• 펄프종이기술
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• 제40권5호
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• pp.36-41
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• 2008

Multi-ply sheet forming has many advantages including the possibility of using wide range of materials in a given structure, lowering production cost, making higher grammage products and so on. But, incorrect structure of sheet makes flow resistance higher so that it shows poor dewatering in press section. One of major factors that affect sheet structure and dewatering property is fines content in each layer. We, therefore, examined the press dewatering of multi-ply sheet that has the different fines content in each layer and the effect of fines distribution on physical properties of sheet to find a technology for optimum utilization of raw materials. In case of two layered sheet, the sheet which was composed of layers with the different flow resistance showed higher dewatering rate than one which has the same flow resistance. And the more difference in fines content for layers existed, the more dewatering occurred. For three layered sheets, dewatering is mainly dependent on fines content of bottom layer. Strength properties were affected by dewatering degree and multi-ply sheet structure.

• 대한전기학회:학술대회논문집
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• 대한전기학회 1993년도 정기총회 및 추계학술대회 논문집 학회본부
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• pp.188-191
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• 1993

Silicon flow sensor which can detect the magnitude and direction of two dimensional air flow was designed and fabricated by CMOS process and bulk micromachining technique. The flow sensor consists of three-layered dielectric diaphragm a heater at the center of the diaphragm and four thermopiles surrounding the heater at each side of diaphragm as sensing elements. This diaphragm structure contributes to improve the sensitivity due to excellent thermal isolation property of dielectric materials and its tiny thickness. The flow sensor has good axial symmetry to sense 2-D air flow with the optimized sensing position in the given structure. Measured sensitivity of our sensor is $18.7mV/(m/s)^{1/2}$.

• Journal of the Korean Society for Industrial and Applied Mathematics
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• 제19권2호
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• pp.197-215
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• 2015

Modeling water flow in variably saturated, porous media is important in many branches of science and engineering. Highly nonlinear relationships between water content and hydraulic conductivity and soil-water pressure result in very steep wetting fronts causing numerical problems. These include poor efficiency when modeling water infiltration into very dry porous media, and numerical oscillation near a steep wetting front. A one-dimensional finite element formulation is developed for the numerical simulation of variably saturated flow systems. First order backward Euler implicit and second order Crank-Nicolson time discretization schemes are adopted as a solution strategy in this formulation based on Picard and Newton iterative techniques. Five examples are used to investigate the numerical performance of two approaches and the different factors are highlighted that can affect their convergence and efficiency. The first test case deals with sharp moisture front that infiltrates into the soil column. It shows the capability of providing a mass-conservative behavior. Saturated conditions are not developed in the second test case. Involving of dry initial condition and steep wetting front are the main numerical complexity of the third test example. Fourth test case is a rapid infiltration of water from the surface, followed by a period of redistribution of the water due to the dynamic boundary condition. The last one-dimensional test case involves flow into a layered soil with variable initial conditions. The numerical results indicate that the Crank-Nicolson scheme is inefficient compared to fully implicit backward Euler scheme for the layered soil problem but offers same accuracy for the other homogeneous soil cases.

• 한국가시화정보학회:학술대회논문집
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• 한국가시화정보학회 2003년도 추계학술대회 논문집
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• pp.75-78
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• 2003

An interfacial instability has recently been observed for the DC- and AC-powered electroosmotic flows of the two miscible electrolyte layers having different concentrations in microchannels. It is rather contrary to our common belief that the flow inside a microchannel is generally stable due to the dominant role of the viscous damping. In this work, we visualized the electroosmotic flow inside a T-channel to validate the numerical predictions. It is clearly shown that the strong vortices (which characterize the interface shapes) are generated at the interface of the two fluids, as was predicted in the numerical analysis.

