• 한국수산과학회지
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• 제30권2호
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• pp.252-263
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• 1997

1993년 거금수로에서 계절별로 수온, 염분을 관측하였으며, 수로내 2개 정점에서 25시간 연속 수온, 염분 관측을 실시하여 이들 자료를 비교, 분석하였다. 수온은 년중 $7.0\~25.0^{\circ}C$의 범위로 동, 하계의 온도차는 약 $18^{\circ}C$이다. 표, 저층간의 온도차는 년중 $0.75^{\circ}C$ 이하로 수로내 해수의 수온 성층은 매우 약하다. 수로방향으로의 수평 온도차도 약 $0.3^{\circ}C$ 이하로, 수로를 따라서의 강한 조류가 거금수로내 수온의 수평, 연직 분포에 크게 영향을 미치고 있음을 시사한다. 염분도 수온과 같이 년중 표, 저층 및 수로 방향에서 수평 염분차가 $0.5\%_{\circ}$ 이하로 작다. 염분은 4월이 $34.0\%_{\circ}$, 8월이 $30.0\%_{\circ}$로, 4월이 8월에 비해 $4\%_{\circ}$정도 높다. 이는 동 시기의 강우량과 일조시간의 분포와 일치해 기상에 직접 영향을 받고 있음을 알 수 있다. T-S diagram에 나타난 계절별 수괴 특성은 동계에서 하계로 갈수록 저온 고염의 고밀도수에서 고온 저염의 저밀도수로 변화하며, 표, 저층간의 밀도차는 춘계와 추계에 거의 0, 동계와 하계에 $1.0\~1.5$로 매우 작다. 1993년 4월 $29\~30$일의 조위 변동에 따른 수온과 염분의 변화는 고조시 수온은 낮고 염분은 높다. 저조시는 그역의 변화를 나타낸다. 1일 중의 수온과 염분의 탁월 변동 주기는 동 해역에서 탁월한 반 일주조의 조석주기와 거의 일치한다. 해역의 성층 정도를 판단하는 성층계수는 년중 $4.0J/m^3$이하로 조류에 의한 저층 연직 혼합이 년중 매우 활발함을 나타낸다. 성층 진단식에 의한 성층과 혼합의 크기는 조류에 의한 혼합항이 $4.7\~14.1J/m^3day^{-1}$로 가장 크다. 관측에서 나타난 계절별 수온, 염분 구조와 일치하는 조류 혼합률 $\varepsilon$의 평가는 0.005였다.

• Journal of Photoscience
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• 제9권2호
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• pp.110-113
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• 2002

We demonstrate here a dynamic structure of bacteriorhodopsin (bR) as revealed by $^{13}$ C NMR studies on [3_$^{13}$ C]_,[1-$^{13}$ C]Ala- and/or Val-labeled wild type and a variety of site-directed mutants at ambient temperature. For this purpose, well-resolved (up to twelve) I$^{13}$ C NMR peaks were assigned with reference to the displacement of peaks due to the conformation-dependent I$^{13}$ C chemical shifts and reduced peak-intensities due to site-directed mutations. Revealed bR structure was not rigid as anticipated from 2D crystals of hexagonal array but a dynamically heterogeneous, undergoing a variety of local fluctuations depending upon specific site with frequency range of 10$^2$ -10$^{8}$ Hz. In particular, dynamics- dependent suppression of peaks turned out to be very sensitive to the motion of 10$^{-4}$ s and 10$^{-5}$ s interfered with frequency of magic angle spinning and proton decoupling, respectively. It is also noteworthy that such dynamic feature is strongly dependent upon the manner of 2D crystalline packing: $^{13}$ C NMR peaks of monomeric bR yielded either highly broadened or completely suppressed signals, depending upon the type of $^{13}$ C-labeled amino-acid residues.

• 한국해양학회지
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• 제25권2호
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• pp.84-95
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• 1990

CTD, 해류계, 인공위성 영상사진을 이용하여 황해 중부의 조석전선 주변역을 조사 한 결과 몇 가지 물리적 특성을 알 수 있었다. 전선은 태안반도 끝 부분을 중심으로 하여 4월 중에 태양열에 의한 해표면 가열과 함께 나타나기 시작하여 8월에 가장 뚜렷 하며 11월에는 표층냉각과 함께 소멸한다. 전선의 북측에서는 전선을 가로지르는 조류 에 의하여 수온 염분의 조석주기 변화가 나타남으로써 전선구조를 보여준다. 경기만에 서 나타나는 전선은 통최상의 조석전선과 달리 한강에서 유출된 담수와 외양수의 만남 에 의하여 형성된다. 표층냉수의 중심에서는 조석혼합역이 연안으로부터 약 50 km 외 양하지 분포한다. 전선의 남측에서도 전선의 구조는 비슷하나 전반적으로 혼합 정도가 약하게 나타난다. 이 연안 혼합역의 연안쪽에서는 금강유출된 담수에 의하여 염분전선 이 좁은 범위에서 흥성된다. 이 염분전선 부근의 일부에서는 용승과 같은 현상이 관측 되었다.

