• 대한전기학회논문지:전기물성ㆍ응용부문C
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• 제53권1호
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• pp.41-46
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• 2004

In this paper, we present a new combined field integral equation (CFIE) formulation for the analysis of electromagnetic scattering from arbitrarily shaped three-dimensional perfectly conducting and piecewise homogeneous dielectric composite body. The conducting/dielectric structures are approximated by planar triangular patches, which have the ability to conform to any geometrical surface. The surface covering the conducting body is replaced by an equivalent surface electric current and the surface of the dielectric by equivalent electric and magnetic currents. The all equivalent currents are approximated in terms of RWG (Rao, Wilton, Glisson) functions. The objective of this paper is to illustrate that the CFIE is a valid methodology in removing defects, which occur at a frequency corresponding to an internal resonance of the structure. Numerical results are presented and compared with solutions obtained using other formulations.

• Advances in robotics research
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• 제2권2호
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• pp.161-182
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• 2018

This paper proposes a novel receding horizon control (RHC) algorithm for formation control of a swarm of unmanned surface vehicles (USVs) using particle swarm optimization (PSO). The proposed control algorithm provides the coordinated path tracking of multi-agent USVs while preventing collisions and considering external disturbances such as ocean currents. A three degrees-of-freedom kinematic model of the USV is used for the RHC with guaranteed stability and convergence by incorporating a sequential Monte Carlo (SMC)-based particle initialization. An ocean current model-based estimator is designed to compensate for the effect of ocean currents on the USVs. This method is compared with the PSO-based RHC algorithms to demonstrate the performance of the formation control and the collision avoidance in the presence of ocean currents through numerical simulations.

• 한국해양학회지
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• 제29권2호
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• pp.83-94
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• 1994

현장 관측, 수리실험 및 수치실험에 의해 진해만 조류 및 조속간차류의 2차원적 변동특성을 연구하였다. 수리 및 수치실험 결과는 현장 관측결과와 비교적 잘 일치하 였다. 가덕수로, 견내량수로 및 진해만의 중앙수로에서 대조기 최강유속은 약 90∼110 cm/s 이고, 소조기 최강유속은 약 30∼40 cm/s 로써 강하게 나타났으며, 조속간 차류 도로 여러개의 와류를 형성하면서 강하게 일어났다. 진해만의 서부해역과 북부해역에 서 대조기 외강유속은 약 30 cm/s 이하, 소조기 최강유속은 약 10 cm/s 이하로써 약하 며, 조속장로 비교적 약하게 일어났다. 가조로 북부해역에서는 북향하는 조속장로 가 조로 이남해역에서는 시계방향으로 회전하는 와류가 발생하였다. 만내에서 표층흐름 은 바람 하천유출수에 의해 강하게 지배되고, 대조류보다 소조기의 흐름이 바람 과 유출수의 영향을 더 많이 받는다.

• 한국콘크리트학회:학술대회논문집
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• 한국콘크리트학회 1997년도 가을 학술발표회 논문집
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• pp.275-280
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• 1997

An experimental study to evaluate corrosion protection systems was undertaken with 47 reinforced concrete slab specimens subjected to cyclic wet and dry saltwater exposure. Corrosion measurements included monitoring marcrocell corrosion currents, which are generally accepted in United States practice. Test results indicate that specimens containing 2 kg/$\textrm{m}^3$ of NaCl an exposed to a 10 percent of NaCl show high values of corrosion currents. For the specimens with water repellent membrane currents kept relatively low numerical values, while test specimens with surface corrosion inhibitor hyprotective systems show high values of corrosion currents. No clear indication of the corrosion inhibitor protective systems might be due to the extremely high chloride exposure of the specimens, which has brought the accelerated corrosion. It would be expected that evaluation of the corrosion protective systems need long-term measurement with specimen exposed les chloride but simulating the real condition.

• Water Engineering Research
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• 제3권1호
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• pp.9-22
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• 2002

In general, two dimensionless numbers are used in predicting the front propagation rate of density currents: the densimetric Froude number and the dimensionless front velocity. The former expresses the front speed in terms of the characteristic length and reduced gravitational acceleration. Previous papers report that the range of this dimensionless number is wide. The other is the dimensionless front velocity, which is a function of the buoyancy flux per unit width. This paper presents the state of the art review of the dimensionless numbers for the front propagation rate of density currents. Values of the densimetric Froude number are found to be consistent when the proper characteristic length is used for normalization. Then, the densimetric Froude number and the dimensionless front velocity are compared by using the experimental data of density currents over a horizontal surface.

• 한국해안해양공학회지
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• 제13권1호
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• pp.46-55
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• 2001

비선형 파랑 모형을 이용하여 해안류를 산정하는 모형이 소개되었다. 기존의 잉여응력을 이용한 수치모형 결과와 비교하였으며, 두 수치모형의 타당성 검토를 위하여 PIV 시스템으로 획득한 실험자료와도 비교하였다. 방파제 및 잠제 후면에서 형성되는 해안류에 대하여 서로 비교한 결과, 소용돌이 흐름의 형태는 유사하나 관측 결과와 비교하여 수치 모형 결과가 대체로 과소평가되고 있다.

