• Proceedings of the Korea Water Resources Association Conference
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• 2022.05a
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• pp.52-52
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• 2022

남조류 (cyanobacteria)의 대량증식에 의한 녹조현상은 수질 악화 및 수중 생태계에 악영향을 끼친다. 기존 연구에서는 시아노박테리아 증식에 영향을 미칠 수 있는 다양한 요인을 식별하였다. 특히, 최근 (2020)에 수행된 한 연구는 2013년부터 2018년까지 4대 강에 위치한 16개의 지점에서수집된 세 가지 환경 변수, 수온, 유속 및 인(phosphorus)농도 데이터를 사용하여 시아노박테리아 발생에 대한 예측 모델을 개발하였으며 온도가 남조류에 발생에 대한 가장 지배적인 요인임을 시사하였다. 온실가스 배출에 의한 기온의 상승으로 특징되는 기후변화는 전 지구에 급격한 환경변화를 유발하고 있으며 이는 남조류 증식에도 영향을 줄 수 있다. 이에 본 연구에서는 한국의 4대 강에서 다년간 수집된 수온(℃) 및 녹조 (cells/㎖) 데이터에 기반하여 온도-환경변수 민감도 (scaling)를 분석함으로써 기후변화와 남조류 증식의 연관성을 판단해 보고자 한다.

• Journal of the Korean Society of Marine Environment & Safety
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• v.29 no.5
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• pp.435-444
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• 2023

Suitable environmental conditions in Saemangeum frequently favor phytoplankton growth. There have been occurrences of sudden phytoplankton blooms, surpassing the algae management standards. A model was designed to prevent such blooms using scientific predictive techniques to forecast and regulate the possibility of phytoplankton blooms. We propose effective and efficient algae control measures concerning every phytoplankton species optimized through the policy control of nutrients (DIN, PO4-P) from rivers and controlling lake salinity using gate operations. The probability of phytoplankton blooms was initially forecast using an artificial neural network algorithm based on observations. The model's Kappa number fluctuated from 0.7889 to 1.0000, indicating good to excellent predictive power. The Garson algorithm was then utilized to assess the significance of explanatory variables for every species. Meanwhile, the probability of phytoplankton blooms was anticipated depending on the DIN and salinity value changes. Therefore, the model predicted the precise DIN and salinity concentrations to inhibit phytoplankton blooms for each species. Hence, the green algae model can create effective proactive measures to avoid future phytoplankton blooms in enormous artificial lakes.

• Korean Journal of Environmental Biology
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• v.28 no.3
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• pp.172-178
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• 2010

The bloom of the genus Stephanodiscus was gradually extinguished after 18 April. Counts of bacterial population were increased as the diatom bloom was disappeared. Numbers of the heterotrophic nanoflagellates and ciliates were also increased during the disappearance of the bloom. The densities of the mesozooplankton, the major predator of the diatoms, started to increase in April. However, their growth was suppressed during the bloom period of the diatoms (from January to March). During the bloom period of the diatoms, the monthly average value of the basic productivity amounted up to 11,765.7 mgC $m^{-2}day^{-1}$, which is relatively high value considering the low temperature and light during that period. The growth rate of phytoplankton in March, when the bloom was beginning to be supressed was 0.007. The growth rate of phytoplankton was negative value in April when the decreasing of the algal density was started.

• Proceedings of the Korea Water Resources Association Conference
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• 2020.06a
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• pp.160-160
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• 2020

