• 한국물환경학회지
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• 제24권3호
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• pp.365-377
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• 2008

Large artificial dam reservoirs and associated downstream ecosystems are under increased pressure from long-term negative impacts of turbid flood runoff. Despite various emerging issues of reservoir turbidity flow, turbidity modeling studies have been rare due to lack of experimental data that can support scientific interpretation. Modeling suspended sediment (SS) dynamics, and therefore turbidity ($C_T$), requires provision of constitutive relationships ($SS-C_T$) and accounting for deposition of different SS size fractions/types distribution in order to display this complicated dynamic behavior. This study explored the performance of a coupled two-dimensional (2D) hydrodynamic and particle dynamics model that simulates the fate and transport of a turbid density flow in a negatively buoyant density flow regime. Multiple groups of suspended sediment (SS), classified by the particle size and their site-specific $SS-C_T$ relationships, were used for the conversion between field measurements ($C_T$) and model state variables (SS). The 2D model showed, in overall, good performance in reproducing the reservoir thermal structure, flood propagation dynamics and the magnitude and distribution of turbidity in the stratified reservoir. Some significant errors were noticed in the transitional zone due to the inherent lateral averaging assumption of the 2D hydrodynamic model, and in the lacustrine zone possibly due to long-term decay of particulate organic matters induced during flood runoffs.

• Journal of the korean society of oceanography
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• 제39권1호
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• pp.26-34
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• 2004

The evolution of intricate and striking patterns of suspended sediments (SS), which are created by certain physical dynamics in the East China and Yellow Seas, has been investigated using satellite ocean color imageries and vertical profiles of particle attenuation and backscattering coefficients. The structure of these patterns can reveal a great deal about the process underlying their formation. Sea surface temperature (SST) analyzed from the Advanced Very High Resolution Radiometer (AVHRR) thermal infrared data were used to elucidate the physical factors responsible for the evolution of suspended sediment patterns in the East China Sea. The concomitant patterns of suspended sediments were tracked from the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) ocean color data. The detailed examination about these patterns gave birth to the definition of the evolution of suspended sediments (SS) into four stages: (1) Youth or Infant stage, (2) Younger stage, (3) Mature stage, and (4) Old stage. We describe about the three directional forces of the tidal currents, ocean warm currents and estuarine circulations that lead to occurrence of various stages of the evolution of suspended sediments that increase turbidity at high levels through out the water column of the inner and outer shelf areas during September to April. The occurrence of these four stages could be repeatedly observed. In contrast, vertical profiles of the particle attenuation ($c_{p}$) and backscattering ($b_{bp}$) coefficients displayed obvious patterns of the propagation of suspended sediment plume from the southwestern coastal sea that leads to eventual collision with the massive sediment plume originating from the Yangtze banks of the East China Sea.

• 한국환경독성학회:학술대회논문집
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• 한국환경독성학회 2003년도 추계국제학술대회
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• pp.31-32
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• 2003

A dynamic multimedia model with 2-dimensional spatial resolution, POPsME (Persistent Organic Pollutants in Multimedia Environments), was evaluated by comparing predicted relative concentrations with those measured. A total of 12 polycyclic aromatic hydrocarbons (PAHs) were tested (phenanthrene, anthracene, fluoranthene, pyrene, chrysene, benz (a)anthracene, benzo(b)fluoranthene, benzo(k)fluoranthene, benzo(a)pyrene, dibenz(a,h)anthracene, benzo(g,h,i)perylene, and indeno(1,2,3-c,d)pyrene). The concentrations were measured in air particulates, water (dissolved phase and suspended solids (ss)), soil, sediment, and leaves of Pinus koraiensis and Prunus serrulata at seven sites in the Seoul and neighboring area (150km x 150km), Korea.

