• 한국해양학회지:바다
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• 제19권2호
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• pp.164-168
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• 2014

거머리말 종자의 적절한 저장 방법과 저장 가능한 기간을 알아보기 위하여 우리나라 남해안에서 채취한 거머리말 종자를 이용하여 다양한 저장 방법과 저장 기간 후 발아율을 조사하였다. 거머리말 종자의 저장 방법은 공기가 공급되는 실온의 해수, $4^{\circ}C$의 해수, $30^{\circ}C$의 해수, 해수가 공급되는 수조, 밀폐된 해수, 냉동, 건조의 방법으로 저장하였다. $4^{\circ}C$의 해수에 저장한 거머리말 종자의 발아율이 가장 높았으며(52.0%), 해수가 유입되는 수조와 실온에서 저장한 종자의 발아율은 각각 17.7%와 27.4%가 나타난 반면, 건조, 냉동한 종자와 $30^{\circ}C$의 해수에 보관한 종자는 전혀 발아하지 않았다. 거머리말 종자의 각 저장 기간은 10, 20, 30, 60, 180일과 240일 동안 저장하였다. 10~60일 동안 저장한 거머리말 종자는 46.4~52.4%의 발아율을 유지하였으나, 저장 기간이 길어질수록 급격히 발아율이 감소하여, 240일 저장한 거머리말은 전혀 발아되지 않았다.

• 동력기계공학회지
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• 제21권2호
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• pp.64-69
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• 2017

The purpose of this study is to investigate the performance characteristics of seawater cooling system for a fishing vessel. The circulation amount of refrigerant, condensation capacity, evaporation capacity, compression work and coefficient of performance(COP) were analyzed as the heat source temperature changed. The experimental setup consisted of an open-type compressor, a shell&tube type condenser, an evaporator and an expansion valve. The heat source was controlled by a constant temperature chamber. The main results of this study are summarized as follows. The condensation capacity increased with increasing heat source temperature, and it was confirmed that the effect of circulating amount of refrigerant was dominant. The amount of heat for vaporization was almost constant even though the temperature of the heat source increased. On the other hand, the compression power was increased. This is because the compression ratio increases as the condensation pressure, the enthalpy difference between inlet and outlet, the amount of circulating refrigerant increases. The performance coefficient of this system showed a tendency decreasing with increasing heat source temperature. Therefore, the basic data of the seawater cooling system for the maintenance of the catch line of the shore fishing boats was acquired through this study, and it is considered that it will be sufficient for the actual design.

• 한국관개배수논문집
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• 제18권1호
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• pp.44-57
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• 2011

The status of fishway installed in domestic dikes showed a cascade types and sluice gate types 36% (four sites) and 64% (seven sites), respectively. Fishway of cascade type was constructed four sites (Iweon, Busa, Geum river, Haenam) and only Geum river was one of them has operated much more effectively since remodeling in a fishway and fishways of the others was not operated because of several problems like a desalination, a shortage of inflow water and variation of management elevation. Fishway of sluice gate type was installed seven sites and three sites (Yeongsan, Yeongam, Geumho) one of them were continuously operated until now. This results has a interesting interpretations. Prolonged discharge of inductive water from fishway can positively affect not only ascending of fishes but also fish fauna of around of the sea. The others of a sluice gate fishway were not operated because of seawater circulation through sluice gate until now. The closed reasons of fishway in domestic dikes may be summarized as follows: impassibility of sluice gate open by shortage of inflow water, problem of proper operating by long distance of between fishway and management office, absence of operating manual, seawater circulation, lack of fishway operating awareness. It was takes a long time for solution of hardware part but software part can be to find the answer through making a fishway operation manual and development of education program for manager. In this paper we deal with fishway in domestic dikes. Proper fishway control by manager was essential for ascending of migration fishes especially at fishway installed in dikes. Thus it was necessary to make manual for fishway operation and effort of continuously maintenance.

