• 한국해양학회지:바다
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• 제17권4호
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• pp.203-224
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• 2012

실질적인 하구환경의 관리를 위해서는 관리구역, 즉 하구역이 먼저 정의되어야 한다. 그러나 하구역의 경계를 설정할 수 있는 과학적 자료의 부족으로 인해 아직까지 체계적인 경계설정 방법이 제시되지 못하고 있다. 본 연구는 하구의 물리화학적 특성 등의 과학적 자료와 더불어 지리 지형적 특성 및 이용개발 특성 등을 종합적으로 고려하여 체계적으로 하구역 경계를 설정하는 방법을 제안하였다. 하구를 하구순환의 유지여부에 따라 열린 하구와 닫힌 하구로 구분하고, 각 유형에 속한 개별 하구에 대해 물리화학, 지리지형학 및 이용개발 특성을 고려하여 하구수역의 경계를 설정한 후에 하구수역에 영향을 미치는 하구육역의 경계를 설정하는 순차적인 방법이다. 이 방법에 따라 국내 274개 하구역의 경계를 시범적으로 설정해본 결과 각 하구별로 가용한 자료의 수준과 지역 특성의 차이를 합리적으로 고려한 하구역 경계 설정이 가능한 것으로 나타났다.

• 한국정밀공학회:학술대회논문집
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• 한국정밀공학회 1994년도 추계학술대회 논문집
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• pp.837-842
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• 1994

The boundary element method was used for studying singularities of an interface crack with contact zones. Because the contact zone size was extremely small in a tention field, a large number of Gaussian points were is used for numerical integration of the Kernels. In order to estimate the contact zone size, iteration method was used. The interface crack tips with contact zones showed no oscillatory behavior and J-integral values across the interface were conserved.

• 전산구조공학
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• 제9권4호
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• pp.127-134
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• 1996

본 논문은 경계요소법에 의한 콘크리트의 진행성 파괴해석에 관한 연구이다. 콘크리트의 파괴진행해석을 위하여 경계요소법에 의한 변위 및 표면력 경계 적분방정식으로부터 균열을 포함한 연속체의 균열 경계적분 방정식을 정식화하였다. 콘크리트의 균열진행을 해석하기 위하여 균열 선단에서의 파괴진행영역을 Dugdale-Barenblatt형 모델을 사용하여 모델링하였고 균열진행영역의 인장연화상태를 선형으로 가정하여 모델링하였다. 정식화된 경계적분방정식에 의한 콘크리트 보와 여러가지 하중상태에 있는 인장시편에 대한 진행성 파괴해석을 실시하였으며 해석치와 실험치의 비교로부터 경계요소법에 의한 진행성 파괴해석방법은 최대하중 및 최대하중 이후의 거동을 포함한 콘크리트 구조물의 비선형 거동을 잘 예측함을 보여주고 있다 .

• 한국진공학회지
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• 제15권2호
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• pp.162-167
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• 2006

[ $GaAs_{1-x}N_{x}$ ]의 전도띠 바닥전자상태의 특성을 Ge 기판위에 성장시킨 $GaAs_{1-x}N_{x}(x{\leq}0.7)$ 박막에 대한 공명라만산란 실험을 수행함으로써 조사하였다. LO(longitudinal optical)-phonon 라만세기의 강한 공명상승이 $E_+$ 뿐만 아니라 $E_0$ 전이에너지 근처에서 관측되었다. 그러나 $E_+$ 전이에너지 아래와 근처에서 관측되는 분명한 LO-phonon 선폭 공명상승과 다양한 X와 L 영역경계 (zone-boundary) phonon의 활성화와는 대조적으로, $E_0$ 전이에너지 근처에서는 어떠한 LO-phonon 선폭 확장공명이나 날카로운 영역경계 phonon의 활성화가 관측되지 않았다. 관찰된 공명라만산란 결과는 GaAsN의 전도띠 바닥전자상태가 비국소화된 bulk GaAs와 거의 흡사한 ${\Gamma}$대칭 상태로 구성되었다는 사실을 의미한다.

• 자원환경지질
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• 제26권4호
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• pp.473-487
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• 1993

The Janggun mine area is occupied by the Proterzoic and the Paleozoic meta-pelites, which are intruded by the Jurassic Chunyang granite. The metamorphic terrain is divided into four zones of progressive metamorphism on the basis of mineral assemblages. The zones are chlorite zone, staurolite zone, andalusite zone, sillimanite zone ascending order. Boundary lines between the zones resemble outline of the Chunyang granite mass. Isograd reactions are chlorite+chloritoid+muscovite=staurolite+biotite+quartz+water, staurolite+chlorite+muscovite+quartz=andalusite+biotite+water, and staurolite+muscovite+quartz=andalusite+biotite+garnet+water between the chlorite zone and the staurolite zone, the staurolite zone and the andalusite zone, and the andalusite zone and the sillimanite zone, repectively. They are univariant reactions in KFMASH component system. Metamorphic conditions estimated from garnet-biotite geothermometers and phase equlibria are $530^{\circ}C$ and lower than 4 kb.

