• 한국항공우주학회지
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• 제30권2호
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• pp.91-97
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• 2002

응축영역 에너지 방정식과 기체 영역에 관한 화염모델을 사용하여 연소실 압력 강하에 반응하는 고체 추진제의 동적 소화 특성을 살펴보았다. 화염모델에서는 기체가 반응영역을 통과하는데 걸리는 시간(잔존시간, r,)이 동적 소화 특성을 결정하는 중요한 인자임을 확인하였다. 본 논문에서는 r,을 확산과 화학반응 시간의 다양한 조합으로 가정하였으며 이를 이용하여 동적 소화 특성을 살펴보았다. 또한 연소실 부피의 유한함에 따른 압력변화와 이에 대한 연소의 동적 반응도 살펴보았다. 동적 소화는 화학반응 시간보다는 확산 시간에 의하여 커다란 영향을 받는 현상임을 확인하였다. 그리고 연소실 부피가 유한한 경우가 무한한 경우보다 복잡한 동적 소화 특성을 보여주었다.

• 대한기계학회논문집B
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• 제32권5호
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• pp.351-358
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• 2008

Extinction characteristics of hydrogen-air diffusion flames at various pressures are investigated numerically by adopting counterflow flame configuration as a model flamelet. Especially, effect of radiative heat loss on flame extinction is emphasized. Only gas-phase radiation is considered here and it is assumed that $H_2O$ is the only radiating species. Radiation term depends on flame thickness, temperature, $H_2O$ concentration, and pressure. From the calculated flame structures at various pressures, flame thickness decreases with pressure, but its gradient decreases at high pressure. Flame temperature and mole fraction of $H_2O$ increase slightly with pressure. Accordingly, as pressure increases, radiative heat loss becomes dominant. When radiative heat loss is considered, radiation-induced extinction is observed at low strain rate in addition to transport-induced extinction. As pressure increases, flammable region, where flame is sustained, shifts to the high-temperature region and then, shrunk to the point on the coordinate plane of flame temperature and strain rate. The present numerical results show that radiative heat loss can reduce the operating range of a combustor significantly.

• 한국항행학회논문지
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• 제11권2호
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• pp.187-195
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• 2007

본 논문에서는 광섬유에서의 색 분산과 비선형효과에 의해 발생되는 신호왜곡을 보상하기 위해 광 위상 공액기를 채택한 1,000km의 전송거리를 갖는 WDM 시스템에서 모든 WDM 채널을 효과적으로 보상할 수 있는 광 위상 공액기의 최적 위치 값과 광섬유 구간의 최적분산 계수 값들을 WDM 채널 신호의 소광비에 따라 도출하였다. WDM 시스템은 40Gbps의 채널 전송률을 갖는 16개 채널로 구성되고 각 채널은 5dB, 10dB, 20dB의 소광비를 갖는 NRZ 형식으로 가정하였다. 모든 WDM 채널들의 효과적 보상을 위해서는 고려한 두 파라미터들 중 하나만을 가지고도 충분하다는 것을 확인하였다. 그리고 이들 각각의 최적 값들은 WDM 채널 신호의 소광비에 의존하지 않는다는 것을 확인하였다. 즉 소광비에 상관없이 광 위상 공액기를 496km에 위치시키거나 두 광섬유 구간의 분산 계수 차이를 0.055ps/nm/km로 하면 모든 WDM 채널들을 2dB 이내의 전력 패널티로 양호하게 전송할 수 있는 것을 확인하였다.

• 한국항행학회논문지
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• 제11권4호
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• pp.437-446
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• 2007

$16{\times}40$ Gb/s WDM 전송 시스템에서 비트 에러율 (BER ; bit error rate)의 효과적 보상과 융통적 WDM 전송 시스템의 설계를 위한 광 위상 공액기 (OPC ; optical phase conjugator)의 최적 위치 값과 광섬유 구간의 최적 분산 계수 값들을 10 dB와 20 dB의 소광비(ER ; extinction ratio)에 따라 도출하였다. 모든 WDM 채널들의 BER의 효과적 보상을 위한 최적 파라미터 값들은 기존 연구들에서 살펴보았던 변조 파형 형식, 전송 채널수와 마찬가지로 신호의 소광비에 의존하는 것을 확인하였다. 그리고 최적 파라미터 값들을 이용한 융통적인 WDM 시스템 설계가 ER이 10 dB인 경우보다 ER이 20 dB인 경우가 더욱 유리한 것을 확인하였다.

• 전기학회논문지
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• 제61권7호
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• pp.937-943
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• 2012

Most of faults occurred in transmission lines are single-phase to ground faults and transient faults. Single-phase auto reclosing is an appropriate scheme to maintain the system stability and restore the system effectively when those faults are occurred. In single-phase auto reclosing scheme, the secondary arc is generated after faulted phase is tripped to eliminate the fault and it is sustained by the capacitive and inductive coupling to the healthy phases. It is important to reclose the faulted phase after fully extinction of secondary arc because of the damage applied to system. Therefore, it is necessary to research on the detection of secondary arc extinction to ensure high success rate of reclosing. In this step, firstly, the accurate modelling of secondary arc should be performed. In this paper, the modelling of secondary arc is performed by using EMTP-RV and the simulation results show that the implemented model is correct and effective.

