• Journal of the korean society of oceanography
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• 제35권4호
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• pp.170-178
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• 2000

Low salinity water was observed during May in the Cheju Strait. Its structure and source were studied by using both the hydrographic data collected not only in the Cheju Strait during 1987-1989 but also in the wider area around Cheju Island extending to the Bank of Changjiang river in 1994 and the current data taken in the Strait during 1987-1989. The water had lower values of temperature, salinity, and density compared with the surrounding water and it was found in the surface layer outside of Tsushima Current Water 10-50 km off Cheju coast. The density of low salinity water was more dependent on salinity than on temperature. The low salinity water flowed into the Strait from the west as a series of intermittent waters whose size was variable in width and in thickness. The low salinity water was originated from the Chanajiang River Diluted Water. In the Cheju Strait, the water showed changes within 3 days on time and 30-50 km on space, and its sudden appearance was marked especially in May. Such strong variability and sudden appearance may be attributed to the beginning stage in May when the fresh water of Changjiang River Diluted Water starts to arrive in the Cheju Strait.

• 한국분무공학회지
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• 제10권1호
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• pp.1-9
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• 2005

When the water jets heated up to the saturation temperature at a high line pressure are sprayed into a reduced (atmospheric) pressure through an air-assisted nozzle, the jets experience sudden exposure into a reduced pressure, get superheated and produce steam bubbles while atomization processes of jets are taking place. This process is called flash atomization. In this study the flash atomization of superheated water jets assisted by air has been studied. Sprays with flash atomization have been photographed at various water and air flow rates and water superheats. It has been found that the spray angle with flash atomization increases with water superheat and water flow rate but decreases with air flow rate. The degree of change of spray angle has been analyzed and correlated as a function of superheat, air and water flow rates.

• 생태와환경
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• 제56권4호
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• pp.420-429
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• 2023

This study was designed to examine the immune response in Korean rockfish during water temperature fluctuation and to elucidate the factors contributing to streptococcal pathogenesis in cultured Korean rockfish, S. schlegeli. We investigated cumulative mortality against Streptococcus iniae (FP5228 strain) infection in the exposed Korean rockfish (39.7±5.8 g) to environmentally relevant temperature (Control, 23℃; High temperature, 28℃ and 23℃ and 28℃ with 12 hours interval exchange, 23↔28℃) for 48 hours. Also, the expression of the mRNA related to the immune response genes (heat shock protein 70, interleukin1β, lysozyme g-type and thioredoxin-like 1) were measured in spleen and head kidney by real-time PCR analysis in the exposed fish to thermal stress. In this study, the combined stress with bacterial challenge in fishes exposed to thermal stress lowered the survival rate than that of control (23℃). The cumulative mortality in the group of control, 28℃ and 23↔28℃ was 24%, 24% and 40% (P<0.05), respectively. Also, thermal stress modulated the mRNA level of immune related genes; heat shock protein 70, interleukin-1β, lysozyme g-type and thioredoxin-like 1 in Korean rockfish. The present study indicates that a high and sudden water temperature change affect immune responses and reduce the disease resistance in Korean rockfish.

• Geomechanics and Engineering
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• 제24권6호
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• pp.531-543
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• 2021

Freezing and thawing of pore water within backfill can affect the stability of retaining wall as the phase change of pore water causes changes in the mechanical characteristics of backfill material. In this study, the effects of freezing and thawing on the mechanical performance of retaining wall with granular backfill were investigated for various temperature and groundwater level (GWL) conditions. The thermal and mechanical finite element analyses were performed by assigning the coefficient of lateral earth pressure according to phase change of soil for at-rest, active and passive stress states. For the at-rest condition, the mobilized lateral stress and overturning moment changed markedly during freezing and thawing. Active-state displacements for the thawed condition were larger than for the unfrozen condition whereas the effect of freezing and thawing was small for the passive condition. GWL affected significantly the lateral force and overturning moment (Mo) acting on the wall during freezing and thawing, indicating that the reduction of safety margin and wall collapse due to freezing and thawing can occur in sudden, unexpected patterns. The beneficial effect of an insulation layer between the retaining wall and the backfill in reducing the heat conduction from the wall face was also investigated and presented.

