• 지구물리
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• 제3권3호
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• pp.141-152
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• 2000

남극반도 엘리펀트섬 북부의 남극-스코시아판 경계부에서 획득한 지구물리 자료(탄성파, 중력자료)는 셰클턴 파쇄대를 따라 지각구조의 급격한 변화를 보여준다. 이들 자료에 의하면 셰클턴 파쇄대의 해저산맥은 남극반도 대륙주변부 앞에서 중단되지만, 파쇄대의 변환단층대는 엘리펀트섬 부근의 주변부까지 계속 연장되며 그 넓이도 확장되고 있음을 보여준다. 즉 셰클턴 파쇄대의 변환단층은 남동쪽으로 내려오면서 (1) 드레이크 해협에서는 지구(graben) 구조의 함몰대, (2) 파쇄대 산맥의 남쪽 끝, 삼중점 바로 남동쪽에서는 해양지각에 대규모 반지구(half-graben) 구조, (3) 남극반도 엘리펀트섬 북쪽 대륙사면을 심하게 변형시키는 단층군으로 그 형태를 변화한다. 셰클턴 파쇄대의 단층대를 따라 두 단계의 판구조 환경 변화가 진행되었다. 첫 번째 단계는 대규모 정단층운동에 의해 반지구구조와 같은 확장구조를 형성시킨 확장력 환경이다. 이 시기는 드레이크 해협의 확장이 진행되었던 중기 마이오신세(약 $10Ma{\sim}20Ma$ 사이)에 해당된 것으로 추정된다. 두 번째 단계는 셰클턴 단층을 역단층운동으로 재활성화 시킨 최근의 압축력 환경으로, 이는 최근 약 6Ma이후 진행된 스코시아판의 서향운동으로 인한 남극판과의 수렴작용에 의한 것이다.

• 한국자기학회지
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• 제12권2호
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• pp.41-45
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• 2002

졸-겔법으로 제조된 La/sub 0.7/Pb/sub 0.3/MnO₃(LPM)박막의 기판 효과에 따른 저 자장 영역에서의 터널형 자기저항 효과에 대하여 연구하였다. 다결정 LPMO 박막은 SiO₂/Si(100) 기판과 그 위에 확산 방지막(diffusion barrier)으로 안정화 지르코니아(yttria-stabilized zirconia, YSZ) 중간층을 도입한 기판에 증착하였으며, 반면에 c-축 방향 성장을 갖는 박막의 경우 LaA1O₃(001) (LAO) 단결정 기판을 사용하였다. LPMO/LAO 박막에서의 rocking curve 측정 결과 full width half maximum (FWHM) 값은 0.32°값을 가짐을 알 수 있었다. 상온(300 K)에서 측정한 자기저항비(MR ratio) 값은 500 Oe리 외부자장을 인가시 LPMO/SiO₂/Si 박막의 경우 0.52%, LPMO/YSZ/SiO₂/Si 박막인 경우는 0.68% 그리고, LPMO/LAO의 경우에는 0.4%에도 미치지 못하는 값을 가졌다. 이때 MR최대값을 나타내는 peaks는 자기이력 곡선의 보자력 부근에서 나타남으로 그 두 결과가 잘 일치함을 보여 주고 있다. 이러한 저 자장 영역에서의 자기저항 값의 타이는 박막 시료의 기판 효과에 의한 grain boundary특성의 차이로부터 기인된다.

• 자원환경지질
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• 제27권1호
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• pp.65-80
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• 1994

The Tertiary $Ch{\check{o}}ngja$ basin is located in the southeastern coastal area of the Korean Peninsula. It is a lozenge shaped fault-bounded basin with circa $5{\times}5km$ areal extent, isolated from other Tertiary basins by the Cretaceous Ulsan Formation in-between. The northwestern boundary of the basin is a domino/listric type normal fault trending $N30^{\circ}E$, whereas its southwestern boundary is a dextral strike-slip fault (trending $N20^{\circ}W$) with a lateral offset of more than 1 km. The basin is bounded by the East Sea on the eastern margin. Basin-fills consist of extrusive volcanic rock (Tangsa Andesites) of Early Miocene (16~22 Ma in radiometric age), unconsolidated fluviatile conglomerate (Kangdong Formation) and shallow brackish-water sandstone ($Sinhy{\check{o}}n$ Formation). The latter yields abundant Vicarya-Anadara molluscan fossils of early Middle Miocene age. The Tertiary strata become younger toward the northwestern boundary-fault of the basin, showing a zonal distribution pattern parallel to the fault: the younger sedimentary formations occupy a narrow zone of 2 km width along the northwestern boundary-fault, whereas the older Tangsa Andesites underlie them unconformably in the eastern and southeastern portions of the basin. The strata in the basin, including the Tangsa Andesites, are tilted (about $20^{\circ}$) toward the northwestern boundary-fault Sedimentary strata thicken toward the boundary-fault, forming a wedge shaped half-graben structure. A number of small-scale syndepositional normal growth faults and graben structures are observed in the sedimentary strata. These extensional structures have the same trend as the normal northwestern boundary-fault which we interpret as a pull-apart detachment fault. These characteristics imply persistent extension during the basin evolution, caused by a NW-SE directed tensional force. The $Ch{\check{o}}ngja$ basin is, thus, a kind of syndepositional tectonic basin evolved in a strike-slip (pull-apart) regime. The latter was caused by a dextral simple shear associated with the NNW-SSE opening of the East Sea. In view of the fact that the normal growth faults do not cut through the uppermost portion of the youngest $Sinhy{\check{o}}n$ Formation, it is inferred that the tensional force came to be inactive in the early Middle Miocene. This is coincident in timing with the termination of the East Sea opening (15 Ma).

