• 대한기계학회:학술대회논문집
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• 대한기계학회 2004년도 춘계학술대회
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• pp.1201-1206
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• 2004

This paper deals with the numerical analysis of natural convection flow induced by the density inversion effect of water inside horizontal pipe. The numerical method is based on SIMPLE/PWIM in general coordinate for its wide applicabilities. The numerical tool was validated through the comparison with the previous results concerning the density inversion effect of water It is shown that the developed numerical tool could predict the flow pattern and the heat transfer phenomena qualitatively And it is also found that the density inversion effect of water has significant effects on the flow pattern.

• 해양환경안전학회지
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• 제10권1호
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• pp.55-59
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• 2004

1995년도 1996년 6월에 실시된 CREAMS 항해 관측 자료를 이용하여 Wasaka bay 연안역의 수온역전 현상을 조사하였다. 수온역전현상은 대부분 20m 이천의 상층부에 위치하였으며, 특히 쓰시마난류와 연안수와의 경계역 부분에 형성되었다. 쓰시마난류는 고온${\cdot}$고염분수의 특징을 가지며, 이러한 고수온은 경계역 부분에서 수온역전 현상을 초래하여 밀도 역전현상을 일으키는 작용을 하는 반면, 고염분은 밀도를 증가시켜 주는 작용을 하여 수온역전에 따른 밀도역전현상을 막아주는 역할을 한다.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.379-382
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• 2003

In gravity data correction process, mass effect of the upper part of base level is removed with Bouguer density. Usually, Bouguer density is estimated as a mean density in the field area. But, this may causes a serious problem when ore body is in the area. To overcome this problem, we tried to apply a new method mixing up mass corrections and inversion (3DGTI). 3-D Gravity Terrain Inversion (3DGTI) includes information of topography and distribution of Bouguer density. For this method does not remove the mass effect above base level, it is no longer useless to use Bouguer density. Numerical model tests have shown that the 3DGIT successfully retrieves the anomalous subsurface density distribution of both surface and deeper layers. Model tests shows that this method shows better results than those of conventional one, especially when main target is ore body. The inversion result well delineates the three-dimensional shape of the intruded granite body and basement.

• 자원환경지질
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• 제27권5호
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• pp.479-489
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• 1994

In this paper, the iterative least-squares inversion method is used to determine shapes and density contrasts of 2-D structures from the gravity data. The 2-D structures are represented by their cross-sections of N-sided polygons with density contrasts which are constant or varying with depth. Gravity data are calculated by theoretical formulas for the above structure models. The data are considered as observed ones and used for inversions. The inversions are performed by the following processes: I) polygon's vertices and density contrast are initially assumed, 2) gravity are calculated for the assumed model and error between the true (observed) and calculated gravity are determined, 3) new vertices and density contrast are determined from the error by using the damped least-squares inversion method, and 4) final model is determined when the error is very small. Results of this study show that the shape and density contrast of each model are accurately determined when the density contrast is constant or vertical density gradient is known. In case where the density gradient is unknown, the inversion gives incorrect results. But the shape and density gradient of the model are determined when the surface density contrast is known.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.340-343
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• 2003

This study presents a practical procedure for the Bayesian inversion of geophysical data by Markov chain Monte Carlo (MCMC) sampling and geostatistics. We have applied geostatistical techniques for the acquisition of prior model information, and then the MCMC method was adopted to infer the characteristics of the marginal distributions of model parameters. For the Bayesian inversion of dipole-dipole array resistivity data, we have used the indicator kriging and simulation techniques to generate cumulative density functions from Schlumberger array resistivity data and well logging data, and obtained prior information by cokriging and simulations from covariogram models. The indicator approach makes it possible to incorporate non-parametric information into the probabilistic density function. We have also adopted the MCMC approach, based on Gibbs sampling, to examine the characteristics of a posteriori probability density function and the marginal distribution of each parameter. This approach provides an effective way to treat Bayesian inversion of geophysical data and reduce the non-uniqueness by incorporating various prior information.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2008년도 공동학술대회
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• pp.167-172
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• 2008

