${\delta}^3$He within the mixed layer was -14$%_o$ and -l5.4$%_o$ in the winter and autumn, respectively. Through the year excess $^3$He occurs in the mixed layer except for a slight depletion of -17$%_o$ in summer. The $^3$He flux of 13$%_o$md$^{-1}$ associated with the concentration gradient at the air-sea interface was calculated from the product of the piston velocity and the excess $^3$He. Tritium decay within the mixed layer could support only 2$%_o$md$^{-1}$ of the flux. Thus, the remaining 11$%_o$md^{-1}$ could be attributed to the flux of tritiugenic $^3$He from the water below the mixed layer. Nitrate and $^3$He were positively correlated within the thermocline layer with the slope of 0.21 ${\mu}$mol kg$^{-1}$ $%_o\;^{-1}$. The annual nitrate flux estimated from the upward flux of $^3$He and the NO$_{3}\;{^-}$-$^3$He relation was 0.8${\pm}$0.2 mol(N) m$^{-2}$yr$^{-1}$. This flux corresponds to an annual new production of 64 g(C) m$^{-2}$yr$^{-1}$, which is consistent with that in the north-west Pacific.

• 한국기후변화학회지
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• 제7권2호
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• pp.103-110
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• 2016

In this study, we researched the characteristics of $CH_4$ and $N_2O$ emission of the wastewater treatment (WWT) process in the dairy industry. For flux measurements at the air-water interface, a floating dynamic flow-through chamber was used above the water surface. $CH_4$ and $N_2O$ concentration from the WWT process was measured by NDIR (Non-Dispersive Infrared) Analyser. In the study, $CH_4$ and $N_2O$ fluxes results showed a distinct difference for each WWT process. 60% of the GHG emissions which was the highest percentage were from the equalization tank. Reactor tank was second with 27% of the total emissions from the WWT. Aeration tank was third with 12% of the total emissions. The tendency was that the more the wastewater was treated, the less GHGs were emitted. $CH_4$ and $N_2O$ showed the same tendency. This indicates that the concentrations and properties of wastewater could affect the tendency.

• 한국해양공학회지
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• 제33권4호
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• pp.313-321
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• 2019

The prediction of the hydrodynamic performance of a planing hull vessel is an important and challenging topic for computational fluid dynamic (CFD) applications to naval hydrodynamics. In this paper, the resistance and planing attitude analysis for a Fridsma hull, which is a prismatic planing hull, in still water are numerically studied using OpenFOAM. OpenFOAM is an open source code package based on C++ libraries and the finite volume method (FVM) for the discretization of the RANS equation. The volume of fluid method (VOF) is used to capture the water-air interface and the SST ${\kappa}-{\omega}$ model is used for the turbulence simulation. The overset mesh method is used to capture the large motion of the hull at higher speeds. Before the extensive analysis, uncertainty analyses using various time steps and grid sizes were performed for one ship speed case of Fn = 1.19. The results of the present study are compared with those of a model test, other CFD research, and Savitsky's empirical formula. The results of the present study, following the trend of other CFD results, slightly over predict the resistance and under predict the sinkage and, more significantly, the trim.