• Structural Engineering and Mechanics
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• 제68권4호
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• pp.443-457
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• 2018

In this article, a comparative study has been made to investigate the scattering behaviour of three layered structure model on torsional surface wave. For such model intermediate layer is taken as fiber reinforced composite, resting over a dry sandy Gibson substratum and underlying by different anelastic media. We consider two distinct mediums for topmost layer. In the first case, topmost layer has been taken as fluid saturated homogeneous porous layer, while in the second case the fluid saturated porous layer has been replaced by a transversely isotropic layer. Simple form expression for the secular equation of torsional surface wave has been worked out in both the cases by executing specific boundary conditions, which comprises Whittaker's function and its derivative, for imminent result that have been elaborated asymptotically. Some special cases have been constituted which are in excellent compliance with recorded literatures. For the sake of comparative study, numerical estimation and graphical illustration have been accomplished to identify the effects of the width ratio of the layers, Biot's gravity parameter, sandy parameter, porosity parameter and other heterogeneity parameters corresponding to the layers and half spaces, horizontal compressive and tensile initial stress on the phase velocity of torsional surface wave.

• 대한기계학회논문집
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• 제19권1호
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• pp.219-230
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• 1995

The flow characteristics of a two-dimensional offset jet issuing parallel to a rough wall is experimentally investigated by using a split film probe with the modified Stock's calibration method. The mean velocity and turbulent stresses profiles in the up and down-stream locations of the wall-attachment regions are measured and compared with those of the smooth wall attaching offset jet cases. It is found that the wall-attachment region on the rough wall is wider than on the smooth wall for the same offset height and the jet speed. The position of the maximum velocity point is farther away from the wall than that for the smooth wall case because of the thick wall boundary layer established by the surface roughness. It is concluded that the roughness of the wall accelerates the relaxation process to a redeveloped plane wall jet and produces a quite different turbulent diffusion behavior especially near the wall from comparing with the smooth plane wall jet turbulence.

• 한국초전도저온공학회:학술대회논문집
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• 한국초전도저온공학회 2003년도 추계학술대회 논문집
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• pp.106-108
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• 2003

We fabricated Ni and Ni-W alloys for use as a substrate in YBCO coated conductor applications and evaluated the effect of W in Ni on texture, microstructure and surface morphology, and hardness of substrate. Pure Ni, Ni-2 at.％W, and Ni-5at.％W alloy substrates were prepared by plasma arc melting, cold rolling, and the recrystallization heat treatment at various temperature (700- 130$0^{\circ}C$). It was observed that Ni-W alloy substrates had stronger cube texture and maintained it at higher annealing temperature, compared to pure Ni substrate : The full-width at half- maximums of in-plane texture was 13.40$^{\circ}$ for Ni substrate and 4.42$^{\circ}$-5.57$^{\circ}$ for Ni-W substrate annealed at 100$0^{\circ}C$. In addition, it was observed that the Ni-W substrate had smaller grain size, shallower boundary depth, and higher hardness, compared to those of pure Ni substrate.

• Korea-Australia Rheology Journal
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• 제20권1호
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• pp.15-26
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• 2008

It has been known that there is a viscoelastic instability in the channel flow past a cylinder at high Deborah (De) number. Some of our numerical simulations and a boundary layer analysis indicated that this instability is related to the shear flow in the gap between the cylinder and the channel walls in our previous work. The critical condition for instability initiation may be related to an inflection velocity profile generated by the normal stress near the cylinder surface. At high De, the elastic normal stress coupling with the streamline curvature is responsible for the shear instability, which has been recognized by the community. In this study, an instability criterion for the flow problem is proposed based on the analysis on the pressure gradient and some supporting numerical simulations. The critical De number for various model fluids is given. It increases with the geometrical aspect ratio h/R (half channel width/cylinder radius) and depends on a viscosity ratio ${\beta}$(polymer viscosity/total viscosity) of the model. A shear thinning first normal stress coefficient will delay the instability. An excellent agreement between the predicted critical Deborah number and reported experiments is obtained.

