• International Journal of Ocean System Engineering
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• 제2권1호
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• pp.1-7
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• 2012

The cross-shore sediment transport in a coastal region causes the important changes in beach morphological properties. The accurate estimation of the cross-shore sediment transport is important for the designing of the marine structures such as seawalls, jetties, breakwaters etc, and the preventing coastal erosion and accretion due to on-off shore sediment transportation. In this study, the experiments on cross- shore sediment transport carried out in a laboratory wave channel for initial beach slopes of 1/8, 1/10 and 1/15. Using the regular waves with different deep-water wave steepness generated by a pedal-type wave generator, the geometrical characteristics of beach profiles under storm conditions and the parameters affecting on-off shore sediment transport are investigated for the beach materials having medium diameters of $d_{50}$=0.25, 0.32, 0.45, 0.62 and 0.80 mm. The experimental results obtained from this study compared with previous experimental work and found to be of the same magnitude as the experimental measurements and followed the expected basic trend.

• 해양환경안전학회지
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• 제12권2호
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• pp.157-163
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• 2006

현재 대기중 $CO_2$ 농도를 감소시키기 위하여 $CO_2$를 해양에 격리 처리하고자 하는 방안이 모색되고 있으나 이러한 방안은 해양생물 및 생태계에 미치는 영향 정도에 따라 그 실현가능성이 결정될 것이다. 본 연구에서는 $CO_2$ 해양격리 처리와 관련하여 수행되어온 연구들을 정리하고, $CO_2$ 농도가 높아진 해양환경에서의 해양생물 특히 어류를 대상으로 수행된 최근의 연구결과를 정리하였다. $CO_2$ 농도의 증가는 어류에 있어 산염기조절, 호흡순환기적 조절 등과 같은 생리적 기능에 영향을 끼치고 결국 어류의 폐사를 초래할 것이다. $CO_2$가 해양생물에게 어떠한 영향을 미치는가에 대한 연구는 주로 천해어종을 대상으로 하여 진행되어 왔으나 향후의 연구는 천해어종에 대한 연구결과를 바탕으로 $CO_2$가 실제로 격리 처리되는 심해에서 $CO_2$에 대한 생물들의 응답에 관하여 조사할 필요가 있다.

• 한국수산과학회지
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• 제24권5호
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• pp.303-314
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• 1991

반폐쇄만이며 하계동안 저층 빈산소수괴(Hypoxic bottom area)가 형성되는 진해만 일대 해역중의 하나인 원문만에서 해양세균의 계절적 분포와 해양세균이 용존산소소모에 미치는 영향을 알기 위하여 하계동안 미소생물의 전자전달계 활성도(Electron transport system activity)로서 잠재적 산소소모량(potential consumption of oxygen)을 구하였다. 해양세균의 계절별 우점종은 추계('89년 10월)에는 Pseudomonas spp., 동계 ('90년 2월)에는 Serratia spp., 춘계('90년 5월)에는 Acinetobacter spp., 하계('90년 8월)에는 Flavobacterium spp.가 우점하였다. 조사기간동안 생균수는 하계('90년 8월)에 표층, 저층, 저질의 평균치가 각각 $2.12\times10^6cells/ml,\;1.34\times10^6cells/ml,\;1.55\times10^7cells/ml$로 높은 분포치를, 동계에는 표층, 저층, 저질의 평균치가 각각 $2.08\times10^5cells/ml,\;1.54\times10^5cells/ml,\;1.28\times10^6cells/ml$로 낮은 분포치를 보여주었다. 또한 전자전달계 활성(Electron Transport System Activity)으로 잠재적 산소소모량을 조사한 결과 하계동안 수괴에서 미소생물군집의 잠재적 산소소모량은 $232.4-637.5{\mu}l/O_2/l/day$, 이중 세균의 잠재적 산소소모량은 $142.6-432.4{\mu}l/O_2/l/day$로서 수괴의 미소생물군집의 잠재적 산소소모량의 약 $55\%$를 차지하여, 하계동안 저층의 산소소모에 큰 영향을 미침을 알 수 있었으며, 세균의 잠재적 산소소모량은 생균수와 밀접한 관계가 있었다.

• 한국환경과학회지
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• 제23권11호
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• pp.1889-1907
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• 2014

The characteristics of meteorological conditions related to changes in atmospheric environment on Jeju Island were investigated during recent years (2010-2012). This analysis was performed using the hourly observed data of meteorological variables (air temperature, wind speed and direction) and air pollutants ($O_3$, $PM_{10}$, $SO_2$, $NO_2$, and CO). Out of 5 pollutants, $O_3$ and $PM_{10}$ concentrations have frequently exceeded national environmental standards in the study area during the study period, with relatively higher concentrations than the others. The concentrations of $O_3$ and $PM_{10}$ in 2010 and 2011 were somewhat higher than those in 2012, and their highest concentrations were mostly observed in spring followed by fall. Nighttime $O_3$ concentrations (with relatively high concentration levels) were almost similar to its daytime concentrations, due to less $O_3$ titration by very low NO concentrations in the target area and in part to $O_3$ increase resulting from atmospheric transport processes. The transport effect related to the concentration variations of $O_3$ and $PM_{10}$ was also clarified in correlation between these pollutants and meteorological variables, e.g. the high exceedance frequency of concentration criteria with strong wind speed and the high concentrations with the westerly/northwesterly winds (e.g., transport from the polluted regions of China). The overall results of this study suggest that the changes in atmospheric environment in the study area were likely to be caused by the transport effect (horizontal and vertical) due to the meteorological conditions rather than the contribution of local emission sources.