경북 문경군 가은읍 가은역 일대 석회암 분포 지역에서 지하 공동의 위치 및 발달 양상을 파악하기 위하여 고정밀 중력탐사를 하였다. 측점 간격은 4m로 하여 모두 약 1,100 측점에서 중력을 측정하였다. 잔여 부게 이상도에서 가장 낮은 중력 이상대를 지나는 3개의 측선에 대하여 MS(minimum support) 역산으로 밀도 분포 단면을 작성하였다. 또한, growing body 역산을 이용하여 3차원 밀도 분포 영상을 구하였다. 2차원과 3차원 밀도 분포도는 공동이 발달한 지역을 잘 가리키고 있으며, 석회암이 지하수에 부분적으로 용해되어 복잡한 형태의 공동 시스템을 구성하고 있고 부분적으로는 상당히 얕은 곳까지 발달해 있을 것으로 해석된다.

• 지구물리와물리탐사
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• 제20권4호
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• pp.226-231
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• 2017

고정밀 중력 탐사는 천부의 소규모 밀도 이상 구조를 명확하게 탐지하는 것을 목적으로 하므로, 정밀한 측정과 보정뿐 아니라 소규모 이상 구조를 명확하게 분석해 낼 수 있는 역산법도 필요하다. 이것은 역산에서의 타당치 않은(ill-posed) 문제를 해결하기 위한 안정자를 밀도가 급격하게 변화하는 경계부를 분명하게 구분할 수 있도록 설계함으로써 가능해 진다. 이 논문은 다양한 탐사 목적에 대응할 수 있도록 여러 가지 역산 알고리즘을 포함하는 2차원 고정밀 중력 역산 패키지를 구성하였다. 패키지는 Matlab 기반으로 작성하였으며, 최선의 역산 결과를 얻을 수 있도록 대화형으로 만들었다. 몇 가지 대표적인 모델에 대한 수치모델링 자료에 역산 패키지에 포함되어 있는 여러 가지 역산 알고리듬을 적용하여 역산 방법들을 비교 및 검토하였다. 마지막으로 실제 탐사 자료에도 적용하였다.

• 충청수학회지
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• 제22권3호
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• pp.519-524
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• 2009

In multivariate analysis, the inversion formula of the Stieltjes transform is used to find the density of a spectral distribution of random matrices of sample covariance type. Let $B_{n}\;=\;\frac{1}{n}Y_{m}^{T}T_{m}Y_{m}$ where $Ym\;=\;[Y_{ij}]_{m{\times}n}$ is with independent, identically distributed entries and $T_m$ is an $m{\times}m$ symmetric nonnegative definite random matrix independent of the $Y_{ij}{^{\prime}}s$. In the present paper, using the inversion formula of the Stieltjes transform, we will find the density function of the limiting distribution of $B_n$ away from zero.

• Journal of Electrical Engineering and Technology
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• 제9권2호
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• pp.649-654
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• 2014

In this paper, an analytical model for Surrounding Gate (SG) metal-oxide- semiconductor field effect transistors (MOSFETs) considering quantum effects is presented. To achieve this goal, we have used variational approach for solving the Poission and Schrodinger equations. This model is developed to provide an analytical expression for inversion charge distribution function for all regions of device operation. This expression is used to calculate the other important parameters like inversion charge density, threshold voltage, drain current and gate capacitance. The calculated expressions for the above parameters are simple and accurate. This paper also focuses on the gate tunneling issue associated with high dielectric constant. The validity of this model was checked for the devices with different dimensions and bias voltages. The calculated results are compared with the simulation results and they show good agreement.

• 설비공학논문집
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• 제7권4호
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• pp.547-555
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• 1995

Melting process of ice in a rectangular cavity with different temperature walls has been studied experimentally. Front shape of ice and melting rate were affected by initial temperature of ice and variation of temperature distribution and density gradient. When the hot wall temperature was below $8^{\circ}C$, the melting rates were higher at the bottom than those of at the top due to the density inversion, but with increasing the hot wall temperature the melting rates at the top were affected by hot wall and were higher than those of at the bottom. When the initial temperature of ice was low, melting rates were low, but with increasing the time melting rates were almost the same with those of each initial temperature of ice.