• 제목/요약/키워드: Simulated sea water

검색결과 144건 처리시간 0.024초

Comparison of RIAMOM and MOM in Modeling the East Sea/Japan Sea Circulation

  • Lee, Ho-Jin;Yoon, Jong-Hwan;Kawamura, Hideyuki;Kang, Hyoun-Woo
    • Ocean and Polar Research
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    • 제25권3호
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    • pp.287-302
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    • 2003
  • The seasonal variations in the circulation of the water mass in the East Sea/Japan Sea have been simulated using a free surface primitive ocean model, RIAMOM (RIAM Ocean Model), comparing the results from GFDL-MOM1 (Geophysical Fluid Dynamics Laboratory Modular Ocean Model, version 1.1, hereafter MOM) with the GDEM (Generalized Digital Environmental Model) data. Both models appear to successfully reproduce the distinct features of circulation in the East Sea/Japan Sea, such as the NB (Nearshore Branch) flowing along the Japanese coast, the EKWC (East Korean Warm Current) flowing northward along the Korean coast, and the NKCC/LCC (North Korean Cold Current/Liman Cold Current) flowing southwestward along Korean/Russian coast. RIAMOM has shown better performance, compared to MOM, in terms of the realistic simulation of the flow field in the East Sea/Japan Sea; RIAMOM has produced more rectified flows on the coastal region, for example, the narrower and stronger NKCC/LCC than MOM has. There is however obvious differences between the model results and the GDEM data in terms of the calculation of the water mass; both models have shown a tendency to overpredict temperature and underpredict salinity below 50m; more diffusive forms of thermocline and halocline have been simulated than noted in GDEM data.

연안어장의 환경변화가 수산자원량에 미치는 영향평가 (Environmental Impact Analysis on Fish Stocks caused by Environmental Change in the Coastal Fishing Ground)

  • 이인철
    • 한국해양공학회지
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    • 제15권1호
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    • pp.36-44
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    • 2001
  • To predict the influence on fish stocks which were caused by environmental change in the fishing ground of shallow sea areas, we have developed the Shallow-Sea Ecological Model(SSEM) which that focuses on living organisms, especially fish and benthos. By applying the SSEM in the Seto-Inland Sea of Japan, we have simulated another aspect of influence on fish stocks that was caused by oxygen deficient water mass and nutrient loads. From the simulated result of the fish stocks, it was indicated that the stock of fish and benthos has shown a relative difference between the western sea and the eastern sea in the Seto-Inland Sea. According the to prediction, results of fish stocks that were caused by oxygen deficient water mass, it was estimated that the pelagicfish stock increases about 6 %, whereas the stocks of demersalfish and benthos decreases about 30% and 70%, respectively. On the other hand, it seemed that there was an increased in the fish stocks of demersalfish and benthos in the eastern sea of Seto-Inland Sea by nutrient loads reduction.

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H 콘도의 건설에 따른 천수만 양식장 안전성 검토 (A Safety Study of the Fish Farm in Cheonsuman after Constructing the H Condominium)

  • 한두희
    • 한국산학기술학회논문지
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    • 제14권8호
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    • pp.4093-4099
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    • 2013
  • 본 논문은 부남호 부근에 대형 콘도를 지을 때 콘도에서 나오는 오폐수가 천수만 가두리 양식장 등에 영향을 미치는가에 관한 것이다. 대표적으로 COD를 모사하였으며, 다른 인자는 수치에 비례하여 예측할 수 있다. 조류의 이동 경로는 평균적으로 방류지점으로부터 서쪽을 향하게 되어 이곳은 가두리 양식장이 없기 때문에 비교적 안전하며, 바닷물이 정지한 상태를 가정하여 모의한 결과 매우 천천히 확산되는 것을 보았지만, 바람 등에 의한 흐름이 있을 경우는 오염물질의 확산을 촉진하여 쉽게 희석되기 때문에 오염물질에 의한 피해의 위험은 크지 않을 것으로 판단된다.

임원에서의 1983년 동해 중부 지진해일 수치모의: 1. 동해에서의 전파 (Numerical Simulations of 1983 Central East Sea Tsunami at Imwon: 1. Propagation across the East Sea)

  • 조용식;이호준
    • 한국수자원학회논문집
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    • 제35권4호
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    • pp.443-452
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    • 2002
  • 본 연구에서는 지난 수십 년간 가장 파괴적인 지진해일로 기록된 1983년 동해에서 발생한 지진해일이 동해를 거쳐 우리나라 동해안으로 전파해오는 과정을 수치해석하였다. 천수방정식에 근거한 수치모형을 이용하였으며, 물리적 분산은 leap-frog 유한차분기법에 의해 발생하는 수치분산으로 어느 정도 대체하도록 하였다. 진원으로부터 지진해일 전파도와 파향선법에 의한 전파제적을 산정하였다.

