• Journal of the KSME
• /
• v.25 no.3
• /
• pp.209-215
• /
• 1985

충격파에 의해 폭말물에 일어나는 화학반응 진행현상을 Forest Fire 모델과 함께 고온 부위에 의한 점화와 표면연소자는 현상학적인 근거위에 개발한 모델 두가지(IAG, Sandia)를 설명하였고 이 위에 고온부위 개념에 물리적인 설명을 부여한 새로운 모델을 소개하였다. 나중 세가지 모 델들을 PBX-9404에 대한 여러 가지 실험결과와 비교하였는 바 화학반응 초기의 압력증가현상은 주로 점화항(고온 부위에 의한)에 기인하는 것으로써 모두 만족할만한 결과를 보여주고 있으며 후기의 현상은 실험치와 약간 달라지는것(크거나 혹은 작거나)이 보인다. 이 오차가 과연 어느 만큼 실험 오차이며, 또 어느만큼이 모델 오차인지에 대하여는 아직 자료의 불충분으로 확정지어 말할 수 없다. 예를 들어 그림 4에서는 실험결과가 이론결과 보다 압력을 더 큰 것으로 나타 내고 있으며 그림 5에서는 그 반대 현상을 보인다 앞으로 이 방면에 더 연구가 진행되어야 하 리라고 고려되며 연후에 이 모델들을 다른 폭발물에 적용시켜 일반화시키는 일이 남아 있다.

• Geophysics and Geophysical Exploration
• /
• v.22 no.1
• /
• pp.21-28
• /
• 2019

We perform a 3D tomographic inversion using surface wave dispersion curves to obtain S-velocity model and radial anisotropy beneath Saudi Arabia. The Arabian Peninsula is geologically and topographically divided into a shield and a platform. We used event data with magnitudes larger than 5.5 and epicentral distances shorter than $40^{\circ}$ during 2008 ~ 2014 from the Saudi Geological Survey. We obtained dispersion curves by using the multiple filtering technique after preprocessing the event data. We constructed SH- and SV-velocity models and consequently radial anisotropy model at 10 ~ 60 km depths by inverting Love and Rayleigh group velocity dispersion curves with period ranges of 5 ~ 140 s, respectively. We observe high-velocity anomalies beneath the Arabian shield at 10 ~ 30 km depths and low-velocity anomalies beneath the Arabian platform at 10 km depth in the SV-velocity model. This discrepancy may be caused by the difference between the Arabian shield and the Arabian platform, that is, the Arabian shield was formed in Proterozoic thereby old and cold, while the Arabian platform is covered by predominant Paleozoic, Mesozoic, and Cenozoic sedimentary layers. Also we obtained radial anisotropy by estimating the differences between SH- and SV-velocity models. Positive anisotropy is observed, which may be generated by lateral tension due to the slab pull of subducting slabs along the Zagros belt.

• Geophysics and Geophysical Exploration
• /
• v.4 no.2
• /
• pp.34-44
• /
• 2001

Forward modeling by construction of synthetic data is usually practiced in a horizontal surface and a few subsurface structures. However, in-situ surveys often take place in such topographic changes that the corrupted field data always make it difficult to interpret the right signals. To examine the propagation characteristic of elastic waves on the irregular surface, a general mesh generation code for finite element method was modified to consider the topography. By implementing this algorithm, the time domain modeling was practiced in some models with surface topography such as mound, channel, etc. The synthetic data obtained by receivers placed on surface also agreed with the analytic solution. The snapshots showing the total wave-field revealed the propagation characteristic of the elastic waves through complex subsurface structures and helped to identify the signals on the time traces. The transmission of Rayleigh waves along the surface, compressive waves, and sheer waves was observed. Moreover, it turned out that the Rayleigh waves behave like a new source at the edge.

