• 환경위생공학
• /
• 제23권3호
• /
• pp.31-38
• /
• 2008

This study was conducted to investigate the effects of environmental factor such as temperature, salinity, turbidity, pH and dissolved oxygen on the growth of Vibrio spp.. In this survey, total 56 seawater samples were obtained from 8 different sites of the Incheon coastal area during the periods from april 2008 to october 2008. Enumeration of Vibrio spp. was determined by using the most probable number(MPN) procedure. Isolation rates of V. parahaemolyticus, V. vulnificus, V. cholerae in all samples tested were 44.0%, 21.4% and 13.1%, respectively. The enumeration of Vibrio spp. was very low correlated with water temperature and pH and negatively correlated with salinity, dissolved oxygen and turbidity. We found salinity to be the parameter most highly correlated with the enumeration of Vibrio spp. The highest rate of antibiotic resistance of V.vulnificus and V.parahaemolyticus was Cefazolin(11.5%), Ampicillin(70.8%), respectively.

• 한국패류학회지
• /
• 제30권2호
• /
• pp.101-106
• /
• 2014

인공종묘로 생산된 동죽, Mactra veneriformis의 크기, 수온, 염분 변화에 대한 여수율과 먹이섭이량의 차이를 조사하였다. 수온의 경우 소형, 대형그룹의 여수율은 $5^{\circ}C$에서 최소값을 보였으며 $20^{\circ}C$에서 가장 높은 값을 보였으나, $25^{\circ}C$에서 급격한 감소 경향을 보였다. 염분에 대한 소형그룹의 여수율은 26‰에서 가장 높은 값을 보였고 8‰에서 가장 낮은 값을 보였다. 대형그룹은 32‰에서 가장 높은 값을 보였고, 8‰에서 가장 낮은 값을 보였다. 본 연구를 통해 동죽의 최적 수온, 염분 환경은 $20^{\circ}C$, 27-32‰이며, $10^{\circ}C$ 이하 또는 $25^{\circ}C$ 이상의 수온과 20‰ 이하의 저염분에서 여수율이 낮아진다는 사실을 확인할 수 있었다.

• 한국수산과학회지
• /
• 제43권6호
• /
• pp.715-722
• /
• 2010

The effects of temperature, salinity and irradiance on the growth of the harmful red tide dinoflagellate Cochlodinium polykrikoides Margelef isolated from the South Sea of Korea were examined in the laboratory. Growth was examined under the following combinations of temperature and salinity: 15, 20, 25 and $30^{\circ}C$, and 15, 20, 25, 30 and 35 psu at a constant irradiance of $180\;{\mu}mol/m^2/s$. No growth was observed with a temperature of $15^{\circ}C$ and a salinitiy of 15 psu. Moderate growth rates of more than 0.30 /day were obtained at $25^{\circ}C$ with salinities of 25.35 psu. These values are similar to in situ observations for this species. The maximum growth rate, 0.35 /day, was obtained at $25^{\circ}C$ and 30 psu. In light experiments, cell growth of C. polykrikoides was conducted with constant temperature ($20^{\circ}C$) and salinity (30 psu) under light photon flux densities (PFD) of 10, 25, 50, 70, 100, 150, 250 and $350\;{\mu}mol/m^2/s$. C. polykrikoides did not grow at $10\;{\mu}mol/m^2/s$. Cell growth was observed at irradiance values of $25\;{\mu}mol/m^2/s$ and above. The irradiance-growth curve was described as ${\mu}=0.30{\cdot}(I-15.27)/(I+27.22)$, (r=0.99). This suggests a compensation PFD of $15.27\;{\mu}mol/m^2/s$ and a maximum growth rate of 0.30 /day. In conclusion, C. polykrikoides prefers high salinity, temperature and irradiance in summer in Korea. These results provide important information for understanding the mechanism of C. polykrikoides blooms and developing technology to predict blooms of this organism in the field.