조류는 계절별 기상 및 수질 조건에 따라 규조, 녹조, 남조의 발생 및 천이가 이루어지는데 최근 기후 변화로 인해 출연종 별 발생 및 천이의 시기 또한 빨라지고 있다. 이 중 남조류의 경우 초여름에 발생하여 급격한 증식으로 대발생되어 녹조현상을 야기하고 이는 해당 수역의 생태계 파괴, 그 이외에도 사회적, 경제적, 환경적인 측면에서 많은 문제를 유발한다. 하천·호소의 조류의 발생과 거동에 대한 이해와 효과적인 대응책 마련을 위하여 현상에 대한 모니터링이 선행되어야 하지만 기존 조사방식은 점, 선 단위의 간헐적 측정을 통해 진행되고 있어 많은 인력과 시간이 필요로 하고 있는 실태이다. 현재 이에 따른 문제 해결을 위한 하천·호소의 원격탐사 기법을 이용한 조류의 발생 및 거동에 대한 모니터링 연구가 많이 진행되고 있다. 본 연구에서는 초분광 영상을 이용한 원격 탐사 모니터링을 위한 선행연구를 위해 400-1000 nm에서 NIR(visNIR)파장을 분석할 수 있는 초분광 카메라 CORNING사의 micro HSITM 410 shark와 영상 흔들림 보정을 위한 DJI사의 로닌-MX를, 이용하여 현재 녹조류, 남조류 5종의 배양액과 방사보정을 위해 99% 반사율의 반사판과 함께 촬영하여 영상을 수집하였다. 수집된 영상을 통하여 방사보정 및 해당 Base 제거를 통한 조류의 분광 정보 추출 과정을 통해 조류별 분광 정보를 추출, 분석하여 해당 조류의 분광특성을 파악하고 기초 라이브러리를 구축하여 제시함으로 추후 하천·호소에서의 초분광 영상 기반 원격탐사 모니터링에 적용하고자 한다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.13 no.4
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• pp.308-319
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• 2008

Temporal variations in plankton assemblages and environmental factors in Asan Bay and their relationships were examined with the data collected from February till early June, 2005. Seawater temperatures showed typical pattern of temporal change observed in temperate waters. Salinity variation was minor. Phytoplankton biomass showed two peaks, one in February only in the inner part of the bay and the other in May in the whole bay. Phytoplankton succession was clearly shown with the increase of seawater temperatures. Diatom (Bacillariophyceae) dominated in February, diatom and cryptomonads (Cryptophyceae) prevailed in May, and dinoflagellates (Dinophyceae) was most abundant in June. Spring bloom in Asan Bay occurred about one month earlier than those observed in temperate seas. Among the inorganic nutrients (N, P and Si), only silicate concentration showed a significant negative correlation with phytoplankton biomass, indicating the sink of this nutrient in the bay to be the uptake by phytoplankton. Nitrate concentration seemed to be a limiting factor in this bay during the study period. Mesozooplankton abundances showed a significant positive correlation with seawater temperatures and a significant negative correlation with phytoplankton biomass. Increase of mesozooplankton abundance followed phytoplankton increase with the time lag of about two months. This increase of zooplankton seemed to be the result of increased seawater temperatures and food.

• Korean Journal of Ecology and Environment
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• v.47 no.4
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• pp.273-281
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• 2014

We conducted the weekly monitoring (December 2012~April 2013) to evaluate the temporal variation and identification of Stephanodiscus spp. that are generally dominant during winter in the Yeongsan River. Phytoplankton species were identified and counted using the optical microscope and scanning electron microscope (SEM). Phytoplankton in the river were grouped into 6 classes (bacillariophyceae, chlorophyceae, cryptophyceae, cyanophyceae, dinophyceae, euglenophyceae), 30 genus and 41 species. Phytoplankton composition showed high abundance of diatoms in winter and Aulacoseira sp., Cyclotella sp. and Stephanodiscus spp. were dominant. Among the species, Stephanodiscus spp. was relatively abundant compared to other diatom species. Stephanodiscus spp. appeared from December 2012 to April 2013 and their abundance peaked in January. Abundance of diatoms especially peaked ($21,080cells\;mL^{-1}$) in January 15, 2013 when Stephanodiscus spp. also bloomed ($20,560cells\;mL^{-1}$). The abundances of Stephanodiscus spp. were gradually decreased from March and reached as low as $60cells\;mL^{-1}$ in April 26. Cyclostephanos (C. invisitatus), Cyclotella (C. meneghiniana), Discostella (D. pseudostelligera, D. woltereckii) and Stephanodiscus (S. hantzschii, S. minutulus, S. parvus) were classified in the circular diatoms. Abundance of S. hantzschii was extremely high compared to S. minutulus and S. parvus.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.2 no.2
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• pp.78-86
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• 1997

