• Proceedings of the Korean Environmental Sciences Society Conference
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• 2007.05a
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• pp.294-297
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• 2007

유기유기물 증가원인의 파악과 근본적인 대책에 대한 연구의 일환으로 부영양화된 연안해역에 대하여 태풍 발생 전후의 수질변동에 대하여 조사하였다. 그 결과를 요약하면 다음과 같다. 1) 용존산소 포화도는 수온과 염분 약층이 형성된 시기에 저층에서 54% 이하로 관측되었다. 태풍이 지나간 직후에는 표층과 저층에서 거의 비슷한 용존산소 포화도$(78{\sim}88%)$가 조사되었다. 그리고, 태풍이 지나간 3일 후 식물플랑크톤이 대량으로 증식한 표층에서 용존산소 포화도가 234%로 아주 높은 값이 관측되었고, 저층(5m)에서도 90%가 조사되어, 태풍과 식물플랑크톤의 이상 증식이 저층의 용존산소 포화도를 높이는 작용을 한 것으로 보인다. 2) 염분이 가장 낮았던 시기에 표층에서 $NA_4-N$, $NO_3-N$, $SiO_2-Si$의 농도가 각각 18.22, 38.90, 52.10uM로 아주 높게 조사되었으며, $NH4-N$, $PO_4-P$, $SiO_2-Si$는 용존산소가 낮은 저층에서도 높게 나타났다. 3) 클로로필은 최고 $311.0{\mu}g/L$가 태풍 후에 관측되었으며, 그 원인 생물은 Scrippsiella trochoidea (42,000cells/mL)였다. 조류성장잠재능력은 태풍발생 후에 아주 높게 조사되었으며, 항상 질소가 부족한 것으로 조사되었다. 4) 화학적 산소요구량은 최고 10.55 mg/L였으며, 태풍으로 저층 퇴적물로부터 부유되는 유기 오탁 물질이 화학적 산소요구량 증가에 미치는 기여도는 크지 않은 것으로 보이며, 화학적 산소요구량 증가의 대부분이 식물플랑크톤의 증식에 기인한 것($r^2=0.612$, p<0.0001)으로 조사되었다.

• Journal of the Institute of Convergence Signal Processing
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• v.9 no.3
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• pp.219-223
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• 2008

The dissolved oxygen (DO) sensors were fabricated by screen printing method, and potable dissolved oxygen measurement system was fabricated for low cost products. The fabricated sensors had high current change and fast response according to dissolved oxygen concentrations in the applied voltage of 0.7 V. The DO measurement system was consisted of MCV, amplifier, filter, power supply and display. DO concentrations were programed to display as digital percentages by converting the analog value. It is expected that the fabricated DO measurement system can replace the expensive commercial DO meter, because it reveals the high accuracy of ${\pm}0.5%$ to the standard solution and the response time of about 100 sec like the commercial DO meter.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.28 no.5
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• pp.549-556
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• 1995

Experiments were carried out to examine the combined effects of hypoxia and hydrogen sulfide on survival, feeding activity and metabolic rata or Blue crab, Portunus trituberculatus. Survival rate of the crab was significantly affected by $\leq2.14mg/l$ dissolved oxygen, and feeding activity was also reduced below 1.41mg/l dissolved oxygen. Metabolic rate of the crab exosed to hypoxia $(\leq3.35mg/l)$ was significantly reduced than that exposed to normoxia. The combined effects of hypoxia $(\leq1.86mg/l)$ and hydrogen sulfide $(12.35 {\mu}g/l)$ on the survival rate were highly toxic than each single effect. Feeding activity was also decreased by the combinedexposure to $\leq1.86mg/l$ dissolved oxygen and $(12.35 {\mu}g/l)$ hydrogen sulfide compared with single effect.

