• 한국산림과학회지
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• 제90권6호
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• pp.683-691
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• 2001

산림의 수원함양기능 지표로서 표층토양에서의 조공극률(組孔隙率)(pF2.7)에 영향하는 인자를 밝히기 위해 1995년 3월부터 10월까지 전국의 활엽수림 표본조사구를 대상으로 입지, 토양, 임분환경인자 등 총 24종에 대하여 spss/pc+를 이용하여 상관 분석하였다. 표층토양에서의 조공극률에 영향을 미치는 인자는 B층 토양에서의 조공극률, 하층식생 피복도, 표층 토양의 유기물함량비, F층 두께 등 4개 인자가 유의한 정(正)의 상관관계를, 표층토양의 견밀도, 10cm 깊이의 토양견밀도가 각각 5%, 1% 수준에서 유의한 부(負)의 상관관계를 나타내었다. Stepwise를 이용한 다중회귀분석결과 산림의 수원함양기능 증대에 영향하는 표층토양에서의 조공극률에 영향하는 인자는 B층 토양에서의 조공극률, 유기물함량비 등 2개 인자이었다.

• Journal of the korean society of oceanography
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• 제31권4호
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• pp.196-206
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• 1996

Vertical profiles of the chlorophyll ${\alpha}$, phytoplankton abundance, nutrients and sigma-t were compared with the vertical distribution of phytoplankton species in conjunction with $^{14}$C primary production in the Southern Waters of the East Sea, Korea. In the upper mixed layer the water column was only weakly stratified and ambient nitrogenic nutrient concentrations were markedly depleted. Dissolved silicate seemed to be another limiting nutrient in the surface layer. The occupation of different water depths by several dominant diatom species was well explained by the degree of silicification of each cell and the silicate concentration of ambient seawater. Subsurface chlorophyll maxima were continuously observed in the lower parts of the euphotic layer and the depth coincided with nutricline, supporting our view that chlorophyll maximum was sustained partially by enhancement of in situ growth of phytoplankton and partially by increase of cellular chlorophyll content. The persistence of chlorophyll maximum layer was attributed to the physiological adaptation of the phytoplankters to low light intensities and to the utilization of regenerated nutrients. Integrated water column production of organic matter by photosynthesis appeared to be better related to phytoplankton cell division than to the cell growth in terms of biosynthesis of pigments and other intracellular components.

• 한국농공학회논문집
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• 제48권5호
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• pp.73-80
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• 2006

The mono-layer cover system is composed of soils only as a filling material and various plants are planted on the surface to control the water balance in the cover system. In this paper, the mono-layer cover system was considered as an alternative landfill final cover system and developed a model that could utilize industrial by-product (especially, coal ash & phosphogypsum) as additive filling materials. The mixture of granite soil, coal ash, and phosphogypsum was placed as a cover material in a box constructed with cement. Laboratory tests were carried out to investigate the environmental effect on the utilization of coal ash & phosphogypsum and to determine the mxing ratio of each materials. In the leaching test, all materials showed lower heavy metal concentration than the threshold values of regulation. The optimum mixing ratio of materials which was applied to field model test was determined to soil (4) : coal ash (1) : phosphogypsum (1) on the volume base. Field model tests were continued from February to July, 2004 in the soil box that was constructed with cement block. It was verified that coal ash and phospogypsum mixed with soil was to be safe environmentally and the water balance of mono-layer cover system was reasonable.

• 한국분말재료학회지
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• 제15권2호
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• pp.101-106
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• 2008

The objective of the present study is to investigate the increase in the functional characteristics of a substrate by the formation of a thin coating layer. Thin coating layers of $Ti_5Si_3$ have high potential because $Ti_5Si_3$ exhibits high hardness. Shock induced reaction synthesis is an attractive fabrication technique to synthesize uniform coating layer by controlling the shock wave. Ti and Si powders to form $Ti_5Si_3$ using shock induced reaction synthesis, were mixed using high-energy ball mill into small scale. The positive effect of this technique is highly functional coating layer on the substrate due to ultra fine substructure, which improves the bonding strength. These materials are in great demand as heat resisting, structural and corrosion resistant materials. Thin $Ti_5Si_3$ coating layer was successfully recovered and showed high Vickers' hardness (Hv=1183). Characterization studies on microstructure revealed a fairly uniform distribution of powders with good interfacial integrity between the powders and the substrate.

