• 열처리공학회지
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• 제26권3호
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• pp.105-112
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• 2013

The microstructural changes of Fe-20Mn-12Cr-1Cu alloy have been studied during high temperature gas nitriding (HTGN) at the range of $1000^{\circ}C{\sim}1150^{\circ}C$ in an atmosphere of nitrogen gas. The mixed microstructure of austenite and ${\varepsilon}$-martensite of as-received alloy was changed to austenite single phase after HTGN treatment at the nitrogen-permeated surface layer, however the interior region that was not affected nitrogen permeation remained the structure of austenite and ${\varepsilon}$-martensite. With raising the HTGN treatment temperature, the concentration and permeation depth of nitrogen, which is known as the austenite stabilizing element, were increased. Accordingly, the depth of austenite single phase region was increased. The outmost surface of HTGN treated alloy at $1000^{\circ}C$ appeared Cr nitride. And this was in good agreement with the thermodynamically calculated phase diagram. The grain growth was delayed after HTGN treatment temperature ranges of $1000^{\circ}C{\sim}1100^{\circ}C$ due to the grain boundary precipitates. For the HTGN treatment temperature of $1150^{\circ}C$, the fine grain region was shown at the near surface due to the grain boundary precipitates, however, owing to the depletion of grain boundary precipitates, coarse grain was appeared at the depth far from the surface. This depletion may come from the strong affinity between nitrogen and substitutional element of Al and Ti leading the diffusion of these elements from interior to surface. Because of the nitrogen dissolution at the nitrogen-permeated surface layer by HTGN treatment, the surface hardness was increased above 150 Hv compared to the interior region that was consisted with the mixed microstructure of austenite and ${\varepsilon}$-martensite.

• 한국수산과학회지
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• 제46권2호
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• pp.201-215
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• 2013

The characteristics of the oceanographic environment in the Aleutian Basin of the Bering Sea during spring in 1996, 1997, and 1999 were clarified. An investigation of the water properties revealed five basic layers in the Bering Sea during spring: (1) a surface layer of warm and low-salinity water induced by solar heating, (2) a subsurface layer of cold and low-salinity water propagated slowly by heat from the surface layer, (3) a thermocline layer where salinity was constant but temperature sharply decreased, (4) a temperature inversion layer, and (5) a deep layer with a gradual decrease in temperature and increase in salinity toward the bottom. The ranges of water temperature and salinity were $1.8-5.5^{\circ}C$ and 31.81-34.08 in 1996, $1.5-7.2^{\circ}C$ and 31.9-34.06 in 1997, and $0.5-5.6^{\circ}C$ and 32.0-34.11 in 1999, respectively. The water temperature of the surface layer was approximately $1.6^{\circ}C$ higher in 1997 than in 1996 and 1999. The lowest temperature at a depth of 100-150 m was about $1^{\circ}C$ lower in 1999 than in 1996 and 1997. Nutrient levels (nitrate, phosphate, and silicate) contributing to the control of the growth of phytoplankton were higher in the Aleutian Basin than in the eastern continental shelf and Bogoslof Island area. This was closely associated with the phytoplankton distribution. Nutrient concentrations were lowest at a depth of 25 m. The high primary production at that depth was confirmed from the vertical distribution of chlorophyll a. Chlorophyll a levels were above $4.0{\mu}L^{-1}$ in some areas in 1996 and 1999, but below $2.0{\mu}L^{-1}$ in most areas in 1997. Zooplankton density was about three times higher in 1999 than in 1997.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2007년도 하계학술대회 논문집 Vol.8
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• pp.111-111
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• 2007

Further scaling the semiconductor devices down to low dozens of nanometer needs the extremely shallow depth in junction and the intentional counter-doping in the silicon gate. Conventional ion beam ion implantation has some disadvantages and limitations for the future applications. In order to solve them, therefore, plasma source ion implantation technique has been considered as a promising new method for the high throughputs at low energy and the fabrication of the ultra-shallow junctions. In this paper, we study about the effects of DC bias and base pressure as a process parameter. The diluted mixture gas (5% $PH_3/H_2$) was used as a precursor source and chamber is used for vacuum pressure conditions. After ion doping into the Si wafer(100), the samples were annealed via rapid thermal annealing, of which annealed temperature ranges above the $950^{\circ}C$. The junction depth, calculated at dose level of $1{\times}10^{18}/cm^3$, was measured by secondary ion mass spectroscopy(SIMS) and sheet resistance by contact and non-contact mode. Surface morphology of samples was analyzed by scanning electron microscopy. As a result, we could accomplish the process conditions better than in advance.