• 무역상무연구
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• 제15권
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• pp.119-136
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• 2001

The purpose of this paper is to consider how to decide the cause of loss or damage to the transport goods when maritime accident occurs. In marine insurance, the underwriter is liable for any loss or damage proximately caused by a risk insured(MIA Art.55). So it is very important to determine the proximate cause of loss or damage to ascertain whether it is to be recoverable under the policy. But there is no definite conception or rule what is the proximate cause. It was left to the tribunal as a question of fact. In this paper, I will suggest the general rules to determine the proximate cause of loss or damage of the transport goods in marine insurance. First, in MIA 1906, there is the rule of proximate causation and it has been established the effective causation by cases since 1918. Second, in Institute Cargo Clauses(B) & (C), there are rules of considerably relaxed standards to determine the causation of loss of or damage using the "attributable to" and "caused by" basis. Third, it is noted, under the complex causation situation, there are difference basises to decide the liability of underwriters between the case of successive occurrence of single risk and the case of concurrent occurrence of several risks. Forth, in practice, it couldn't be ascertained the underwrier's liability by a definite rule and it should be fully considered the circumstances and conditions of the loss.

• 한국중재학회지:중재연구
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• 제5권1호
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• pp.233-255
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• 1995

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 1991년도 제13회 대기보전학술연구발표회 요지집
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• pp.5-6
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• 1991

• Journal of the korean society of oceanography
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• 제39권1호
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• pp.96-106
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• 2004

A total of 116 surface sediment samples were obtained on the Yellow Sea and analyzed for grain size and geochemical elements in order to interpret the present sediment transportation. Thirty-nine cores and 3,070 line-km shallow seismic profiles are analyzed for sedimentary records of Yellow Sea in the past. Results show that the boundary of sediment transport between Korean side and Chinese side is about between $123^{\circ}E$ and $124^{\circ}E$. The similar result is produced from Shi et al. (in this publication). Two cyclonic patterns of surface sediments are recognized in the northeastern and southwestern Yellow Sea, while the strong front zone of the mud patch and sandy sediments are found in the southeastern Yellow Sea (the southwestern part of Korean coasts). The formation of fine-particle sediment packages, called for Northwest Mudbelt Deposit (NWMD), Hucksan Mudbelt Deposit (HSMD) and Jeju Mudbelt Deposit (JJMD), are resulted from eddies (gyres) of water circulations in the Yellow Sea. NWMD has been formed by cyclonic (anticlockwise) eddy. NWMD is composed of thick, homogeneous, relatively semi-consolidated gray clay-dominated deposit. On the other hand, HSMD and JJMD are formed by anticyclonic (clockwise) eddies. They are thick, homogeneous, organic-rich gray, silt-dominated deposit. Both core and surface sediments show that the middle zone across Chinese and Korean side contains bimodal frequency of grain-size distribution, indicating that two different transport mechanisms exist. These mud packages are surrounded by sand deposits from both Korea and China seas, indicating that Yellow Sea, which is the shallow sea and epicontinental shelf, is formed mostly by sand deposits including relict sands. The seismic profiles show such as small erosional/non-depositional channels, sand-ridges and sand-waves, Pleistocene-channelfilled deposits, a series of channels in the N-S major channel system, and thick Holocene sediment package, indicating that more complex sedimentary history exists in the Yellow Sea.

• 한국수산과학회지
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• 제53권4호
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• pp.486-491
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• 2020

This study was investigated the survival and hatching rate of fertilized eggs in olive flounder Paralichthys olivaceus at water temperature, salinity, duration of transport and different stock densities during commercial transport. The observed optimal temperature during transport was 17.5℃ similar to the natural environmental conditions. The proper salinity was observed to be at 33 psu (practical salinity unit) in both surviving and hatching rate. In terms of the duration of transport, there were no differences until 12 hours between survival and hatching rate, but shorter time of transport would be better. With the best conditions during transport, 20,000 eggs/L were handled in both survival and hatching rate. These results can be essential in the production and transport of healthy olive flounder seeds.

• 한국해양바이오학회지
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• 제2권4호
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• pp.201-208
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• 2007

Polychlorinated biphenyls (PCBs) are anthropogenic contaminants found globally in water, ice, soil, air and sediment. Modern analytical techniques allow us to determine these chemicals in environmental matrices at parts per trillion levels or lower. Environmental forensic on PCBs opens up new avenues of investigation such as transport and fate of water masses in oceans, sedimentation, onset of primary production, migration of marine mammals, their population distribution and pharmacokinetics of drugs inside organisms. By virtue of persistence, bioaccumulation, bioconcentration and structure-activity relationship PCBs emerge as unconventional chemical tracers of new sort.