• Ocean Science Journal
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• 제40권2호
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• pp.79-89
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• 2005

Laboratory radiotracer experiments were conducted to determine assimilation efficiencies (AE) from ingested algal food and oxic sediment particles, uptake rates from the dissolved phase, and the efflux rates of Cd, Cr and Zn in the Asiatic clam Corbicula fluminea. Among three elements, AE from both algal and sediment food was greatest for Cd, followed by Zn and Cr. The AEs of tested elements from algal food (Phaeodactylum tricornutum) were consistently higher than those from sediments at a given salinity and temperature. The influence of salinity (0, 4 and 8 psu) and temperature (5, 13 and $21^{\circ}C$) on the metal AEs was not evident for most tested elements, except Cd AEs from sediment. The rate constant of metal uptake from the dissolved phase $(k_u)$ was greatest for Cd, followed by Zn and Cr in freshwater media. However, in saline water, the $(k_u)$ of Zn were greater than those of Cd. The influx rate of all tested metals increased with temperature. The efflux rate constant was greatest for Cr $(0.02\;d^{-1})$, followed by Zn $(0.010{\sim}0.017\;d^{-1})$ and $Cd\;(0.006\;d^{-1})$. The efflux rate constant for Zn in clam tissues depurated in 0 psu $(0.017\;d^{-1})$ was faster than that in 8 psu $(0.010\;d^{-1})$. Overall results showed that the variation of salinity and temperature in estuarine systems can considerably influence the metal bioaccumulation potential in the estuarine clam C. fluminea. The relatively high Cd accumulation capacity of C. fluminea characterized by the high AE, high dissolved influx rate and low efflux rate, suggested that this clam species can be used as an efficient biomonitor for the Cd contamination in freshwater and estuarine environments.

• 한국양식학회지
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• 제9권4호
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• pp.321-327
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• 1996

Production of resting egg from the Korean rotifer, Brachiunus plicatilis (L and S-type) was investigated at different temperatures (L-type : 20, 24, $28^{\circ}C$, S-type : 28 32, $36^{\circ}C$) and salinities (10, 20,30 ppt). The rotifer was cultured in 25 ml test tube and fed on Nannochloris oculata. With regard to mixis rate, L-type rotifer showed higher rate at lower temperature, and the highest rate was observed at 20 ppt of salinity at each temperature of the experiment. However, for S-type rotifer, the optimum temperature and salinity were $28\~32^{\circ}C$ and 20 ppt, respectively. The highest number of resting egg was 173 eggs/ml in 16 days at $24^{\circ}C$, 10 ppt for L-type rotifer and 410 eggs/ml in 14 days at $28^{\circ}C$, 10 ppt for S-type rotifer. The maximum number of resting egg produced per 10,000 rotifers was 8,122 eggs at $20^{\circ}C$, 20 ppt for L-type rotifer and 8,700 eggs at $28^{\circ}C$, 20 ppt for S-type rotifer. The maximum number of resting egg produced $10^8$ cells of N. oculata was 50.7 eggs for L-type rotifer ($24^{\circ}C$, 20 ppt) and 79.6 eggs for S-type rotifer ($32^{\circ}C$, 10 ppt). The number of resting egg produced per day was $1\~11$ eggs/ml for L-type rotifers and $21\~35$ eggs/ml for S-type rotifer in 9 combination experiments. In this study, S-type rotifer is better than L-type rotifer in resting egg production, and the optimum temperature and salinity for resting egg production were $20^{\circ}C$, 20 ppt for L-type rotifer and $28^{\circ}C$, 20 ppt for S-type rotifer. This result shows the difference of Korean rotifer in the optimum condition for resting egg production from other rotifers reported earlier.

• 수산해양기술연구
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• 제34권1호
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• pp.67-73
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• 1998

In order to find out the environmental factors influencing the catch of anchovy lift nets in kamakbay, the three oceanographic factors, i. e., the water temperature, the salinity, the amount of chlorophyll-a were observed respectively from August 1 to 12, 1995 and from September 20 to 26, 1995, and each of them was compared with the catch of anchovy by the lift net. The results obtained are summerized as follow : 1) The water temperature was ranged from 17.3 to 29.6$^{\circ}C$ and its difference between the surface and bottom was 1 to 3$^{\circ}C$. In the three areas, A, B and C, the area A was the hightest in temperature, the area B being a second, and the area C being the lowest. 2) The salinity was ranged from 32.20 to 33.47$\textperthousand$ and its difference between the surface and bottom was not significant. In the three areas, the area A was the highest in salinity, the area B being a second, and the area C being the lowest. 3) The amount of chlorophyll-a was ranged from 0.19 to 5.30mg/m supper(3) and its difference among the three areas was not significant. Daily variation of the amount was very irregulated because the position operated was changed daily. 4) A comparison of the water temperature, the salinity and the amount of chlorophyll-a with the catch gave that the water temperature and the amount of chlorophyll-a had large influence on the catch and the salinity did not so. However, the influence of the amount of chlorophyll-a was larger than that of the water temperature. 5) The catch of anchovy was large respectively during two hours after sun set and during two hours before sun rise.