• 수산해양기술연구
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• 제57권3호
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• pp.214-227
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• 2021

The distribution of tidal current and tidal induced residual current, topographical eddies and tidal residual circulation in the waters surrounding the Geumo Island-An Island channel were identified through numerical model experiments and vorticity balance analysis. Tidal current flows southwest at flood and northeast at ebb along the channel. The maximum flow velocity was about 100-150 cm/s in neap and spring tide. During the flood current in the neap tide, clockwise small eddies were formed in the waters west of Sobu Island and southwest of Daebu Island, and a more grown eddy was formed in the southern waters of Geumo Island in the spring tide. A small eddy that existed in the western waters of Chosam Island during the ebb in neap tide appeared to be a more grown topographical eddy in the northeastern waters of Chosam Island in spring tide. Tidal ellipses were generally reciprocating and were almost straight in the channel. These topographical eddies are made of vorticity caused by coastal friction when tidal flow passes through the channel. They gradually grow in size as they are transported and accumulated at the end of the channel. When the current becomes stronger, the topographic eddies move, settle, spread to the outer sea and grow as a counterclockwise or clockwise tidal residual circulation depending on the surrounding terrain. In the waters surrounding the channel, there were counterclockwise small tidal residual circulations in the central part of the channel, clockwise from the northeast end of the channel to northwest inner bay of An Island, and clockwise and counterclockwise between Daebu Island and An Island. The circulation flow rate was up to 20-30 cm/s. In the future, it is necessary to conduct an experimental study to understand the growth process of the tidal residual circulation in more detail due to the convergence and divergence of seawater around the channel.

• Nuclear Engineering and Technology
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• 제53권11호
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• pp.3635-3642
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• 2021

Natural circulation systems (NCSs) are extensively applied in nuclear power plants because of their simplicity and inherent safety features. For some passive natural circulation systems in floating nuclear power plants (FNPPs), the ocean is commonly used as the heat sink. Condensation induced water hammer (CIWH) events may appear as the steam directly contacts the subcooled seawater, which seriously threatens the safe operation and integrity of the NCSs. Nevertheless, the research on the formation mechanisms of CIWH is insufficient, especially in NCSs. In this paper, the characteristics of flow rate and fluid temperature are emphatically analyzed. Then the formation types of CIWH are identified by visualization method. The experimental results reveal that due to the different size and formation periods of steam slugs, the flow rate presents continuous and irregular oscillation. The fluid in the horizontal hot pipe section near the water tank is always subcooled due to the reverse flow phenomenon. Moreover, the transition from stratified flow to slug flow can cause CIWH and enhance flow instability. Three types of formation mechanisms of CIWH, including the Kelvin-Helmholtz instability, the interaction of solitary wave and interface wave, and the pressure wave induced by CIWH, are obtained by identifying 67 CIWH events.

• 자원환경지질
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• 제34권5호
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• pp.447-460
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• 2001

부산지역의 지열수는 Na-Cl형으로서 한국의 타지역에서 산출되는 지열수에 비해 전기전도도(921~6,520 ${\mu}$S/cm)와 총용존고체함량(608~3,390 mg/L)이 비교적 높다. 부산지역 지열수는 Mg를 제외한 주요 이온들이 온도가 증가함에 따라 농도가 대체로 증가하는 약한 정의 상관관계를 나타낸다. 주요 양이온의 함량은 Na>Ca>K>Mg의 순으로 나타나며, 해수에 비해 Ca가 부화되어 있고, Mg가 결핍되어 있다. 이 지열수의 Br 함량은 모두 해수보다 낮으며, 온도가 증가함에 따라 증가하는 정의 상관관계를 보인다. 이를 종합하면, 부산지역 지열수는 심부로 순환하는 해수가 주변 모암과의 상호반응에 의해 해수에 비해 상대적으로 증가된 Ca와 Sr의 함량과 상대적으로 결핍된 Mg, Na와 K의 함량을 갖는 지열수를 형성한 것으로 여겨진다. 또한 주요 이온들과 온도와의 상관관계로 볼 때, 높은 염도의 지열수가 상승하는 동안 저온의 주변 지하수와 혼합되어 냉각과 함께 희석작용이 있었던 것으로 보인다. 이 지열수의 기원과 진화를 정확히 규명하기 위해서는 안정동위원소 연구와 함께 전체 지구화학계에 대한 물-암석 반응 모델링이 수행되어야 할 것이다.

