• 대한환경공학회지
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• 제22권5호
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• pp.919-926
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• 2000

정수장 여과지 모형실험장치를 이용하여 수중입자입도분석에 의한 모래 및 이중여재 여과지에 대한 여과특성 및 효율 평가를 탁도분석과 비교하여 실시하였다. 수중입자입도분석은 여과지의 효율 평가를 위한 훌륭한 평가방법으로 탁도분석에 비해 민감도가 뛰어나 여과유출수의 탁질누출 현상을 뚜렷이 관찰할 수 있었다. 모래여과지의 경우는 여과지속시간 내내 비교적 양호한 수질을 보여, 허용수두하에서는 초기탁질누출보다는 여과말기의 수위상승에 대한 주위가 필요하다. 반면에 이중여재 여과지의 경우는 내부여과에 의한 탁질의 침투가 이루어지므로 최적운영을 위해서는 적절한 여재구성과 각 여과지별로 연속적인 수질모니터링에 의한 탁질누출제어가 요구된다. 또한 보다 안정적이고 효율적인 수질의 확보를 위해서는 여과보조제의 사용도 고려되어야 할 것이다.

• 한국해안해양공학회지
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• 제7권4호
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• pp.340-345
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• 1995

천해역으로 표층 방류되는 온배수 특성을 배출추 인근의 수심이 20m 내외로 일정한 대상 임해발전소를 선정하여 다수의 정점에서 계절별로 수신별 수은을 관측함으로써 방류수온의 수평적인 분포와 연직구조를 심도 있게 파악하였다. 서해안 천해역에서 관측된 표층온배수 특성은 전적으로 주변조류속에 의해 지배되며, 유속이 강한 창낙조시에는 자유？ 형태를 저 유속의 게류시는 플륨의 성향을 나타냈다. 다소 주변유속의 강도에 따라 차이는 있으나 초기 ？모멘텀이 지배하는 근역의 경계는 배출구로부터 200-300m 정도인 것으로 파악되었다. 이 구간에서는 수온의 연직적인 구조가 확인하고 배출구로부터 유하거리에 따라 수온이 지수적으로 감소함을 보이나 800m 이후에는 표층방류임에도 불구하고 난류확산으로 연직변화가 거의 나타나지 않았다. 특성길이 혼합모형(CORMIX3)을 이용하여 실측자료와의 비교점토가 이루어졌는데 실제의 제 현상을 대부분 잘 재현하였다. 수평확산의 범위를 포함하여 전반적으로 만족스러운 결과가 유도되었으며 특히 근역 및 중간역을 잘 모의할 수 있었다.

• Ocean and Polar Research
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• 제26권4호
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• pp.595-606
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• 2004

Hydrographic survey in the Korea Strait has long history that has begun in August 1917 at the Busan - Tsushima cross section, still continues to date. However, chemical properties of bottom cold water found exclusively in the western channel of the Korea Strait during summer did not receive much scientific attention. The aim of the study is to decipher the enigmatic origin of the Korea Strait Bottom Cold Water (KSBCW) in terms of chemical properties. The physicochemical properties of the KSBCW are extracted from the CREAHS II hydrographic data. OMP method was applied to analyze origin of the KSBCW quantitatively. The KSBCW is well defined by low temperature below $10^{\circ}C$. The cold waters exhibited the local presence near the coast at about 120m depth with a thickness of 20m to 30m. The cold water was characterized by relatively cold, saline and higher chemical concentrations than adjacent waters. The KSBCW seems to have different origin kom that of the coastal upwelled waters at the Ulgi-Gampo because it is saline, denser and contains considerably less dissolved oxygen than upwelled waters. The physicochemical properties are reported to have noticeable annual variations which suggest the complex origin of the KSBCW. OMP analysis show that the KSBCW is a mixture of three water types; TMW (24%), ESIW (36%) and ESPW (40%). Relationship between the KSBCW and the east Sea circulation is traced by mapping the water masses that have similar T, S and DO of KSBCW. The result showed that the KSBCW is most possibly an extension of southward flowing coastal intermediate waters. Front these results, we expect that the monitoring KSBCW will provide us valuable information about the East Sea circulation.