• 한국수산과학회지
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• 제34권2호
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• pp.91-97
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• 2001

1회성의 수온급변 실험으로서 크게 2가지 형태의 수온변화 조건을 주었다: $20^{\circ}C$로부터 시간당 $2^{\circ}C$씩 수온을 떨어뜨려 $10^{\circ}C$까지(소요시간 5시간) 낮춘 다음, 21시간 유지한 것 (Exp.I)과 $20^{\circ}C$로부터 시간당 $2^{\circ}C$씩 수온을 상승시켜 $30^{\circ}C$까지 (소요시간 5시간)올린 다음, 21시간 유지한 것 (Exp. II). 수온을 $20^{\circ}C$로부터 $10^{\circ}C$로 급격하게 낮춘 실험에서 실험어의 Ht는 넙치대 $11.6\pm0.2\sim15.5\pm0.1\%$, 넙치소 $9.0\pm0.4\sim13.5\pm2.0\%$, 쥐노래미 $18.3\pm3.6\sim23.2\pm3.8\%$의 범위로서 쥐노래미가 넙치에 비하여 높은 값을 나타냈다. 코티졸 농도는 넙치소에서 유의한 변화를 보이지 않은 반면, 넙치대와 쥐노래미에서 실험개시시에 각각 $5.2\pm8.5ng/mL,\;2.7\pm0.4ng/mL$였던 것이 $10^{\circ}C$ 하강시에 각각 $164.0\pm53.1ng/mL,\;207.9\pm25.4ng/mL$로 크게 높아졌다. 젖산은 넙치대에서는 실험개시시에 비해 차이를 보이지 않았으나, 넙치소와 쥐노래미에서 개시시 보다 낮아져 글루코스 농도의 변화와 비슷하였다. 수온을 $20^{\circ}C$로부터 $30^{\circ}C$로 급격하게 높인 Exp. II에서 실험어의 Hb 변화는 모든 어종에서 수온급상승에 따라 약간 높아지는 경향을 보이다가 실험개시시의 수준으로 회복되었다. 쥐노래미에서는 수온급변에 따라 MCV는 상승하는 반면, MCHC는 하강하였다. 넙치대·소의 코티졸 농도는 Exp. I의 결과와 같이 큰 변화를 나타내지 않았다. 그러나 쥐노래미에서는 실험개시시의 $2.7\pm0.2ng/mL$로부터 $44.7\pm9.1ng/mL$로 높아졌다. 글루코스 농도는 모든 어종에서 실험개시시 보다 높아져 Exp.Ⅰ결과와는 반대되는 경향을 나타냈다.

• 한국농공학회지
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• 제31권2호
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• pp.43-53
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• 1989

In this research programs, a series test was conducted to show the effects of freeze/thaw process on the various soil properties. The tests were carried out taken from the west sea shore of Korean peninsular and the west sea shore of Scotland, and their results are as follows; 1. There was a positive total heave in a freezing run, although water may he expelled for the sample initially. The water flow must he reverse' from expulsion to intake. 2. The confining pressure had an overriding influence on the heave and frost penetration, a sudden change of the axial strain at failure with strain rate was observed occuring at a strain rate between 10-5 and 10-6, and the initial friction angle of frozen clay was appeared zero. 3. There was shown a significant decrease in liquid limit of soil which was subjected to freeze/thaw process for the initial value of about 20% because of soil particles aggregation. 4. The cyclic freeze/thaw caused a sinificant reduction in shear strength and its thixotropic regain. The frozen/thawed soil exibited negative strength regain, particularly at high freeze/thaw cycles. 5. The freezing temperature greatly influenced on the failure strength of soils and this. Trend was more pronounced the lower the freezing temperature and shown the ductile failure with indistinct peaks.

• Current Applied Physics
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• 제18권11호
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• pp.1313-1319
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• 2018

The coil-to-globule behavior of poly{${\gamma}$-2-[2-(2methoxyethoxy)ethoxy]ethoxy-3-caprolactone} (PMEEECL) as a ${\gamma}$-substituted poly (${\varepsilon}$-caprolactone) was investigated via atomistic molecular dynamics (MD) simulation. For this purpose, radius of gyration, end-to-end distance and radial distribution function of the chain in the presence of water were calculated. Consequently, the lower critical solution temperature (LCST) of PMEEECL chain at which the coil-to-globule transition takes place, was determined in each calculated parameter curve. The simulation results indicated that the LCST of PMEEECL was occurred at close to 320 K, which is in a good agreement with previous experimental results. Additionally, the appearance of sudden change in both Flory-Huggins interaction parameter (${\chi}$) and interaction energy between the PMEEECL chain and water molecules at about 320 K confirmed the calculated LCST result. The radial distribution function (RDF) results showed that the affinity of the PMEEECL side chain to water molecules is lower than its backbone.

