• 한국소음진동공학회논문집
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• 제19권2호
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• pp.184-191
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• 2009

This study examined small-size specimen's effectiveness that is used to evaluate floor impact sound performance. Floor impact sound level of small-size specimen is higher than full-size. This is due to excessive impact power of Bang machine. Impact hammer that has small impact power relatively can solve this problem. But, according to the size of specimen, mode shape and frequency that influence to structural borne sound is changed. Slab mode of full-size specimen was changed to frequency design of resilient materials. But in case of small-size specimen, there is no change of vibration mode by resilient materials change, Vibration mode of small-size specimen is the same. Therefore, it is not proper that use small-size specimen in floor impact sound estimation.

• 한국광학회지
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• 제15권1호
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• pp.22-27
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• 2004

본 논문에서는 광도파로와 광섬유사이에서 광손실을 줄이기 위한 모드 크기 변환기를 설계하였다. 설계된 모드 크기 변환기는 주기적으로 분리된 테이퍼 광도파로로 구성된 모드 크기 변환기이며, 공정상의 적용이 용이한 수평 테이퍼 구조를 선택하였다. 높이와 폭이 3$\mu\textrm{m}$${\times}$3$\mu\textrm{m}$이며 1.5%실리카 광도파로의 경우 파장이 1550nm 파장에서 최적의 모드 크기 변환기 설계 파라미터는 테이퍼 영역의 길이가 500$\mu\textrm{m}$이고, 분리된 광도파로의 길이는 5$\mu\textrm{m}$이며, 주기의 Duty-Cycle은 0.95, 광도파로와 광섬유의 접속면에서의 폭은 1.3$\mu\textrm{m}$이였다. 이 때 결합손실은 0.33㏈/point로 광섬유와 광도파로를 직접 연결할 때 보다 1.27 ㏈/point가 감소하였다.

• 한국입자에어로졸학회지
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• 제9권1호
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• pp.7-21
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• 2013

Twelve-hour size-resolved atmospheric aerosols were measured to determine size distributions of water-soluble organic carbon(WSOC) during daytime and nighttime, and to investigate sources and formation pathways of WSOC in individual particle size classes. Mass, WSOC, ${NO_3}^-$, $K^+$, and $Cl^-$ at day and night showed mostly bimodal size distributions, peaking at the size range of $0.32-0.55{\mu}m$(condensation mode) and $3.1-6.2{\mu}m$(coarse mode), respectively, with a predominant condensation mode and a minor coarse mode. While ${NH_4}^+$ and ${SO_4}^{2-}$ showed unimodal size distributions which peaked between 0.32 and $0.55{\mu}m$. WSOC was enriched into nuclei mode particles(< $0.1{\mu}m$) based on the WSOC-to-mass and WSOC-to-water soluble species ratios. The sources and formation mechanisms of WSOC were inferred in reference to the size distribution characteristics of inorganic species(${SO_4}^{2-}$, ${NO_3}^-$, $K^+$, $Ca^{2+}$, $Na^+$, and $Cl^-$) and carbon monoxide. Nuclei mode WSOC was likely associated with primary combustion sources during daytime and nighttime. Among significant sources contributing to the condensation mode WSOC were homogeneous gas-phase oxidation of VOCs, primary combustion emissions, and fresh(or slightly aged) biomass burning aerosols. The droplet mode WSOC could be attributed to aqueous oxidation of VOCs in clouds, cloud-processed biomass burning aerosols, and small contributions from primary combustion sources. From the correlations between WSOC and soil-related particles, and between WSOC and sea-salt particles, it is suggested that the coarse mode WSOC during daytime is likely to condense on the soil-related particles($K^+$ and $Ca^{2+}$), while the WSOC in the coarse fraction during nighttime is likely associated with the sea-salt particles($Na^+$).

• 대한전자공학회:학술대회논문집
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• 대한전자공학회 2008년도 하계종합학술대회
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• pp.793-794
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• 2008

The block size of intra prediction mode can differentiate the texture area from the homogeneous area of image. This information can be used to enhance the size resolution of image. Specifically, in this paper, we apply the bicubic interpolation or the bilinear interpolation adaptively selected the intra prediction mode of the H.264 compression.

• 한국통신학회:학술대회논문집
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• 한국통신학회 1984년도 추계학술발표회논문집
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• pp.22-24
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• 1984

The mode spot size is a fundamental parameter of a single mode optical fibre which determines especially the spilces and the microbending loss. The spot-size measurement is recognised to be a useful mean to define the cut-off wavelength of single-mode fibres, ESI parameters and to predict the modal dispersion. To determine the ESI parameters, this paper is based on the use of a Ronchi ruling.