• Progress in Superconductivity
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• 제6권2호
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• pp.133-137
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• 2005

We fabricated the Au/Ni template for YBCO coated conductors and evaluated texture formation and the microstructural evolution. The cube textured Ni substrate was fabricated by rolling and recrystallization annealing, and subsequently Au layer formed on the substrate by electroless-plating method. The texture was evaluated by pole-figure with x-ray goniometer with orientation distribution function (ODF) analysis. The surface roughness and grain boundary morphology of template were characterized by atomic force microscopy (AFM) We observed that Au layer deposited epitaxially on Ni substrate and formed a strong cube texture when plating time was optimized. The full-width at half-maximum (FWHM) was $8.4^{\circ}$ for out-of-plane and $9.98^{\circ}$ for in-plane texture for plating time of 30 min. Microstructural observation showed that the Au layer was homogeneous and dense without formation of crack/microcrack. In addition, we observed that root-mean-square (RMS) and depth of grain boundary were 14.6 nm and 160 $\AA$ for the Au layer, respectively, while those were 27.0 nm and 800 $\AA$ for the Ni substrate, indicating that the electoless-plated Au layer had relatively smooth surface and effectively mollified grain groove.

• Wind and Structures
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• 제15권1호
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• pp.17-26
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• 2012

Modeling swirling wakes is of considerable interest to wind farm designers. The present work is an attempt to develop a computational tool to understand free, far-wake development behind a single rotating wind turbine. Besides the standard momentum and continuity equations from the boundary layer theory in two dimensions, an additional equation for the conservation of angular momentum is introduced to study axisymmetric swirl effects on wake growth. Turbulence is simulated with two options: the standard ${\kappa}-{\varepsilon}$ model and the Reynolds Stress transport model. A finite volume method is used to discretize the governing equations for mean flow and turbulence quantities. A marching algorithm of expanding grids is employed to enclose the growing far-wake and to solve the equations implicitly at every axial step. Axisymmetric far-wakes with/without swirl are studied at different Reynolds numbers and swirl numbers. Wake characteristics such as wake width, half radius, velocity profiles and pressure profiles are computed. Compared with the results obtained under similar flow conditions using the computational software, FLUENT, this far-wake model shows simplicity with acceptable accuracy, covering large wake regions in far-wake study.

• 한국해양학회지
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• 제30권4호
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• pp.355-364
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• 1995

f-plane 혹은 $\beta$-plane을 갖고 강체 회전중인 균질수에 외부로부터 고밀도의 유체 를 계속 주입시 주입된 고밀도 류의 확장형태와 이와 대응하는 기존의 균질수(상층수) 의 흐름을 관찰하였다. 고밀도류는 주입후 편향력에 의해 서안을 따라 흐르면서 내부 로 침투 확장하여 회전축에 비대칭인 모양을 보인다. 특히 $\beta$-plan에서는 바닥 경사도 의 증가에 따른 압력 경도력의 증가에 의한 서안을 따라 흐르는 속도가 증가되고 결국 편향력의 증가로 서안에서의 폭이 f-plane보다 좁게 나타난다. 그러나 남쪽에 이르러 서는 유입수의 국지적인 두께증가로 인해 확장 속도가 동시에 경계면상에서 의 혼합을 유발시키기도 한다. 유입된 고밀도류의 상층의 와도발생과 관련한 역할은 확장경로상 의 국지적인 지형효과의 유발과 유입으로 인한 상층수의 수직운동, 즉 vortex-tube stretching 효과를 발생시키는 것으로 볼 수 있으나 f-plane의 경우는 후자에 해당하 는 반시계 방향의 축대칭류를 생성시킴으로써 지형효과는 서안 경계층에만 존재하는 것으로 관찰되었으며 이때의 지형효과는 북향의 매우 약한 서안 경계류로 나타나고 있 다. 한편 $\beta$-plan에서 의 유입수의 역할은 실험면적의 동쪽반인 내부흐름에서는 h보다 는 dh/SUB $\beta$/dt의 크기가 우세하여 결국 상대와도의 감소경향인 시계방향의 음의 와 도(negative vorticity)의 발생과 서쪽반에서는 경계면의 경사 (tilting)에 의한 지형 효과가 극대화되어 유입수의 방향과 정반대인 강한 흐름이 나타나고 있다.