To clarify the phytoplankton blooms in Lake Shihwa after the construction of a dyke, a study on the environmental factors, the distribution of chlorophyll-a, phytoplankton standing stocks, dominant species and primary productivity was carried out in Lake Shihwa and adjacent coastal areas from October, 1995 to August, 1996. Lake Shihwa is brackish water with mixing of freshwater from tributaries and the remaining salt water at the bottom. The dense phytoplankton bloom of average value of 168.6 ${\mu}gChl-a\;l^{-1}$ have occurred throughout the year in Lake Shihwa which is eutrophicated by the large input of nutrients from inflowing 5 tributaries and Shihwa Industrial Complex. The major organisms of algal bloom in Lake Shihwa were diatoms, Cyclotella atomus, Nitzschia sp. and Chaetoceros sp. in autumn and winter, and dinoflagellate Prorocentrum minimum and Chrysophyceae in spring and summer. The autumn and winter diatom blooms were limited by the depletion of silicate in the lake. Diatom blooms have occurred in the coastal areas adjacent to Shihwa lake from winter to summer due to the inflow of nutrient rich-water from Lake Shihwa. The primary productivities in the Lake Shihwa ranged from 2,653 mgC $m^{-2}\;day^{-1}$ to 9,505 mgC $m^{-2}\;day^{-1}$ with an average of 3,972 mgC $m^{-2}\;day^{-1}$. However, most of the high primary production was limited to the shallow euphotic zone due to the inhibition of light penetration. The primary productivities during autumn and winter were limited by the depletion of silicate. Lack of photosynthesis and the decomposition of falling organic matter under the middle of water column accelerated the depletion of dissolved oxygen in the bottom layer.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.17 no.1
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• pp.9-15
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• 2012

Worldwide development of harmful algal blooms causes serious problem for public health and fisheries industries. To evaluate the algicidal impact on the harmful algae bloom species in aquatic ecosystems of coast, a new algicide thiazolidinedione derivative (TD49) were tentatively examined in the growth stages (i.e., lag, logarithmic and stationary phase) of rapidophyceae $Heterosigma$ $akashiwo$, $Chattonella$ $marina$ and $Chattonella$ sp..Three strains could easily destroy in the lag phase due to relatively weak cell walls than those of the logarithmic and stationary phase. It is thought that inoculation of TD49 substances into initial or developmental natural blooms with a threshold concentration ($2{\mu}M$) can maximize the algicidal activity. Also, bio-chemical assays revealed that the algicidal substances from all culture strains were likely to be extracellular substances because those cells have easily destroyed in cell walls. On the other hand, natural zooplankton communities were influenced within the exposure experiments of $2{\mu}M$, which is showed the maximum algcidal activity of tested organisms. These results indicate that although the TD49 substance is potential agents for the control of $H.$ $akashiwo$, $C.$ $marina$ and $Chattonella$ sp. in the enclosed eutrophic bay and coastal water, more detailed research of acute toxicity effect on high trophic organism in marine ecosystems need to be conducted.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 1997.10a
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• pp.52-53
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• 1997