• 대한기계학회논문집
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• 제13권6호
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• pp.1321-1329
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• 1989

본 논문에서는 성층화된 용액ㅇ네 수평방향으로 온도구배가 가해지는 경우에 있어서 두 부력인자의 상대적 크기에 따라 나타나는 유동형태와 그에 따른 온도, 농도 분포 및 열전달특성을 수치적으로 연구하고자 한다.

• 한국토양환경학회지
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• 제2권3호
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• pp.59-67
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• 1997

다층토양구조에서 유기물과 토양의 깊이가 토양수 이동에 미치는 영향을 조사하기 위하여 풍건한 유기퇴비를 토양에 0, 2, 4, 6%로 처리한 단층과 다층 토양구조를 가진 토양칼럼을 이용하여 포화수리전도도를 측정하였다. 한편 측정된 수리전도도는 현장에서 실제 측정없이 적용하기 위하여 Jury가 제시한 효율적 수리전도도공식을 이용하여 환산한 후 이 수치를 실제값과 비교하여 보았다. 단층과 다층 토양구조의 수리전도도는 토양에 가해진 유기물 함량이 증가함에 따라 수리전도도는 급격히 감소하였으나 다층구조의 경우 토양칼럼의 길이가 길어짐에 따라 길이가 증가된 만큼의 점진적으로 수리전도도가 증가되는 것이 조사되었다. 그러므로 다층구조의 토양에서 실제의 수리전도도값을 얻기 위해서는 Jury 의 효율적 수리전도도공식의 변형이 필요하다.

• 마이크로전자및패키징학회지
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• 제23권4호
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• pp.87-92
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• 2016

전자소자의 방열모듈에서 두께 방향의 열방출 특성에 대한 중요성이 증가하고 있다. 금속과 금속의 본딩 및 유전체와 금속의 본딩 구조를 갖는 2가지 종류의 2층 층상재료를 제조한 후 두께 방향으로 열확산계수를 측정하였다. 금속(STS439)과 금속(Al6061)으로 이루어진 2층 층상재료에서는 섬광법(LFA)으로 열확산계수를 측정했을 때, 열흐름의 방향을 반대로 변화시켜도 열확산계수의 변화가 없었다. 그런데, 유전체(AlN-Polymer)와 금속(Al6061)의 2층 층상재료에서는 열흐름의 방향을 반대로 인가하였을 때 열확산계수는 17.5% 정도 다르게 나타났다. 유전체와 금속의 단면구조를 갖는 2층 층상재료에서, 금속에서 유전체 방향으로 측정한 열확산계수가 유전체에서 금속 방향으로 측정한 열확산계수에 비해 17.5% 작게 나타난 이유는, 금속내의 전자가 갖고 있던 에너지가 유전체 쪽으로 전달되기 위해서는 계면 주변에서 포논의 에너지 형태로 변환될 때 저항이 생기기 때문이다.

• 한국정밀공학회:학술대회논문집
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• 한국정밀공학회 2009년도 춘계학술대회 논문집
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• pp.225-226
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• 2009

• 한국섬유공학회:학술대회논문집
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• 한국섬유공학회 2001년도 학술발표회 논문집(Proceedings of the Korean Textile Conference)
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• pp.217-220
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• 2001

• 한국물환경학회지
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• 제26권2호
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• pp.332-342
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• 2010

A model has been developed to investigate in-river sediment and phosphorus dynamics. This advective-dispersive model is coupled with hydrodynamics and sediment transport submodels to simulate suspended sediment, total dissolved phosphorus, total phosphorus, and particulate phosphorus concentrations under unsteady flow conditions. It emphasizes sediment and phosphorus dynamics in unsteady flow conditions, in which the study differs from many previous solute transport studies, conducted in relatively steady flow conditions. The diffusion wave approaximation was employed for unsteady flow simulations. The first-order adsorption and linear adsorption isotherm model was used on the basis of the three-layered riverbed submodel with riverbed sediment exchange and erosion/deposition processes. Various numerical methods were tested to select a method that had minimal numerical dispersion under unsteady flow conditions. The responses of the model to the change of model parameter values were tested as well.