• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2002년도 춘계학술대회 논문집
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• pp.243-250
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• 2002

According to Ocean Korea 21, a basic plan established by the Ministry of Maritime Affairs and Fisheries (MOMAF) of Korea in May 2000, Korea Research Institute of Ships and Ocean Engineering (KRISO) proposed a program for the development of a deep-sea unmanned underwater vehicle (UUV) to explore deep sea for scientific purpose. KRISO has launched a project in May 2001 under the support of MOMAF. The deep-sea unmanned underwater vehicle will be applied to scientific researches in deep-sea as well as in shallow water. For operation of underwater vehicles in shallow water near the Korean Peninsula, a special design is required because of strong tidal current. In addition, MOMAF requires the vehicle to be designed for the purpose of long range survey, a long-term observation, and precise works in a specific area. Thus, KRISO has planned to design the system with the functional combination of both ROV and AUV. This paper presents the design of the deep-sea unmanned underwater vehicle.

• Ocean and Polar Research
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• 제32권1호
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• pp.15-22
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• 2010

Calcium carbonate ($CaCO_3$) content was measured from 3 box core (BC060301, BC060303, BC070301) sediments, in addition to pilot core (PC313) sediments, from deep waters within the Western Pacific Ocean. At the two collection sites (BC060301, PC313) located close to the equator, downcore variation exhibited low $CaCO_3$ content during the interglacial period and high $CaCO_3$ content during the glacial period. Variation of coarse fraction (>$63\;{\mu}m$) content also followed changes in $CaCO_3$ content, indicating that dissolution effect of bottom water decreased during the glacial period. Such variation pattern is typical of the Pacific Ocean. However, downcore variation at the two collection sites (BC060303, BC070301) in the Philippine Sea contrasted the trend of the previous two cores (i.e., high $CaCO_3$ content during the interglacial period and low during the glacial period). This pattern is typical of the Atlantic Ocean. Such results may be attributed to the increasing dilution effect, initiated possibly by the increased transportation of terrigenous materials from nearby continent and archipelago during the glacial period when sea level was low. Alternatively, it is possible that the non-carbonate biogenic particles may have been responsible for dilution. Because of these uncertainties, the record of $CaCO_3$ variation in the deep Western Pacific Ocean is not regionally consistent.

• Ocean and Polar Research
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• 제26권2호
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• pp.219-230
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• 2004

The aims of this study are to construct database using geostatistics and Geographic Information System (GIS), and to derive the spatial relationships between manganese nodule abundance and each factor affecting nodule abundance, such as metal grade, slope, aspect, water depth, topography, and acoustic characteristics of the subbottom using the GIS and probability methods. The greater is the copper and nickel grade, the higher is the rating. The distribution pattern of nickel grade is similar to that of copper grade. The slopes are generally less than $3^{\circ}$, excluding seamounts and cliff areas. There is no increment in the rating with increasing slope. The rating is highest for slopes between 2.5 and $3.5^{\circ}$ in block B2 and between 3 and $6^{\circ}$ in block C1. The topography is classified into five groups: seamount, hill crest, hill slant, hill base or plain, and seafloor basin or valley. The ratings prove lowest for seamount and hill crest. The results of the study show a decrease in the rating with an increase in water depth in the study area. There was a poor relationship between manganese nodule abundance and the thickness of the upper transparent layer in block C1. Using GIS, it is possible to analyze a large amount of data efficiently, and to maximize the practical application, to increase specialization, and to enhance the accuracy of the analyses.

• 대한전기학회:학술대회논문집
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• 대한전기학회 2007년도 심포지엄 논문집 정보 및 제어부문
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• pp.319-321
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• 2007

This paper introduces a general overview of the 6000m class deep-sea ROV. Hemire and Henuvy. and then describes its motion control system. It is developed by Korea Ocean Research & Development Institute(KORDI) for 6 years since 2001. sponsored by the Ministry of Maritime Affairs and, Fisheries (MOMAF). Hemire is remotely operated by a fiber optic telemetry. where 6 thrusters are controlled by operator in manual mode and by auto depth control and auto heading control in auto mode. In this paper. operational mechanism of manual and automatic mode with some convenient functions for operator is desc.ribed. Finally, results of sea trial conducted at the Philippine sea where a depth is 5.770m are shown.

• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2004년도 학술대회지
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• pp.285-289
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• 2004

Oceanographic observation and qualitative analysis for deep ocean water in the East Sea were carried out from January 2003 to January 2004, in order to understand the characteristics of deep sea water in the East Sea. Temporal and spatial variation of water masses were discussed from survey of the study area including the coastal sea of Kwangwon province in where the polar front mixing cold and warm water masses were formed. On the basis of the vertical profiles of temperature, salinity and dissolved oxygen, water masses in the study area were divided into 5 major groups; (1) Low Saline Surface Water (LSSW) (2) Tsushima Surface water (TSW) (3) Tsushima Middle Water (TMW) (4) North Korea Cold Water (NKCW) and (5) East Sea Proper Water (ESPW). In winter, surface water in coastal sea of Kwangwaan Kosung region were dominated by North Korean Cold Water (NKCW). As Tsushima warm current were enforced in summer, various water masses were vertically emerged in study area, in order of TSW, TMW, NKCW and ESPW. It is highly possible that the LSSW which occurred at surface water of september is originated from influx of fresh water due to the seasonal rainy spell. Nevertheless water masses existed within surface water were seasonally varied, water quality characteristics of East Sea Proper Water (ESPW) under 300 m did not changed all the seasons of the year.

• 한국유기농업학회지
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• 제14권1호
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• pp.85-95
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• 2006

해양심층수 처리가 과채류 육묘 시 도장억제에 미치는 영향을 검토한 결과 다음과 같다. 심층수의 처리 농도에 따른 플러그 묘의 생육을 조사해 본 결과 초장, 생체중, 건물중이처리 농도가 높아짐에 따라 비례적으로 감소하였다. 토마토 초장의 경우 심층수 처리구에서는 약 8%, 25%, 32%결과를 보였고, 고추는 각 약 9%, 26%, 27% 감소하였고, 오이 초장의 경우에는 심층수 처리구에서는 약 21%, 50%, 58% 감소하였다. 생체중의 경우 처리 농도가 높아짐에 따라 지상부의 생체중보다 지하부의 생체중이 급격히 감소하는 경향을 보였다. 토마토 심층수 처리구의 지상부의 생체중 감소률은 각 12%, 23%, 33%이고, 지하부는 각 2%, 30%, 52% 감소하였다 고추의 경우 지상부의 생체중은 1.1%, 5.7%, 15.4% 감소하였고, 지하부의 생체중은 22.1%, 25%, 47.1% 감소하였다. 오이는 지상부 생체중은 8.1%, 36%, 51% 감소하였고, 지하부 생체중은 6.2%, 11%, 65% 감소하는 결과를 보였다. 엽면적은 농도가 증가함에 따라 감소하였다. 건물중의 경우 생체중과 마찬가지로 처리 농도가 증가함에 따라 감소하였다. 심층수 30% 처리구에서는 지하부의 생장이 약 50% 정도 감소하는 결과를 보였다. 또한 묘 소질 평가지수의 하나인 조직의 충실도(compactness)는 토마토의 경우 20%심층수에서 가장 높은 수치를 나타냈고, 오이의 경우에서도 20% 심층수 처리구에서 가장 높게 나타났다. 고추 유묘에서도 20%의 해양심층수를 공급할 때 가장 충실도가 높았다.

• 한국해양환경ㆍ에너지학회지
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• 제15권3호
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• pp.198-207
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• 2012

본 연구에서 식물플랑크톤 뿐 아니라 동물플랑크톤을 포함하는 생태계 모델을 이용하여 해양 심층수의 해역 비옥화의 효과를 검증하였다. 모델은 2종의 식물플랑크톤, 3종의 동물플랑크톤, 질산염, 암모늄염, 규산염, 입자성 유기질소, 용존 유기질소, 입자성 규소 총 11개 요소로 구성된 NEMURO에 기초하고 있다. NEMURO의 11개 요소 외에도 두 종의 식물플랑크톤내 질소 셀 쿼터와 대형 식물플랑크톤내 규산염 셀 쿼터를 추가하였다. 해역 비옥화 효과를 조사하기 위해서 이즈 오시마 섬에서 실험을 실시하였지만, 본 실험에서 심층수의 유무에 의한 명확한 차이를 확인할 수 없었다. 이 실험 결과의 원인들을 모델 시뮬레이션에 의해 조사하였으며, 그 원인의 하나는 실험에 사용된 표층수의 높은 영양염 농도이다. 다른 원인은 무기질소 섭취율이 $NH_4$에 대한 $NO_3$의 비율에 관련되어 있으므로 무기질소의 총 농도의 증가가 광합성 속도를 반드시 증진시키지 않는다는 것이다. 이 모델로 실험 결과들을 재현할 수 있었기 때문에 우리는 이 모델을 이용하여 해양 심층수에 의한 해역 비옥화의 효과를 검증하였다. 해양 심층수의 공급 간격이 너무 짧거나 해양 심층수의 양이 너무 많을 때 해역 비옥화 효과는 나타나기 어려운 것으로 밝혀졌다. 해양 심층수의 첨가가 너무 비번하거나 너무 많이 첨가하면 플랑크톤 농도의 희석이 식물플랑크톤의 광합성 증진 효과를 초과해 버린 것으로 추측된다.

