• 한국해양학회지:바다
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• 제12권4호
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• pp.273-279
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• 2007

동해 남서부 해역 울릉분지 일대 대륙붕과 대륙사면에서 퇴적속도를 추정하기 위해 저배경방사능 우물형 고순도 게르마늄 감마선 검색기를 이용하여 $^{210}Pb$, $^{226}Ra$와 $^{137}Cs$를 측정하였다. 추정된 퇴적속도는 대륙붕에서 가장 높고 (0.6-1.1 cm/yr), 대륙붕의 정점 B1005로부터 외해로 갈수록 거리가 증가함에 따라 퇴적속도는 지수함수적으로 감소하여, 분지에서 0.2 cm/yr 이하로 계산되었다. $^{137}Cs$의 투과깊이을 이용하여 퇴적속도에 대한 퇴적 후 퇴적물 혼합작용의 영향을 평가한 결과, 정점 BS-1을 제외하고 다른 정점들에 대하여 퇴적속도 추정에서 생물교란의 영향이 미미하다고 판단되어, 추정된 퇴적속도는 이 지역의 퇴적속도를 잘 나타내고 있다고 판단되었다. 기존의 여러 연구들과 이 연구의 결과로부터 대한해협을 통해 공급된 퇴적물들이 한반도 동남해역 연안에 이르러 대륙붕지역에 주로 퇴적되며, 나머지는 한반도 동쪽 대륙사면과 분지에 퇴적되는 것으로 추정할 수 있다. 또한 $^{210}Pb$ 수직분포는 이 지역의 퇴적과정이 매우 복잡할 가능성을 제시한다.

• 대한환경공학회지
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• 제34권11호
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• pp.780-785
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• 2012

침전지 구조물에서의 조류 부착현상은 4월말에서부터 10월초까지 나타났고, 침전지 청소 7일 후부터 부착조류가 관찰되었으며, 운전기간이 경과할수록 부착조류의 양은 점진적으로 증가하였다. 부착 조류 종들은 남조류인 Oscillatoria sp.와 Phormidium sp., 규조류 인 Synedra sp., 녹조류인 Mougeotia sp.와 Oedogonium sp.가 관찰되었으며, 부유성 규조류인 Stephanodiscus sp.도 부착조류의 군집에서 자주 관찰되었다. 침전지 월류 조류 종들은 규조류인 Cymbella sp., Navicula sp., Synedra sp.와 Stephanodiscus sp.가 관찰되었고, 녹조류의 경우는 Mougeotia sp.와 Cosmarium sp., 남조류는 Anabaena sp.가 관찰되었다. 황산동의 투입효과를 살펴보기 위해 침전지 트러프의 단위 면적당($cm^2$) 부착조류의 농도를 조사한 결과, 황산동을 투입한 침전지의 경우는 침전지 청소 후 14일과 28일 경과 후에 단위 면적당 부착조류의 농도가 각각 $4{\mu}g/L/cm^2$와 $19{\mu}g/L/cm^2$로 나타나 조류 부착현상이 매우 더디게 진행된 반면, 황산동을 투입하지 않은 침전지의 경우는 침전지 청소 후 14일과 28일 경과 후의 부착조류 농도가 각각 $59{\mu}g/L/cm^2$와 $147{\mu}g/L/cm^2$로 나타나 시간의 경과에 따라 다양한 부착조류가 부착하여 성장하였다. 공업용수 처리수의 수질에 미치는 영향을 조사하기 위하여 공업용수도용 배수지의 침전물을 분석한 결과, 적갈색의 미세한 침전물들에서 규조류의 파편들이 검출되었으며, 녹조류와 남조류의 경우는 분해되어 침전물의 유기물 성분으로 존재하면서 산화철과 결합하여 침전물을 형성하였다.

• 상하수도학회지
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• 제23권6호
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• pp.865-870
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• 2009

In this study, the adequacy of Reynolds numbers and Froude numbers derived from about sixty domestic water treatment plants (WTPs) were analyzed in order to estimate the characteristics of hydraulic behavior within the rectangular shaped sedimentation basins used widely. From the results of analysis, most of domestic WTPs have satisfied the criteria regulated as that Reynolds number should less than 1,000(dimensionless). On the other hand, they have not been able to satisfy the Froude number criteria, which should be higher than $1.0{\times}10^{-6}$. The reasons why most of domestic WTPs could not satisfy the criteria are that its criteria basis has been not only inadequate, but also the concept of external flow occurred around a settling particle has been ignored. Accordingly, this study proved the feasibility of Archimedes number, which indicates the ratio between particle Reynolds number and Froude number, to evaluate the hydraulic efficiency and its function of scale factor.

