• Proceedings of the Korean Vacuum Society Conference
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• 2012.02a
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• pp.199-199
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• 2012

최근 그래핀의 대면적 합성 및 롤투롤 전사 공정의 개발로 그래핀의 상용화가 가시화 되고 있다. 하지만, 그래핀의 독특한 특성인 선형적이고 밴드갭이 없는 에너지 띠 분포 때문에 반도체 소자로서의 직접적인 적용에는 한계가 있다. 이러한 문제를 해결하기 위한 돌파구로써, 그래핀 복합체의 연구와 개발이 활발히 진행되고 있으며 본 연구에서는 그래핀 복합 적층 구조를 다룬다. 이는 디스플레이, 초고속 반도체 소자, 고성능 광전자소자 및 초고감도 센서 등 다양한 분야에 대한 그래핀의 실용화 가능성이 높아진 것을 의미한다. 특히, 높은 가시광 투과도와 낮은 면저항으로 기존 투명 전극에 대표적으로 사용되고 있는 ITO (Indium Tin Oxide)를 그래핀으로 대체하는 것에 관한 연구가 활발히 진행되고 있다. 하지만 그래핀이 높은 전자이동도를 가지는 것에 비하여 비저항과 투과도 측면에 있어서는 ITO의 성능을 뛰어넘지 못하는 실정이다. 따라서 본 연구에서는 ITO가 가지는 취약점인 기판과의 약한 접착력, 높은 취성, 기판과의 열팽창률 차이 등의 공정상 문제점을 극복하고자 하였다. 그래핀 복합 적층 필름은 플라스틱 기판 (PET) 위에 열 화학기상증착법(Chemical Vapor Deposition, CVD)을 이용하여 합성한 그래핀을 전사하고, ITO 용액을 도포한 다음 다시 그래핀을 씌워 제작하여 샌드위치 구조(sandwich structure)를 형성하였다. 완성된 필름은 광학적, 전기적 특성 분석을 수행하였다. 광학적 분석으로는 라만 분광을 이용한 그래핀 품질평가와 파장대에 따른 광 투과도, 그리고 반사도 측정을 하였으며, 전기적 특성은 면저항을 측정함으로써 분석한다. 결함이 적고, 대면적에 걸쳐 한 층을 이루어야 하는 고품질 그래핀의 요구사항에 따라 라만 분광의 G, 2D, D 띠를 분석하였다. G와 2D 띠의 비율을 통해 그래핀의 층 수를, D 띠의 강도를 통해 결함의 유무를 판단하였다. 또한, 가시광 영역에서 90% 이상의 광 투과도를 보여야 하는 투명 소자의 요구사항 달성 정도를 UV-VIS를 이용하여 확인하였다. 마지막으로, 제작한 필름의 면저항 또한 4-프로브 멀티미터를 이용하여 측정하고, 일반적인 터치스크린의 면저항인 $500{\Omega}/sq$를 만족하는지 평가하였다.

• The Journal of the Institute of Internet, Broadcasting and Communication
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• v.23 no.3
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• pp.71-76
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• 2023

In this paper, TE(transverse electric) scattering problems by a resistive strip grating between a grounded double dielectric layer are analyzed by applying the FGMM(fourier galerkin moment method) known as a numerical method of electromagnetic fileld. The boundary conditions are applied to obtain the unknown field coefficients, the scattered electromagnetic fields are expanded in a series of Floquet mode functions, and the resistive boundary condition is applied to analysis of the resistive strip. Overall, as the resistivity decreased, the magnitude of the current density induced in the resistive strip increased, and the reflected power also increased. In case of uniform resistivity, the reflected power decreased as the relative permittivity of the dielectric layers increased or the thickness of the dielectric layer increased. The numerical results for the presented structure in this paper are shown in good agreement compared to those of the existing papers.

• Magazine of the Korea Institute for Structural Maintenance and Inspection
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• v.19 no.2
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• pp.32-38
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• 2015

• Journal of the Korean Vacuum Society
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• v.2 no.1
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• pp.23-27
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• 1993

NiSi2(111)을 Si(111) 표면 위에 증착하여 그 구조를 STM으로 연구하였다. 실리사이드는 그 표면이 (1$\times$1)의 구조를 띠고 여분의 trimer를 흡착 분자 구조로 가짐을 관찰하였다. 이 trimer로부터 실리사이드의 두 가지 구조 A, B를 구별할 수 있었다. 표면에 관착된 결함으로부터 표면구조는 내부와 같음을 보였다.

• Journal of the Korean Magnetics Society
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• v.3 no.3
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• pp.169-172
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• 1993

총에너지 FLAPW(Full-Potential Linearized Augmented Plane Wave) 띠 방법을 이용하여 Li 단층의 구조적, 전자적 성질을 연구하였다. 삼각형 격자와 사각형 격자 구조에 대해 Wigner-Seitz의 반경 $r_{s}$를 변화시키면서 총에너지를 계산한 결과 삼각형구조가 안정하였으며, $r_{s}$가 3.7 a.u. 일때 평형이 되었다. 삼각형구조의 자성을 연구하기 위해, 스핀분극을 계산한 결과 $r_{s}$가 4.2 a.u. 일때 금속 강자성 전이가 일어나며 $r_{s}$가 5.3 a.u. 에서 완전 스핀분극이 되었다.