• 해양환경안전학회:학술대회논문집
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• 해양환경안전학회 2003년도 추계학술발표회
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• pp.181-185
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• 2003

한국 서해는 주변해역에 비해 얕은 수심과 낮은 저열량으로 다른 해역에 비해서 대기의 역할이 더 중요하다. 이들의 관계를 파악하기 위해 국립수산과학원의 정선관측 자료, 연안정지 자료와 기상청 자료를 사용하였다. 수온, 염분과 기상인자들은 8월에 최고치가 되고, 2월에 최소치가 되는 계절변동을 한다. 수온과 염분은 수심이 깊어질수록 최고$\cdot$저 값에 이르는 시간지연이 나타난다. 수심 100m에 달하는 311-07점의 75m수층의 수은의 시계열은 10월에 최고치, 4월에 최저치에 달한다. 기상인자와 수온, 염분과의 상관관계를 분석하였다. 기상인자는 기온, 풍속, 강수량을 사용하였다. 수온-기온, 수온-강수, 염분-풍속은 정관계를 보였다. 그리고 수온-풍속, 염분-기온, 염분-강수는 역관계를 나타내었다. 307-05의 염분을 제외한 모든 연구해역에서 수심 20m를 기준으로 표층보다 2개월에서 4개월 느리게 최대치가 되었다. 307-05의 염분은 기상인자와의 관계에서 50m 수층에서 시간지연을 보였다.

• 수산해양교육연구
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• 제26권1호
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• pp.214-222
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• 2014

Hagfish Eptatretus burgeri is classified as a agnathans and has many different physiological properties compared with vertebrates. In this study, we examined effects of water temperature and salinity on blood properties and oxygen consumption in hagfish. In the experiment of water temperature change, hematocrit (Ht), red blood cell (RBC) and glucose of hagfish blood revealed the lowest values at $15^{\circ}C$. Oxygen consumption of hagfish had significantly increased with rising water temperature, and the increasing rate was twice as much when the temperature was manipulated every $5^{\circ}C$. Also, oxygen consumption during the night time (a short photoperiod) was significantly higher than that of the daytime. Q10 level was 3.50 in the light period and 3.92 in the dark period. No significant change in plasma glucose level was showned in changing salinity from 30 psu to 22 psu, while it had rapidly increased at 20 psu ($13.7{\pm}4.0mg/dL$) and thereafter all hagfish were dead at 18 psu. However, osmolarity, $Na^+$, $K^+$ and $Cl^-$ levels had significantly decreased when salinity decreased. This results are expected to develop the artificial rearing techniques of natural hagfish.

• 유기물자원화
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• 제8권2호
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• pp.124-129
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• 2000

본 논문은 퇴비화의 분해속도와 처리효율이 염분농도에 따라 어떻게 변화하는가를 조사하기 위해 이루어졌다. 실험에 사용된 음식물쓰레기의 시료는 경기도 포천군에서 채취하였으며 이 시료의 수분함량, pH 및 C/N비를 적정범위로 조정하였다. 염분함량이 1%, 5%및 10%인 3종류의 시료를 조제하여 온도조절과 공기공급량이 조절가능한 반응조에 넣고 호기성 퇴비화가 진행되는 동안 반응조내의 온도, pH, C/N비 및 이산화탄소와 산소 농도 등을 측정하였다. 최고온도는 반응조 1(염분함량 1%)에서 $59^{\circ}C$, 반응조 2(염분함량 5%)에서 $49^{\circ}C$ 및 반응조 3(염분함량 10%)에서 $45^{\circ}C$로 나타났다. 이산화탄소 발생량은 온도상승과 상관관계를 보였으며 낮은 염분함량에서 피크값을 나타냈다. 퇴비화가 진행되는 동안 반응조 1, 반응조 2 및 반응조 3의 pH는 8.9, 8.6 및 7.2로 상승하였으며 C/N비는 18.9, 19.1 및 22.1로 천천히 감소하였다. 반응조 1, 반응조 2 및 반응조 3의 최종함수율은 51.1%, 53.7% 및 55.0%로 나타났다. 퇴비화기간 동안의 염분농도의 증가는 미생물의 분해활동을 지연시키는 원인이 되는 것으로 생각된다. 한편, 효율적인 퇴비화를 위해 시료중의 염분함량은 5% 미만으로 유지되어야 한다.