東海에서의 파랑추산을 위한 심해파랑모형에 대한 연구 (Deep Water Wave Model for the East Sea)

  • 윤종태
    • 한국해양공학회지
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    • 제13권2호통권32호
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    • pp.116-128
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    • 1999
  • A deep water wave prediction model applicable to the East Sea is presnted. This model incorporates rediative transter of energy specrum, atmospheric input form the wind, nonlinear interaction, and energy dissipation by white capping. The propagation scheme by Gadd shows satisfactory results and the characteristics of the nonlinear interaction is simulated well by discrete interaction approximatiion. The application of the model to the sea around the Korean Peninsula shows reasonable agreement with the observation.

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해진시 개단무리말뚝의 거동에 관한 모형실험 연구 (An Experimental Study on the Behavior of Open-ended Pipe Piles Ggroup to the Simulated Seaquake)

  • 남문석;최용규;김재현
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 1999년도 봄 학술발표회 논문집
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    • pp.447-454
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    • 1999
  • The compressive capacity and the soil plugging resistance of single open-ended pipe pile were completely decreased in the previous study on the behavior of shorter single pile during simulated seaquake induced by the vertical component of earthquake. But the capacity of single open-ended pipe pile with greater penetration and the capacity of piles group with shorter penetration were expected to be stable after seaquake motion. In this study, first, 2-piles or 4-piles are driven into the calibration chamber included in saturated fine medium sand with several simulated penetrations, and the compressive load test for each piles group was performed. Then, about 95 % compressive load of the ultimate capacity was applied on the pile head during the simulated seaquake motion. Finally, In confirm the reduction of pile capacity during the simulated seaquake motion, the compressive load test for each single pile or piles group after seaquake motion was performed. During the simulated seaquake, the compressive capacity of open-ended pipe piles with greater penetration ( 〉about 27 m) was not degraded even in deep sea deeper than 220 m and soil plug within open-ended pipe pile installed in deep sea was stable after seaquake motion. Also, in the case of 2-piles or 4-pile groups, the compressive capacity after seaquake motion was not degraded at all regardless of pile penetration depth beneath seabed, sea water depth and seaquake frequency.

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Numerical simulation of Hydrodynamics and water properties in the Yellow Sea. I. Climatological inter-annual variability

  • Kim, Chang-S.;Lim, Hak-Soo;Yoon, Jong-Joo;Chu, Peter-C.
    • Journal of the korean society of oceanography
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    • 제39권1호
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    • pp.72-95
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    • 2004
  • The Yellow Sea is characterized by relatively shallow water depth, varying range of tidal action and very complex coastal geometry such as islands, bays, peninsulas, tidal flats, shoals etc. The dynamic system is controlled by tides, regional winds, river discharge, and interaction with the Kuroshio. The circulation, water mass properties and their variability in the Yellow Sea are very complicated and still far from clear understanding. In this study, an effort to improve our understanding the dynamic feature of the Yellow Sea system was conducted using numerical simulation with the ROMS model, applying climatologic forcing such as winds, heat flux and fresh water precipitation. The inter-annual variability of general circulation and thermohaline structure throughout the year has been obtained, which has been compared with observational data sets. The simulated horizontal distribution and vertical cross-sectional structures of temperature and salinity show a good agreement with the observational data indicating significantly the water masses such as Yellow Sea Warm Water, Yellow Sea Bottom Cold Water, Changjiang River Diluted Water and other sporadically observed coastal waters around the Yellow Sea. The tidal effects on circulation and dynamic features such as coastal tidal fronts and coastal mixing are predominant in the Yellow Sea. Hence the tidal effects on those dynamic features are dealt in the accompanying paper (Kim et at., 2004). The ROMS model adopts curvilinear grid with horizontal resolution of 35 km and 20 vertical grid spacing confirming to relatively realistic bottom topography. The model was initialized with the LEVITUS climatologic data and forced by the monthly mean air-sea fluxes of momentum, heat and fresh water derived from COADS. On the open boundaries, climatological temperature and salinity are nudged every 20 days for data assimilation to stabilize the modeling implementation. This study demonstrates a Yellow Sea version of Atlantic Basin experiment conducted by Haidvogel et al. (2000) experiment that the ROMS simulates the dynamic variability of temperature, salinity, and velocity fields in the ocean. However the present study has been improved to deal with the large river system, open boundary nudging process and further with combination of the tidal forcing that is a significant feature in the Yellow Sea.

