• Proceedings of the Korea Water Resources Association Conference
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• 2018.05a
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• pp.451-451
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• 2018

박층류 자연정화공법은 수로의 폭을 넓히고 수심을 낮추어 박층류를 조성하고, 이를 이용하여 하천을 정화하는 공법이다. 박층류가 조성되면 낮은 수심에서 상대적으로 느린 유속 조건이 형성되며 이 때 박층부에 침전된 오염물질은 자갈층 표면에 형성된 생물막에 의해 산화 분해되어 제거된다. 박층류에 의한 오염물질 제거는 생물막의 형성, 생물 산화를 위한 용존산소량 등이 중요한 인자로 작용하며, 박층부를 조성하기 위해서는 수심 10 cm, 유속 30~50 cm/s 의 조건이 적절하다. 본 연구에서는 박층류에 의한 자연정화 성능을 평가하기 위하여 용인시 오산천 일부 구간 고수부지에 사석자갈을 이용한 박층류 자연정화공법이 적용된 차집수로를 설치하고, 오산천으로 유입되는 농수로의 물을 공급하여 오염물질의 농도 변화를 측정하였다. 측정된 항목은 T-N, T-P, COD, DO 등이며, 측정 결과 박층류 자연정화 수로를 유출부에서의 오염물질의 농도가 유입부에서보다 저감되는 것을 확인 할 수 있었다.

• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.418-418
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• 2019

낮은 수심, 저 유속의 수로 자갈층에 형성된 생물막을 이용하여 오염물질을 제거하는 박층류 자연정화기법의 효율적인 설계와 운영지침을 얻기 위하여 경기도 용인시 오산천 일부 구간에 현장적용을 위한 Test-bed를 조성하여 박층류 자연정화수로에서의 오염물질 제거 효율을 조사하였다. 오염물질은 녹조발생의 주요 원인물질인 인과 질소를 대상으로 하였고, 연구 조건은 일반적인 하천수에서의 오염 조건과 비점오염원으로부터 오염물질이 유입된 오염조건의 두 가지 조건을 가정하여 제거효율을 분석하였다. 분석 결과 모든 조건에서 박층류 수로를 통과할 때 오염물질의 농도가 감소함을 확인할 수 있었다. 특히 T-P 3 mg/L 이상, T-N 20 mg/L 이상의 고농도의 오염물질 유입시에 박층류 자연정화수로는 평상시보다 높은 60% 이상의 높은 제거 효율을 보였는데, 이를 통하여 박층류 자연정화기법이 고농도의 오염물질 제거에서도 제한적이지 않고 오히려 더 효과적임을 알 수 있었다.

• Proceedings of the Korea Water Resources Association Conference
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• 2006.05a
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• pp.618-622
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• 2006

충적 선상지(alluvial fan)는 자갈이나 유사가 과도하게 이송되어 부채모양으로 퇴적된 것으로서, 하류로 하폭이 증가하는 곳에서 형성된다. 충적 선상지는 유사가 이송하는 하천, 토석류, 그리고 박층류에 의해 형성된다. 토석류는 자갈에서부터 상대적으로 작은 진흙에 이르기까지 운반하는 밀도체이다. 충적하천의 흐름은 사행하천 및 망상하천에 이르는 흐름을 말하며, 박층류는 기본적으로 비하천 홍수류로서, 한 홍수사상에 대하여 선상지에서 부분분할로 형태로 흐른다. 본 연구에서는 충적 선상지에 대한 공학적인 문제를 검토하기 위한 예비연구로서 유입부에서 유사량의 유입조건에 따른 충적 선상지 델타의 형성 과정을 수치모형을 이용하여 파악하였다. 본 모형은 2차원 모형으로서, 이동경계좌표계를 사용하였고, 수치해석 기법으로는 CIP법이 이용되었으며, wet/dry를 고려하여, 유입 유사량의 변화에 따른 특성을 파악하였다. 초기에는 급격하게 선상지의 높이가 급격하게 증가하며, 유입 유사량의 증가에 따라 선상지의 높이가 평형상태를 유지하는 시간이 짧은 것을 보여주고 있다. 선상지의 면적은 유입 유사량이 적을 경우에는 평형상태가 지속적으로 유지되며, 완만한 증가 현상을 보여주었다. 유입 유사량이 증가할 경우에는 초기에 급격한 상승을 하다가 평형상태가 없이 지속적으로 상승하는 것을 보여주었다.

• Ecology and Resilient Infrastructure
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• v.6 no.4
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• pp.208-216
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• 2019

This study investigated design factors and removal efficiencies of a sheet flow channel as natural type water improvement techniques in the stream. The channel was designed considering the design factors, then constructed and monitored in the test bed of the Osan stream's floodplain. Water lever, velocity, discharge, T-P, T-N, and NO₃-N were monitored and the removal efficiencies and design formula were suggested. Overall efficiencies of T-P, T-N, and NO₃-N range 10 - 20%, and they show consistent relations with residence times. Minimum velocity requirement is also suggested from the relation of algae conditions and velocities. Relation formula of residence time and removal efficiency will be applicable in the design and operation process of a sheet flow channel.

