• 한국전자파학회논문지
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• 제13권4호
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• pp.401-406
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• 2002

마이크로스트립 다층 구조 회로가 MMIC 분야에서 다양하게 적용되고 있다. 이에 따라 서로 다른 높이를 갖는 유전체 층 사이의 효율적인 마이크로스트립 선로 전송을 위해 3차원 계단형 불연속을 갖는 선로에서의 정확한 전달 특성 해석, 등가회로의 유도가 요구된다. 본 연구에서는 FDTD 수치해석 방법과 측정을 통해 얻어진 불연속면의 5 파라미터를 이용하여 T 형 등가회로와 소자 값들을 유도하였으며, 해석 및 측정 결과는 1~5 ㎓ 범위에서 잘 일치함을 확인할 수 있었다.

• Journal of Welding and Joining
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• 제18권3호
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• pp.68-75
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• 2000

The incomplete penetration(IP) discontinuity in butt joint weld, which is detected during safety analysis of the steel bridge by nondestructive evaluation(NDE) method, is classified as unacceptable defect according to the NDE codes and standards. In fact, there are a little allowance in butt joint weld in the view point of design criterion, and also detected IP discontinuity should be classified and evaluated for the fatigue strength and residual life estimation. In this study, we performed fatigue test to evaluate the fatigue strength of high strength steel(SWS490A) containing IP discontinuities in various size, the results compared and classified according to the bridge construction standard specification which published by korea administration of construction and traffic. Experimental results could be used to evaluate and estimate the IP discontinuities considering different stress range in butt joint bridge weld during periodic safety inspection.

• Journal of Mechanical Science and Technology
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• 제16권4호
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• pp.522-531
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• 2002

In order to study the thermal-hydraulic behavior of the cable-in-conduit-conductor (CICC), a numerical model has been developed. In the model, the high heat transfer approximation between superconducting strands and supercritical helium is adopted. The strong coupling of heat transfer at the front of normal zone generates a contact discontinuity in temperature and density. In order to obtain the converged numerical solutions, a moving mesh method is used to capture the contact discontinuity in the short front region of the normal zone. The coupled equation is solved using the finite element method with the artificial viscosity term. Details of the numerical implementation are discussed and the validation of the code is performed for comparison of the results with thse of GANDALF and QSAIT.

• 한국전산구조공학회:학술대회논문집
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• 한국전산구조공학회 2002년도 가을 학술발표회 논문집
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• pp.112-119
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• 2002

In this paper, an Extended Finite Element Method is proposed by adding discontinuity and singularity enrichment functions to the standard FEM approximation. In this method, the singularity and the discontinuity of the crack are efficiently modeled by using initial regular mesh without refining mesh near the crack tip, so that it enables express the asymptotic stress field near crack tip and crack surface successfully. The developed method was verified by evaluating crack tip stress profile and stress intensity factor of mode Ⅰ/mode Ⅱ fracture problems and the results showed the effectiveness and robustness for fracture problem.

• 대한조선학회지
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• 제23권4호
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• pp.1-10
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• 1986

A container ship, due to wide hatch openings, has characteristics of poor torsional rigidity, strong coupling of horizontal-torsional modes and significant discontinuity in the longitudinal variation of hull sections. In the mathematical formulation of the problem the hull is modeled as a beam and the transfer matrix method is utilized. The cross decks between cargo hatch opening are separated from the main hull and regarded as equivalent springs restraining torsion of hull. The effect of shear deformation of ship-side plating on torsion is taken into account in addition to St. Venant's and bending torsional rigidities. Compatibility requirements at cross section discontinuity are approximately considered. Developing the practical calculation procedure and the computer programs for application to an actual ship, some parametric studies on modeling methods of the cross deck, the compatibility condition, added-mass center etc. are out for the purpose of comparison.

• 비파괴검사학회지
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• 제27권6호
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• pp.582-590
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• 2007

Imperfectly jointed interface serves as mechanical waveguide for elastic waves and gives rise to two distinct kinds of guided wave propagating along the interface. Contact acoustic nonlinearity (CAN) is known to plays major role in the generation of these interface waves called generalized Rayleigh waves in non-welded interface. Closed crack is modeled as non-welded interface that has nonlinear discontinuity condition in displacement across its boundary. Mathematical analysis of boundary conditions and wave equation is conducted to investigate the dispersive characteristics of the interface waves. Existence of the generalized Rayleigh wave(interface wave) in nonlinear contact interface is verified in theory where the dispersion equation for the interface wave is formulated and analyzed. It reveals that the interface waves have two distinct modes and that the phase velocity of anti-symmetric wave mode is highly dependent on contact conditions represented by linear and nonlinear dimensionless specific stiffness.