• 한국물환경학회지
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• 제25권1호
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• pp.48-57
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• 2009

A two-dimensional (2D), laterally-averaged hydrodynamic and water quality model, CE-QUAL-W2 was applied to evaluate the performance on simulating the effect of flushing from Daecheong Reservoir on the downstream water quality variations during the flushing events held on November, 2003 and March, 2008. The hydraulic and water quality simulation results were compared with field measurement data, as well as a one-dimensional (1D), unsteady model (KORIV1) that revealed limited capability in the previous study due to missing the resuspension process of river bottom sediments. The results showed that although the 2D model made satisfactory performance in reproducing the temporal variations of dissolved matters including phosphate, ammonia and nitrate, it revealed poor performance in simulating the increase of biological oxygen demand and suspended sediment (SS) concentrations during the passage of the flushing flow. The reason of the error was that the resuspension process of the 2D model is only the function of shear stress induced by wind. In reality, however, as shown by significant correlation between bottom shear stress ($\tau$) and observed SS concentration, the resuspension process can be significantly influenced by current velocity in the riverine system, especially during flushing event. The results indicate that the resuspension of river bottom materials should be incorporated into the water quality modeling processes if $\tau$ is greater than a critical shear stress (${\tau}_c$) for better simulation of flushing effect.

• 한국수산과학회지
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• 제40권6호
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• pp.394-410
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• 2007

Anchovy spawn from the end of May to mid-October, when the water temperature is $14.8-27.2\;^{\circ}C$ and the salinity is 26.0-33.6 psu. The main spawning season is between July to August, when the water temperature is $21.7-27.2\;^{\circ}C$ and the salinity is between 26.0-32.2 psu. The main spawning grounds of anchovy are coastal areas shallower than 50 m around the islands located in the Jeju Strait. Anchovy larvae are distributed near the fronts between Chuja-do, Jangsu-do, Yeoseo-do, and the open sea rather than in the spawning grounds. Anchovy eggs and larvae density increased in accordance with the high level of $Chlorophyll-{\alpha}$ during the summer season (July-August). In terms of the suspended sediment (SS) levels along the northern coast of the Jeju Strait, high densities of anchovy eggs (12.0-18.0 mg/L) were observed, mainly in the area affected by the coastal waters of the southern sea with high SS levels, while larvae (10.0-19.0 mg/L) tended to be distributed over a wide area with high SS levels, including the open sea. In terms of the dissolved oxygen (DO) content, eggs (5.4-6.8 mg/L) were observed in coastal areas with a high DO content, while larvae (4.2-6.4 mg/L) were distributed widely in areas with a relatively low DO content, from the southern coast to the open sea.

• 한국패류학회지
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• 제26권4호
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• pp.267-273
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• 2010

경기만 4개 지역 바지락 양식장의 저질조성에 따른 바지락 서식밀도 및 형태적 특성에 대하여 2007년 1월부터 12월까지 조사하였다. 저질조성에서 외리와 종현은 니사질로 분급이 양호하였으며, 백미리는 역질니토로 분급이 불량하였고, 내리는 니사질역으로 분급이 매우 불량하였다. 서식밀도는 저질조성과 상관없이 씨뿌림에 의하여 외리와 백미리에서 높았으며, 내리와 종현동에서 낮게 나타났다. 비만도는 저질조성에서 분급이 매우 불량한 내리와 분급은 양호하지만 먹이생물인 클로로 필-a가 높았던 외리에서 높게 나타났다. 조사기간 동안 수온은 $3.2-27.0^{\circ}C$ 범위로 나타났으며, 염분은 21.7-33.3 %, 용존산소는 5.6-12.7 mg/l, pH는 7.36-8.82였다. 부유물질은 3.2-1,266.0 mg/l, 클로로필-a는 $0.3-36.1{\mu}g/l$로 나타났다. 각 조사지역의 연간 바지락 비만도 및 성장은 해수중의 클로로필 농도와 유관한 것으로 사료되며, 이는 바지락의 먹이와 관련이 잇는 것으로 사료되었다.