• 한국터널지하공간학회 논문집
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• 제13권5호
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• pp.413-430
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• 2011

최근 들어, 폭발하중에 대해여 안전한 사회기반시설에 대한 관심이 증가하고 있다. 폭발하중은 가스폭발이나 폭탄 폭발에 의하여 발생된다. 본 연구에서는 가스폭발하중을 받는 터널구조물을 각 부재로 나누어 1자유도 질량-스프링-감쇠기 모델로 치환하여 해석하는 모델을 개발하였다. 간이 모델을 사용하여 터널설계 요인인 최대 폭발하중크기, 지속시간, 부재 두께, 토피고에 대하여 민감도 해석을 수행하였다. 또한, 유한요소법을 사용하여 가스폭발에 대한 터널의 동적거동과 주변지반에 발생되는 파괴영역에 대하여 조사하였다. 1자유도 질량-스프링-감쇠기 모델과 FEM 해석결과의 비교로부터 터널의 중앙벽에 대한 동적거동결과는 거의 차이가 없음을 보여주었다.

• 한국압력기기공학회 논문집
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• 제12권1호
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• pp.126-133
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• 2016

Recently, the research and development of Sodium-cooled Fast Reactors (SFRs) have made progresses. However, liquid sodium, the coolant of an SFR, is chemically unstable and sodium fire can be occurred when liquid sodium leaks from sodium pipe. To reduce the damage by the sodium fire, many fire walls and fire extinguishers are needed for SFRs. LBB concept in SFR might reduce the scale of sodium fire and decrease or eliminate fire walls and fire extinguishers. Therefore, LBB concept can contribute to improve economic efficiency and to strengthen defense-in depth safety. The LBB assessment procedure has been well established, and has been used significantly in light water reactors (LWRs). However, an LBB assessment of an SFR is more complicated because SFRs are operated in elevated temperature regions. In such a region, because creep damage may occur in a material, thereby growing defects, an LBB assessment of an SFR should consider elevated temperature effects. The procedure and method for this purpose are provided in RCC-MRx A16, which is a French code. In this study, LBB assessment was performed for PGSFR IHTS hot-leg pipe according to RCC-MRx A16 and the applicability of the code was discussed.

• 한국수산과학회지
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• 제43권4호
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• pp.351-361
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• 2010

Among common estuarine submerged plants, seagrasses are the most extensively studied due to their ecological importance in estuarine ecosystems. Seagrass meadows are important biological habitats for a wide variety of marine animals and plants. They are a source of organic carbon for commercially important animals. Furthermore, seagrasses act as nutrient filters in estuarine and coastal marine ecosystems. As such, mapping the distribution of seagrass beds is important for management and conservation strategies. In order to survey the seagrass distribution within the Seomjin Estuary, We directly observed seagrass beds in Kwangyang and Hadong using SCUBA. The distribution area, species composition, morphology, density, biomass and productivity of seagrass meadows were examined. Seagrass meadows were distributed in the intertidal and subtidal zones of the Galsa tidal flats, and in the subtidal zone of the neighboring POSCO area. Patches of Zostera japonica was found at patches at the Galsa tidal flats intermediate point. The total estimated seagrass distribution area of the Seomjin Estuary was $1.84\;km^2$. Of the total, $1.83\;km^2$ was Zostera marina (eelgrass) and $0.01\;km^2$ was Zostera japonica (dwarf eelgrass). Zostera japonica was found in intertidal zones. Zostera marina was found from the intertidal to subtidal zones at a 2 m mean sea level (MSL) depth. The leaf productivity of Zostera marina was $4.47g\;DW\;m^{-2}\;day^{-1}$. The annual production of eelgrass was $1,632\;g\;DW\;m^{-2}\;yr^{-1}$, which corresponds to $731g\;C\;m^{-2}\;yr^{-1}$. The total production of eelgrass was $3,002\;tons\;DW\;yr^{-1}$, which corresponds to $1,343\;tons\;C\;yr^{-1}$.

• Ocean and Polar Research
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• 제26권2호
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• pp.299-309
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• 2004

Conductivity-temperature-depth (CTD) data obtained along a meridional section in the eastern tropical Pacific in July 2003 have been analyzed to identify various water masses, and to examine the hydrographic structure and zonal geostrophic currents in the upper 1000 m. Water mass analysis shows the existence of subtropical and intermediate waters, characterized by layers of subsurface salinity maximum and minimum, originating from both hemispheres of the Pacific. Vertical section of temperature in the upper 200 m shows the typical trough-ridge structure associated with the zonal current system for most of the tropical Pacific. Water with the lowest salinity of less than 33.6 was found in the upper 30 m between $8.5^{\circ}N$ and $10.5^{\circ}N$ in a boundary zone between the North Equatorial Current and North Equatorial Countercurrent. Temporal changes in water properties observed at $10.5^{\circ}N$ over a period of 9 days suggest both the local rainfall and horizontal advection is responsible for the presence of the low-salinity water. Development of a barrier layer was also observed at $10.5^{\circ}N$. In the North Equatorial Current region a local upwelling was observed at $15^{\circ}N$, which brings high salinity and cooler subtropical water to the sea surface. A band of countercurrent occurs in the upwelling region between $13^{\circ}N$ and $15^{\circ}N$.