• Journal of Electrical Engineering and Technology
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• 제11권5호
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• pp.1179-1189
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• 2016

• Asian Journal of Atmospheric Environment
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• 제4권1호
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• pp.55-61
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• 2010

The sensitivity of aerosol light extinction coefficient to the aerosol chemical composition change is estimated by (1) calculating the aerosol water content and chemical concentrations by a gas/particle equilibrium model and (2) calculating the aerosol light extinction coefficient by a Mie theory based optical model. The major chemical species are total (gas and particle phase) sulfuric acid, total nitric acid, and total ammonia which are based on the measurement data at Seoul and Gosan. At Seoul, since there were enough ammonia to neutralize both total sulfuric acid and total nitric acid, the dry ionic concentration is most sensitive to the variation of the total nitric acid level, while the total mass concentration (ionic concentration plus water content) and thus, the aerosol light extinction coefficient are primarily determined by the total sulfuric acid. At Gosan, since the concentration of ambient sulfuric acid was the highest among the inorganic species, sulfate salts determined aerosol hygroscopicity. Thus, both ionic and total mass concentration, and resultant aerosol light extinction coefficient are primarily determined by the sulfuric acid level.

• Nano
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• 제13권12호
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• pp.1850137.1-1850137.9
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• 2018

A series of silica surface-capped with hexamethyldisilazane (denoted as $H-SiO_2$) were prepared by liquid-phase in-situ surface-modification method. The as-obtained $H-SiO_2$ was incorporated into acrylic amino (AA) baking paint to obtain AA/$H-SiO_2$ composite extinction paints and/or coatings. $N_2$ adsorption-desorption tests were conducted to determine the specific surface area as well as pore size and pore volume of $H-SiO_2$. Moreover, the effects of $H-SiO_2$ matting agents on the physical properties of AA paint as well as the gloss and transmittance of AA-based composite extinction coatings were investigated. Results show that $H-SiO_2$ matting agents possess a large specific surface area and pore volume than previously reported silica obtained by liquid-phase method. Besides, they have better dispersibility in AA baking paint than the unmodified silica. Particularly, $H-SiO_2$ with a silica particle size of $6.7{\mu}m$ and the dosage of 4% (mass fraction) provides an extinction rate of 95.2% and a transmittance of 79.3% for the AA-based composite extinction coating, showing advantages over OK520, a conventional silica matting agent. Along with the increase in the silica particle size, $H-SiO_2$ matting agents cause a certain degree of increase in the viscosity of AA paint as well as a noticeable decrease in the gloss of the AA-based composite extinction coating, but they have insignificant effects on the hardness and adhesion to substrate of the AA-based composite coatings. This means that $H-SiO_2$ matting agents could be well applicable to preparing low-viscosity and low-gloss AA-based matte coatings.

• 한국광학회지
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• 제12권3호
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• pp.212-218
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• 2001

직접변조한 2.5Gbit/s 송신기에 있어서 DFB-LD에 인가되는 바이어스 전류에 따른 출력 광신호의 소광비와 처핑의 관계를 살펴보았고, 이상분산 영역 전송실험을 통행 변조된 광신호가 8-10dB의 소광비를 가질경우(바이어스 전류가 발진임계전류의 1.5배에서 1.8배) 소광비와 처핑으로 인한 총 전송 패널티가 최소가 됨을 알 수 있었다. 또한 240km 이상분산 영역 전송실험을 통해 직접변조된 광신호의 소광비와 SPM의 상관관계도 분석하였다. SPM을 고려할 경우 본 실험과 같은 구성에서 전송거리가 200km 미만인 경우는 10.2dB의 소광비에서 200km 이상인 경우는 8.4dB의 소광비에서 가장 좋은 수신감도를 얻을 수 있었다.

• 한국지구과학회지
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• 제23권1호
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• pp.59-71
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• 2002

Theoretical models of radiative transfer are developed to simulate the 85 GHz brightness temperature (T85) observed by the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) radiometer as a function of rain rate. These simulations are performed separately over regions of the convective and stratiform rain. TRMM Precipitation Radar (PR) observations are utilized to construct vertical profiles of hydrometeors in the regions. For a given rain rate, the extinction in 85 GHz due to hydrometeors above the freezing level is found to be relatively weak in the convective regions compared to that in the stratiform. The hydrometeor profile above the freezing level responsible for the weak extinction in convective regions is inferred from theoretical considerations to contain two layers: 1) a mixed (or mixed-phase) layer of 2 km thickness with mixed-phase particles, liquid drops and graupel above the freezing level, and 2) a layer of graupel extending from the top of the mixed layer to the cloud top. Strong extinction in the stratiform regions is inferred to result from slowly-falling, low-density ice aggregates (snow) above the freezing level. These theoretical results are consistent with the T85 measured by TMI, and with the rain rate deduced from PR for the convective and stratiform rain regions. On the basis of this study, the accuracy of the rain rate sensed by TMI is inferred to depend critically on the specification of the convective or stratiform nature of the rain.