• 수산해양기술연구
• /
• 제34권2호
• /
• pp.117-134
• /
• 1998

The study on the Assembling Mechanism of the Hairtail, Trichiurus lenpturus, at the Fishing Grounds of the Cheju Strait had been investigated by analyzing the relationship of the oceanographic conditions and the fishing ground of the Hairtail in the Cheju Strait. 1. The fishing grounds of the hairtail at the Cheju Strait are formed at the bottom of a high temperature of the tidal front at the coast. area of northern Cheju Island, the tip of the linguiform is high in salinity at the eastern and western entrances of Cheju Island, low salinity eddy on the surface and its surrounding front, various water masses in the Strait and coastal waters of the South Sea in Korea. 2. The fishing grounds of the Hairtail at the Cheju Strait begins with the sea surface temperature higher than $15^{\circ}C$ and the incoming of low salinity water now from the East China Sea. 3. Estimation of optimum temperature and salinity per season based upon analysis for relationship between temperature of water and salinity of the bottom layer and the catch is : 15.2~$16.4^{\circ}C$, 34.20~34.40${\textperthousand}$ in spring(June); 14.4~ $17.0^{\circ}C$, 33.70~34.30${\textperthousand}$ in summer(July~September); and 15.7~ $18.6^{\circ}C$, 33.70~34.50$\textperthousand$ in autumn(October~December). Hairtail are mostly caught at the Yellow Sea Warm Current and Tsushima Current with temperature over $14.5^{\circ}C$ and salinity over 33.70${\textperthousand}$ at the bottom layers of the Cheju Strait. 4. Considering the relationship between the amount of hairtail catch and the water temperature of bottom layer, when the bottom water being above $14.0^{\circ}C$ flowed into Cheju Strait through the western entrance of the strait in summer, the ca-h appears to have been abundant. In contrast, the catch has been poor when the temperature of such water was recorded to be below $13^{\circ}C$ Therefore, distribution patterns of water at the bottom layer can be used as a forecast index whether the catch of a certain year will be good or poor.

• Ocean and Polar Research
• /
• 제27권3호
• /
• pp.277-288
• /
• 2005

Spatial distribution and vertical structures of water masses around the Antarctic continental margin are described using synthesized hydrographic data. Antarctic Surface Water (AASW) over the shelf regime is distinguished from underlying other water masses by the cut-off salinity, varying from approximately 34.35 to 34.45 around Antarctica. Shelf water, characterized by salinity greater than the cut-off salinity and potential temperature less than $-17^{\circ}C$, is observed on the Ross Sea, off George V Land, off Wilkes Land, the Amery Basin, and the Weddell Sea, but in some shelves AASW occupies the entire shelf. Lower Circumpolar Deep Water is present everywhere around the Antarctic oceanic regime and in some places it mixes with Shelf Water, producing Antarctic Slope Front Water (ASFW). ASFW, characterized by potential temperature less than about $0^{\circ}C$ and greater than $-17^{\circ}C$, and salinity greater than the cut-off salinity, is found everywhere around Antarctica except in the Bellingshausen-Amundsen sector. The presence of different water masses over the Antarctic shelves and shelf edges produces mainly three types of water mass stratifications: no significant meridional property gradient in the Bellingshausen and Amundsen Seas, single property gradient where ASFW presents, and a V-shaped front where Shelf Water exists.

• 미생물학회지
• /
• 제26권4호
• /
• pp.339-347
• /
• 1988

The rate of bacterial degradation of hydrocarbon was estimated for the measurment of the self-purification capacity of the aquatic ecosystem. Strain ND601P-2, selected as petroleum degrading bacteria from Nakdong River Estuary with high degradability of petroleum, transformed 42% of hexadecane to $CO_{2}$ or cell mateials under the conditions of $25^{\circ}C$, 0.03M NaCl, 167mg-$NH_{4}^+/1, 950 mg-PO_{4}^{3-}$/1, 50 mg-hexadecane/1. The mineralization rate was found to be significantly affected by the temperature and the $Q_{10}$ value was 2.2. Teh optimal salinity of the strain ND601P-2 was 2o/oo. The increased salinity caused the elevation of % respiration value and the prolonged lag phase.

• 미생물학회지
• /
• 제29권5호
• /
• pp.339-343
• /
• 1991

Heterotrophic activity, total bacteria and salinity were determined seasonally in the estuary of Naktong River over half tidal cycle. Heterotrophic activity was determined by the uptake of [U- $^{14}$ C]glucose. Heterotrophic activity fluctuated with the tides and was decreased as salinity increased. Teh great activity occurred near low ebb tide at all seasons except summer. The main environmental factor affecting hetreotrophic activity was the salinity rather than water temperature in the estuary of Naktong River. In order to estimate the effect of salt, salt was added to estuarine water. Vmax for glucose of salt-added water was 17% and 77% of original estuarine water at station 1 and 2 respectively and slight increase was observed at station 3. Respiration rate and Kt+Sn for glucose of salt-added sample increased at all 3 stations. The increase of the Kt value implies the reduced affinity of bacterial population for glucose. The effects of salinity on the heterotrophic activity were more extensive in the upper region of estuary than at the mouth.