• 대한자원환경지질학회:학술대회논문집
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• 대한자원환경지질학회 2003년도 춘계 학술발표회 논문집
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• pp.27-31
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• 2003

During the past decade, integrated stratigraphy has been effectively applied to many sedimentary basins to analyze stratigraphic response to tectonic evolution. This application has been beneficial to hydrocarbon exploration in the basins because it provides a better understanding of temporal and spatial relationships of hydrocarbon source and reservoir rocks as a function of basin evolution. Like the maturation, migration, and trapping of hydrocarbons, ore-forming processes in hydrothermal deposits may be causally linked to particular phases of basin evolution. Consequently, applying integrated stratigraphy to mineral exploration may be a logical and helpful approach to understanding ore-forming processes and predicting their occurrence, location, and origin. (omitted)

• 한국수자원학회논문집
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• 제33권S1호
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• pp.784-787
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• 2000

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2000년도 학술발표회 논문집
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• pp.1003-1008
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• 2000

• 한국물환경학회지
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• 제21권1호
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• pp.40-45
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• 2005

Sedimentation is one of the most common and important units in conventional water treatment plant. Structure such as various baffle walls and inclined plate settler may be obstacles to the horizontal flow when it is poorly designed. Therefore, the effects of these structures on characteristics of hydraulic flow must be evaluated to improve the settling efficiency of the floc. The hydraulic characteristic of the two sedimentations at Y water treatment plant (YWTP), which have different deflector baffles inside the settling basin, were investigated by tracer (fluoride) test. The inclined plate settler installed inside settling basin caused an undesirable impact on horizontal flow and produced dead zone. Solid baffle wall under the plate settler could help to minimize the formation of density currents and flow short circuiting. NaF used as a tracer was recovered more than 90% at investigated all basins. Morill index ($t_{90}/t_{10}$), Modal index ($t_p/T-HRT$) and short-circuiting index ($[M-HRT-t_p]/M-HRT$) were determined from tracer test results performed at YWTP. Those indices ranged 2.95~3.02, 0.40~0.53 and 0.32~0.46, respectively.

• 한국양식학회:학술대회논문집
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• 한국양식학회 2003년도 추계학술발표대회 논문요약집
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• pp.126-126
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• 2003

Performance of a laboratory scale closed seawater recirculating aquaculture system was evaluated. Twenty-kg Korean rockfish (130 fish) with an average body weight of 153.8 g was stocked. Over 107-day culture period, fish reached final density of 51.7 kg/m$^3$ (initial density, 33.3 kg/m$^3$) on the culture tank volume basis. On a daily basis, water addition was 3.4% of the total water volume in the system. Total ammonia nitrogen (TAN)concentrations were below 1 mg/L and nitrite nitrogen (NO$_2$-N) concentrations were within the range of 1-3 mg/L on most sampling days. TAN was removedin bead and sand filters and it was removed or produced in the sedimentation basin. Basically, NO$_2$-N was removed in the bead and sand filters while it was either removed or produced in the sedimentation basin. Nitrate nitrogen (NO$_3$-N) was produced in the bead filters and removed in the sand filter and sedimentation basin. Foam fractionator performed well in the recirculating system. The maximal daily removal values for total suspended solids (TSS) and protein were 10,9 g and 1.4 g, respectively. Whole water quality parameters were within the levels commonly recommendedfor fish culture on most of the sampling days. However, further studies are needed to evaluate the commercial feasibility of this system because of the small-scale system used in present experiment. At least, present study still provides some basic information for further studies of this kind of system.

• Ocean and Polar Research
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• 제25권4호
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• pp.493-501
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• 2003

Performance of a laboratory scale closed seawater recirculating aquaculture system was evaluated. Twenty-kg of korean rockfish (130 fish) with an average body weight of 153.8g was stocked. Over a 107-day culture period, fish reached final density of $51.7kg/m^3$ (initial density, $33.3kg/m^3$) on the basis of the culture tank volume. On a daily basis, added water amounted to 3.4% of the total water volume in the system. Total ammonia nitrogen (TAN) concentrations were below 1mg/l and nitrite nitrogen $(NO_2-N)$ concentrations were within the range of 1-3mg/l on most sampling days. TAN was removed from bead and sand filters and it was removed or produced in the sedimentation basin. Basically, $NO_2-N$ was removed in the bead and sand filters, while it was either removed or produced in the sedimentation basin. Nitrate nitrogen $(NO_3-N)$ was produced in the bead filters and removed from the sand filter and sedimentation basin. The foam fractionator performed well in the recirculating system. The maximal daily removal values for total suspended solids (755) and protein were 10.9g and 1.4g, respectively. Whole water quality parameters were within the levels commonly recommended for fish culture on most of the sampling days. However, further studies are needed to evaluate the commercial feasibility of this system because of the smallscale system used in present experiment. At least, the present study still provides some basic information for further studies of this kind of system.

• 한국해안해양공학회지
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• 제3권1호
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• pp.38-44
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• 1991

간단한 box 모형이 장방형 해분에서의 세립 퇴적물의 퇴적현상을 설명하기 위하여 이용되었으며. 이 모형에 필요한 침식 및 퇴적률의 계수를 조사하여 남해안 가막양만에 적용하여 보았다. 해분이 외해와 연결되어 있고 외해의 부유퇴적물 농도가 일정하면 해분내에서 한 조석 주기 동안의 평균 부유퇴적물 농도는 일정한 값을 유지하게 되고 조류의 게류시 부근에는 퇴적이 일어나고 최대 유속시 부근에는 바닥 퇴적물의 재부유 및 침식이 일어나는 것을 보여주고 있다. 가막양만 처럼 퇴적이 우세한 해분에서는 조석 주기 중 퇴적이 일어나는 시간과 최대 퇴적률이 침식에 비하여 크게 나타나고 있으며, 이러한 퇴적 우세 해분의 부유퇴적물 평균농도는 외해의 부유퇴적물 농도보다 낮은 값을 보이고 있다. 또한. 조류의 유속변화에 따른 해분내기 부유퇴적물 농도변화는 고조의 약 한 시간 전에 최대값을 나타내고 저조의 약 한 시간 후에 최소값을 나타낸다.