• 한국어류학회지
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• 제23권3호
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• pp.217-224
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• 2011

동해에서 바다뱀과 엽상자어 7개체(TL 14.6~68.0mm)를 채집하여, 미토콘드리아 DNA 12S rRNA 861 bp 염기서열로 종을 동정하고, 이들의 개체발생을 기술하고, 진화적 관계를 고찰하였다. 바다뱀과 엽상자어 7개체는 날붕장어 성어와 유전거리(d=0.000)에서 잘 일치하였다. 날붕장어 엽상자어 7개체는 9개의 소낭이 항문 앞까지 존재하고, 전체 근절수가 154~158개, 전장에 대한 체고가 10% 이하이며, 흑색소포가 항문 뒤부터 꼬리지느러미 앞까지 8개 분포하는 형태적 특징을 보였다. 엽상자어의 형태 및 분자 분석결과를 통해 날붕장어는 진화학상 바다뱀아과 및 갯물뱀아과 사이에 위치하는 그룹으로 사료된다.

• 한국어류학회지
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• 제7권2호
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• pp.203-207
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• 1995

섬진강의 2차지류의 하나인 동복천에서 Cobitis longicorpus와 Misgurunus anguilicaudatus와 자연교잡종에 의하여 형성된 것으로 생각되는 개체가 발견되어 이를 비교 검토하였다. Hybrid의 형태적 특징은 눈밑에 가시가 있고 제 1반문의 위치가 짙으며, 혼서하고 있다는 점 등은 C. longicorpus의 특징이었고 체측 등쪽 반문의 특징과 등지느러미와 꼬리지느러미에 나타나는 반문, 골질반이 완만한 혹모양을 하고 있는 점은 C. longicorpus와 M. anguilicaudatus의 중간적 특징이었다. 계수형질의 결과 등지느러미 기점의 위치와 미병고에 있어서는 M. anguilicaudatus와 비슷하고 체고와 미병고/미병장의 비는 C. longicorpus와 M. anguilicaudatus의 사이 값을 나타낸 것이 특징이었다. 이를 제외한 나머지 계수형질의 값들은 C. longicorpus와 유사하여 상기 두 종의 hybrid로 보는 것이 타당하다고 판단된다.

• Ocean and Polar Research
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• 제34권3호
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• pp.305-323
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• 2012

The ocean's response to the Pinatubo and 1259 volcanic eruptions was investigated using an ocean general circulation model equipped with an energy balance model. Volcanic eruptions release gases into the atmosphere which increases the aerosol optical depth and acts to reduce the incoming short-wave radiation. For example, there was a huge volcanic eruption (Pinatubo) in 1991 which reduced the global mean radiative forcing by about 3 W $m^{-2}$. Two numerical experiments were simulated. The first experiment features the Pinatubo eruption and the second experiment simulates the much larger volcanic eruption that occurred in 1259 when the radiative forcing was reduced by 7 times compared to the Pinatubo event. With the reduced radiative forcing due to the Pinatubo eruption at about 3 W $m^{-2}$ and 1259 eruption at about 21 W $m^{-2}$, the global mean sea surface temperature (SST) decreased to its lowest in the second year after each event by about $0.4^{\circ}C$ and $1.6^{\circ}C$, respectively. Sea surface salinity (SSS) increased substantially in the northern North Pacific, northern North Atlantic, and the Southern Ocean. The reduced SST together with SSS increased ocean convection, which yielded an increase in North Atlantic Deep Water, Antarctic Bottom Water, and North Pacific Intermediate Water production and their outflows. The increase in overturning circulation eventually increased the pole-ward ocean heat fluxes. In conclusion, huge volcanic eruptions perturb the ocean substantially and their hallmarks last for more than a decade, confirming the importance of volcanic eruptions in illustrating the decadal-climate variability recorded in the paleoclimate proxy data for the past million years.