• Computational Structural Engineering
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• v.10 no.3
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• pp.46-51
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• 1997

본 고에서는 3차원 전선구조해석에 사용하는 직접구조해석기법 및 준직접구조해석기법에 대하여 설명하고 실선계산을 통하여 두 기법의 차이를 비교하였다. 직접구조해석은 준직접구조해석에 비하여 방대한 시간 및 노력이 요구되기 때문에 전선구조해석의 목적으로 사용하기에는 추천할 기법은 아니나 준직접구조해석의 검증, 피로해석 및 신로도 해석 등 응력의 확률 기준이 필요한 경우에는 필수적으로 수행해야 할 것이다.

• 전기의세계
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• v.29 no.9
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• pp.551-560
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• 1980

본고의 내용은 다음과 같다. 1. 절연전선의 구조 2. 절연전선의 사고특징 3. 절연전선의 단선 및 낙하방지 4. 고장보호 계전방식 5. 검토

• 한국해양학회지
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• v.25 no.2
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• pp.84-95
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• 1990

Observations by CTD castings, moored current meters and satellite imageries reveal some physical characteristics of the area around the tidal mixing front found in the mid-Yellow Sea off Korea. Tidal mixing is the greatest at the promontory of Taean Peninsula with a front around it. The front appears in April with the start of solar heating, becomes most clear in August and disappears in November with the start of surface cooling. In the north of the front, tidal fluctuations of temperature and salinity induced by tidal currents manifest the existence of the front, Differently from the usual tidal mixing front, the front in Kyunggi Bay is formed by presence of the water discharged from the Han River which meets the offshore water at the front. Near the surface cold center, vertically well-mixed zone extends to about 50 Km offshore from the coast, Farther south, this structure is generally retained but with lesser degree of vertical mixing. Within the relatively well-fixed coastal zone, the fresh water discharged from the Kum River makes another salinity front of smaller extent. At some places around this salinity front, an Upwelling-like feature is remarked.

• Computational Structural Engineering
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• v.22 no.4
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• pp.89-94
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• 2009

최근에 선박의 도킹해석은 3차원 전선 구조 해석을 통해 수행되어 왔으나 도킹해석 모델을 구성하는데 많은 시간과 노력이 필요하였다. 전선구조해석 모벨을 만들기 위해 필요한 선박구조 도면이 완성되기 전인 초기 설계단계에서 도킹시 반목배치를 조기에 확정하고, 구조 안정성을 확보하기 위한 노력이 요구되어 왔기 때문에 간이화된 도킹 해석 프로그램을 개발하게 되었다. 2차원 격자구조를 이용한 도킹해석기법을 통해 얻은 반목에서의 지지력이 3차원 전선해석모델을 사용하여 얻은 반목에서의 반력 결과와 비교해 타당한 결과를 보여 주고 있음을 확인하였다. 간이화된 도킹용 해석 프로그램을 개발하였으며, 다음과 같은 기능을 갖추어 사용자가 쉽게 격자 구조 모델을 생생하고 해석을 수행할 수 있도록 구성하였다. 향후 각 요소의 단면 특성치를 자동으로 산정하는 기능이 추가되어야 한다. 그리고 부유식 도크(Floating dock)에서의 도킹해석은 본 개발의 대상이 된 건식 도크(Dry dock)에서의 경우와 다른 고려사항이 추가되어야 하기 때문에 향후 추가적인 연구와 개발을 통해 새로운 기능으로 포함될 것이다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.8 no.3
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• pp.327-339
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• 2003

During the winter in February 1998, January and April 1999, interdisciplinary research was conducted in a large area including the South Sea of Korea and northern East China Sea to examine distribution and structure. Water masses identified from the observed data are Warm Water originated from Tsushima Warm Current, Yellow Sea Cold Water (Northern or Central Cold Water) and Korean Southern Sea Cold Water. In the southern Yellow Sea, Warm Water originated from Tsushima Warm Current, flowing into the Cheju Strait after turning around the western Cheju Island, makes a front of '┍' shape, which is bounded by the Yellow Sea Central Cold Water in the southern part of Daeheuksan Island and by the Yellow Sea Northern Cold Water in the eastern part of the Yangtze Bank. This front changes its corner shape and position with strength of the warm water extension toward northwestern Yellow Sea. The position and structure of the fronts off the southwestern tip of the Korean peninsular and near the Yangtze Bank varies with observation period. In the front in the South Sea of Korea, cold coastal water which if formed independently due to local cooling, ,sinks along the sloping bottom. We explained the processes of variations in the distribution and structure of these winter fronts in terms of up-wind and down-wind flow by the seasonal monsoon, heat budget through the sea surface and density difference across the fronts.