• Ocean and Polar Research
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• 제34권3호
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• pp.287-296
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• 2012

In the theory of source-driven abyssal circulation, the forcing is usually assumed to be steady source (deep-water formation). In many cases, however, the deep-water formation occurs instantaneously and it is not clear whether the theory can be applied well in this case. An attempt is made to resolve this problem by using a simple reduced gravity model. The model basin has large depth change compared for its size, like the East Sea, such that isobaths nearly coincide with geostrophic contours. Deep-water is formed every year impulsively and flows into the model basin through the boundary. It is found that the circulation driven by the impulsive source is generally the same as that driven by a steady source except that the former has a seasonal fluctuation associated with unsteadiness of forcing. The magnitudes of both the annual average and seasonal fluctuations increase with the rate of deep-water formation. The problem can be approximated to that of linear diffusion of momentum with boundary flux, which well demonstrates the essential feature of abyssal circulation spun-up by periodic impulsive source. Although the model greatly idealizes the real situation, it suggests that abyssal circulation can be driven by a periodic impulsive source in the East Sea.

• 한국수산과학회지
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• 제39권spc1호
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• pp.203-213
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• 2006

The spatial patterns of meiobenthic communities in deep-sea sediment were examined. Sediment samples for analyzing of meiobenthic community structure were collected using a remote operated vehicle (ROV), multiple corer TV grab at 20 stations at five sites. In all, 15 meiofauna groups were recorded. Nematodes were the most abundant taxon. Benthic foraminiferans, harpacticoid copepods, polychaetes, and crustacean naupii were also dominant groups at all sites. The total meiofauna density at the study sites varied from 49 to 419 ind./$10cm^2$. The maximum density was recorded at a site located in Challenger Deep in the Mariana trench where simple benthic foraminifera with organic walls flourish. These distinctive taxa seem to be characteristic of the deepest ocean depths. Active hydrothermal sediments contain up to 150 harpacticoid copepods per $10cm^2$ of sediment. In a inactive ridge sediments, devoid of macrofaunal organisms:, the abundance of harpacticoid copepods never exceeded 15 ind./$10cm^2$. Multivariate analysis (multidimensional scaling) revealed significant differences in community structure among the three regions; near an active hydrothermal vent, in the deepest ocean depths and at typical deep-sea bed sites.

• Journal of Ecology and Environment
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• 제29권2호
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• pp.175-183
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• 2006

The discovery of deep-sea hydrothermal vents and their ecosystems is a monumental landmark in the history of Ocean Sciences. Deep-sea hydrothermal vents are scattered along the global mid-ocean ridges and back-arc basins. Under sea volcanic phenomena related to underlying magma activities along mid-ocean ridges generate extreme habitats for highly specialized communities of animals. Multidisciplinary research efforts during past three decades since the first discovery of hydrothermal vents along the Galapagos Rift in 1977 revealed fundamental components of physiology, ecology, and evolution of specialized vent communities of micro and macro fauna. Heterogeneous regional geological settings and tectonic plate history have been considered as important geophysical and evolutionary factors for current patterns of taxonomic composition and distribution of vent faunas among venting sites in the World Ocean basins. It was found that these communities are based on primary production of chemosynthetic bacteria which directly utilize reduced compounds, mostly $H_2S$ and $CH_4$, mixed in vent fluids. Symbioses between these bacteria and their hosts, vent invertebrates, are foundation of the vent ecosystem. Gene flow and population genetic studies in parallel with larval biology began to unveil hidden dispersal barrier under deep sea as well as various dispersal characteristics cross taxa. Comparative molecular phylogenetics of vent animals revealed that vent faunas are closely related to those of cold-water seeps in general. In perspective additional interesting discoveries are anticipated particularly with further refined and expanded studies aided by new instrumental technologies.