• 한국양식학회지
• /
• 제10권3호
• /
• pp.357-362
• /
• 1997

참가자미의 종묘생산을 위한 생물학적 기초자료를 얻기 위하여 난발생에 미치는 수온과 염분의 영향을 조사하였다. 수정란의 정상적인 부화는 9-$15^\circC$에서 가능하였으며 생존율은 $12^\circC$에서 가장 높게 나타났다. 난발생의 각 단계에 이르기까지의 수온 (T : \circC$)에 따른 발생속도 (t : hour)는 수온이 높을수록 빨랐으며, 그 관계식은 다음과 같았다. 8세포기 1/t=0.0284T-0.0554 (r=0.9999) 상실기 : 1/t=0.0137T-0.0527 (r=0.9998) Kupffer씨포 출현기 : 1/t=0.0035T-0.0133 (r=0.9762) 부화자어기 : 1/t=0.0012T-0.0007 (r=0.9981) 참가자미의 난발생이 개시되는 생물학적 영도는 평균 $2.6^\circC$로 나타났다. 설정 수온별로 수정에서 부화에 이르기까지의 평균 소요시간은 $9^\circC$에서 95.5시간, 12$12^\circC$에서 72.5시간 및 $15^\circC$에서 56.0시간이었다. 염분별 부화까지의 생존율은 35-$38\textperthousand$에서 높게 나타났다.

• 환경생물
• /
• 제17권2호
• /
• pp.209-215
• /
• 1999

온도, pH및 염도 stress가 굴(Crassostrea gigas)의 malate dehydrogenase isozyme에 미치는 영향을 전기영동법으로 분석하였다. 대조군의 MDH isozyme은 2개의 band가 양극 쪽으로 이동되어 분리되었다. 각 실험 온도와 pH를 12시간 노출시킨 실험군에서는 1개의 band만 양극 쪽에서 분리되었고, 24시간과 48시간 노출한 실험군에서는 2개의 band가 모두 양극 쪽에서 분리되었다. 염분 농도가 5ppt 와 3ppt에서 12시간 노출시켰을 때 각각 2개의 band가, 10ppt와 40ppt에서는 각각 3개의 band가 분리되었고, 24시간과 48시간 노출 실험군에서는 2개의 band가 양극 쪽에서 분리되었다. 모든 isozyme pattern에서 각 band의 활성도는 실험 조건에 따라 각각의 특이성이 나타났다. 결과적으로 MDH isozyme의 변화는 굴이 환경 stress에 대한 생화학적 반응의 결과로 간주된다.

• 한국수산과학회지
• /
• 제28권1호
• /
• pp.7-14
• /
• 1995

1992년부터 1993년까지 수행된 득량만의 양식생산성 향상을 위한 종합적 해양조사의 일환으로 수온과 염분 관측을 실시한 결과 중에서 하계의 자료를 비교 분석하였다. 두 해에 여름철의 기상조건은 서로 대조적이었는데 1992년에는 비가 적고 맑은 날이 많았던데 비해 1993년에는 흐린 날이 많고 강수량 또한 많아 이상저온 현상이 심했다. 이러한 기상의 영향은 만내의 수온과 염분의 분포에 직접적으로 영향을 주었다. 바람이 대체로 약한 여름에는 태양복사에 의한 열 공급과 조류에 의한 연직혼합 및 해수순환에 의한 열 수송에 의해서 수온분포가 결정되는데, 염분분포에는 열 공급 대신에 강수에 의한 담수의 공급이 중요해진다. 서부와 북동부의 천해역이 고온저염수가 분포하여 입구로부터 상류 방향으로 수온은 증가하고 염분이 감소하는 1992년과는 달리 1993년에는 등온선과 등염선이 만의 종축과 평행한 경향이 강하여 많은 강수량과 함께 복사열의 공급이 감소 한데다가 만의 종축 방향으로 흐르는 조류와 항류의 영향이 상대적으로 증가된 결과로 해석된다. 한편, 연직분포에 있어서는 조류가 강한 대조기에는 성층이 파괴되며 소조기에는 성층이 발달하는 현상을 보여주었다.