• Proceedings of the KIEE Conference
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• 2008.04b
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• pp.185-187
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• 2008

ACSR-OC 전선은 알루미늄, 아연 및 철 등 세 가지 금속이 서로 접촉되는 이질구조이므로 도체 내에 전해질의 수용액이 존재할 경우 전해부식이 일어나기 쉽고 표면이 손상되었을 경우는 서지의 고정점으로 작용하여 단선될 우려가 있다. Al 절연전선이 염분에 의해 발생되는 변화를 살펴보았다. 시료는 10년이상 현장에서 사용한 후 천거한 전선과 신품에 대해 기계적 강도시험(KSC 3113의 5.4.3 (인장하중시험)), 소선의 성분분석(SEM) 및 현미경 관찰을 실시하였다. 실험결과, 철거전선 표면에서는 알루미늄 외 산소, 염소(Cl), 나트륨(Na) 등이 관찰되었으며 소선은 부식 또는 진행 중이어서 전선의 인장력이 저하되어 있었다. 또 표면이 손상된 전선에 대해 파괴시험, 현미경 관찰 등을 실시하여 절연에 미치는 영항을 조사하였다.

• Korean Journal of Ichthyology
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• v.11 no.1
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• pp.72-85
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• 1999

A study on the larval fish assemblage around the front area was conducted in the Korea Strait in August, 1993. The front was found in the shelf break located in $35{\sim}36^{\circ}N$. A total of 125 species were found in the study area. Of these Engraulis japonicus was the most dominant species comprising 84.3% of the total fish larvae collected and followed by Maurolicus muelleri accounting for 7.7%. Gobiidae, Callionymidae and Pomacentridae showed higher frequency of occurrence. These five species can be divided into three groups. First group was comprised in the larval fish species such as E. japonicus and Callionymidae which were found in the whole study area. The second group was comprised of Gobiidae and Pomacentridae which were found in the warm area located in the southern part of the front area. The other species was M. muelleri found in the cold area located in the northern part of the front area including the front area. The assemblage, geological distribution and body length composition of the fish larvae in the Korea Strait would be mainly determined by the spawning ecology of the fishes, and the geological distribution and structure of the front which is formed in the ocean boundary between the Tsushima Current and the East Sea Cold Water.

• Journal of the Korean Geographical Society
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• v.45 no.6
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• pp.748-765
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• 2010

This study aims to investigate the difference of synoptic characteristics over East Asia according to the persistence of rainfall in Korea during the Changma season (June and July). In the cases of consecutive rainfall which lasts four or more days, there are developed ridges in 850hPa level east of the Korean peninsula which introduce stagnation of the synoptic cyclone over Korea. An cold area in 850hPa level moves southward from the Northern China in one day before the beginning the rainfall day in Korea and it aids the development of the stationary front in East Asia. When rainfall lasts a day or two, cyclones pass over Korea in rainy day and the stationary front in East Asia is not intensified. In both cases the synoptic cyclones near the Korean peninsula shows a deep-baroclinic structure, while in the former cases over the southwestern part of Japan a subtropical frontal zone which has a shallow structure appears near Japan. In latter cases the frontal structures are same near Korea and Japan. So, this means that the Changma is not necessarily similar to the Baiu of Japan in all cases.

• Fire Science and Engineering
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• v.15 no.1
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• pp.108-115
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• 2001

In this paper, we analyzed the properties change of electric wire when the thermal stress was applied to 600V grade polyvinyl chloride insulated wire (IV). In the structure analysis, normal wire has the properties of direction on the surface, but in case of deteriorated wire at above $400^{\circ}c$, it formed the carbide, the crack and the crystal. The surface composition rate of normal wire was Cu : 100%, but the section composition of the deteriorated wire at $800^{\circ}c$ showed Cu : 78.89%, O : 21.11%. In result of analyzing the differential scanning calory of copper wire, the new reaction peak was observed on the deteriorated wire at above $700^{\circ}c$. In case of the deteriorated wire as $150^{\circ}c$ at the differential thermal analysis, an endothermic reaction appeared at $264^{\circ}c$ lower than the reactive point of normal wire. The occupation rate of oxygen according to the deterioration of copper wire is about 20% at $500^{\circ}c$.

• International Union of Geodesy and Geophysics Korean Journal of Geophysical Research
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• v.21 no.1
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• pp.17-30
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• 1993

The basic processes responsible for the generation of oceanic fronts were reviewed. In particular the process of a shelf sea front produced by tidal stirring was identified from the one dimensional model of the water column in the coastal area, which incorporates the microscale process for the formation of a tidal front. Also a new criterion to predict its location was suggested. The time evolutions of the distributions of density and turbulent kinetic energy calculated from the model show that the criterion for the formation of a thermocline can be predicted as $R{\delta}^4$~ constant for large $\delta$ ($\delta$＞0.5), but the dependence on $\delta$ decreases as $\delta$ goes to O, where $R=H^4Q/{K_b}^3$,{\;}{\delta}=1-Do/H$, Q is the buoyancy flux at the surface, $K_b$ is the eddy diffusivity maintained at the bottom and Do is the depth of a thermocline in the absence of bottom mixing. The depth of a thermocline was found to decrease as the bottom mixing increases for a given value of Do. The results were interpreted in comparison with the previous studies.