• 한국수자원학회논문집
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• 제47권2호
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• pp.145-159
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• 2014

본 연구에서는 충주댐을 대상으로 유역모델인 SWAT과 저수지모델인 CE-QUAL-W2를 연계 적용하여 기후변화에 따라 저수지로 유입되는 하천의 유량 및 탁수발생량을 모의하고, 저수지내의 탁수변화 및 부영양화 영향평가를 통한 저수지 수환경 변화를 전망하였다. 먼저 SWAT을 적용하여 강우시 저수지 유입하천의 유량 및 수질을 모의하여 모델의 재현성을 검토하였으며, 모형의 보정(2000~2005)과 검증(2006~2010) 결과 모델 예측값과 실측값이 적절하게 일치하는 것으로 나타났다. SWAT의 결과를 CE-QUAL-W2의 하천유량 및 유입수 수질경계조건 입력자료로 활용하고, 보정(2010년)과 검증(2008년)을 통하여 저수지 내 시간에 따른 물수지, 수온 변화, 부유물질(SS), T-N, T-P 및 부영양화(Chl-a) 양상 등을 분석하고 모델의 재현성을 검토하였다. 이후 기후변화 시나리오 적용에 따른 저수지 내수환경변화를 모의하기 위한 기후변화자료로 IPCC AR4 GCM(ECHO-G)을 고해상도지역 기후 시나리오로 개선시킨 RCM(MM5)의 A1B 시나리오를 다시 태풍사상을 고려한 인공신경망 기법에 의해 상세화하여 이용하였다. 기후변화 시나리오에 따른 기온증가의 영향으로 미래로 갈수록 상층수온은 증가하는 반면 심층수온은 감소하는 경향을 보였다. SS 최고유입농도는 평수년에 비해 풍수년에 17%, 갈수년에 0.2% 가량 증가하는 것으로 나타났다. 호소내 SS 10mg/L 이상 점유일수는 평수년에 비해 풍수년이 6일, 갈수년이 17일 증가하였고, 점유율 역시 풍수년에 24%, 갈수년에 26%가량 증가하는 것으로 분석되었다. 미래로 갈수록 기후변화가 충주댐 탁수장기화에 영향을 미치는 것으로 분석되었다. Chl-a의 최고농도는 평수년에 비해 풍수년에 19%, 갈수년에 3% 가량 조류의 농도가 증가되는 것으로 나타나 조류의 영향이 커지는 것을 알 수 있었다.

• 한국토양비료학회지
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• 제45권4호
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• pp.642-648
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• 2012

주암호 상수원 상류지역인 죽산천에 위치한 죽산천 인공 습지의 수생태학적 특성을 평가하기 위해 수질에서의 영양 염류 처리효율, 수생식물의 무기성분 흡수량 및 퇴적물내 화학적 특성을 평가하였다. 수질에서의 영양염류 처리효율은 COD와 SS를 제외하고 전반적으로 낮았다. 죽산천 인공 습지의 주요 우점종의 영양염류 흡수량을 조사한 결과, T-N 및 T-P 흡수량은 8월에 노랑꽃창포 > 수련 > 노랑어리 연꽃 순으로 최대흡수량을 나타내었다. 퇴적물내 O.M 함량은 시기별로 큰 차이가 없었고, T-N 및 T-P의 함량은 봄에서 여름으로 시기가 변함에 따라 낮아져서 겨울까지 낮은 함량을 유지하였다. 퇴적물내 microbial biomass C:N:P의 비율은 봄, 여름, 가을 및 겨울이 각각 117~140:1~4:1, 86~126:5~6:1, 68~101:2~6:1 및 47~138:2~4:1로 나타났다. 죽산천 인공습지는 질소와 인의 처리효율이 낮고, 겨울철 수질 정화효율이 낮아 습지의 정화효율 향상을 위한 개선이 필요할 것으로 판단된다.