• 한국해양환경ㆍ에너지학회지
• /
• 제19권3호
• /
• pp.173-184
• /
• 2016

통영 거제연안역에서의 해양생태계 관측 결과를 군집분석하여 이 해역에서의 계절에 따른 수온 염분 분포 특징을 파악하고자 하였다. 춘계, 추계 및 동계에는 연안역이 외해역에 비해 수온이 $1{\sim}2^{\circ}C$ 정도 높았으며, 특히 2014년 동계의 저층은 표층과는 달리 남-북 방향으로 등수온선을 형성하였다. 염분 또한 2013년 동계에는 저층에서 남-북 방향의 등염분선을 형성하였다. 따라서, 표 저층의 등수온 및 등염분선의 방향이 서로 달라, 수괴의 이동 패턴도 서로 다르다는 사실을 확인하였다. 반면 하계 표 저층에는 수온이 약 $10^{\circ}C$, 염분은 외해 2 psu, 거제연안 10 psu 이상인 성층이 형성되었다. 군집분석 결과, 이 해역의 수괴는 크게 세 개의 군집으로 나눌 수 있었으나, 해수의 유입 등에 의해 복잡한 군집을 이루는 경우도 있었다. 이러한 군집분석 결과는 군집의 형태가 남-북 방향으로 형성되는 시기를 제외하고는 비교적 적합한 것임을 회귀분석을 통해 확인하였다.

• 한국수자원학회논문집
• /
• 제46권11호
• /
• pp.1115-1128
• /
• 2013

본 연구의 목적은 충주호 유역을 대상으로 2차원 횡방향 평균 수리 및 수질모형인 CE-QUAL-W2를 이용하여 호소내 수온분포, 부유물질 및 부영양화 과정의 변화특성을 모의하고 모형의 적용성을 평가하는 것이다. 지형 및 단면자료 구축을 위해 충주호를 남한강 본류(branch 1)와 유입 경계부(branch 2~7)로 구분하여 격자를 구성하였다. 호소 수질모델링을 위한 주요 입력 자료로 기상자료, 호소의 수온과 탁도 초기조건, 하천의 유량과 수온, 수질 경계조건 자료를 구축하였다. 이후 실측된 수온, 부유물질(SS), 총질소(TN), 총인(TP), 조류(Chl-a)에 대하여 모형의 보정(2010) 및 검증(2008)을 수행하여 모형의 적용가능성을 평가하였다. 충주호의 수온은 4월부터 표층수온이 증가하여 7월초에 성층현상이 발생되고 12월에는 연직수온분포가 일정하게 유지되었다. 집중호우 발생 후에는 성층구조가 교란되어 수온약층이 약 10 m가량 하강하였다. SS는 수온과 동일한 패턴으로 집중호우 발생 후에 증가하다가 12월에 안정화되었으며, 2008년 7월에 발생된 중층밀도류의 분포 현상을 잘 재현하였다. TN, TP의 경우 농도의 범위를 잘 재현하였지만, 모형 내에서 질소성분의 침강속도 및 인의 흡착-침전과정이 적절히 모의되지 않아 오차가 발생하였다. Chl-a의 경우 2010년과 2008년 여름의 조류의 성장패턴을 잘 반영하였지만, 모형이 횡방향 평균 유속과 농도를 사용함에 따른 모형의 한계점이 나타났다.

• Nuclear Engineering and Technology
• /
• 제54권11호
• /
• pp.4348-4358
• /
• 2022

The thermal-hydraulics phenomena in a containment during an accident will necessarily include radiative heat transfer (i) within the gas mixture due to the high radiative absorption and emission of steam and (ii) between the gas mixture and the surrounding structures. The analysis of some previous PANDA experiments (PSI, Switzerland) demonstrated the importance of the proper modelling of radiation for the benefit of numerical simulations. These results together with dedicated scoping calculations conducted for the present experiments indicated that the radiative heat transfer is considerable, even for a very low amount of steam (≈2%). The H2P2 series conducted in the large-scale PANDA facility at the Paul-Scherrer-Institut (PSI) in the framework of the OECD/NEA HYMERES-2 project is intended to enhance the understanding of thermal radiation phenomena and to provide a benchmark for corresponding numerical simulations. Thus, the test matrix was tailored around the two opposite extremes: either gas compositions with small steam content such that radiative heat transfer phenomena can be neglected. Or gas mixtures containing larger amounts of steam, so that radiative heat transfer is expected to play a dominant role. The H2P2 series consists of 5 experiments designed to isolate the radiation phenomena from convective and diffusive effects as much as possible. One vessel with a diameter of 4 m and a height of 8 m was preconditioned with different mixtures of air / steam at room and elevated temperatures. This was followed by the build-up of a stable helium stratification at constant pressure in the upper part of the vessel. After that, helium was injected from the top into the vessel which leads to an increase of the vessel pressure and a corresponding elevation-dependent and transient rise of the gas temperature. It is shown that even the addition of small amounts of steam in the initial gas atmosphere considerably impacts the radiative heat transport throughout all phases of the experiments and markedly influences i) the monitored gas peak temperature, ii) the temperature history during the compression and iii) the following relaxation phase after the compression was stopped. These PANDA experiments are the first of its kind conducted in a large scale thermal-hydraulic facility.

