• 대한방사선기술학회지:방사선기술과학
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• 제5권1호
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• pp.55-62
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• 1982

Measurement of triiodothyronine($T_3$) concentration is useful for the diagnosic and treatment of thyroid gland diseases. Fundermental studies of measurement of $T_3$ concentration by radioimmunoassay were performed and values determined by commercially available kit, Coat-A-Count, Diagnostic Products Corporation. The optimal utilization of the radioimmunoassay in measuring $T_3$ concentrations is dependant not only on high quality performance of the assay, but also on their appropriate application to the clinical situation. These are several aspects that must be considered in every individual case. These include factors such as accurate pippeting in reagent preparation in the assay and through decanting to remove all visible moisture after incubation steps and so forth. In attempt to assess quality control of the radioimmunoassay of serum $T_3$, serum pools with high, medium, low $T_3$ concentrations were assayed for each of 5 samples. The results obtained with this study were as follow: 1. The coefficient of variation(C. V.) for the standard curve ranged between $0.2{\sim}3.5%$. 2. It was necessary that both incubation time and temperature should correctly be maintained all the in the assay performance. 3. The precison with the $T_3$ RIA procedure was good. 4. The measured values of serially diluted serum $T_3$ concentration with Ong/dl standard solution was proportional to the predicted values. However dilution curve of distilled water was not strait. 5. Calculated $T_3$ values of patient serum in normal group was $107.8{\pm}25.90ng/dl$ in male patient and $127.29{\pm}24.08ng/dl$ in female patient.

• Journal of the korean society of oceanography
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• 제37권1호
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• pp.27-34
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• 2002

We measured the alkenone concentration of bulk sediments from a piston core collected from the Ulleung Basin in the East Sea in order to reconstruct past sea surface temperatures (SST). Sediment ages are well constrained by AMS $^{14}C$ dates of the planktonic foraminifera Globigerina bulloides. Coretop alkenone SST calibration with modern surface temperatures and sediment trap dat (Hong et al., 1996) indicate that the SST estimated from alkenones most likely represent the temperatures of late fall. Downcore variations in the alkenone saturation index indicate that between 19 and 15 kyr BP the surface waters were about $3^{\circ}C$ warmer than today. Between 15 and 11 kyr BP, the temperatures were about $3^{\circ}C$ lower than today. A rapid SST increase of about $3^{\circ}C$ occurred at approximately 10 kyr BP. After considering the factors which might influence the SST reconstruction from the $U^{k'}_{37}$ values, we conclude that the alkenone temperature estimates are reliable. The reason for glacial warming in the East Sea is not clear, although there is a possibility that it could be caused by shift in the season of maximum alkenone production from summer during the last glaciation to late fall during the Holocene. Cooling between 15 and 11 kyr BP may be due to inflow of cold water into the East Sea such as via the Oyashio Current or ice-melt water. Warming at the early Holocene could be due to inflow of the Tsushima Current into the East Sea through the Korea Strait.

• 수산해양기술연구
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• 제51권4호
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• pp.527-534
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• 2015

The twenty six specimens of leptocephali (15.8-32.6 mm TL) of the family Congridae, collected from southeastern waters offshore of Jeju Island during August 2014, and were identified by means of morphology and genetics. Those specimens were identified as belonging to the family Congridae based on various combinations of morphological characters. An analysis of the partial 12S rRNA sequences (886 base pairs) of mitochondrial DNA showed that our specimens must be Gnathophis nystromi, because their sequences were concordant with those of G. nystromi adult (genetic distance= 0.001), furthermore their total myomeres being consistent with those of G. nystromi adult. Catch rates of G. nystromi leptocephali were higher in the offshore regions than coastal regions of Jeju Island. The smallest leptocephali (< 20 mm TL) were collected offshore from Jeju Island. We hypothesize that one of the spawning grounds of G. nystromi is located offshore in the Jeju Island. In conclusion, the hatched preleptocephali of G. nystromi might have been transported from offshore near Jeju Island to the Korea Strait by the Kuroshio Current and Tsushima Warm Current.