• 대한원격탐사학회지
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• 제28권3호
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• pp.267-276
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• 2012

Terminal lakes are widely distributed in the arid and semi-arid Gobi of Mongolia, and serves as important water resource for local people and livestock. However, such lakes are subject to great fluctuations in its size depending on climatic conditions and human water utilization. The Orog Lake is one such example that has shown remarkable fluctuation in recent years. In this study, we investigated the temporal changes of Orog Lake surface area by using 16-day MODIS 250 m NDVI products from 2000 to 2010. The results were compared with climate variability represented by monthly precipitation and temperature. Our results show that the Orog Lake gradually shrank for the period from 2000 to 2010, but with a significant range of seasonal and inter-annual variability. The lake area showed considerable seasonal variations, as it expanded in spring and fall, primarily due to snow melt and summer precipitation, respectively. Extreme drought period from 2000 to 2002 triggered the substantial reduction in lake area, leading to dry-up in year 2005, 2006, 2007, and 2009. After dry-up once occurred in 2005, the lake repeated reappearance and disappearance depending on seasonal and annual precipitation. Our findings implicate that the ground water fluctuated around the lake bottom level since 2005. This suggests the highly vulnerable nature of Orog lake, which greatly depends on future precipitation change.

• 환경위생공학
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• 제5권2호
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• pp.89-99
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• 1990

Morphology, anatomy and diurnal acid fluctuations were investigated monthly for the succulent C4 dicot Portulaca grandiflora Hook. growing under natural environmental conditions. Modified Kranz-Type sturcture and typical CAM-like cells were shown in leaves and stems, respectively. Values of indices of mesophyll succulence inleaves stems were 5.62 and 16.68, respectively. The number of stomata were 1476$\textrm{cm}^{-2}$ in leaves while the stomata in stems were not observed through growing seasons from spring to summer. However, on Sep. 16, 1981 in defoliate autumn season, stomata were begun to be produced for the first time in stems and the number were increased gradually to 216$\textrm{cm}^{-2}$ on Oct. 29. This feature can be interpreted as a seasonal plant dimorphism. P. grandiflora exhibited a diurnal fluctuation of titratable acidity in leaves and stems. Seasonal amplitudes of acid fluctuation in stems were as follows: 27 $\mu$eq./g.f.wt. on Sep. 21; 57$\mu$eq/g.f.wt. on Oct. 3; 80$\mu$eq./g.f.wt. on Oct. 21. Such the results in seasonal amplitude were able to consider due to decrease of light period and cool night air temperature according to change of season. Also, the naturally defoliated stems which had already stomata exhibited usual diurnal acid fluctuation, on the other hand the treated stems which possessed artificially closed stomata showed a few of acid fluctuation. Especially, stomata in stems are developed by seasonal dimorphism and activated stomata participate in CAM behavior of stems.

• 한국군사과학기술학회지
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• 제4권2호
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• pp.256-262
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• 2001

Viscous solutions of supersonic side jet nozzle and supersonic jet impinging on a flat plate are simulated using three-dimensional Navier-Stokes solver. For rapid and abrupt control of a missile in supersonic flight, side jet on a missile body is found to be a useful devise as evidenced by recent missile development at several nations. The magnitude of the side jet and the duration of it decide the level of control of such a missile system. The aerodynamic characteristics of the side jet devise itself are examined in terms of key parameters such as the side jet nozzle geometry, the chamber pressure and temperature. On the other hand, the jet impinging flow structure exhibits such complex nature as shock shell, plate shock and Mach disk depending on the flow parameters. Among others, the dominant parameters are the ratio of the nozzle exit pressure to the ambient pressure and the distance between the nozzle exit plane and the impinging plane. As the plate is placed close to the nozzle, the computed wall pressure at or near the jet center oscillates with large amplitude with respect to the mean value. The amplitude of wall pressure fluctuations subsides as the plate/nozzle distance increases, and the frequency of the wall pressure is estimated on the order of 10.0 KHz. Objectives of this paper are to show accurate simulation of nozzle flow itself and to demonstrate the jet flow structure when the jet interacts with a wall at a close range.