• 한국대기환경학회지
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• 제10권2호
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• pp.124-129
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• 1994

Aerosol size distribution was determined using Anderson sampler for the anions( sulfate nitrate and chloride ) and TSP. Ionic species concentration and size distribution have been investigated in the daytime and nightime individually. Size classified samples were extracted with distilled water and analyzed for C $l^{[-10]}$ , N $O_3$$^{[-10]}$ and S $O_4$$^{2-}$, by ion chromatography. The size distribution of these ions and TSP was analyzed to investigate the seasonal and diurnal variation of concentrations as follows: (1)Size distribution of TSP showed bi- modal type in the daytime, but indicated tri-mode distribution in the nightime without any seasonal variation. (2)Sulfate concentrations were higher in fine- mode both in the daytime and nightime but fraction of sulfate was higher in coarse-mode during the Yellow Sand Period. (3)Nitrate and Chloride ions are dominant in fine-mode in winter while dominant in coarse-mode in the summer.

• 대한전자공학회논문지SD
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• 제41권12호
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• pp.43-49
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• 2004

본 논문에서는 슈퍼하이델타(Super High Delta) 실리카 광도파로와 단일 모드 광섬유 사이의 결합손실을 줄이기 위한 모드 크기 변환기를 설계하였다. 새로운 모드 크기 변환기는 물리적 크기를 최소화하기 위해 주기적으로 분리된 테이퍼 도파로를 사용하였으며 공정을 간단히 하기 위해 수평형 테이퍼를 사용하였다. 또한 결합손실을 개선하기 위해 모드 크기 변환기 주변에 트렌치 구조를 삽입하였다. 최적의 모드 크기 변환기 설계에서 결합손실은 트렌치 구조가 삽입되지 않은 경우는 0.33dB/point 이며 트렌치가 삽입된 경우는 0.2dB/point이다.

• 대한전자공학회논문지SD
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• 제41권4호
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• pp.83-90
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• 2004

본 논문은 메모리 크기의 제약을 많이 받는 내장형 마이크로프로세서의 문제를 해결하기 위해 32-bit 명령어와 24-bit, 16-bit 명령어를 혼합 사용하여 3가지 명령어 모드를 갖는 새로운 명령어 셋(X32V ISA)을 제안하였으며, 이를 기반으로 32-bit 5 stage pipeline RISC 마이크로프로세서를 설계하였다. 이를 검증하기 위해서 X32V ISA 전용 시뮬레이터를 이용하여 멀티미디어 프로그램의 프로그램 코드 사이즈를 산출하였다. 그 결과로 Light mode와 Ultra light mode는 Default mode에 비해 각각 최소 8%, 27%의 프로그램 코드 사이즈 감소를 확인하였으며, Xilinx FPGA를 이용하여 33MHz 동작 환경에서 X32V ISA의 모든 명령어 수행을 검증하였다.

• 환경위생공학
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• 제9권2호
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• pp.24-31
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• 1994

Aerosol size distribution were determined in Seoul by Anderson sampler from October 1989 to September 1991 for the major ionic species(SO$_{4}$$^{2-}$, NO$_{3}$$^{-}$, Cl$^{-}$, Na$^{+}$, Na$^{+}$, K$^{+}$, Ca$^{2+}$ and Mg$^{2+}$) and TSP( Total Suspended Particles ). The seasonal variations in concentrations and size distribution have been investigated. The size distributions of TSP and each of ionic species were bimodal throughout the year. The size distribution of these ions were divided as follows; (1) fine- mode dominant for SO$_{4}$$^{2-}$ and N%'. (2) coarse- mode dominant for NO$_{3}$$^{-}$, Cl$^{-}$, Ca$^{2+}$ and Mg$^{2+}$. (3) both- mode dominant for TSP.

• 한국입자에어로졸학회지
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• 제17권3호
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• pp.43-54
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• 2021

Size distributions of atmospheric particulate matter (PM) and its water-soluble organic and inorganic components were measured between January and February 2021 at an urban site in Gwangju in order to identify the major factors that determine their size distributions. Their size distributions during the study period were mainly divided into two groups. In the first group, PM, NO₃^-, SO₄^2-, NH₄⁺ and water-soluble organic carbon (WSOC) exhibited bi-modal size distributions with a dominant condensation mode at a particle size of 0.32 ㎛. This group was dominated by local production of secondary water-soluble components under atmospheric stagnation and low relative humidity (RH) conditions, rather than long-range transportation of aerosol particles from China. On the other hand, in the second group, they showed tri-modal size distributions with a very pronounced droplet mode at a diameter of 1.0 ㎛. These size distributions were attributable to the local generation and accumulation of secondary aerosol particles under atmospheric conditions such as atmospheric stagnation and high RH, and an increase in the influx of atmospheric aerosol particles by long-distance transportation abroad. Contributions of droplet mode NO₃^-, SO₄^2-, NH₄⁺ and WSOC to fine particles in the second group were significantly higher than those in the first group period. However, their condensation mode contributions were about two-fold higher in the first group than in the second group. The significant difference in the size distribution of the accumulation mode of the WSOC and secondary ionic components between the two groups was due to the influx of aerosol particles with a long residence time by long-distance transport from China and local weather conditions (e.g., RH).