• Korean Journal of Poultry Science
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• v.16 no.3
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• pp.139-147
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• 1989

An experiment was carried out to investigate the effects of dietary energy levels and protein feeding systems on the performance of laying hens. Total 960 White Leghorn pullets were alloted in 10 treatments consisted of 1 metabolizable energy levels (2,900 and 2,600 kcal/kg) and 5 protein feeding systems (17-17-15%, 17-15-13%, 15-15-15%15-15-13% and 15-13-13% in phase I, II and/or III, respectively) from 20 to 80 weeks or age. As metabolizable energy level increased from 2,600 to 2.900 kcal/kg of diet, e99 Productions in phase I and II were not different but decreased in phase III. Egg weight was not different, but daily feed intake and viability were decreased in phase I, II and III. Feed conversions in phase I and II were improved but in phase III it was not different. On the other hand, as dietary Protein level increased from 13 to 17%, egg production and egg weight were increased, and feed conversion was improved , but daily feed intake and viability were not affected by the dietary protein level. For the laying period of 60 weeks, metabolizable energy level of 2,600 kcal/kg of diet and 17, 15 and 13% dietary protein levels in phase I, II and III, respectively, were considered to be adequate to support the optimum productivity.

• Journal of IKEEE
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• v.2 no.2 s.3
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• pp.194-199
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• 1998

In the atmospheric wireless optical communication system, the low power transmission can be accomplished by the high directivity of laser beam. But, the transmitted optical signal undergoes the serious influences by the atmospheric effects like absorption, scattering, and turbulence because the transmission channel is the atmospheric space. In this paper, therefore, we obtain the link equation for an atmospheric wireless optical LOS communication link under the atmospheric effects and find the repeaterless transmission length to estimate the system performance through the computer simulation. From the results of the computer simulation, we present the transmission length that is possible to transmit without a repeater at given data rates and know that data rate is decreased rapidly when the transmission length is increased slightly at given bit error rate.

• The KIPS Transactions:PartA
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• v.16A no.5
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• pp.307-318
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• 2009

Modeling and rendering of atmospheric phenomena such as clouds is one of most difficult research themes in the field of computer graphics, mainly due to its complexity, huge volume, ubiquitousness, etc. In this paper, we represent a system for real-time modeling and rendering of clouds, mainly aiming at the computer games and flight simulation applications. Our implementation generates various kinds of clouds including cirrus, stratus, and cumulus, through intuitive real-timeuser interactions. Then, additional details are automatically attached to them, using our own methods based on meta-balls or hierarchical spherical particles. After processing multiple scattering and anisotropic scattering, resulting particles are rendered into billboards, to finally achieve real-time processing.

• Journal of the Korea Computer Industry Society
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• v.6 no.2
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• pp.259-264
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• 2005

This paper have derived an expression(the fringe modle is used) for the photocurrelation-correlation function for a cross-beam laser velocimeter, taking into account the effects of atmospheric turbulence on the amplitude and phase of the incident beams. the result, as long as the atmospheric disturbances do not greatly damp out sinusoidal variations of the photocurrent-correlation function in the time it takes a particle to travel the fringe-separation distance, the disturbances do not hinder the determination of the velocity of the partides from the correlation funtion.(the scattering particles are assumed to have a well-defined V).

• Journal of Korean Society for Atmospheric Environment
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• v.4 no.2
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• pp.28-37
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• 1988

Light scattering coefficient of visible light by atmospheric aerosol over the size range 0.01-10$\mu$m is determined from scattering efficiency and aerosol size distribution. Aerosol number distribution as a function of particle diameter dN/dlog D decreases rapidly as increasing particle size. Distribution of scattering coefficient d$\sigma_s/dlog$ D is mostly accumulated in diameter 0.1-2.0 $\mu$m showing its maximum in the vicinity of 0.6$\mu$m. This means that the visible light in the atmosphere is mainly scattered by these particles. Diurnal variation of scattering coefficient $\sigma_s$ appears its maximum in the morning, while minimum in the afternoon which agrees with the aerosol number distribution in the size range 0.1-2.0 $\mu$m.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
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• 2014.10a
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• pp.360-361
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• 2014

등명기 및 통신, 해상관측장비 등에 필요한 충분한 소비전력 확보와 축전지 장수명을 위한 목적이다. 태양광 발전 시스템에서 태양광은 자동차의 연료와 같다. 따라서 기존 육상 태양광 시스템에서 발전하는 성과와 해상 등부표 위 한정된 면적 공간에서 발전 가능성을 정확히 분석하기 위해 연료에 대한 고도의 지식과 미래 신뢰성을 확보하는 것이 필수적이다. 해상 해수면 등부표 위에 탑재되는 독립형 태양광발전 시스템의 성과를 예견하는 데에는 일사량의 변화가 가장 큰 불확실성을 나타낸다. 그 이유는 대기와 해상기후의 상태에 따라 태양광이 대기를 통과하면서 전달 산란 채광 흡수되는 작용이 다르고 불안정한 대기와 해상의 롤링과 피칭으로 수광(채광) 조건이 변화무쌍하기 때문이다. 등부표의 한정된 면적과 공간에서 전력공급을 할 수 있는 한계가 있다. 정보통신기술(ICT) 발달에 따른 소비전력 연동시스템 증가로 인해 절대적인 전력량 확보가 필요하다.

