• 대한기계학회논문집B
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• 제41권7호
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• pp.481-487
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• 2017

충격파와 경계층의 간섭 현상은 경계층이 박리하고, shock train이 발생하며, 유동장은 매우 복잡한 형태로 된다. 이러한 현상은 반사 충격파와 비정상 경계층이 간섭하는 충격파관에서도 발생한다. 그러나 충격파관에서 발생하는 shock train 현상에 대한 연구는 미비한 실정이다. 본 연구에서는 2차원 축대칭 충격파관을 사용하여 수치해석을 수행하였으며, 충격파관에서 발생하는 shock train의 유동 특성을 상세히 조사하기 위하여 압축성 Navier-Stokes 방정식을 적용하였다. 본 연구의 수치해석 결과를 바탕으로 상세한 파동선도를 통해 실험 결과와 비교하였다.

• Restorative Dentistry and Endodontics
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• 제38권4호
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• pp.222-226
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• 2013

Objectives: The aim of this study was to assess the influence of operator experience level on the lifespan of the WaveOne Primary file (Dentsply Maillefer, Ballaigues, Switzerland) in extracted teeth. Materials and Methods: Moderately curved canals of extracted maxillary and mandibular molars were randomly distributed into 2 groups: experienced and inexperienced operators. Ten files were allocated to each group (n = 10). Each canal was prepared until the working length was reached, and the same file was used to prepare additional canals until it separated. The number of canals prepared before file separation was recorded. The fragment length of each file was measured, and the location of the fragment in the canal was determined. Data were statistically analysed using the independent 2-sample t-test. Results: The 2 operators prepared a total of 324 moderately curved canals of maxillary and mandibular molars. There was no significant intergroup difference in the mean number of canals prepared (p = 0.27). The average lifespan of the WaveOne Primary file was 17.1 and 15.3 canals, and the longest lifespan was 25 and 20 canals, when used by experienced and inexperienced operators, respectively. There were no statistically significant intergroup differences in separated fragment length and location. Conclusions: Within the limitations of this study, operator experience level appears to have no effect on the lifespan of the WaveOne Primary file in preparation of moderately curved canals. Single teeth with multiple canals can be prepared safely even by a novice operator by using a single file.

• 한국항해항만학회지
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• 제36권3호
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• pp.175-180
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• 2012

플로팅 상부구조물은 일반 건축물과 형태는 같지만 기초가 땅이 아닌 하부 부체에 지지되는 구조물로 파랑하중에 의한 영향을 크게 받으며, 파랑하중에 의한 하부구조물의 변형이 접합부에 영향을 미쳐 상부구조물의 이용자에게 사용성 및 안전성의 문제를 발생시키게 된다. 이에 따라 본 논문에서는 3차원 플로팅 구조물의 상부구조물과 하부구조물을 일체화한 전해석을 통하여 강접합과 반강접 접합에 대해 탄성 해석을 실시하였다. 구조물의 전해석과 하부구조물을 제외한 분리해석을 비교 분석 하였으며 탄성 해석을 통해 파랑하중의 CASE를 나누어 파랑하중의 변화에 따른 구조물의 모멘트 및 변위를 접합부에 따라 분류하고 비교하였다.

• 지구물리와물리탐사
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• 제18권2호
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• pp.74-84
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• 2015

탄성 거꿀 참반사 보정(elastic reverse-time migration)을 통해 물리적으로 의미가 있는 영상을 얻기 위해서는 탄성 파동방정식(elastic wave equation)을 통해 재구성된 벡터 파동장(reconstructed vector wavefield)으로부터 P파와 S파를 분리하는 파분리 알고리듬이 필요하다. 그리고 이방성을 고려한 탄성 거꿀 참반사 보정으로의 확장을 위해서는 이방성을 고려한 탄성 모델링 알고리듬 뿐만 아니라 이방성을 고려한 파분리가 필요하다. 이방성 탄성매질에서의 파분리는 등방성 탄성매질에서 주로 이용하는 Helmholtz decomposition과는 달리 탄성매질의 수직 속도 및 이방성 계수에 따라 계산된 유사미분필터(pseudo-derivative filter)를 이용한다. 이 필터는 적용에 많은 계산이 필요하기 때문에 이 연구를 통해 많은 양의 병렬계산을 효율적으로 수행할 수 있는 GPU (Graphic Processing Unit)를 이용하여 이방성 파분리를 수행하는 알고리듬을 개발하였다. 또한 GPU를 이용해 파분리를 수행하는 알고리듬을 포함하고 MPI (Message-Passing Interface)를 이용하는 효율성 높은 이방성 탄성 거꿀 참반사 보정 알고리듬을 개발하였다. 개발된 알고리듬의 검증을 위해 Marmousi-II 탄성모델을 기초로 수직 횡등방성(vertically transversely isotropy; VTI) 탄성모델을 구축하여 수치모형 실험을 수행해 다성분 합성탄성파탐사자료를 생성하였다. 이 합성탄성파 자료에 개발된 이방성 탄성 거꿀 참반사 보정 알고리듬을 적용하여 GPU와 MPI를 효과적으로 이용한 계산속도 향상과 이방성 파분리에 의한 영상결과의 정확도 향상을 보여주었다.