수역의 유기오염 개선을 위하여 생활하수, 산업폐수 등의 저하시키는데 주안점을 두어왔으나 공공수역에서의 제거되지 않은 질소와 인의 유입으로 부영양화가 진행되어 하천에는 남조류가 대량발생하고 해역에는 적조가 광역에서 발생하여 큰 사회문제가 되고 있고, 질소와 인의 유입으로 인한 자생 COD가 전체COD의 약 절반을 차지하고 있는 실정이다. 따라서 앞으로의 수질을 개선하기 위해서는 조류증식의 제한인자인 질소와 인의 규제가 필요할 뿐만아니라 하수처리장에 고차처리를 적용하거나, 해양의 회석자용을 이용한 Ocean을 적용하여 연안해역 수질을 관리해야 할 것이다. 따라서 본 연구는 수영만을 대상으로 Ocean Outfall과 폐수처리시절을 적절하게 조합하기 위해서 3차원 생태계모델을 적용하여 유기물질 뿐만 아니라 영양염류인 질소와 인의 농도를 예측하여 환경기준을 만족시키고 비용을 최소화 할 수 있는 폐수처리공법과 해중방류관의 위치를 선정하고자 하였다. 본 연구결과 수영만의 1994년 COD는 II등급, DIN과 DIP는 III등급이었다. 현재의 활성슬러지공법으로 질소와 인을 제거하지 않고 방류할 경우 2001년에 는 하수처리량의 증가로 인해 COD의 경우 1994년 보다 조금 감소하지만 DIN 과 DIP는 1994년과 같은 III등급을 유지하였다. 고도처리공법을 도입할 경우 COD의 농도는 광안리와 해운대해수욕장에서 I등급을 보이고, DIP의 농도도 수영만 전체에서 강등급을 보이지만, DM의 농도는 광안리해수욕장에서 II등급, 해운대해수욕장에서 IH등급을 보였다 하수처리장 유출수를 Ocean Outfall을 이용하여 하수처리장으로부터 4km에 서 방류할 경우의 COD농도는 I등급을 보이고, DE 농도도 광안리와 해운대해 수욕장에서는 I등급을 보이고, DU의 농도는 ll등급을 보여 수질이 개선된 것 을 볼 수 있다. 이상에서와 같이 광안리와 해운대해수욕장의 해역환경기준 ll등급을 만족 하는 하수처리방법은 Ocean Outfall이었다. 수영하수처리장에 인을 처리하기 위한 화학적 침전법의 경우 956억원이 소요되고, 질소를 제거하기 위한 질소제거공정을 추가 건설 할 경우는 2181억원이 전요된다. 그리고 두공정을 같이 건설할 경우에는 3137억원의 비용이 소요된다 수영하수처리장에서 4km 거리와 관경을 2m의 Ocean Outfall 건설비용은 325 억원 정도가 소요되는 것으로 산출되었다. 고차처리시 증가되는 비용으로 건설할 수 있는 Ocean Outfall의 길이는 인 제거공정을 첨가하는 경우에는 18km을 건설할 수 있고, 질소제거공정을 첨가 하는 경우에는 46km를 건설할 수 있는 것으로 산출되었다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.10 no.1
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• pp.8-18
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• 2005

We studied seasonal distribution of the microphytobenthos and their primary production with $C^{14}$ method and carried out pigment analysis with HPLC in an estuarine mudflat of the Ganghwa Island, Korea from May 2002 to April 2004. The abundances of microphytobenthos were higher at the middle than upper part and lower part of intertidal flat. Abundances of microphytobenthos ranged from $2.3{\times}10^5\;cells\;cm^{-2}$ to $140.9{\times}10^5\;cells cm^{-2}$. The bloom of microphytobenthos was observed in the early spring and then it decreased from spring to summer and autumn. The pennate diatom was a predominated group among the microphytobenthos in this area. The dominant species were Paralia sulcata, Cylindrotheca closterium and Nitzschia sp.. Nitzschia sp. and Cylindrotheca closterium were predominant in February. The results of pigment analysis suggest the presence of diatoms, euglenophytes, chlorophytes, cyanobacteria, cryptophytes, chrysophytes, prymnesiophytes, dinoflagellates and prasinophytes. The biomass of microphytobenthos ranged from 1.18 to 34.25 mg chl-a $m^{-2}$, with a mean of 7.60 mg chl-a $m^{-2}$. The mean ratio of Fuco/Chl a was 0.7 which indicates that most of biomasses of microphytobenthos were due to diatoms. The ratios of Chl b/Chl a ranged from 0 to 0.82(with a mean of 0.17), implying that euglenophytes and chlorophytes lived together in special period seasonally. Temporal variation of primary production ranged from 4.2 to 113.0 $mgC{\cdot}m^{-2}{\cdot}hr^{-1}$(mean value was 33.9 $mgC{\cdot}m^{-2}{\cdot}hr^{-1}$ and initial slope$({\alpha})$ was measured from 0.002-0.005$(mgC\;mgchl-a^{-1}\;hr^{-1}){\cdot}({\mu}E\;m^{-2}\;s^{-1})^{-1}$. Assimilation number$(P_m)$ was in the range of 0.50-1.32 $mgC{\cdot}mgChl-a{\cdot}hr^{-1}$ and daily primary production ranged from 20.9 to 678.1 $mgC{\cdot}m^{-2}{\cdot}d^{-1}$(mean value was 206.72 $mgC{\cdot}m^{-2}{\cdot}^{-1}$).