• 열처리공학회지
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• 제15권5호
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• pp.213-218
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• 2002

In order to develop the economic and environmental water-soluble black coloring agent, some adequate chemical mixtures were mixed and this solution was applied to coat quenched and tempered 51B20 steel bolt. Some basic properties of the solution and characteristics of the coated film in addition to the corrosion resistance were investigated. The developed 100 kg of water-soluble black coloring agent solution was a chemical mixture consisted of 10 kg of aqueous coloring agent, 40 kg of surface active agent, 0.3 kg of anti-foam agent and $50{\ell}$ of water. The coated film of the bolt was composed of hard layer of about $2{\mu}m$ and the disbondable soft layer of about $4{\mu}m$ above the hard layer. Many surface active agents peaks and a few hydrophilic peaks were observed in the coated film. Surface roughness value of the coated bolt was lower than that of the non-coated bolt. Corrosion resistance of the coated bolt considerably improved and also relatively showed a good polarization resistance at test condition of $40^{\circ}C$ colorizing temperature and 5% the solution concentration in 3% NaCl anodic polarization test. Initial appearance time of the surface rust was greatly retarded owing to the coated film in salt spray test.

• 생태와환경
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• 제36권3호통권104호
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• pp.277-285
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• 2003

주암호의 수직 수평적 수온 구조의 계절변화를 이해하기 위하여, 2000년 3월부터, 2001년 5월까지 수온을 관측하였다. 관측된 수온자료와 기상자료를 이용하여, 수온 변화에 직접적인 영향을 미치는 열수지를 정량적으로 계산하였다. 겨울에는 호수가 대기로 열을 빼앗겼는데, 12월에 최대 109.45w/$m^2$의 열을 잃었다. 표층수의냉각으로 대류가 일어나, 수직적으로 균일한 수온을 보였다. 수평적으로는 수온의 차이를 보여, 호수로 물이 유입되는 상류 쪽은 수온 $3^{\circ}C$, 댐 부근에서는 약 $5^{\circ}C$의 물이 존재했다. 봄이 되면서 주로 표층을 통해 얻는 열로 인해 표층 수온이 상승하여, 수직적인 온도 차이를 보였다. 여름에는 표층을 통해 유입되는 열의 양이 증가하여, 7월에 최대 101.95w/$m^2$였다. 표층 가열과 함께, 상류로부터 크게 증가한 유량으로 인해 주암호 내부의 열이 증가하여 8월에는 표층 수온이 최대 $29^{\circ}C$ 이상이 되었다. 그러나 저층수는 약 $7^{\circ}C$였다. 가을이 되면서 표층을 통해 열을 잃게 되어 표층수의 수온이 낮아졌고, 표면혼합층은 두꺼워졌다. 기온이 더 낮아지는 겨울에는 표층을 통한 열 손실이 더 증가하여 2월에 수온이 가장 낮아졌고, 수직적으로 균일한 수온 특성을 보였다. 이러한 수온구조는 3월까지 지속되었다.

• Journal of the korean society of oceanography
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• 제32권3호
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• pp.93-102
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• 1997

Coastal circulations during the (surface condition of an) idealized cold-air outbreak are numerically investigated with two-dimensional, non-hydrostatic model in which a constant bottom-slope exists. The atmospheric forcing during a cold-air outbreak is incorporated as the surface cooling and the wind stress. When the offshore angle of the wind-stress vector, defined as the angle measured from the alongshore axis, is smaller than 45 degrees, a strong downwelling circulation develops near the coast. A sharp density front, which separates the vertically homogeneous region from the offshore stratified region, is formed near the coast and propagates offshore with time. Onshore side of the density front, small-scale circulation cells which are aligned in the direction perpendicular to the bottom begin to develop as the near-coast homogeneous region broadens. The surface cooling enhances greatly the development of the surface mixed layer by convective motions due to hydrostatic instability. The convective motions reach far below the hydrostatically unstable layer which is attached to the surface. The small-scale circulation cells are appreciably modified by the convetion cell and the density front develops far offshore compared to the case of no surface cooling. As to the effect of the bottom slope, the offshore distance of the density front increases (decreases) as the bottom slope decreases (increases), which results from the fact that the onshore volume-transport (Ekman transport) of the low-density upper seawater remains almost constant when the wind-stress is maintained constant. It is shown that the bottom slope is an essential factor for the formation of both the density front and the alongshore current when the surface cooling is the only forcing.

