• 한국환경과학회지
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• 제8권2호
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• pp.171-176
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• 1999

To estimate the residence times of aerosols in air, the activities of $^{210}Pb$ and $^{210}Po$ in aerosols were measured at 4 sites in Pusan. All aerosol samples were collected by a high volume air sampler from January to October 1996. The activities $^{210}Pb$ and $^{210}Po$ in Pusan were varied from 11.77 to 67.57 dpm/1000$m^3$ and from 2.63 to 15.91 dpm/1000$m^3$, respectively. The mean activities were 34.62 dpm/1000$m^3$ for $^{210}Pb$ and 8.24 dpm/1000$m^3$ for $^{210}Po$. The highest values of the activities of $^{210}Pb$ and $^{210}Po$ were appeared at P3 site and the lowest values at P4 site. During the sampling period, the trends of the activities of $^{210}Po$ and $^{210}Pb$ were similar to total suspended particulate matter(TSP) concentrations. The mean residence times of atmospheric aerosols calculated from $^{210}Po$/$^{210}Pb$ activity ratio was about 60~80 days in Pusan. The longest residence time of atmospheric aerosols was in January because of the lack of rainout and washout, but the shortest residence time was in August, largely due to scavenging effect by frequent rains. The activities of $^{210}Po$ and $^{210}Pb$ in atmospheric aerosols were different in time and space, which seems that the distribution of $^{210}Po$ and $^{210}Pb$ activities and scavenging processes in air may be controlled by the local and meteorological conditions.

• 한국해양환경ㆍ에너지학회지
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• 제12권4호
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• pp.248-254
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• 2009

영산강 하구해역에서 계절별로 물질순환과 영양염 플럭스 특성을 파악하기 위해 단순 박스모델을 이용하여 담수수지, 염분수지, 영양염 물질수지를 산정하였다. 외해, 시스템영역으로 유입되는 계절적 평균담수의 양은 $36.481{\times}10^6{\sim}663.634{\times}10^6m^3/month$로 나타났다. 염분수지에 의해 계산된 담수존재량은 $2.515{\times}10^6{\sim}5.812{\times}10^6m^3$이었고 평균 체류시간은 0.26~2.03일로 계산되었다. 평균체류시간은 계절별로 큰 차이를 보였는데 강우가 집중된 하계 풍수기에는 0.26일의 짧은 체류시간을 보인 반면 추계 갈수기에는 2.03일의 평균체류시간을 나타내었다. 해수교환량은 $1,248{\times}10^6{\sim}9,489{\times}10^6m^3/month$으로 하계 풍수기에 해수교환량이 가장 크게 나타났다. 영양염의 부하량은 DIP과 DIN가 각각 2.9~61.22 ton/month, 76.63~1,149.91 ton/month로 계산되었다. 영양염의 체류시간은 DIP의 경우 0.45~1.10일의 범위를, DIN의 경우 0.28~1.92일의 범위를 보였고, 담수체류시간과 비교하면 DIP과 DIN는 하계를 제외한 전 계절에서 담수 체류시간 보다 짧은 체류시간을 보여 영양염이 빠르게 순환되는 것을 알 수 있었다. 특히 DIP는 동계에 외해에서 상대적으로 높은 농도를 보이고 같은 시기에 해수교환에 의한 플럭스가 시스템 영역내로 유입되는 결과를 보여 외부 유입원 존재를 추정하게 하였다.

• 한국물환경학회지
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• 제29권1호
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• pp.81-87
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• 2013

Changes of organic carbon after the entrance into dam reservoirs were investigated using water samples collected in May, September, and October in 2010 from the inflow sites and the outlets of four selected dam reservoirs-Soyang, Chungju, Chungju regulation, and Uiam. Increase of refractory dissolved organic carbon (R-DOC) was observed only for large dam reservoirs with long residence times whereas the trend was not found for relatively small reservoirs. The effects of residence times on organic carbon changes were further confirmed by significant positive correlations between monthly residence times and the relative increase of either dissolved organic carbon (DOC) or R-DOC concentrations. Comparison of spectroscopic characteristics of DOC revealed that the changes in the large reservoirs in May might result from in-lake processes. The inflow of terrestrial sources of DOM during storms appears to largely affect the DOC quality of the large reservoirs for the rest of the sampling periods. The mechanism, however, did not fully explain the behaviors of DOC for the small sized reservoirs. Our combined results suggested that both residence time and the input of allochthonous carbon sources might substantially influence the quantity of DOC as well as its quality in dam reservoirs.