• KSBB Journal
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• v.24 no.1
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• pp.65-69
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• 2009

The biological production of a potent anticancer agent, epothilone, by Sorangium cellulosum was carried out using flask and fermentor cultures. Soluble starch was selected as the main carbon source and the concentrations of lactose and yeast extract were optimized at 4 and 0 g/L, respectively, when using the flask cultures. In the fermentor cultures, the cells were cultivated at a high DO level of more than 80% of air saturation in the growth stage and then the DO level was controlled at about 50, 20 or 1-2% when the carbon source was exhausted. The epothilone production increased with decreasing DO level after the exhaustion of the carbon source, and the maximum concentration of epothilone was 5.4 mg/L. It was found that the DO level had significant regulation effects on the epothilone production.

• Journal of the Korean Society of Marine Environment & Safety
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• v.16 no.4
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• pp.339-344
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• 2010

Oxygen depleted water mass can damage aquatic animals not only in direct way but also in indirect way by generating toxic substances including occurrence of hydrogen sulfide and ammonia which are also highly detrimental to animal life in the water mass. An oxygen dissolution device was developed, which makes turnover of the oxygen rich (over 20 mg/L) surface water down to the bottom where hypoxia is evident and tested the device in terms of oxygen recovery in the oxygen depleted bottom water. the device with turnover rates of $3.6\;m^2$/min at the liquid oxygen injection rate of 48~26.3 L/min could recover dissolved oxygen level to 7~25 mg/L at depth 7 m to lead to the dissolution level of over 90% by the supply of liquid oxygen. The running advantage of the device is that it does not require any auxiliary tank and higher energy for operation. Therefore, it can be highly useful device to relieve damages to the farmed animals in the oxygen depleted waters.

• Korean Journal of Environmental Biology
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• v.32 no.3
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• pp.216-224
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• 2014

Decrease in dissolved oxygen concentrations associated with temperature fluctuation is an important criteria to evaluate the mortality rate of the species. Based on this parameter, we investigated the survival rate, physiological response and histological change of warty sea squirt. It was found that the survival rate of the warty sea squirt species was 63.3% at $23^{\circ}C$ and 56.6% at $26^{\circ}C$ respectively. However, exposure of six days at $29^{\circ}C$ caused deaths among species, which indicated the 6day-$LT^{50}$ of the tested species to be $24.58^{\circ}C$ ($19.48{\sim}35.48^{\circ}C$). Further, after 11 day of exposure, the dissolved oxygen concentration has been found to decrease, with the survival rate of 20% at $4.0mg\;L^{-1}$ and deaths at $2.0mg\;L^{-1}$, thus 11day-$LC^{50}$ calculated to be $3.88mg\;L^{-1}$ ($3.29{\sim}4.57mg\;L^{-1}$). In addition, decrease in rate of oxygen consumption and excretion of ammonia was also noted at this critical water temperature and dissolve doxygen concentration. Moreover, there has been common histopathological changes were observed in warty sea squirt's gill pouch, digestive tract, and tunic as follows such as: proliferation of epithelial cells, condensation and necrosis, permeation of phagocyte and blood cell, loss of cilium and muscular fiber degeneration. Based on our study results, we suggest that these parameters can also be useful to evaluate the survival rate and physiological response in other species.

• Journal of the Korean Society for Marine Environment & Energy
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• v.7 no.4
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• pp.159-163
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• 2004

This study was performed to estimate the water quality of pH, salinity, dissolved oxygen, ammonium and sulfur hydroxides of sediment in shrimp aquaculture farms of Southwestern coastal of Korea from June to September, 2003. We surveyed the status of water quality and achieved the improve water and sediment quality to restraint the production of ammonium and sulfur hydroxides from sediment of shrimp aquaculture farms. The concentrations of dissolved oxygen increased from noon to the evening for 6 hour and decreased to 2.98 ppm at six o'clock in the next morning and increased repeatedly, even though DO level has a different level in sunny day and cloudy day. This results suggest that the most importance time of the control of DO in shrimp aquaculture farm is next early morning and if the DO concentration increased continuously which may be growing up the concentrations of NH₄/sup +/ and H₂S. The measured of pH and salinity were suitable to growth of shrimp. However, the level of ammonium and sulfur hydroxides produced from the sediments of shrimp aquaculture farms were 2.30 ppm and 0.075 ppm, respectively, which are exceeded to the concentration of guide line for the growth of shrimp. In the results of this study, we found it difficult to improve the water quality using of the present frame of shrimp aquaculture farms. Then, we can improved water quality of DO, NH₄/sup +/ and sediment quality of ORP, H₂S and also achieved down to the rate of shrimp fatal by changed the frame of shrimp aquaculture farms in the scale of laboratory.