• 설비공학논문집
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• 제10권1호
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• pp.11-21
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• 1998

A numerical study is made on the ice-formation for water flow inside a stenotic tube. The study takes into account the interaction existing between the laminar flow and the stenotic port in the circular tube. In the solution strategy, the present study is substantially distinguished from the existing works In that the complete set of governing equations in both the solid and liquid regions are resolved. In a channel flow between parallel plates, the agreement of predictions and available experimental data is very good. Numerical results are mainly obtained by varying the height and length of a stenotic shape and additionally for several temperatures of the wall and inlet of tube. The results show that the shape of stenotic port has the great effect on the thickness of the solidification layer in the tube. As the height of a stenosis grows and the length of a stenosis decreases, the ice layer thickness near the stenotic port is thinner due to backward flow caused by the sudden expansion of water tunnel. It is also found that the ice layer becomes more fat In accordance with Reynolds number and the temperature of the wall and inlet of tube decreased.

• 한국지반신소재학회논문집
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• 제9권3호
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• pp.39-45
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• 2010

동절기 온도가 영하로 떨어짐에 따라서 지표면 부근의 수분을 포함한 흙은 공극속의 수분이 얼음으로 변하면서 부피가 팽창하고, 이렇게 팽창된 지반은 주변 구조물에 영향을 미쳐 지반 구조물의 안전에 위험한 영향을 초래할 수 있다. 동상현상은 토립자, 간극수, 공기로 구성된 다상(multi phase) 구조 속에서 동결이 형성됨에 따른 수분의 이동과 수분이 얼음으로의 상변화(phase change) 등 다변수의 복합적인 물리적 현상을 포함하고 있기 때문에 현재까지 다차원 수치해석에 구성방정식으로 사용할 수 있는 검증되고 신뢰성 있는 모델은 아직도 연구 단계에 있다. 본 논문에서는 간극수의 상변화에 따라 갑작스러운 열용량 증대로 발생하는 수치해석상의 문제를 극복할 수 있는 효율적인 간편식을 유도하고, 포화된 토사나 다공성 암반이 동결할 때의 거동을 재현할 수 있는 열전도 구성방정식과 해석법을 제안하였다. 제안된 식을 사용한 수치해석 결과는 알려진 이론해 및 실내 모형시험 결과와 잘 일치하였다.

• 한국해양학회지:바다
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• 제6권3호
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• pp.115-125
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• 2001

금강하구언에서 낙조동안 인위적으로 방류된 담수의 하구 내 거동을 파악하고자 1997년 5월과 1998년 7월에 각각 수로방향으로 설정된 3개 지점에서 표층 염분변화를 관측하였으며, 1999년 7월에는 군산-장항간 도선항로를 따라 18일간 표층염분과 수온을 관측하였다. 관측된 염분변화의 특징으로부터 방류된 담수가 하구 내에서 거동${\cdot}$소멸하는 과정을 분석하였다. 담수가 방류되면 저염수는 하구 폭 전반에 걸친 강한 염분전선을 형성하며 담수거동은 기본적으로 조석운동에 동조되어 수로를 따라 왕래하고, 이 전선의 통과로 염분은 급격한 변화를 보인다. 수문개폐로부터 한 조석주기 이후의 하구 폭 평균염분의 시간적 변화로부터 해석된 수로방향의 공간적 분포는 전선역에 담수희석수가 응축되며 표층염분이 상류쪽으로 갈수록 점진적으로 증가하는 것으로 제시되었다. 이러한 염분의 전선역 분포는 두 시간정도의 하구언 수문 개방에 의한 급작스런 담수공급과 중단에 의해 발생한 것으로 해석되었다. 매일 담수방류의 반복은 수문 개방시기에 의해 이전의전선과 새로운 전선의 분리(이중전선) 혹은 병합을 만들고, 담수공급이 2일 이상 중단되면 염분이 증가되며 전선이 소멸한다. 또한, 표층염분 변화에 나타나는 변동과 변이는 하구언에서 인위적으로 행해지는 담수 방류량 차이에 의해 발생하는 염분전선의 세기와 통과시기의 공간적 차이, 그리고 일시적인 하구수로 방향을 따른 염분전선 등에 의한 것으로 해석되었다.