• 수산해양기술연구
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• 제51권4호
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• pp.512-519
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• 2015

A historical tragic disaster happened by capsizing the passenger ship Sewol at South Western Sea of Korea in 16, April 2014. The ship which left Incheon harbour to bound for Jeju port passed Maengol strait and reached to approach of Byung Pung island, and then capsized and sank with a sudden inclination to the portside in the mean time of starboard the helm. In this time, the ship which has very poor stability without sufficient ballast waters and with over loading cargo listed port side caused by the centrifugal force acting to the outside of turning. A lot of cargoes not fastened moved to the port side consequently, and the ship came to beam end to capsize and sank in the end. No crews including especially captain would offer their own duties in a such extremely urgent time, as a result, enormous number of victims broke out including a lot of student. In this report, author carried out some calculation on the factors which influenced on the stability of the ship, i.e. the ship's speed, the rudder angle, the weight of cargoes and distance of movement, the surface effect of liquid in the tank. We found out that the most causes of capsize were the poor stability with heavy cargoes and insufficient amount of ballast water against the rule, and the cargoes unfastened moved one side to add the inclination as well. Above all, the owner be blamable because of the illegally operating the ship without keeping the rule.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2011년도 추계학술대회 초록집
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• pp.159.2-159.2
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• 2011

Hyundai Heavy Industries has developed a tidal current energy converter utilizing the accumulated technology as the world largest constructor for ship and offshore structures. The model has two sets of turbines in both ends in order to utilize the bi-directional current flows in flood and ebb tide. The torque produced by turbine in tidal current is directly delivered to generator along the horizontal axis, in which the turbine, gear, generator, gear and turbine are connected successively. The manufactured model for field test has the turbine diameter of 5 meters to produce the maximum power of 500kW at maximum current speed of 5m/s. The technical verification of tidal power converter was performed by means of small scale model test in towing tank as well as field test at the Strait of Uldolmok located in Jindo of Jeollanamdo province. Field test was performed by mounting the tidal current converter on the SEP(Self Elevating Platform) which could lower the 4 vertical legs on the seabed and could elevate platform over the water surface using the hydraulic power for itself. The field test performed for a month shows that power output is similar or larger compared with the expected one in design stage. This paper presents the development of tidal current energy converter and real sea field test by Hyundai Heavy Industries. This project has finished successfully and provided the technical advance toward commercial services for tidal current power generation in the south-west region in Korea.

• 한국수산과학회지
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• 제27권1호
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• pp.47-58
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• 1994

Field observation and numerical experiments with a two-dimensional depth-integrated model were undertaken in order to investigate some of the effects on the flow structure resulting from the construction of a bridge connecting Kohung Peninsula and the Narodo Islands on the southern coast of Korea. Tidal currents passing through the straits between the Narodo Islands showed that, although the phase lagged one hour behind that passing through the strait between Kohung Peninsula and Naenarodo Island, it still kept strong flows of more than 80cm/sec near the bottom. The seawater temperature and salinity within the study area seemed to be higher southward but uniform vertically. The results of the drogue experiments in the straits between the Narodo Islands showed that the drogues moved northward of Sayangdo in the early part of the flood tide, but southward in the late part of the flood tide and finally stopped a mile from the east coast of Surakdo. On the other hand, the numerical computation showed that the flow structures after construction of the bridge piers were basically in line with those before construction of the bridge piers, except for the slight variations of velocities in the vicinity of the bridge piers. A large scale clockwise circulation has been confirmed in the south area of Namsungri of Kohung Peninsula from the computational results of tide-induced residual currents. Referring to these computational results, the impact category on the flow structures due to the bridge piers construction has been estimated to be within around 2km. The results were in good agreement with the field observations.