• Journal of the Korean Society of Food Science and Nutrition
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• v.14 no.3
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• pp.284-288
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• 1985

To examine changes of antinutritional oligosaccharides, particularly raffinose and stachyose, of mung beans during germination, mung beans (Phaseolus aureus) were germinated at $25^{\circ}C$ for 7 days after soaking for 15 hr. The 80% ethanol extracts of mung bean sprouts were analyzed by Kieselgel thin-layer chromatography using a solvent system, ethylacetate, acetic acid and water (3:1:1, v/v). The moisture level was increased greatly after soaking followed by stabilization along to the 3rd day of germination. The level was increased slightly on the 4th day and thereafter stabilized. Antinutritional oligosaccharides, raffinose and stachyose was diminished significantly on a thin-layer chromatogricadtly on the 1st and 2nd day of germination, and disappeared almost thereafter.

• Journal of Biosystems Engineering
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• v.22 no.1
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• pp.11-20
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• 1997

Thin layer drying tests of short gain rough rice were conducted in an experimental dryer equiped with air conditioning unit. The drying tests were performed in triplicate at three air temperatures of $35^circ$, $45^circ$, $55^circ$, and three relative humidities of 40%, 55%, 70%, respectively. Previously published thin layer equations were reviewed and four different models widely used as thin layer drying equations for cereal grains were selected. The selected four models were Pages, simplified diffusion, Lewis's and Thompson's models. Experimental data were fitted to these equations using stepwise multiple regression analysis. The experimental constants involved in tow equations were represented as a function of temperature and relative humidity of drying air. The results of comparing coefficients of determination and root mean square errors of miosture ratio for low equations showed that Page's and Thompsons models were found to fit adequately to all drying test data with coefficient of determination of 0.99 or better and root mean square error of moisture ratio of 0.025.

• Journal of the Korean Chemical Society
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• v.19 no.1
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• pp.43-49
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• 1975

Small amounts of iodine compound in mineral oils are usually effective in reducing friction of metallic surfaces. Such improvement in frictional behaviour of wear characteristics was explained by the formation of a diiodide layer lattice structure at the metallic contact surfaces. The lubrication mechanism, however, by which organoiodine compounds functions is not based on the formation of such lattice structure iodide. It was tested and shown, by a static surface chemical reactivity test, wear and EP tests, and a hot wire method, that compound such as N-iodopyridinium dichlorodate, a double charge transfer complex, reacted with metals as an interhalogen compound and that the resultant thin film product reduced appreciable the friction of metallic surfaces, more than compounds such as methyl iodide, diiodomethane, and iodoform. These results suggest that the action of iodine, included in organoiodine compounds, is not that of a classical layer structure iodide, and an entirely new mechanism may be derived from a further studies on charge transfer complex compounds of organoiodine compounds.

• Journal of computational fluids engineering
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• v.4 no.2
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• pp.67-73
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• 1999

In the present paper, three types of the flow solvers were used to investigate the influence on the airfoil shape optimization. The adopted equations, i.e., Euler, thin layer Navier-Stokes and full Navier-Stokes ones. are solved using implicit LU-ADI decomposition scheme. The gradient projection method with the sinusoidal function was used as an optimization algorithm. The present numerical method was applied to the drag minimization problems under the initial shape of NACA0012 airfoils.

• 한국전산유체공학회:학술대회논문집
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• 1999.05a
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• pp.171-176
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• 1999

In the present paper, three types of the flow solvers were used to investigate the influence on the airfoil shape optimization. The adopted equations, i.e., Euler , thin layer Navier- Stokes and full Navier-Stokes ones, are solved using implicit LU-ADI decomposition scheme. The feasible direction algorithm with the sinusoidal function was used as an optimization algorithm. The present numerical method was applied to the drag minimization problems under the initial shape of NACA0012 airfoils.

• 한국해양학회지
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• v.22 no.1
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• pp.1-8
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• 1987

The Sinyangri Formation crops out in the vicinity of the Seongsan Peninsula, Cheju Island. Based on sedimentary structures, texture and composition, the lithologic sequence has been classified, in ascending stratigraphic order, into three lithofacies: parallel laminated sandstone facies (Facies I): conglomerate facies(Facies Il); and cross stratified sandstone facies (F acies Ill). Wedge-to-parallel, seaward-inclined in low angle less than 10$^{\circ}$lamina -sets with alternations of coarseand fine-grained sediments in the Facies I are the characteristic sedimentary structures in the foreshore depositional environment. Grains of this faciesare well sorted with good roundness compared with the other two facies, partly showing inverse graded bedding. Facies II,largely composed of claset-supported,very poorly-sorted conglomerates,does not pinch out but occurs continuously along the Sinyangri beach.Interstitial spaces between the clasts are mostly infilled with volcanic-ash and small amounts of well-rounded shell fragments.Maximum bed thickness as well as the size of imbedded basaltic clasts decreases to the south(toward Sinyangri). Large clasts with parallel lamination originated from the underlying Facies i,are generally elongated parallel to the bedding plane and display no systematic horizontal variations in size indicative of in-situ clasts.In view of the facts above it seems that large gravels from the basaltic rocks are transgressive lag conglomerates which are partly affected by the combination of longshore currents and propagating wave.Local occurrence of cross-strata dipping toward the south in the upper part of Facies IIreinforces the evidence of the action of longshore currents. Facies IIIis characterized by bidirectional trough cross-starifiction and wave ripples associated with the upper shoreface(surfzone) environments.In summary,the Sinyangri Formation represents the depositional environments of foreshore to upper shoreface truncated by disconformity between Facies Iand II.