• Membrane Journal
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• v.17 no.4
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• pp.352-358
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• 2007

A nonporous hollow fiber membrane contactor was used to control the concentration of oxygen dissolved in an aqueous solution, which was predicted along the hollow fiber membrane using a computer simulation. The governing ordinary differential equations were derived for the occurrent flows of the feed aqueous solution and the feed gas mixture in a membrane contactor and they were numerically solved using the 5th Runge-Kutta-Verner method with a personal computer, where the program was coded utilizing a software of the Compaq Visual Fortran 6.6. It is found that the concentration of oxygen dissolved in water increases from 30 to 64 ppm as the length of the hollow fiber increases from 0.4 to 1.2 m when the membrane of fibers are equal to be 16,000; the flow rate of the feed gas is kept to be 0.536 mol/sec; its pressure is maintained to be 486 kPa; the flow rate of the water is 16.69 mol/sec. As the flow rate of the water increases from 9.26 to 26.85 mol/sec, the concentration of oxygen decreases from 40 to 20 ppm with the constant fiber length of 0.4 m. Finally, it is observed that the concentration of oxygen increases from 33 to 69 ppm as the pressure of the feed gas increases from 298 to 847 kPa.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2006.11a
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• pp.283-284
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• 2006

해초지와 해초가 없는 수괴에서 식물플랑크톤의 군집 특성을 비교 분석하기 위하여 해황과 해초지의 규모가 다른 가막만의 원포연안과 여자만의 백일도 주변 해역에서 식물플랑크톤을 채집하고, 수온, 염분, 용존산소, Chlorophyll a와 영양염을 2006년 2월부터 8월까지 조사하였다. 조사 기간동안 해초의 유무에 따른 수온과 염분의 차이는 보이지 않았으나, 용존산소, Chlorophyll a와 영양염 농도는 유의한 차이를 보였다. 또한 거머리말 해초지와 조사 시기에 따른 수온, 염분, 용존산소, Chlorophyll a와 영양염 농도도 유의한 차이를 보였다. 그리고, 원포의 수온은 백일도보다 낮았으나, 염분은 유의하게 높았다. 식물플랑크톤의 현존량과 종조성은 조사 시기에 따라 차이를 보였으며, 현존량은 해초지에서 낮게 나타났다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.8 no.2
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• pp.177-186
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• 2003

The influences of horizontal and vertical flow components including the stratification of water column and the wind field on the formation of oxygen-deficient water in summer in Jindong Bay, northern part of Chinhae Bay, were examined. Temperature, salinity and dissolved oxygen in seawater, and direction and velocity of wind were observed in Jindong Bay from March 1998 to February 1999. Low concentration of 5 mg/L in dissolved oxygen (DO) appeared at the bottom layer from May to September. Extremely low DO concentration less than 3 mg/L was investigated in summer (July to August) when stratification was strongest due to abrupt vertical gradients of temperature and salinity in water column. Bottom waters with the extremely low DO concentration were observed even in spring (May to June) at the inner part of the bay. In summer (August to September), the bottom waters with the low DO concentration (less than 5 mg/L) existed at the water depth from 4 to 6 m, being moved upward to the surface layer compared to other seasons. Vertical components of residual flow, calculated by the direction and velocity of wind, in Jindong Bay in summer showed that locally prevailed northerly and westerly wind resulted in downwelling flow at the outer part of the bay and conversely, upwelling at the inner part of the bay. In addition, bottom current at the outer part corresponding to the downwelling area directed to the inner part, probably resulting in a transport of the particulate organic matter settled at the bottom waters to the inner part of the bay. The oxygen-deficient watermass, which was formed at the bottom layer of the inner part, was likely to transported to the surface layer by the upwelling flow.