• Ocean and Polar Research
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• 제43권4호
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• pp.255-267
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• 2021

To understand the composition and community changes of benthic species by water depth (5 m, 20 m, 30 m) in the cage facilities, net substrate made of fish cages were installed at intervals of 2 months from March to September 2019, which is the main period of sessile organism recruitment. Water temperature and salinity varied in the ranges of 1~5℃ and 1~4 mg/L at 5 m from June to August, respectively, and less difference was observed according to water depth in other investigation periods. A total of 37 benthic animals were recruited, and Kamptozoa unid., Caprella scaura and Jassa slatteryi were verified during the entire study period. Mytilus galloprovincialis, a Mediterranean mussel, showed seasonality dominant only from spring to early summer (March to July). The community structure classified by temporal and spatial factors, and Bugula neritina, Kamptozoa unid., and Sertularella sp. contributed to the formation of the community. The depth of 5 m was exposed to environmental changes in water temperature and salinity temporally, so there was a seasonal variation in the composition of the sessile organism, but at depths of 20 m and 30 m, there was less significant environmental change and it showed relatively stable than 5 m.

• 생태와환경
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• 제54권4호
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• pp.384-389
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• 2021

본 연구는 2020년 10월 23일에 경기도 가평군 설악면에 위치한 청평호에서 수행되었으며, 어군탐지기를 이용해 획득한 자료를 기반으로 어류의 수평 및 수직 분포 패턴을 분석하였다. 어군탐지 조사가 수행된 구간의 총 수면적은 782,853 m²였으며, 수심(water depth, WD)이 10~12 m인 구간이 전체 수면적의 31.7%로 가장 넓게 분포하는 것으로 나타났다. 다양한 WD 구간별로 어류의 개체 밀도 산출 결과, 4~6 m 구간에서 0.98 개체/100 m²로 가장 높게 나타나, 수면적 대비 가장 많은 어류가 분포하는 것으로 확인되었다. Heat map 분석 결과 청평호 구간에서는 가평대교의 우안측에서 어류의 밀도가 가장 높게 나타났으며, 이러한 수평 분포 특성에서 특별한 경향성은 확인할 수 없었다. 어류의 수직분포 분석 결과, 어류가 관측된 수심(Fish depth, FD)이 6 m 이하인 경우가 전체 관측 대비 86.6%로 나타났다. 수심 대비 어류의 관측 수심(Relative height, RH) 분석 결과, 수심이 깊어질수록 어류가 상대적으로 표층에 분포하는 경향성을 확인할 수 있었다. 이와 관련해서는 수체의 수심별 수온 차이 등 다양한 원인이 있을 것으로 예상되며 추가적인 연구가 필요하다.

• 생태와환경
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• 제55권2호
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• pp.145-155
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• 2022

환경부 생물측정망 ('08~'18) 조사결과를 이용하여 저서성 대형무척추동물인 멸종위기 2급 염주알다슬기 (연체동물문, 복족강)의 물리적 서식생태 특성을 분석한 결과 다음과 같은 결론을 얻었다. 첫째, 적정 수심범위는 0.53~17.17 cm였으며, 중위값은 16.73 cm, 평균값은 21.32 cm, 최빈값은 5.17 cm였다. 둘째, 적정 유속범위는 48.40~81.03 cm s^-1였으며, 중위값은 65.23 cm s^-1, 평균값은 65.65 cm s^-1, 최빈값은 64.77 cm s^-1였다. 셋째, 적정하상입경 (𝜱_m) 범위는 -4.36~-2.26이었으며, 중위값은 -3.51, 평균값은 -3.63, 최빈값은 -3.24였다. 넷째, 염주 알다슬기의 하천 내 물리적 미소서식처 특성은 여울구간의 조립질 하상으로 확인되었다.

• 자원환경지질
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• 제35권6호
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• pp.491-508
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• 2002