• 동굴
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• 제45권46호
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• pp.9-31
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• 1996

The Mt. Peakdu is situated in north of the main peninsula, commanding geographically coordinated between longitude W($127^{\circ}$ 15' - $128^{\circ}$ 00') to E($128^{\circ}$ 15'- $129^{\circ}$ 00'), between latitude from S($41^{\circ}$ 15'- $42^{\circ}$ 00') to N($42^{\circ}$ 10'- $42^{\circ}$ 40'). The Manjyang-Gul in Cheju volcanic island is situated in the south of the main peninsula, commanding the Korean Strait, geographically coordinated longitude N($33^{\circ}$ 32' 26") and E($126^{\circ}$ 46' 48"). The quantitative analysis using XRF of volcanic rock samples for the north of Lu- Ming- Feng in Mt. Peakdu Group and the Manjang-Gul in Cheju island was Performed. The major chemical components by group analysis are as follows; Peakdu-Mt. Cheju Peakdu-Mt. Cheju (1) $Na_2O$(3.29Wt% and 3.27Wt%) (2) MgO (3.95Wt% and 6.l5Wt%) (3) $Al_2O_3$((17.64Wt% and 15.l7Wt%) (4) $SiO_2$((50.62Wt% and 50.99Wt%) (5) $P_2O_5$ (0.36Wt% and 0.30Wt%) (6) $K_2O$ (1.37Wt% and 1.04Wt%) (7) CaO (8.56Wt% and 8.06Wt%) (8) $TiO_2$ (2.37Wt% and 2.l5Wt%) (9) MnO (0.llWt% and 0.l6Wt%) (10) $Fe_2O_3$(9.l2Wt% and 12.56Wt%) The Group analysis data were compared in the relation within the age of formation for $0.16{\pm}0.08Ma$ in Mt. Peakdu Group, and $0.42{\pm}42Ma$ or $0.42{\pm}42Ma$ in Cheju island for K-Ar age. The crystal structure are mixed crystal of monoclinic, hexagonal and triclinic system in Mt. Peakdu Group and mixed structure of triclinic and cubic system in Cheju volcanic island.ic island.

• 한국정보통신학회:학술대회논문집
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• 한국해양정보통신학회 2010년도 추계학술대회
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• pp.303-310
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• 2010

오늘날 세계경제를 견인하는 국제무역의 약 98%는 해양을 통해 이루어지고 있다. 이러한 사실은 해양의 안보가 세계경제뿐만 아니라 세계의 안보에도 핵심적 요소가 되고 있음을 시사한다. 따라서 이제는 국제사회가 국제해양안보협력의 문제를 근본에서부터 평가하고 보다 발전시킬 때가 되었다. 그러나 해양안보협력의 문제는 각 국가들이 상이한 해양안보문제에 직면하고 있고 이러한 안보문제를 해결하기 위한 안보협력을 위해서는 많은 인력과 예산이 투입되어야 하기 때문에 그렇게 쉬운 일이 아니다. 따라서 본 논문은 소말리아와 말라카 해협 등 국제적 핵심해상교통로 상에서의 해적대응을 위한 해양안보협력현황을 평가하고 이 평가에 기초하여 보다 발전적인 해양안보협력방안을 제시하기 위한 목적으로 작성하였다.

• 한국수산과학회지
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• 제15권2호
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• pp.171-177
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• 1982