Data analysis of simulated fuel-loaded sea transportation tests under normal conditions of transport

  • JaeHoon Lim;Woo-seok Choi
    • Nuclear Engineering and Technology
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    • 제56권2호
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    • pp.375-388
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    • 2024
  • In this study, to evaluate the shock and vibration load characteristics of used fuel, a sea transportation test was conducted using simulated fuel assemblies under normal transport conditions. An overall test data analysis was performed based on the measured strain and acceleration data obtained from cruise, rotation, acceleration, braking, depth of water, and rolling tests. In addition, shock response spectrum and power spectral densities were obtained for each test case. Amplification and attenuation characteristics were investigated based on the load path. The load was amplified as it passed from the overpack to the simulated used fuel-assembly. As a result of the RMS trend analysis, the fuel-loading position of the transportation package affected the measured strain in the fuel rod, and the maximum strains were obtained at the spans with large spacing. However, even these maximum strains were very small compared to the fatigue strength and the cladding yield strength. Moreover, the fuel rods located on the side exhibited a larger strain value than those at the center.

Effect of climate change and sea level rise on taking water of South Thai Binhirrigation system in Vietnam

  • Nguyen, Thu Hien;Nguyen, Canh Thai
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2015년도 학술발표회
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    • pp.222-222
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    • 2015
  • Vietnam is one of the most vulnarable countries affected by climate change and sea level rise. One of the consequences of climate change and sea level rise is the increase of salinity intrusion into the rivers which is challenging to irrigation systems in coastal areas. This indicates the necessary to study the ability of taking water through sluice gates of irrigation systems in coastal zones, especially in the dry season with the effects of climate change and sea level rise in the future. In this paper, Nam Thai Binh irrigation system is selected as a case study. The irrigation system is one of 22 biggest irrigation systems of the Red River delta in Vietnam located in coastal region. The computed duration is selected in dry season to irrigate for Winter-Spring crops. The irrigation water for the study area is taken from different sluice gates along the Red River and the Tra Ly River. In this paper, MIKE-11 model was applied to assess the ability of taking water for irrigation of the study area in current situation and in the context of climate change and sea level rise senario in 2050 (under the medium emissions scenario (B2) published by the Ministry of Natural Resources and Environment of Vietnam published in 2012) with different condition of water availability. The operation of the gates depends on the water levels and sanility conditions. The sanility and water level at different water intake gates of Nam Thai Binh irrigation system were simulated with different senarios with and without climate change and sea level rise. The result shows that, under climate change and sea water level rise, some gates can take more water but some can not take water because of salinity excess and the total water taking from the different gates along the rivers decrease while the water demand is increase. The study indicates the necessary to study quantitatively some recommended solutions in the study area particularly and in coastal region generally in Vietnam to ensure water demand for irrigation and other purposes in the context of climate change and sea level rise in the future.

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모사해수 조건에서 회분식 실험을 이용한 제강슬래그의 카드뮴 흡착 특성 평가 (Assessment of the Sorption Characteristics of Cadmium onto Steel-making Slag in Simulated Sea Water Using Batch Experiment)

  • 김은협;이성수;이광헌;김용우;박준범;오명학
    • 한국지반공학회논문집
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    • 제27권4호
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    • pp.43-50
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    • 2011
  • 본 연구에서는 국내 해안지역에 존재하는 카드뮴을 산업 폐기물인 제강슬래그를 이용하여 제거하고자, 제강슬래그의 카드뮴 제거 성능을 평가하였다. 이를 위해 회분식 실험으로 등온흡착 실험과 동적흡착 실험을 수행하였다. 등온 흡착 실험을 통해 제강슬래그의 카드뮴 제거는 Langmuir 모델이 Freundlich에 비해 잘 맞음을 확인하였고 최대 흡착량(${\beta}$)을 계산할 수 있었다. 동적흡착 실험결과의 경우, 유사이차 모델을 이용해 해석하였고 카드뮴의 초기농도가 높을수록 평형 흡착량 ($q_e$)은 증가하였고 반응상수 ($k_2$)와 초기반응속도 (h)는 줄어들었다. 모사해수 조건에서 $q_e$는 증류수 조건과 큰 차이가 없었지만 $k_2$와 h는 증류수에 비해 줄어들었다. 또한, 유사이차 모델을 통해 예측된 $q_e$이 등온흡착 실험에서 구한 평형 흡착량 ($C_s$)과 유사해 동적흡착 실험결과로 등온흡착 실험결과를 예측하는 것이 가능함을 확인하였으며 유사이차 모델을 이용해 목표 제거율에 도달하는 반응시간을 계산할 수 있었다.