• 한국시뮬레이션학회:학술대회논문집
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• 한국시뮬레이션학회 1999년도 춘계학술대회 논문집
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• pp.6-10
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• 1999

We present a simulation result to the analysis of the effects of cell residence time distributions upon the expected channel occupancy time based on an analytic mobility model. Numerical examples show that exponential distribution provides upper and lower bound to the expected channel occupancy times of new calls and handoff calls. This fact reveals that the assumption of exponential distribution as the cell residence time distribution as the cell residence time distribution may over- or under-estimate cellular mobile systems.

• 해양환경안전학회지
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• 제17권4호
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• pp.339-343
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• 2011

본 연구에서는 EFDC모델과 입자추적모델을 이용하여 마산만의 담수유입에 의한 폐쇄성 내만의 물질체류시간을 산정하였다. 마산만의 해수유동을 재현하고 이를 바탕으로 평균체류시간을 계산하였다. 마산만의 조석에 의한 평균물질체류시간은 만 북측과 돝섬 부근까지가 약 110일이내, 모도 주변 해역이 약 40일, 부도에서 외해까지 약 20일 정도로 산정되었다. 담수유입에 따른 마산만의 4개 소해역별 평균물질체류시간은 I과 II영역에서 약 81일로 감소하였으나, 마산만의 외해측에 위치한 III과 IV영역은 각각 58일과 17일로 증가하였다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제8권1호
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• pp.42-47
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• 2003

토양 및 지하수 복원 과정에서 벤젠과 에틸렌이 혼합되어 배출될 경우 이를 biofilter에 의해 처리한 결과, 에틸렌은 생분해가 잘 되지 않는 화합물인데도 불구하고 체류시간이 10～15분에서는 96%이상 높은 생물학적 처리를 보여 biofilter운전 가능성이 제시되었다. 2～15분 체류시간에서 혼합 VOCs중 벤젠은 모든 조건에서 100% 제거되었다. 체류시간이 15분일 경우 벤젠과 에틸렌의 최대 제거능은 각각 4.3과 1.4g/$\textrm{m}^3$hr로서 벤젠이 에틸렌에 비해 3배 정도 컸다. 체류시간이 작을수록 에틸렌 분해율 감소로 인하여 이산화탄소 발생도 감소함을 발견하였으며 벤젠과 에틸렌이 모두 제거되는 운전에서 최고 이산화탄소 발생률은 3,169 [mg-$CO_2$/(g-${C_2}{H_4}$＋${C_6}{H_6}$)]이었다. 벤젠 산화 미생물은 Bacillus mycoides와 Pseudomonas fluorescens로 동정되었고, 에틸렌 산화 미생물은 Pseudomonas putida와 Pseudomonas fluorescens로 각각 동정되었다.

• 한국해양공학회지
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• 제22권6호
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• pp.20-26
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• 2008

In this paper, in order to set up the management system of water quality environment in Gwangyang Bay, the cluster analysis of water quality environment, the estimation of inflowing pollutant loads and residence time of pollutants in this bay was carried out. The Gwangyang Bay was divided into eight sea areas by cluster analysis and spatio-temporal change of water quality. The river discharges in the Bay were calculated about $11,681{\times}103m^3/day$ from the numerical simulation by Tank model. In addition, inflowing pollutant loads of COD, SS, TN, TP, DIN and DIP in Gwangyang Bay were estimated at 398 ton-COD/day, 2,846 ton-SS/day, 195 ton-TN/day, 5 ton-TP/day, 126 ton-DIN/day and 3 ton-DIP/day, respectively. Moreover, residence times of COD, TN and TP in the Bay was estimated at 6 days-COD, 20 days-TN and 195 days-TP, respectively in the dry season, and 3 days-COD, 6 days-TN and 21 days- TP, respectively, in the flood season. The central part of Gwangyang Bay (Region IV) has the longest residence time of overall pollutants.