대한해협에서의 해수의 광학적 성질을 조사하기 위하여, 1950년 7월에 대한해협 체주도의 15개 관측점에서 투명도, 수색, 태양광의 4가지 색(Clear;$400\sim720nm,\;Red: 600\sim700nm,\;Green : 475\sim600nm,\;Blue; 400\sim475nm$)에 대한 해수의 표면조도 및 수중조도 등을 조사한 결과를 요약하면 다음과 같다. 1. 본 조사해역의 평균투명도는 18.3m($11.5\sim24m$)였고, 평균수색은 3.5($3\sim4$)였다. 2. 해수의 평균흡수계수는 적색광이 $0.129(0.090\sim0.270), 백색광이 0.098(0.063\sim0.183), 청색광이 0.087(0.036\sim0,142), 녹색연이 0.081(0.044\sim0.142)$순으로 적게 나타났다. 3. 해수의 흡수계수 $\kappa$와 투명도 D와의 관계는 적색광이 $\kappa=2.33/D$, 백색광이 $\kappa=1.72/D$, 음색광이 $\kappa=1.44/D$, 녹색광이 $\kappa=1.41/D$순으로 작게 나타났다. 4. 태양열선의 표면광에 대한 평균해중투과율은 녹색광(수심 5m층에서 $63.20\%$, 15m층에서 $30.47\%$, 30m층에서 $10.03\%$, 50m층에서 $2.24\%$), 청색광(수심 5m층에서 $62.70\%$, 15m층에서 $30.00\%$, 30m층에서 $9.75\%$, 50m층에서 $1.70\%$), 백색광(수심 5m층에서 $57.90\%$, 15m층에서 $23.40\%$, 30m층에서 $6.23\%$, 50m층에서$1.00\%$), 적색광(수심 5m층에서 $48.95\%$, 15m층에서 $14.81\%$ 30m층에서$2.76\%$, 50m층에서 $0.28\%$)의 순으로 적게 나타났다. 5. 천명도지에서의 태양열의 해중투과율은 녹색광이 표면광의 $23.89\%(16.5\sim38\%)$, 청색광이 $23.42\%(14\sim44\%)$, 백색광이 $17.29\%(12.7\sim27\%)$, 적색광이 $9.70\%(4.5\sim13\%)$의 순으로 적게 나타났다.

• 한국수산과학회지
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• 제17권3호
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• pp.219-229
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• 1984

1983년 7월 $25{\sim}31$일의 대한해협에서 실시한 관측자료를 사용하여 대한해협 서수도 수계의 화학적 성분을 분석 조사하였다. 그 결과 낙동강 유출수, 쓰시마 난류수, 거제도 연안수 및 울산 연안수의 4개의 수계로 구분되었다. 한편 낙동강 유출수의 영향은 거제도쪽 보다 부산영도인 동해 남부 연안쪽이 더 컸다. 이들 수계의 특성으로 먼저 낙동강 유출수는 투명도 3m 이하, 수색 7인 황토색 물로 표면의 수온, 염분, 용존산소, 인산염은 각각 $18{\sim}19^{\circ}C,\;31\%0$ 이하, $4.5{\sim}50ml/l,\;0.25{\sim}0.5{\mu}g-atom/l$이었고 또 질산염과 규산염은 해역중 가장 높은 간인 $10.0{\mu}g-atom/l$ 이상이었다. 쓰시만 난류수는 투명도 15m 이상, 수색 $4{\sim}2$의 맑은 물로 표면수온 $23^{\circ}C$내외 염분$32{\sim}33\%0$의 고온 저염수이다. 또한 표면의 용존산소는 5.0ml/l이상, 인산염, 질산염, 규산염은 각각 0.25, 2.0, $2.5{\mu}g-atom/l$ 이하로 해역중 가장 낮은 값이었다. 거제도 연안수는 표면수온 $20{\sim}21^{\circ}C$, 염분 $33\%0$이상의 비교적 저온 고염이고 표면 용존산소량이 5.0ml/l 이하, 인산염 $0.5{\mu}g-atom/l$ 내외 질산염과 규산염은 각각 $3.5{\mu}g-atom/l$ 이하로 나타났다. 또한 울산 연안수는 관측 해역중 가장 표면수온이 낮은 $16^{\circ}C$ 이하, $33.5\%0$ 이상의 저온고염이고, 용존산소, 인산염, 질산염, 규산염은 상당히 높은 값을 가져 저층수의 연안용승으로 인한 것이 아닌가 생각된다.