• 한국추진공학회:학술대회논문집
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• 한국추진공학회 2003년도 제21회 추계학술대회 논문집
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• pp.91-94
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• 2003

An experimental study has been carried out in a supersonic blow-down wind tunnel for examining the influence of streamwise vortices on normal shock-wave/boundary layer interaction. It has been reported by the earlier investigator the streamwise vortices generated by the blowing jets can significantly suppress the shock-induced separation and reduce the wave drag. The blowing jets generate the streamwise vortices with 45$^{\circ}$ angle in the spanwise direction. The shock waves are visualized by a Schlieren optical system. Appropriate measurement systems are provided for the characterization of shock wave/boundary layer interaction. The chamber pressure ratio and blowing pressure ratio are varied from 1.5 to 2.4 and 1.0 to 2.0 respectively.

• 대한기계학회논문집A
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• 제20권11호
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• pp.3463-3473
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• 1996

The characteristics of wave propagation along a catenary depend on various impedance conditions; i.e., spatial impedance of catenary, impedance of boundaries. In this study, wave propagation along a simple catenary system is studied with arbitrary impedance conditions such as impedance of pantograph, boundary, catenary etc. Seven coupled equations which determine the characteristics of wave propagation along catenary system have been derived and numerically solved. Results demonstrate the role of each impedance condition in the dynamics of catenary system, i.e. the way in which the conditions affect waves on catenary as well as contact force of pantograph. The formulation and suggested solution method can be certainly used for desinging an optimal catenary system for a given pantograph.

• Progress in Superconductivity
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• 제11권2호
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• pp.112-117
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• 2010

We examine phase transition of the spin density wave and $\pi$ phase shifted superconductivity in the Fe pnictide superconductors. The phase diagram is described in the plane of the temperature T and the doping x with the combination of Ginzburg-Landau expansion of the free energy near the multi-critical temperature $T_c$ and the self-consistent numerical iterations of the gap equations. The phase separation or coexistence is determined by computing the 4-th order terms of the free energy which is confirmed by the numerical calculations. We can show the phase coexistence when the spin density wave is incommensurate. And the first order phase transition is observed near the boundary between commensurate and incommensurate spin density wave.

• 한국해양공학회지
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• 제18권3호
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• pp.13-19
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• 2004

The structural behavior of a worn tire, attached to carbon fiber steel pile by current and wave forces, has been investigated through the numerical method. The finite element model has been developed, by considering that the composite material of rubber and cord is orthotropic, the rubber is isotropic, and that all the material behaves as linear elastic. The pressure distribution by wave and current, around the worn tire, has been estimated through the adjustment for the concept of flow separation. Also, the structural behavior of the worn tire has been examined, by comparing the situation wherein the space between the pile is reinforced, and tire as elastic and isotropic material, with the one left empty. Through this comparison, it is determined that the space between pile and tire has to be filled with elastic and isotropic material, in order to avoid the failure by wave and current action.

• 대한조선학회논문집
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• 제35권2호
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• pp.38-50
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• 1998

부유식 방파제의 특성을 파악하기 위하여 수면 근처에 고정된 상자형 방파제 경우의 방파성능을 실험하고 수치계산과 비교하였다. 상자의 폭과 흘수를 변화시키고 파의 주기와 경사도(wave steepness)를 변화시킴으로써 비교적 다양한 변수변화에 따른 영향을 확인하고자 하였다. 투과계수와 방파제에 작용하는 힘을 실험으로부터 측정하고 선형포텐셜이론에 의해 계산된 결과와 비교함으로써 방파제가 수면근처에 고정된 경우 투과계수와 파력에 대한 흘수 및 파장의 영향을 논하였다. 배열의 경우 폰툰사이의 간격이 투과계수와 파력에 미치는 효과를 논하였고, 전반적으로 계산이 실험의 결과를 효과적으로 예측할 수 있음을 확인하였다.

• 대기
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• 제17권3호
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• pp.231-240
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• 2007

The flow regimes of continuously stratified flow over a double mountain and the effects of a double mountain on wave breaking, upstream blocking, and severe downslope windstorms are investigated using a mesoscale numerical model (ARPS). According to the occurrence or non-occurrence of wave breaking and upstream blocking, three different flow regimes are identified over a double mountain. Higher critical Froude numbers are required for wave breaking and upstream blocking initiation for a double mountain than for an isolated mountain. This means that the nonlinearity and blocking effect for a double mountain is larger than that for an isolated mountain. As the separation distance between two mountains decreases, the degree of flow nonlinearity increases, while the blocking effect decreases. A rapid increase of the surface horizontal velocity downwind of each mountain near the critical mountain height for wave breaking initiation indicates that severe downslope windstorms are enhanced by wave breaking. For the flow with wave breaking, the numerically calculated surface drag is much larger than theoretically calculated one because the region with the maximum negative perturbation pressure moves from the top to the downwind slope of each mountain as the internal jump propagating downwind occurs.