• Journal of the KSME
• /
• v.31 no.8
• /
• pp.735-744
• /
• 1991

확산모델과 파모델의 결과에 있어 큰 차이가 일어나는 경우를 요약하면 다음과 같다. 1) 과도기 간이 짧다. 2) 작동온도가 아주 낮다. 3) 온도구배가 상당히 크다. 이때3)의 경우는 서로 다른 물질들이 접촉된 경우 또는 높은 열유속이 있는 경우 또는 얇은 표면층 등을 갖는 문제들의 공 통적인 특징이다. Non-Fourier 열전도 문제를 이용해 온도 분포를 예측해야 하는 실제적인 몇 가지 예를 살펴 보면 레이저 기술 또는 절대온도 영(zero)에 접근하는 온도에서의 액체 헬륨을 다루는 저온공학연구 또는 1/$10^{6}$Inch 정도의 표면조도가 관심사인 정밀공학 등을 들 수 있다. 또한 상당히 높은 강도의 열원이 작용될 때 고체에서의 크랙이나 보이드(void) 같은 국소 결함은 확산거동이 나타나기에 요구되는 시간보다 짧은 시간 구간에서 발생되어질 수 있으며, 크랙발생의 방향과 같은 것들은 hyperbolic 모델에의해 예측되어져야만 한다. 특히 움직이는 열원 또는 propagating crack tip을 갖는 경우에 그들 주위에서의 온도장을 규정짓는 가장 중요한 변 수는 열마하수 M이며, 아음속에서 초음속 영역으로 천이될 때 물리적 양들의 변화에 있어서 일어나는 현상들은 열충격의 형성에 기인하는데 이러한 현상들은 확산 모델로서는 예측될 수 없는 특징들이다. 이상에서 살펴볼 때 non-Fourier 모델에 대해 관심을 기울일 필요가 있다고 사료된다.

• Korean Journal of Materials Research
• /
• v.7 no.8
• /
• pp.694-700
• /
• 1997

TiC(001) 면위에 Mg 금속을 단원자층으로 증착시킨 후 산화 및 열처리 과정을 거쳐서 MgO 초박막을 성장시키고, 성장된 MgO 막의 전자상태 및 표면포논을 UPS, XPS 및 HREELS를 사용하여 측정하였다. 전도성 기판위에 epitaxial 산화물막을 성장시킨 후 성장된 막의 전자구조 및 표면포논을 측정함으로써 벌크에서 분리된 2차원적 특성을 갖는 '표면 모델'의 물성을 연구하고자 하였는데, 이러한 '표면모델'은 잘 배열된 원자구조를 얻을 수 있고 두께가 충분히 얇아서 전하축적을 피할 수 있기 때문이다. 기판으로는 MgO와 같은 암염형 결정구조를 갖고 있고, 격자상수 차이가 2.6% 로서 매우 작으며, 비저항이 매우 낮은 전이 금속 탄화물 중의 하나인 TiC(001) 면을 사용하였다. TiC(001)면에 증착된 MgO층의 UPS He-l 스펙트럼을 측정한 결과 O2p및 XPS스펙트럼은 열처리를 전후로 하여 변하지 않았으며, 이로부터 상온에서 산소의 확산만으로 MgO 상이 형성됨을 알 수 있었다. MgO초박막의 표면 포논을 HREELS를 사용하여 검출하였다. 거시적 포논중에서 F-K 파 및 Rayleigh 모드가 관찰되었는데, F-k파는 MgO막의 2차원성으로 인하여 벌크의 경우보다 높은 진동 에너지를 갖고 있었고 Rayleigh모드는 벌크 MgO와 유사한 분산관계를 보였다. 미시적 포논중에서 Wallis(S/sub 2/)모드가 측정되었는데, 그 진동에너지는 벌크에서와 같고 off-specular방향에서도 소멸되지 않았다.