• 자원환경지질
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• 제24권4호
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• pp.435-446
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• 1991

Ductile shear zones developed in Jurassic granites in the Yonggwang area show NE trend at the eastern part and nearly EW trend at the western part, respectively. Judged from shear sense indicators, they have resulted from dextral strike-slip movement. The intersection of both trends is thought to be due to the truncation and offset of NE shear zone Chonju Shear zone by the brittle Yonggwang fault which runs in near EW direction with sinistral movement sense. The simple shear deformation was predominate through the deformation in this ductile shear zone. Based on this deformation mechanism, the shear strain (${\gamma}$) estimated in domain 1 increases from 0.14 at the shear zone margin to 9.41 toward the center of shear zone. Total displacement obtained only from this measured section(JK 59 to JK14) appecars to be 1434.5 meters. The sequential development of microstructures can be divided into three stages; weakly-foliated, well-foliated and banded-foliated stages. In the weakly-foliated stage dislocation glide mechanism might be predominant. In the well-foliated stage grain boundary migration and progressive misorientation of subgrains was remarkable during dynamic recovery and recrystallization. In the banded-foliated stage grain boundary sliding and microfracturing mechanisms accompanied with crushing and cracking were marked. According to strain analysis from quartzites of the metasedimentary rocks, strain intensity (${\gamma}$) of the samples within the ductile shear zone ranges from 2.7 to 5.7, while that of the samples out of the ductile shear zone appears to be about 1.7.

• Structural Engineering and Mechanics
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• 제48권6호
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• pp.775-789
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• 2013

The current paper proposes a boundary element formulation, applicable to 2-D and 3-D elastostatics problems using a unified approach for transformations of the domain integrals into boundary integrals. The method is applicable to linear problems encompassing both finite and infinite multi-region domains allowing non-vanishing body forces. Numerical results agree quite well with the analytical solutions; while the present method offers easy formulation with less numerical efforts in comparison to FEM or some BEM which need interior points to treat arbitrary body forces. It is demonstrated that the method has the potential to have profound impact on engineering design, notably in dam-foundation interaction.

• 전산구조공학
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• 제8권2호
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• pp.147-151
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• 1995

이 논문에서는 시간영역 경계요소법을 사용하여 탄성-점탄성 복합구조체의 변위와 응력을 구하는 과정을 다루고 있다. 종속영역법을 도입하여, 구조물을 탄성영역과 점탄성영역으로 나누었다. 구조물의 공유경계면에 변위연속조건과 표면력 평형조건을 적용하여, 경계요소공식을 유도하였다. 예제의 문제에 대한 수치해석 결과를 제시하였다.

• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 2000년도 가을 학술발표회논문집(I)
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• pp.589-594
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• 2000

The necessary strength and ductility to avoid structural damage under moderate earthquake can be achieved by properly detailed transverse reinforcement in the plastic hinge zone. However, most structural walls have a higher aspect ratio(M/Vl\ulcorner) without well confined boundary regions. Therefore there is a need for adequate detailing in the plastic hinge zone, particularly boundary regions. In this paper, the fabricated interlocking spirals is introduced as a new seismic detailing for ductile behavior of the structural walls to be able to substitute for existing complicated detailing with ties. This paper also investigates the behavior characteristics of structural walls with interlocking spirals including confinement of the concrete and strength associated with flexure and shear.

• Journal of Welding and Joining
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• 제31권3호
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• pp.31-38
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• 2013

The transition of serrated grain boundary and its effect on liquation behavior in the simulated weld heat-affected zone (HAZ) have been investigated in a wrought Ni-based superalloy Alloy 263. Recently, the present authors have found that grain boundary serration occurs in the absence of adjacent coarse ${\gamma}^{\prime}$ particles or $M_{23}C_6$ carbides when a specimen is direct-aged with a combination of slow cooling from solution treatment temperature to aging temperature. The present study was initiated to determine the interdependence of the serration and HAZ property with a consideration of this serration as a potential for the use of a hot-cracking resistant microstructure. A crystallographic study indicated that the serration led to a change in grain boundary character as special boundary with a lower interfacial energy as those terminated by low-index {111} boundary planes. It was found that the serrated grain boundaries are highly resistant to boron enrichment, and suppress effectively grain coarsening in HAZ. Furthermore, the serrated grain boundaries showed a higher resistance to susceptibility of liquation cracking. These results was discussed in terms of a significant decrease in interfacial energy of grain boundary by the serration.