• Geomechanics and Engineering
• /
• 제22권3호
• /
• pp.245-254
• /
• 2020

The interaction between the frozen soil and building structures deteriorates with the increasing temperature. A nuclear magnetic resonance (NMR) stratification test was conducted with respect to the unfrozen water content on the interface and a shear test was conducted on the frozen soil-structure interface to explore the shear characteristics of the frozen soil-structure interface and its failure mechanism during the thawing process. The test results showed that the unfrozen water at the interface during the thawing process can be clearly distributed in three stages, i.e., freezing, phase transition, and thawing, and that the shear strength of the interface decreases as the unfrozen water content increases. The internal friction angle and cohesive force display a change law of "as one falls, the other rises," and the minimum internal friction angle and maximum cohesive force can be observed at -1℃. In addition, the change characteristics of the interface strength parameters during the freezing process were compared, and the differences between the interface shear characteristics and failure mechanisms during the frozen soil-structure interface freezing-thawing process were discussed. The shear strength parameters of the interface was subjected to different changes during the freezing-thawing process because of the different interaction mechanisms of the molecular structures of ice and water in case of the ice-water phase transition of the test sample during the freezing-thawing process.

• 한국조경학회지
• /
• 제15권2호
• /
• pp.139-148
• /
• 1987

Exochorda serratifolia, broad-leaved shrub has beautiful flowers and is resistant to cold, shade and decease. New this native plant is considered to be worth being exploited as the outstanding plant for landscaping and horticulture. So this study was executed to utilize Exochorda serratifolia as the planting material for landscaping and horticulture through the survey of its habitat environment and the experimennt of its seed physiology and germination, vegetative propagation, culture and utilization, etc.. The results are as follows ; 1. The color of the flower is white, blooming in the early and middle of May and the seeds ripen late in Sep.. 2. The elevation, elevation, gradient and direction of the native habitat were 250m, 20-25$^{\circ}$and northern side respectively. 3. The soil pH of the natural habitat was 5.3 and soil fertility was poor. 4. Exochorda serratifolia appeared as indicator within P. densiflora community and its neighboring species were Q. mongolica, Q. dentata, R. mucronulatum, L. obtusiloba, E. oxyphillus, C. heterolphylla, var thunbergii, etc.. 5. The optimum temperature for seed germination was found at 20$^{\circ}C$ and the longer the stratification period at 5$^{\circ}C$ was, the lower the germination rate was. 6. The treat merits of GA and Kinetin increased the seed germination rate, especially under the dark condition but their high concentrations decreased the seed germination rate. 7. The rooted rate of the greenwood cutting was the highest at IBA 100ppm plot of vermiculite bed but its high concentration decreased the rooted rate conspicuously. 8. In the tissue culture, the each 1.0 ppd plot of NAA, Kinetin and NAA 1.0ppm + Kinetin showed the best growth. And the mixture of NAA 1.0ppm and Kinetin showed better growth than the single treatment of NAA or Kinetin did. 9. Transplanted Exochorda serratifolia showed healthy growth with shaded environmental condition(42.1% light intensity), therefore they can be cultivated as a shade tolerant landscape plant. 10. It was considered that Exochorda serratifolia was applicable to group planting at shade places or under trees in parks, homes, etc..

• 대한토목학회논문집
• /
• 제10권4호
• /
• pp.159-171
• /
• 1990

본 연구의 목적은 담수호에 적합한 Multiple Box모형을 개발, 적용하여 장기 수질예측을 할 수 있도록 하므로써 담수호에서의 수질관리 방안을 제시하는데 있다. 모형은 수문 부모형과 수질 부모형으로 구성되어 있으며, 수질 부모형에서 고려한 수질항목은 수온, Chlorophyll-a, BOD, DO, N과 P 등이었다. 본 모형의 적용은 아산호를 대상으로 시행하였으며, 호의 수문환경조건을 고려하여 호를 상층은 2개의 Box, 하층은 1개의 Box 등 총 3개의 box로 분할하였다. 수질예측모형을 아산호에 적용한 결과 대체로 장기적 수질변화추세를 잘 나타내고 있는 것으로 평가되었다. 개발된 수질모형의 미래의 오염부하량을 입력하여 수질개선 방안들을 비교한 결과, Chlorophyll-a의 경우 무린세제의 도입이, BOD와 T-N의 경우 고도하수처리시, T-P의 경우 축산폐수의 저감시 각각 효과가 큰 것으로 평가되었다.