• Environmental Sciences Bulletin of The Korean Environmental Sciences Society
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• 제3권2호
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• pp.113-119
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• 1999

The quality of the effluent from an activated sludge aeration tank can deteriorate when the substrate removal rate decreases due to an abrupt reduction in the DO concentration, which is affected by such operating conditions as the loading rate, temperature, wastewater composition, and so on. In this research, a DO control system that includes a PI (proportional-integral) controller/Hiraoka controller was developed and applied to a pilot-scale activated sludge process, then its acceptability was estimated. The applicability of the respiration rate to DO control was also estimated. The respiration rate indicated a variety of input organic loading rates, which is the main disturbance to the DO concentration in an aeration tank. When the influent concentration incrementally decreased and increased between CODcr 1,000 mg/l and 100 mg/l, the control system with a PI controller exhibited a good llperformance-the average DO concentrations were 2.00$\pm$0.14 mg/l and 1.88$\pm$0.15 mg/l (set value was 2.0 mg/l), respectively, and the settling time was just 10 minites. When the control system was operated for 4 days, the DO concentration was 1.99$\pm$0.18 mg/l and 32.6% of the air flowrate was saved. However, the fluctuations in the respiration rates and air flowrates were severe, which could be harmful to the stability of the biomass and mechanical stability of the blower. A possible approach to solve this problem may be the simultaneous control of the loading rate and DO concentration.

• 한국환경과학회지
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• 제25권3호
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• pp.361-371
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• 2016

Ministry of Environment has been operating water quality monitoring network in order to obtain the basic data for the water environment policies and comprehensively understand the water quality status of public water bodies such as rivers and lakes. The observed water quality data is very important to analyze by applying statistical methods because there are seasonal fluctuations. Typically, monthly water quality data has to analyze that the transition comprise a periodicity since the change has the periodicity according to the change of seasons. In this study, trends, SOM and RDA analysis were performed at the Mulgeum station using water quality data for temperature, BOD, COD, pH, SS, T-N, T-P, Chl-a and Colon-bacterium observed from 1989 to 2013 in the Nakdong River. As a result of trends, SOM and RDA, the Mulgeum station was found that the water quality is improved, but caution is required in order to ensure safe water supply because concentrations in water quality were higher in the early spring(1~3 month) the most.

• 한국환경과학회지
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• 제26권2호
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• pp.221-230
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• 2017

To determine the effect of air pollution reduction policies, the long-term trend of air pollutants should be analyzed. Kolmogorov-Zurbenko (KZ) filter is a low-pass filter, produced through repeated iterations of a moving average to separate each variable into its temporal components. The moving average for a KZ(m, p) filter is calculated by a filter with window length m and p iterations. The output of the first pass subsequently becomes the input for the next pass. Adjusting the window length and the number of iterations makes it possible to control the filtering of different scales of motion. To break down the daily mean $PM_{10}$ into individual time components, we assume that the original time series comprises of a long-term trend, seasonal variation, and a short-term component. The short-term component is attributable to weather and short-term fluctuations in precursor emissions, while the seasonal component is a result of changes in the solar angle. The long-term trend results from changes in overall emissions, pollutant transport, climate, policy and/or economics. The long-term trend of the daily mean $PM_{10}$ decreased sharply from $59.6ug/m^3$ in 2002 to $44.6ug/m^3$ in 2015. This suggests that there was a long-term downward trend since 2005. The difference between the unadjusted and meteorologically adjusted long-term $PM_{10}$ is small. Therefore, we can conclude that $PM_{10}$ is unaffected by the meteorological variables (total insolation, daily mean temperature, daily mean relative humidity, daily mean wind speed, and daily mean local atmospheric pressure) in Busan.

• 한국응용곤충학회지
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• 제34권4호
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• pp.321-327
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• 1995

밀양에서 월동하는 애멸구 개체군의 월동생태에 관한 정확한 자료를 얻고자 본 연구를 수행하였다. 월동 애멸구의 영구성 비율은 12월상순에 4령충(약 60%)이 가장 많았으며, 다음은 3령충(약 30%), 5령충(약 6%), 2령충(약 3.4%), 성충 및 1령충 순서였다. 이러한 월동 애멸구의 영구성 비율과 순서는 채집시기에 따라 변화였으며, 그 결과 3월상순에는 5령충(47-50%)이 가장 많았고, 다음은 4령충(44-46%)이었으며, 4월상순에는 성충이 약 75-81%를 차지하였다. 월동 애멸구의 발육상황을 수치로 나타낸 평균령기는 월동기간동안 계속하여 증가하는 경향이었으며, 채집년도간 평균령기의 차이는 연도간 월동기간중의 온도차이에 따른 월동 애멸구 영구성 비율의 차이에 따른 결과였다. 애멸구의 체중도 월동기간동안 계속하여 증가하였다. 월동기간동안 애멸구으 채집밀도는 보리밭보다 휴반에서 월등하게 높았다. 월동기간동안 애멸구 약충기생봉에 의한 기생률은 평균 약 21%였다.