• 한국표면공학회지
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• 제54권5호
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• pp.238-247
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• 2021

PEO (plasma electrolytic oxidation) was applied to modify the surface of AZ31 magnesium alloy in this study. The mixed solution of sodium hydroxide (NaOH) and sodium silicate (Na₂SiO₃) was used as the electrolyte, and 0 - 0.05 g/L of Ca-GP (Glycerol Phosphate Calcium salt) was added in the electrolyte as an additive. PEO treatment was conducted at a current density of 30mA/cm² for 5 minutes using a DC power supply. The surface properties were identified by SEM, XRD and surface roughness analyses, and the corrosion resistance was evaluated by potentiodynamic polarization and immersion tests. In addition, the biocompatibility was evaluated by immersion test in SBF solution. As the concentration of Ca-GP was increased, the surface morphology was denser and more uniform, and the amount of Ca and the thickness of oxide layer increased. Only Mg peak was observed in XRD analysis due to very thin oxide layer. The corrosion resistance of PEO-treated samples increased with the concentration of Ca-GP in comparision with the untreated sample. In particular, the highest corrosion resistance was identified at the group of 0.04g Ca-GP through potentiodynamic polarization and immersion tests in saline solution (0.9 wt.%NaCl). During the immersion in saline solution, pH rapidly increased at the beginning of immersion period due to rapid corrosion, and then increase rate of pH decreased. However, the pH value in the SBF temporarily increased from 7.4 to 8.5 during the day, then decreased due to the inhibition of corrosion with HA(hydroxyapatite) formation.

• 보존과학회지
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• 제26권3호
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• pp.247-258
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• 2010

무령왕릉 출토 목관재 6점의 칠도막 편에 대하여 광학 현미경 관찰, 적외선 분광분석 및 SEM-EDS 분석을 실시하였다. 목관재에 도장된 옻칠 기법은 크게 네 가지 방법으로 분류되었다. 목재 표면에 그을음(미립자의 흑색 안료)을 혼합한 흑색 안료층이 밑층으로 존재하면서 그 위로 칠이 1회(그룹 II) 도장된 것과 3회(그룹 I) 도장된 것, 흑색 안료층이 존재하지 않으면서 칠 도장이 1회(그룹 IV)와 2회(그룹 III) 되어있는 것으로 분류되었다. 이는 목관의 제작기법과 부재의 결구 방법을 밝히는데 좋은 정보가 될 것으로 생각된다. 적외선 분광분석을 통해 무령왕릉 칠도막은 자외선에 의한 열화 요인이 적은 것으로 나타났다. 이는 이동이 어려운 목관의 크기와 무덤이라는 매장 환경 등에 기인한 결과로 보인다. 또한 SEM-EDS 분석결과 현재까지 고대 칠분석에서 보고된 바 없는 Ca, Fe, Cu의 성분이 확인되어 의미가 있다.

• 한국해양학회지
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• 제30권1호
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• pp.39-56
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• 1995

1992년 3월부터 6월까지 속초앞 해역에서 동일한 난수성 소용돌이가 계속 관측되 었다. 이 난수성 소용돌이는 1991년에 형성되어 속초앞 해역에서 월동을 한 후 1992년 4~6월에는 약간 북상하였다. 3월에 관측되었을 때 소용돌이의 크기는 직경이 약 160km, 수심 약 330 m 였고, 상층 내부에 약 1$0^{\circ}C$, 34.2 psu의 균질층(혼합층)이 최대 폭 약 130 km , 수심 약 230 m 로 존재하고 있었으나 6월에는 약간 축소되었다. 낭수 성 소용돌이 표층의 최대유속은 약 65cm/s였으며, 수심 200 m에서도 약 20cm/s 이상의 큰 유속을 갖고 있었다. 이러한 유속구조는 대체로 지형류 평형을 잘 유지하고 있었으 나, 6월에는 약간의 차이가 나타났다. 또한 동한난류의 표층유속은 50~70 cm/s로 나 타나 소용돌이의 북향류와 비슷했으며, 동한난류는 주로 수심 200m 이내의 상층에서만 존재했다.