• 한국수산과학회지
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• 제50권2호
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• pp.207-218
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• 2017

Seawater with salinity of 32.5 psu or less is observed in the southern Japan/East Sea (JES) every autumn. It is confined to a surface layer 30-45 m in depth that expands to cover the entire JES in October. Two sources of "autumn low-salinity water" have been identified from historical hydrographic data in the western JES: East China Sea (ECS) water mixed with fresh water discharge from the Yangtze River (Changjiang) and seawater diluted with melted sea ice in the northern JES. Low-salinity water inflow from the ECS begins in June and reaches its peak in September. Low-salinity water from the northern JES expands southward along the coast, and its horizontal distribution varies among years. A rare observational study of the entire JES in October 1969 indicated that water with salinity less than 33.0 psu covered the southwestern JES; the lowest salinity water was found near the Ulleung Basin. In October 1995, the vertical distribution of salinity observed in a meridional section revealed that water with salinity of 33.6 psu or less was present in the area north of the subpolar front.

• 한국해안·해양공학회논문집
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• 제26권3호
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• pp.184-195
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• 2014

낙동강 하구역은 하구둑이 건설된 이후, 담수는 갑문 개폐에 의해서 인위적으로 방출되고 해수유입은 하구둑에 의해 억제되어왔다. 이로 인해 인위적인 수문 개방에 의한 해수와 담수의 수렴 및 혼합은 낙동강 하구역의 해수순환에 큰 영향을 미치는 것으로 나타났다. 홍수기 방류 중 낙동강 하구역의 수로별 유동 환경과 하구 흐름 특성을 조사하기 위해 유속 및 염분 관측을 수행하였다. 분석 결과 지형적 특징 및 방류의 영향에 의해 수로별 유속 및 염분 분포 특징이 상이하게 나타났다. 낙동강 하구역의 홍수기 방류에 의한 영향은 각 수로별 잔차유속 및 염분 수직분포에 다르게 작용하며, 지형적 특징은 염분침투 범위에 영향을 미침으로써 상대적으로 고염의 물이 정체되는 구간이 존재한다.

• 상하수도학회지
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• 제32권2호
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• pp.97-106
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• 2018

In this study, the effect of chemically enhanced backwash(CEB) coping with algal(Heterosigma Akashiwo) inflow was evaluated in the seawater desalination pretreatment process using ceramic membrane. In order to confirm the possibility of long-term filtration operation, the recovery rate of transmembrane pressure(TMP) due to the CEB using NaOCl was examined. When the membrane flow rate was 83.3 LMH, the TMP was maintained within 200 kPa for 84 hours in seawater influent. As the algal counts of 30,000 cell/mL were injected into the influent of seawater, however, the TMP rapidly increased and exceed maximum value. Membrane fouling caused by the algae was very poorly recovered by usual physical backwash. The CEB was performed for 30 min(3 min circulation / 27 min immersion) with 300 mg/L of NaOCl. As a result of the CEB application, it was possible to maintain a stable operating of filtration during 10 days and the average recovery rate of TMP by the CEB was 98.1%. It has been confirmed that the CEB using NaOCl is very effective in removal of membrane fouling by algae, resulted in stable membrane filtration for the long-term operation.

• 한국환경과학회지
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• 제29권3호
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• pp.273-282
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• 2020

Residence time is defined as the time taken for a material in a system to leave the system. The residence time characteristics in shellfish aquaculture determine the dispersion of excretion from aquaculture farms, along with the supply of food by seawater exchange. In this study, we estimated the spatial distribution of average residence time in the shellfish farming area using a particle tracking model. As a result, a relatively short average residence time of about 20 days or less was calculated in most areas, but an average residence time of more than 40 days was calculated in the inner areas. Relatively long average residence times were calculated along the west coast compared to the east coast, with the longest average residence time of more than 50 days in the northwestern areas. It can be inferred that the disturbance of the benthic ecosystem caused by shellfish farms is likely to be large because of the relatively weak dispersion of excrement from shellfish farms located on the west coast, especially in the northwest region. This distribution of average residence time is important for understanding the potential effects of seawater exchange on the environmental sustainability of shellfish farms, along with the seawater circulation characteristics of Jaran Bay.