화산 쇄설물을 모재로 하여 발달한 제주도 토양은 많은 양의 비정질 물질을 포함하는 Andisols이 대부분을 차지하고 있으나, 강수량이 상대적으로 적은 제주도 서부 지역에서는 Andisols의 특징을 보이지 않는 토양이 발달하고 있다. 서부 해안에 접해 있는 당산봉에는 이와 같이 층상규산염광물이 우세한 non-Andic토양이 나타난다 본 연구는 당산봉 토양에 나타나는 층상 규산염 광물의 조성 및 풍화에 따른 이들 점토광물의 진화 과정을 밝히는데 그 목적이 있다. 연구 지역 토양은 A층과 C층이 발달해 있으며 B층은 나타나지 않는다. pH(($H_{2}0$)는 일반적인 화산 쇄설물 기원 토양(<6.0)보다 높은 6.6-7.3으로 하부로 갈수록 증가한다. pH(NaF)는 9.49-9.81로 비정질 물질의 존재를 지시하는 9.4보다 높게 나타나며, 선택적 용해법을 이용하여 구한 비정질 물질의 양은 0.55-1.02 wt%로 매우 낮다. 유기물 함량은 표토에서 2.00wt%로 Andisol에 비해 매우 낮다. 주 구성 광물은 석영, 장석, 감람석이며, 점토 입도를 구성하는 층상규산염 광물은 입도와 풍화정도에 따라 차이를 보인다. <0.2$\mu\textrm{m}$ 입도의 주 구성 점토 광물은 스멕타이트, 카올리나이트/스멕타이트 혼합층광물, 일라이트이다. 카올리나이트/스리타이트 혼합층광물의 카올리나이트의 비율은 85-86%로 깊이에 관계없이 일정하다. 풍화가 진행될수록 스멕타이트의 함량은 감소하며, 카올리나이트/스멕타이트 혼합층광물의 함량은 증가한다. 2-0.2$\mu\textrm{m}$ 입도의 주 구성 점토 광물은 질석, 스멕타이트, 일라이트, 카올리나이트, 녹니석이다. 녹니석은 표토에서만 나타나며, 하부에서는 나타나지 않는다. 녹니석/스멕타이트 혼합층광물 내의 녹니석 함량은 59-70%이며 풍화가 진행될수록 양은 증가한다. 그러나 풍화의 정도가 낮은 제일 하부에서는 녹니석/스멕타이드 혼합층광물이 나타나지 않는다. 질석과 스멕타이트의 일부는 층간이 hydroxy-Al/Mg/Fe으로 채워진 hydroxy-interlayered vermiculite(HIV)와 hydroxy-interlayered smectite(HIS)의 형태로 나타난다. HIV는 A층과 C층 모두에서 나타나며, 층간 물질은 hydroxy-Fe/Al이다. 층간의 hydroxy-Fe/Al의 양은 표토로 갈수록 증가하며, HIV를 형성하는 질석의 층 전하도 표토에서 높게 나타난다. HIS는 C층에서만 나타나며, 층간 물질은 hydroxy-Mg/Al이며, hydroxy-Mg가 우세하다. 본 지역의 토양에서는 풍화가 진행될수록 스멕타이트는 카올리나이트와 질석, HIS로 진화하였으며, 질석은 HIV를 거쳐 녹니석으로 진화하였을 것으로 사료된다.

• 한국패류학회지
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• 제23권2호
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• pp.155-164
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• 2007

A new species, Arca koumaci Lutaenko et Maestrati n. sp. (Bivalvia: Arcidae), is described from New Caledonia. The species is characterized by the small size, the convex shell with a strong posterior umbonal ridge covered by spikes, the widely curved ventral margin, and presence of cancellate sculpture and convergent marginal teeth. Presence of spikes on the posterior ridge is a unique morphological feature recorded for the first time in the genus. It is proposed that the only subgenus, namely Pliocene A. (Arcoptera) Heilprin, 1887, apart from nominative, can be recognized in the genus. Three morphological types are distinguished within the genus based on shell shape and sculpture. Bathymetric analysis shows that representatives of Arca inhabit water depths down to 175 m, and more than half of Recent species were found below 50 m. Types of A. bouvieri P. Fischer, 1874, Arca boucardi Jousseaume, 1894, Arca avellana Lamarck, 1819, and Arca retusa Lamarck, 1819 are illustrated.

• 천문학회보
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• 제39권2호
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• pp.96.2-96.2
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• 2014

Using solar occultation data obtained by Cassini/Visual Infrared Mapping Spectrometer (VIMS), we were able to retrieve the 1 - 5 mm optical-depth spectra of the Titanian haze, for which only selected wavelength and altitudinal ranges were previously analyzed. We found that the gross 1 - 5 mm shapes of the retrieved haze spectra are significantly different from the spectra of tholin samples in the literature. We also derived the vertical variation of the spectral structure of the $3.3-3.4{\mu}m$ absorption feature of the Titan haze from the VIMS data recorded between 250 and 700 km altitude. We found a marked change between 480 and 580 km in the relative amplitudes of the 3.33 and $3.38{\mu}m$ features which are characteristic of aromatic (double C=Cchains or rings) or aliphatic (single C-C chains) structural groups, respectively. Dicussions on this spectral and altitudinal variation will be presented.

• 수산해양교육연구
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• 제29권1호
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• pp.297-305
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• 2017

This study was analysed the species composition of demersal fishes caught by a bottom trawler, KAYA, in the winter season during 4 years and the study area was the eastern fishing ground in depth of about 110m, 40 miles eastward from Jeju Island, Korea. A total of 54 species were collected, including 40 species of Pises, 9 species of Mollusks, 5 species of Crustaces. The number of individuals and biomass of unit area was $7,978ind/km^2$ and $1,800kg/km^2$, respectively. The dominant species in winter season were Dentex tumifrons, Carangoides equula, Callanthias japonicus, Thamnaconus modestus and Pagrus major. And these also were caught every year. The ranges of the diversity index(H') were 1.97 to 2.40, the richness(R) 1.91~4.59, the evenness(E) 0.54~0.83 and the dominance(D) 0.42~0.61.