• 한국수산과학회지
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• 제16권4호
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• pp.335-340
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• 1983

양식 김에 미치는 수온, 염분 및 해수중의 현탁부니의 영향을 조사하였다. 1. 김의 광합성률은 실험수온 $8{\sim}16^{\circ}C$까지는 수온이 높아짐에 따라 증가하였으나 $18^{\circ}C$에서는 감소되었다. 2. 실험염분 $21.5{\sim}33.5\%0$ 범위에서, 김의 광합성률은 $29.5\%0$에서 다소 증가하였고 $21.5\%0$에서는 감소하였다. 3. 김의 광합성률은 부니의 농도가 증가함에 따라 또 처리일수가 경과함에 따라 현저히 감소하였다. 4. 김의 광합성률에 미치는 염분과 부니의 복합영향을 보면, 저염분영향이 큰 $21.5\%0$에서 부니의 영향이 컸고, $33.5\%0$에서도 비슷한 경향을 보였다. 5. 김의 생체량은 부니의 농도가 증가함에 따라 또 처리일수가 경과함에 따라 현저히 감소하였다.

• 한국해양학회지
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• 제27권4호
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• pp.290-302
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• 1992

기후학적인 관측자료와 담수 효과를 고려한 수치실험에서 얻어진 두가지의 계절별 염분 분포를 열대 대서양 500 m 상층부에 대하여 조사하였다. 해표면 염분의 계절 변 화는 담수의 초과를 가져오는 열대수렴대(ITCZ)의 이동 및 강물 방출 시기에 밀접한 관계가 있었다. 본 연구에서 얻어진 계절별 염분 분포는 Defant (1981)와 Levitus (1982) 등의 이미 존재하는 기후 자료와 대체로 비슷하나, 본 연구의 자료가 온도 분 포에 더 잘 일치하였다. 밀도에 대한 온도 효과와 비교할 때 염분 효과는 100 m 이심 에서는 무시할 만하나 혼합층에서 염분 효과는 상당히 중요하였다. 관측된 염분 분포 와 모델에서 계산된 염분 분포사이에 뚜렷한 차이가 염분값의 위도에 따른 기울기에서 나타났다. 모델에서 유도된 염분은 관측값보다 적도부근의 해양에서 대체로 높게 나타 났으나, 아열대 해역에서는 낮게 나타났다. 남동 대서양 해역과 같은 관측자료가 매우 적은 곳에서 염분 차이는 크게 나타났고, 이런 해역에서 정교한 모델값이 좀 더 정확 한 듯 보인다. 또한 관측값과 모델에서 얻어진 값과의 불일치에 대한 가능한 원인들도 분석하였다.

• 한국해양공학회지
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• 제13권3B호
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• pp.3-13
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• 1999

The diffusion characteristics of the high temperature and salinity water discharged in Chinhae Bay under BMP(Barge-Mounted Plants) desalination processes were simulated to access environmental impact. The 3-D baroclinic flow model is formulated by integrating the basic equations with respect to each control volume and by transforming them into a finite difference form using the space-staggered grid system. With a 3-D baroclinic flow model, the tide-induced and density-induced current was computed and confirmed by comparing with observed data. From the results of numerical experiment, it is expected that the maximum diffusion lengths of the high temperature and salinity which increase $0.6^{circ}C$ and 0.2 after discharging are 1 km and 3.5km, respectively. It may be expected that the discharge has an effect on surrounding area of discharge, but not an effect on whole area of Chinhae Bay.

• Journal of Advanced Marine Engineering and Technology
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• 제38권2호
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• pp.208-216
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• 2014

In case of any coastal ocean near the mouth of huge rivers, low salinity water can be formed due to its large amount of freshwater discharge. For the acoustic analysis on the low salinity environment, some oceanographic data of the East China Sea and the Atlantic Ocean were collected through KODC (Korea Oceanographic Data Center) and NODC (National Oceanographic Data Center) online service. In this paper, the T-S gradient diagram is introduced to show a relation between the gradients of temperature and salinity in view of acoustic surface channel formation. Existence of haline channel, quantitative contribution of gradients of salinity and temperature, effectiveness of the channel formation can be known by the T-S gradient diagram. After applying the collected data into the diagram, tropical regions of the Atlantic Ocean show strong haline channel due to its nearly invariant temperature and drastic change of salinity with depth. The averaged transmission loss in the channel is about 5.7 ~ 7.5 dB less than that out of the channel by the results of acoustic propagation model (RAM: Range independent Acoustic Model). On the other hand, the East China Sea and temperate region of the Atlantic ocean have weaker haline channel with less difference of the averaged transmission loss between in and out of the channel as 3.2 ~ 6.0 dB. Although data samples used in this study have limitation to represent the general physical structures of the three ocean regions, the T-S gradient diagram is shown to be useful and acoustic field affected by low salinity environment is investigated in this study.