• 한국해양공학회지
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• 제23권2호
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• pp.47-52
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• 2009

A Lagrangian particle tracking model coupled with the Princeton Ocean Model were used to estimate the average residence time of coastal water in Masan Bay, Korea. Our interest in quantifying the transport time scales in Masan Bay was stimulated by the search for a mechanistic understanding of this spatial variability, which is consistent with the concept of spatially variable transport time scales. Tidal simulation was calibrated through a comparison with the results of semi-diurnal current and water elevation measured at the tidal stations of Masan, Gadeokdo. In the model simulations, particles were released in eight cases, including slack before ebb, peak ebb, slack before flood, and peak flood, during both spring and neap tides. The averaged values obtained from the particle release simulations were used for the average residence times of the coastal water in Masan Bay. The average residence times for the southeastern parts of Somodo and the Samho River, Masan Bay were estimated to be about 20~50days and 70~80days, respectively. The spatial difference for the average residence time was controlled by the tidal currents and distance from the mouth of the bay. Our results might provide useful for understanding the transport and behavior of coastal water in a bay and might be used to estimate the dissimilative capacity for environmental assessment.

• 한국환경과학회지
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• 제29권3호
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• pp.273-282
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• 2020

Residence time is defined as the time taken for a material in a system to leave the system. The residence time characteristics in shellfish aquaculture determine the dispersion of excretion from aquaculture farms, along with the supply of food by seawater exchange. In this study, we estimated the spatial distribution of average residence time in the shellfish farming area using a particle tracking model. As a result, a relatively short average residence time of about 20 days or less was calculated in most areas, but an average residence time of more than 40 days was calculated in the inner areas. Relatively long average residence times were calculated along the west coast compared to the east coast, with the longest average residence time of more than 50 days in the northwestern areas. It can be inferred that the disturbance of the benthic ecosystem caused by shellfish farms is likely to be large because of the relatively weak dispersion of excrement from shellfish farms located on the west coast, especially in the northwest region. This distribution of average residence time is important for understanding the potential effects of seawater exchange on the environmental sustainability of shellfish farms, along with the seawater circulation characteristics of Jaran Bay.

• 한국해양환경ㆍ에너지학회지
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• 제3권4호
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• pp.76-90
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• 2000

물질수송 해석을 위한 박스모델 형태의 물질수지모델을 이용하여, 주변의 많은 환경적 변화 요인을 내재하고 있는 금강하구를 대상으로 계절별 영양염 물질순환 특성을 평가하였다. 담수 유입 및 유출은 계절에 따라 약 4～14배의 큰 차이를 나타내었다. 물수지에 의한 담수유 출량은 1.014×10/sup 8/～12.566×10/sup 8/m³/month로 나타났으며, 담수유출량의 99.7%가 하천수의 유출에 의한 것으로 나타났다. 염분수지에 의해 계산된 담수존재량은 0.339×10/sup 8/～0.652×10/sup 8/m³이었고, 평균체류시간은 1.6～10.0일, 해수교환시간은 2.2～11.9일로 계산되었다. 평균체류시간은 계절별로 큰 차이를 보였는데 강우집중시기인 하계 풍수기에는 1.6일의 짧은 체류시간을 보인 반면 동계 갈수기에는 10.0일의 평균체류시간을 나타내었다. 영양염 수지로 계산된 DIP의 유입flux의 범위는 5.57～32.68ton/month이었고, DIN 유입flux는 234.93～2,373.39ton/month로 계산되었다. 영양염의 체류시간을 보면, DIP의 경우 1.1～6.4일의 범위를, DIN의 경우 1.8～10.9일의 범위를 보였고, 담수체류시간과 비교하면, DIP는 0.39～2.31배, DIN은 0.83～l.13배를 나타내었다. DIP의 경우 하계를 제외한 전 계절에서 담수 체류시간보다 짧아 DIP가 빠르게 순환되었으나, DIN의 경우 하계와 동계에 담수체류시간보다 긴 순환비를 보여 영양염이 축적됨을 알 수 있다.