• Korean Journal of Remote Sensing
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• v.35 no.6_1
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• pp.1011-1030
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• 2019

Remote sensing sensors used in satellites or aircrafts measure electromagnetic waves passing through the earth's atmosphere, and thus the information on the surface of the earth is affected as it is absorbed or scattered by the earth's atmosphere. Although satellites have different wavelength ranges and resolutions depending on the purpose of onboard sensors, in general, atmospheric correction must be made to remove the influence of the atmosphere in order to accurately measure the spectral signal of an object on the earth's surface. The purpose of atmospheric correction is to remove the atmospheric effect from remote sensing images to determine surface reflectivity values and to derive physical parameters of the surface. Until recently, atmospheric correction algorithms have evolved from image-based empirical methods or indirect methods using in-situ observation data to direct methods that numerically interpret more complex radiative transfer processes. This study analyzes the research records of atmospheric correction algorithms developed over the past 40 years, systematically establishes the current state of atmospheric correction technology and the results of major atmospheric correction algorithms and presents the current status and research trends of related technologies.

• Korean Journal of Remote Sensing
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• v.13 no.2
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• pp.99-120
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• 1997

Solar radiation is scattered and absorbed atmospheric compositions in the atmosphere before it reaches the surface and, then after reflected at the surface, until it reaches the satellite sensor. Therefore, consideration of the radiative transfer through the atmosphere is essential for the quantitave analysis of the satellite sensed data, specially at shortwave region. This study examined a feasibility of using radiative transfer code for estimating the atmospheric effects on satellite remote sensing data. To do this, the flux simulated by LOWTRAN7 is compared with CAGEX data in shortwave region. The CAGEX (CERES/ARM/GEWEX Experiment) data provides a dataset of (1) atmospheric soundings, aerosol optical depth and albedo, (2) ARM(Aerosol Radiation Measurement) radiation flux measured by pyrgeometers, pyrheliometer and shadow pyranometer and (3) broadband shortwave flux simulated by Fu-Liou's radiative transfer code. To simulate aerosol effect using the radiative transfer model, the aerosol optical characteristics were extracted from observed aerosol column optical depth, Spinhirne's experimental vertical distribution of scattering coefficient and D'Almeida's statistical atmospheric aerosols radiative characteristics. Simulation of LOWTRAN7 are performed on 31 sample of completely clear days. LOWTRAN's result and CAGEX data are compared on upward, downward direct, downward diffuse solar flux at the surface and upward solar flux at the top of the atmosphere(TOA). The standard errors in LOWTRAN7 simulation of the above components are within 5% except for the downward diffuse solar flux at the surface(6.9%). The results show that a large part of error in LOWTRAN7 flux simulation appeared in the diffuse component due to scattering mainly by atmispheric aerosol. For improving the accuracy of radiative transfer simulation by model, there is a need to provide better information about the radiative charateristrics of atmospheric aerosols.

• The Journal of the Korea institute of electronic communication sciences
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• v.18 no.6
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• pp.1049-1056
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• 2023

The height of the atmospheric boundary layer indicates the peak developed when turbulence is generated by mixing heat and water vapor, and is generally determined through thermodynamic methods. Wind profilers produce atmospheric information from the scattering of signals sent into the atmosphere. A method for making the spectrum of turbulent components, turbulent kinetic energy dissipation rate, and refractive index structure coefficient was presented to determine the atmospheric boundary layer depth. Compared with the vertical distribution characteristics of potential temperature and specific humidity based on radiosonde data, the determination method of the atmospheric boundary layer height from wind profiler output was evaluated as very useful.

• Proceedings of the Korean Vacuum Society Conference
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• 2013.08a
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• pp.175-175
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• 2013

현재 치과에서 상용되는 치아미백법은 과산화수소와 레이저를 사용하여 의사가 직접 치료를 하고 있다 [1]. 단기간에 높은 미백효과를 얻기 위해, 고농도의 과산화수소를 이용하게 되는데, 이는 암 또는 심장병 등을 유발시키는 원인이 될수 있음으로 인체에 매우 유해하다 [3,4]. 우리는 식품의약품안정청에서 규제하고 있는, 카바마이드 퍼옥사이드(15%)를 사용하였다. 카마바이드 퍼옥사이드(15%), 수증기, 저온 대기압 플라즈마 제트를 사용하여 미백효과를 관찰하였다. 기체 유량은 1,000 sccm 이며, 공기와 질소를 사용하였다. 미백효과를 보기 위한 대상으로는 우치(牛齒)를 사용하였으며, 플라즈마를 처리하여 미백효과를 관찰하였다. 실험 대조시료군으로는 카바마이드 퍼옥사이드(15%)와 수증기(0.4%)를 첨가한 다음, 공기 플라즈마와 질소 플라즈마를 조사하여 비교해보았다. 수증기를 첨가한 이유는 활성산소의 농도를 높이기 위함이며, 탁월한 미백효과를 얻을 수 있다. 실험을 통하여 우치에 카바마이드 퍼옥사이드(15%)와 수증기(0.4%)를 처리한 경우 플라즈마의 미백효과가 탁월함을 보였다. 이때 CIE색좌표 ($L^*a^*b^*$)에서 명도도가 높아짐을 보았다. 미백효과에 대한 측정은 측색분광기(cm-3500d)를 이용하였다. 라만은 빛이 어떤 매질을 통과할 때 빛의 파장을 변화시켜 빛의 일부는 진행방향에서 이탈해 다른방향으로지행하는 현상을 산란이라고 한다. 이를 이용하여 빛의 파장을 변화시키는 현상을 라만산란이라고 한다. 이것을 이용하여 같은 우치의 표면을 플라즈마 처리 전 후를 라만을 통해 측정하였다. 대기압 저온 플라즈마에서 발생되는 ROS는 미백효과에 큰 영향을 미친다. 모든 실험의 플라즈마 처리시간은 최대 20분까지로 하였다.