• Journal of the korean society of oceanography
• /
• 제35권3호
• /
• pp.129-152
• /
• 2000

The Cheju Current (CC), defined here as a mean eastward flow in the Cheju Strait, mostly carries water of high temperature and salinity originating from the Kuroshio in winter and spring, the Cheju Warm Current Water (CWCW). The strong core of the eastward component of the CC is found close to Cheju Island (Cheju-Do, hereafter) in winter and spring with a peak speed of about 17.0 cm/s. The eastward flow weakens towards the northern Cheju Strait, and a weak westward flow occurs occasionally close to the southern coast of Korea. The volume transport ranges from 0.37 to 0.45 Sv(1 Sv=10$^6$ m$^3$/s) in winter and spring. Seasonal thermocline and harocline are formed in summer and eroded in November. The occurrence of the CWCW is confined in the southern Cheju Strait close to Cheju-Do below the seasonal thermocline in summer and fall, and cold water occupies the lower layer north of the CWCW which is thought to be brought into the area from the area west of Cheju-Do along with the CWCW. Stratification acts to increase both the speed of the CC with a peak speed of greater than 30 cm/s and the vertical shear of the along-strait currents. The strong core of the CC detached from the coast of Cheju-Do and shifted to the north during the stratified seasons. The volume transport in summer and fall ranges 0.510.66 Sv, which is about 1.5 times larger than that in winter and spring. An annual cycle of the cross-strait sea level difference shows its maximum in summer and fall and minimum in winter and spring, whose tendency is consistent with the annual variability of the CC and its transport estimated from the ADCP measurements. Moored current measurements west of Cheju-Do indicate the clockwise turning of the CC, and the moored current measurements in the Cheju Strait for 1530 days show the low-frequency variability of the along-strait flow with a period of about 37 days.

• Nuclear Engineering and Technology
• /
• 제24권1호
• /
• pp.86-97
• /
• 1992

이 논문의 목적은 C-E System 80+ 원자로에서의 직접용기주입 설계를 가압 열 충격의 견지에서 평가하는 것이다. 영의 출력에서의 주증기관 파단과 0.05 ft$^2$면적의 소형파단 냉각재상실사고가 가능성있는 가압열충격 사고로 선정되었다. 원자로 다운카머 영역에서의 유체 성층효과를 예측하기 위하여 주증기관 파단사고에 대하여는 COMMIX-IB 전산코드를, 그리고 0.05 ft$^2$소형파단 냉각재상실사고에 대하여는 REMIX 전산코드를 사용하여 유체혼합해석이 수행되었다. 압력과 온도의 과도변화를 받는 원자로용기 벽내의 응력분포는 두 사고에 대하여 OCA-P전산코드를 사용하여 계산되었다. 해석결과, 붕괴열의 고려가 없는 소형파단 냉각재 상실사고의 경우 용기내 균열발생의 가능성이 있으나 붕괴열을 고려하면 용기의 수명기간중 균열발생의 가능성은 없다.

• 한국환경과학회지
• /
• 제11권12호
• /
• pp.1205-1215
• /
• 2002

To evaluate the change for water quality after the water gate operation in Shiwha lake, in situ survey were conducted on september in 2000 and January, march, jane in 2001. Chemical characteristics and eutrophication level was estimated from the survey data. The water quality of the Shihwa lake was greatly affected by pollutant load from rainfall, and formation of stratification in summer and winter was increased to effect on nutrient release from sediment. Especially, high concentration of chlorophyll-a was occurred in autumn, due to increased nutrient, high water temperature and low salinity after rainfall runoff. The mean concentration of DIN, DIP were 0.346mg/L, 0.0217mg/L in surface water and 0.826mg/L, 0.0415mg/L in bottom water, respectively, which were over III grade of seawater standard. Also high percentage of ammonia nitrogen to DIN in bottom water for autumn and winter was affected by released nutrient from sediment. Correlation analysis of chlorophyll-a versus TSS was shown that organic matter was affected by autochthonous organic matter stem from the algae, these factor showed reverse correlation about salinity. Closely correlations among to the water quality constituent in continuity survey was appeared. The results of eutrophication index estimation showed the high potentiality of red tide occurrence in Shiwha lake, particularity in summer or fall. Overall water quality was greatly improve to compared with measuring data during 1997~1998 at the beginning water gate operation, which reported by KORDI. Therefore, to improve of water quality in Shiwha lake, we need to establish of management plan about nutrient release from sediment, rainfall runoff, maximum of seawater exchange.

• 한국화재소방학회논문지
• /
• 제22권5호
• /
• pp.55-60
• /
• 2008

본 연구는 수분무 소화설비의 효용성에 대한 기초평가를 수행할 목적으로 FDS 수치시뮬레이션을 수행하였다. 화재강도(20MW, 50MW) 및 풍속의 변화에 따른 화재시 온도 및 연기농도에 대한 안전성 확보 효과를 분석하였다. 터널내 풍속이 없는 경우 수분무는 냉각효과에 의한 온도 및 연기농도 감소효과가 아주 우수하여 대피자의 안전성 확보에 효과적이었다. 화재강도가 커질수록 연기이동 억제효과는 감소한 결과를 나타났다. 또한 터널내 기류가 존재하는 경우에는 냉각효과에 의해서 연기의 성층화를 교란하며, 대피시 가시도를 저하시키는 것으로 나타났다. 따라서 수분무 소화설비는 화재발생시 대피자가 대피한 후에 이루어져야 할 것으로 판단된다.