• 한국해양학회지
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• 제29권2호
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• pp.95-106
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• 1994

김 등 (1993)에 의해 개발된 3차원 해수유동 수치모델을 사용하여 진해만의 조류 및 취송류를 해석하였다. 만내의 흐름은 주로 지형, 바람 및 하천유출에 의해 지배되 며, 만 입구의 수로보다 내만에서 바람 의 영향을 더 강하게 받는다. 계산된 조류는 현장관측과 잘 일치한다. 조류 및 조석잔차류의 수평 및 연직 유속은 만 입구의 수로 에서는 강하나, 진해만의 서부해역과 북부해역에서는 상대적으로 약하게 일어났다. 저 층과 표층 사이에 유속우 위상차가 일어나며, 위상차는 소조기보다 소조기보다 대조기 에 더 뚜렷하게 나타났다. 또한 만내에서 표층흐름은 바람 및 하천유출류에 의해 강하 게 지배되며, 이러한 현상은 대조기보다 소조기에 더 뚜렷하게 나타났다.

• Ocean and Polar Research
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• 제30권3호
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• pp.313-324
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• 2008

In order to understand the variation of ENSO-related oceanic environments in the tropical and North Pacific Ocean, spatio-temporal variations of sea surface temperature anomaly (SSTA) and sea surface height anomaly (SSHA) are analyzed from distributions of complex empirical orthogonal functions (CEOF). Correlations among warm pool variation, southern oscillation index, and ocean surface currents were also examined with respect to interannual variability of the warm pool in western tropical Pacific. Spatio-temporal distributions of the first CEOF modes for SSTA and SSHA indicate that their variabilities are associated with ENSO events, which have a variance over 30% in the North Pacific. The primary reasons for their variabilities are different; SST is predominantly influenced by the change of barrier layer thickness, while SSH fluctuates with the same phase as propagation of an ENSO episode in the zonal direction. Horizontal boundary of warm pool area, which normally centered around $149^{\circ}E$ in the tropics, seemed to be expanded to the middle and eastern tropical regions by strong zonal currents through the mature phase of an ENSO episode.

• BMB Reports
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• 제49권10호
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• pp.542-547
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• 2016

Acid-sensing ion channels (ASICs) are proton-gated cation channels widely expressed in the nervous system. Proton sensing by ASICs has been known to mediate pain, mechanosensation, taste transduction, learning and memory, and fear. In this study, we investigated the differential subcellular localization of ASIC2a and ASIC3 in heterologous expression systems. While ASIC2a targeted the cell surface itself, ASIC3 was mostly accumulated in the ER with partial expression in the plasma membrane. However, when ASIC3 was co-expressed with ASIC2a, its surface expression was markedly increased. By using bimolecular fluorescence complementation (BiFC) assay, we confirmed the heteromeric association between ASIC2a and ASIC3 subunits. In addition, we observed that the ASIC2a-dependent surface trafficking of ASIC3 remarkably enhanced the sustained component of the currents. Our study demonstrates that ASIC2a can increase the membrane conductance sensitivity to protons by facilitating the surface expression of ASIC3 through herteromeric assembly.

• 한국연안방재학회지
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• 제4권1호
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• pp.7-19
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• 2017

In this study, waves and currents observed by acoustic AWAC, VECTOR and Aquadopp Profiler in Anmok coastal waters were analysed to account for the variability of wave and current and to understand the mechanism of sediment transport generated by wave-induced current in the surf-zone. The monthly variation of wave and residual currents were analysed and processed with long-term observed AWAC data at station W1, located at the water depth of about 18m measured during from February 2015 to September 2016. Wave-induced currents were also analysed with intensive field measurements such as wave, current, suspended sediment, and bathymetry data observed at the surf-zone during in winter and summer. The statistical result of wave data shows that high waves coming from NNE and NE in winter (DEC-FEB) are dominant due to strong winds from NE. But in the other season waves coming from NE and ENE are prevalent due to the seasonal winds from E and SE. The residual currents with southeastern direction parallel to the shoreline are dominant throughout a year except in winter showing in opposite direction. The speed of ebb-dominant southeastern residual currents decreasing from surface to the bottom is strong in summer and fall but weak in winter and spring. By analysing wave-induced current, we found that cross-shore current were generated by swell waves mainly in winter with incoming wave direction about $45^{\circ}$ normal to the shoreline. Depending on the direction of incoming waves, longshore currents in the surf-zone were separated to southeastern and northwestern flows in winter and summer respectively. The variation of observed currents near crescentic bars in the surf-zone shows different direction of longshore and cross-shore currents depending on incoming waves implying to the reason of beach erosion generating the beach cusp and sandbar migration during high waves at Anmok.