• Journal of the Society of Naval Architects of Korea
• /
• v.30 no.2
• /
• pp.98-111
• /
• 1993

Two-dimensional nonlinear free-surface wave problems are analyzed with consideration of viscosity. Navier-Stokes equation and continuity equation are solved by the application of Finite Analytic Method, and MAC scheme is used far the treatment of free surface. Surface tension effect is also considered and laminar flow is assumed. The free-surface waves in shallow water, the flows around a vortex-pair with free surface and the wave ahead of a rectangular body are simulated to test the present numerical scheme. In the shallow water problem, viscous effect due to the friction on the bottom is observed. In the second problem, the approach of a vortex-pair to the free surface is simulated to examine the interaction of vortex-pair with the free surface. In the third problem, the wave ahead of a semi-infinite floating body is simulated.

• Journal of the Korean Society for Nondestructive Testing
• /
• v.24 no.3
• /
• pp.259-267
• /
• 2004

A finite element method is used to simulate interaction of laser-based ultrasounds with surface breaking tracks in elastic media. The laser line source focused on the surface of semi-infinite medium is modeled as a shear dipole in 2-D plane strain finite elements. The shear dipole-finite clement model is found to give correct directivity patterns for generated longitudinal and shear waves. The interaction of surface waves with surface breaking cracks (2-D machined slot) is considered in two ways. Both the source and receiver are fixed with respect to the cracks in the first case, while the source is moving in another case. It is shown that the crack depth tested in the range of 0.3-5.0mm $({\lambda}_R/d=0.21{\sim}3.45)$ can be measured using the corner reflected waves produced by the fixed laser source. The moving laser source is found to cause a large amplitude change of reflected waves near crack, and the crack whose depth is one order lower than the wavelength ran be detected from this change.

• Journal of the Korean Society for Aeronautical & Space Sciences
• /
• v.40 no.5
• /
• pp.375-384
• /
• 2012

This paper presents numerical results comparing the performance of the 2008 Wilcox $\mathcal{k}-{\omega}$ turbulence model to the one of the 1988 Wilcox $\mathcal{k}-{\omega}$ model for supersonic flows. A comparison with experimental data is offered for a shock wave/turbulent boundary layer interaction case and two ramp injector mixing cases. Furthermore, a comparison is performed with empirical correlations on the basis of skin friction for flow over a flat plate and shear layer growth for a free shear layer. It is found that the maximum injectant mass fraction of some ramp injector cases is better predicted using the 1988 Wilcox model. On the other hand, the 2008 model performs better in simulating shock-boundary layer cases.

• Journal of Energy Engineering
• /
• v.24 no.1
• /
• pp.114-122
• /
• 2015

In the high convective gas flow condition, irregular shaped water waves from which droplet entrainment occurs are generated under horizontally stratified two-phase flow condition. KAERI proposed a new mechanistic droplet entrainment model based on the momentum balance equation consisting of the shear stress, surface tension, and gravity forces. However, this model requires correlation or experimental data of several physical parameters related to the wave characteristics. In the present study, we tried to measure the physical parameters such as wave slope, wave hypotenuse length, wave velocity, wave frequency, and wavelength experimentally. For this, an experiment was conducted in the horizontal rectangular channel of which width, height, and length are, respectively, 40 mm, 50 mm, and 4.2 m. In the present test, the working fluids are chosen as air and water. The PIV technique was applied not only to obtain images for phase interface waves but also to measure the velocity field of the water flow. Additionally, we developed the parallel wire conductance probe for the confirmation of wave height from PIV image. Finally, we measured the physical parameters to be used in the validation of new droplet entrainment model.

• Journal of the Korea Institute of Information and Communication Engineering
• /
• v.7 no.3
• /
• pp.478-484
• /
• 2003

The electromagnetic wave scattering problems from inhomogeneous material bodies are considered. The formulation is made in terms of mixed potentials for the moment methods (MoM). The surfaces of a three-dimensional inhomogeneous scatterer of arbitrary shape are divide into triangular patches for descretization. Application of the boundary conditions leads to the coupled surface integral equations to be satisfied for the unknown surface equivalent electric and magnetic currents. The radar cross-section (RCS) for some structures is computed and the results are compared with the reported data.