• The Journal of the Petrological Society of Korea
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• v.25 no.1
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• pp.85-88
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• 2016

The new rocks of the oceanic crust, like basalt, are created in the mid-oceanic ridge, and the magnetic polarities of the rocks are supposed to be oriented as following the Earth's magnetic field. An extensive magnetic survey of total field at sea level reveals mainly unusual north-south magnetic stripes parallel to the axis of the mid-oceanic ridge, especially in the Atlantic Ocean. From this stripes the Earth's magnetic field is considered as repeatedly 'flipped'(the N pole becoming the S pole, and vice versa) and many times over geological time. The discovery of stripes of alternately normal and reversed-magnetized rocks forming the ocean floor has been a key evidence for the sea-floor spreading, continental drift, and plate tectonics. This study introduces a simple apparatus to explain a possible mechanism of the magnetic reversal in the new oceanic crust, which makes a magnetic stripe adjacent to the mid-oceanic ridge. The apparatus shows a bar magnet effect of adjoined stripes to have a special magnetic polarity on the rocks in the center of the mid-oceanic ridge. The new magnetic stripe seems to be generated not only by Earth's magnetic field, but also by neighbored stripes in the mid-oceanic ridge, acting as a bar magnet.

• Applied Chemistry for Engineering
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• v.3 no.2
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• pp.240-246
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• 1992

The electronic structure of oxygen atom of cation-exchanged zeolite was investigated by utilizing X-ray photoelectron spectroscopy(XPS). The obtained $O_{1S}$ spectra of $Na^+-$, $Fe^{2+}-$ and $Fe^{3+}-$ exchanged zeolite X and Y were deconvoluted to demonstrate electronic binding energy of framework oxygens. There were 2-3 bands in each spectrum. The characteristics of separated band have been studied in terms of binding energy and relative area of $O_{1S}$ electron with respect to the exchanged cation. Those bands were assigned to the bridged oxygen in framework (band 1), cation bonded oxygen in cationic site (band 2) and oxygen in water coordinated to the cation (band 3) each other. The band 1 occupying the majority area of $O_{1S}$ spectrum was shifted to higher region on binding energy according to the decrease of Al content in zeolite.

• The Journal of the Institute of Internet, Broadcasting and Communication
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• v.20 no.1
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• pp.77-82
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• 2020

In this paper, E-polarized electromagnetic scattering problems by a conductive strip grating between a double dielectric layer are analyzed by applying the FGMM(Fourier-Galerkin moment method) known as a numerical method of electromagnetic fileld. The boundary conditions are applied to obtain the unknown field coefficients, and the conductive boundary condition is applied to analysis of the conductive strip. The numerical results for the normalized reflected and transmitted power are analyzed by according as the width and spacing of conductive strip, the relative permittivity and thickness of the double dielectric layers, and incident angles. Generally, as the value of the dielectric constant of the double dielectric layer increases, the reflected power increases and the transmitted power decreases, respectively. As the dielectric constant of the double dielectric layer increases, the current density induced in the strip center increases. The numerical results for the presented structure of this paper are shown in good agreement compared to those of the existing papers.

• The Journal of the Institute of Internet, Broadcasting and Communication
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• v.20 no.1
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• pp.83-88
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• 2020

In this paper, H-polarized electromagnetic scattering problems by a conductive strip grating between a grounded double dielectric layer are analyzed by applying the FGMM(Fourier-Galerkin Moment Method) known as a numerical method of electromagnetic fileld. The boundary conditions are applied to obtain the unknown field coefficients, and the conductive boundary condition is applied to analysis of the conductive strip. The numerical results for normalized reflected power are analyzed by according as the width and spacing of conductive strip, the relative permittivity and thickness of the grounded double dielectric layers, and incident angles. Generally, as the value of the dielectric constant and dielectric thickness of a grounded double dielectric layer increases, the reflected power increased. And as dielectric thickness of a grounded double dielectric layer increases, the current density induced in the strip center increases. The numerical results for the presented structure of this paper are shown in good agreement compared to those of the existing papers using the PMM(Point Matching Method).

• Journal of the Korean Magnetics Society
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• v.14 no.3
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• pp.94-98
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• 2004

The electronic structures and magnetism of MgCCo$_3$(001) surface terminated by the plane with the MgCo-Term (Mg, Co terminated) and the CCo-Term (C, Co terminated) were investigated using the all-electron full-potential linearized augmented Plane-wave method. For the MgCo-Term, the magnetic moment of Co atom of the surface is strongly enhanced to 1.00$\mu$$_{B}$, while the magnetic moment of Co atom of the subsurface is similar to that of the center layers. For the CCo-Term, the magnetic moments of Co atoms are enhanced to 0.75 and 0.80$\mu$$_{B}$ for the surface and subsurface layers, respectively. The magnetic moments of C and Mg atoms are coupled antiferromagnetically to that of the neighbour Co atoms. From the calculated density of states, we see that the enhancements of magnetic moments of Co atoms are closely related to localization of the Co-3d states.