• Fisheries and Aquatic Sciences
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• v.2 no.2
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• pp.129-134
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• 1999

Haloptilus caribbeanensis Park, 1970 (Copepoda, Calanoida, Augaptilidae) is redescribed in detail on the basis of an adult female collected from Suruga Bay, Japan. This is the first record of the species from the Indo-Pacific region. Morphology of the Pacific specimen agrees well with that of the Caribbean Sea and Gulf of Mexico specimens, except for the numbers of mandibular teeth. The former has five teeth and the latter six teeth on mandible. The segmentation and segmental aesthetasc numbers of female antennules of H. caribbeanensis are compared with those of five species of Haloptilus (H. angusticeps, H. fons, H. longicomis, H. ornatus and H. spiniceps). These characters show morphological differentiation at the species level. H. caribbeanensis has no aesthetasc on the proximal segments II, IV, and VI of the female antennules.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.28 no.4
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• pp.401-411
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• 1995

Flavobacterium spp., Pseudomonas spp., and Vibrio spp. were isolated from samples(sediments) of Sagami Bay and Suruga Bay(in Japan) at 810-4,000m in depth. Among isolated strains, Vibvio sp.-86 and sp.-87 strains were identified as barophilic and psychrophilic ones. They grew in 400 atm and showed best growth at 100 atm. Marine bacteria grown at 400 atm were long rod shape and 30 to 50times longer than those grown at 1 atm. which were short rod shape and formed flocks (aggregates). Vibrio sp,-86 strain grew at $5-37^{\circ}C\;and\;0,5-9.0\%\;NaCl\;(3.0\%\;of\;optimum\;concentration),$ while Vibrio sp.-87 strain grew at $1-7\%\;NaCl\;(2,0\%\;of\;optimum\;concentration).$ The fatty acid compositions of Vibrio sp.-86 strain grown at 1 atm were $C_{20}-C_{22:0},\;C_{l6:1},\;and\;C_{16:0}$ in the order of their abundance and at 400 atm the order were $C_{18:1},\;C_{18:0},\;and\;C_{20}-C_{22}$, whereas those of Vibrio sp.-87 strain at 1 atm were $C_{6:1},\;C_{14:1},\;and\;C_{20}-C_{22}$ and at 400 atm the order were $C_{14:1},\;C_{12:0},\;and\;C_{16:1}$ The amino acids compositon of Vibrio sp.-86 strain grown at 1 atm were abundant in the order of aspartic acid, methionine, and glutamic acid and those at 400 atm were abundant in the order of methionine, glutamic acid, and aspartic acid. The amino acids composition of Vibrio sp.-87 strain grwon at 1 atm were abundant in the order of methionine, glutamic acid, and aspartic acid and those at 400 atm were abundant in the order of methionine, glutamic acid, and isoleucine.

• 한국해양학회지
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• v.15 no.2
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• pp.79-88
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• 1980

Diaphus suborbitalis는 일본 준하만에 있어서 중 심층성 어류 micronekton의 주요종이다. 본연구에서는 본종의 생태규명의 일환으로서 지리분포와 일주수직이동의 양식을 밝혔다. 시료는 1971년 5월부터 1977년 4월까지 동경대학 해양연구소 연구선 담청환과 저인망어선에서 채집했다. 채집에는 6ft.의 IKMT, 구경 160cm의 대형플랑크톤네트(ORI), 구경 56cm의 MTD플랑크톤네트와 저인망을 사용했다. 1971년 5∼6월의 만내전역에 걸친 조사에 의하면, 본종은 연안성이 강하여 만의 안쪽부분으로부터 만서부에 있어서의 200∼500m 등심선에 따른 해역에 분포의 중심을 갖고, 만중앙부와 만남동부 및 만입구에서는 출현량이 적다. 이것은 본종이 Sergestes lucens, Diaphus watasei, Maurolicus muelleri등과 함께 만내에서 대륙붕사면 주변해역에 분포의 중심을 갖는 생물군집의 일원임을 나타내고 있다. 어군탐지기와 Net채집에 의한 시료에 의하면, 본종의 층간의 서식층은 수심 200∼400m 전후의 대륙붕사면의 근저층이다. 일몰시부터 음파산란층(DSL)을 형성하는 다른 생물과 함께 상승하기 시작하여, 야간은 수심 50m 전후층을 중심으로 분포한 후 새벽녘에 하강을 개시하여 다시 층간의 서식층으로 이동한다.

• Journal of the Earthquake Engineering Society of Korea
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• v.26 no.5
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• pp.181-190
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• 2022

In assessing the seismic safety of nuclear power plants, it is essential to analyze the structures using the observed ground motion. In particular, spatial variation in which the characteristics of the ground motion record differ may occur if the location is different within the site and even if the same earthquake is experienced. This study analyzed the spatial variation characteristics of the ground motion observed at the structure and site using the earthquake records measured at the Hamaoka nuclear power plant. Even if they were located on the same floor within the same unit, there was a difference in response depending on the location. In addition, amplification was observed in Unit 5 compared to other units, which was due to the rock layer having a slower shear wave velocity than the surrounding bedrock. Significant differences were also found in the records of the structure's foundation and the free-field surface. Based on these results, the necessity of considering spatial variation in the observed records was suggested.