• 한국지진공학회:학술대회논문집
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• 한국지진공학회 2003년도 춘계 학술발표회논문집
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• pp.45-49
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• 2003

The velocity structure beneath the CHNB broadband station is determined by receiver function analysis using by from teleseismic P waveforms. The detailed broadband receiver functions are obtained by stacking method for source-equalized vertical, radial and tangential components of teleseismic P waveforms. A time domain inversion uses the stacked radial receiver function to determine vertical P wave velocity structure beneath the station. The crustal velocity structures beneath the stations are estimated using the receiver function inversion method in the case at the crustal model parameterized by many thin, flat-tying, homogeneous layers. The result of crust at model inversion shows the crustal velocity structure beneath the CHNB station varies smoothly with increasing depth, and there are six discontinuity around 2.5km, 6.25km, 12.5km, 22.5km and 27.5km depth, with Moho discontinuity at about 32.5km depth.

• 한국지진공학회:학술대회논문집
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• 한국지진공학회 2003년도 추계 학술발표회논문집
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• pp.3-7
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• 2003

The velocity structure beneath the CHNB broadband station is determined by receiver function analysis using by from teleseismic P waveforms. The detailed broadband receiver functions are obtained by stacking method for source-equalized vertical, radial and tangential components of teleseismic P waveforms. A time domain inversion uses the stacked radial receiver function to determine vertical P wave velocity structure beneath the station. The crustal velocity structures beneath the stations are estimated using the receiver function inversion method in the case at the crustal model parameterized by many thin, flat-lying, homogeneous layers. Events divide into 4 groups. four azimuths corresponding to events in group a(southwest), b(south), c(southeast), d(northeast). The result of crust at model inversion shows the crustal velocity structure beneath the CHNB station varies smoothly with increasing depth. The conard discontinuity lies around 18 km and moho discontinuity lies range from 30 to 34 km.

• 자원환경지질
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• 제35권5호
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• pp.455-463
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• 2002

자료의 부족 및 육.해양을 동시에 감안해야 하는 상황으로 인하여 아직까지 한반도 중부 대륙에서 해양지역으로 이어지는 대륙연변부에서의 심부지각구조에 관한 심층적인 지구물리학적 연구는 이루어지지 못하였다. 본 연구에서는 중력자료를 이용하여 대륙과 해양을 잇는 대륙연변부 북위37$^{\circ}$~38$^{\circ}$, 동경128$^{\circ}$~132$^{\circ}$지역에 대한 심부지각구조를 해석하였다. WCA보정을 이용하여 해상지역의 선상중력자료에 나타나는 탐사측선상의 잡음으로 판단되는 고주파성분을 제거하고, 보정된 해상지역의 free-air 중력이상을 동일한 고도 기준면을 갖는 육상지역의 부게 중력이상과 결합하였다. 연구지역의 중력이상을 4개 지역으로 나누고, 각각의 지역에 대한 파워스펙트림 분석에 의해 산출한 모호면으로 판단되는 밀도 경계면은 한반도 내륙 부에서 대륙주변부를 지나 동해 울릉분지 쪽으로 갈수록 심도가 점점 얕아지는 양상을 보인다. 파워스펙트럼 결과에 의해 기초 모델로 설정하고 모델링을 실시한 결과, 모호면의 심도는 한반도 내륙지역에서는 약 33~35 km로 나타나고, 대륙주변부에서의 모호면의 심도는 18~28 km로서 한반도 내륙지역에 비해 얕아진다. 이와 같은 구조적 특성은 울릉분지의 주변부를 따라 나타나고 있는 중력변화에서도 잘 나타나고 있다. 울릉도 남쪽 해역에서의 모호면은 약 16~17 km로 대륙 쪽의 모호면 깊이보다 훨씬 얕다. 이와 같이 중력자료로부터 구한 지각모델의 결과는 인근 지역에서 이루어진 탄성파탐사를 통한 지각모델링 결과와 매우 유사하게 나타났다.

• 한국석유지질학회지
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• 제13권1호
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• pp.17-23
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• 2007

ArcGP 중력자료를 이용하여 다산과학기지가 위치한 북극 스발바드 군도의 중력특성을 파악하였다. 지형자료와 유사한 형태로 분포하는 free-air 중력이상에서 보이던 대륙 연변부의 가장자리 효과는 부게보정 후 보이지 않고, 육상지역의 CTOPO30 지형자료를 이용한 지형보정을 거친 완전 부게 중력이상에서 육상지역에서 해양지역으로 갈수록 중력이상이 증가하는 즉, 모호면의 상승과 관련이 깊은 특성이 관찰된다. 파워스펙트럼 분석을 통해 결정된 절단파수를 이용할 필터링 후 계산된 고주파 영역의 잔여이상에서 육상지역의 단층대를 따라 발달하는 특징적인 고이상대와 두꺼운 퇴적층에서 기인한 저이상대가 나타나며 해양지역 대륙사면의 최하부에서 기반 함몰 내지는 기반암 상부의 두꺼운 퇴적층과 관련이 있는 저이상대가 발달하고 있다. 역산 모델링을 통해 저주파 영역 성분에서 계산된 모호면의 기복은 스발바드 군도에서 유라시안 판 경계인 Knipovich ridge쪽으로 갈수록 상승하는 즉, 대륙주변부에서의 전형적인 특성을 보여준다.