• 한국전산유체공학회지
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• 제12권4호
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• pp.74-84
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• 2007

The flowfield characteristics in a straight rectangular channel have been investigated through a numerical model to analyze the regenerative cooling system that is used in rocket engine cooling. The supercritical hydrogen coolant introduces strong property variations that have a major influence on the developing flow and heat transfer characteristics. Of particular interest is the improved understanding of the physical characteristics of such flows through parametric studies. The approach used is a numerical solution of the full Navier-Stokes equations in the three dimensional form including the arbitrary equation of state and property variations. The present study compares constant and variable property solutions for both laminar and turbulent flow. For laminar flow, the variation of aspect ratio is examined, while for turbulent flow, the effects of variation of channel length and Reynolds number are discussed.

• 디지털융복합연구
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• 제16권5호
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• pp.231-237
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• 2018

논문에서는 길쌈 부호화 시공간 블록 부호 시스템의 오류 성능에 대한 채널 변화 및 채널 추정 오류의 영향에 대해 살펴보았다. 본 논문에서는 직교 방식의 Alamouti 시공간 블록 부호 및 준직교 방식의 Jafarkhani 시공간 블록 부호의 두 가지 시공간 블록 부호 방식을 고려하여, 길쌈 부호화 시공간 블록 부호 시스템들에서 채널 변화 및 추정 오류 정도에 따른 오류 성능 변화를 모의실험을 통해 분석하였다. 분석 결과 채널 변화 속도가 느린 경우에는 시간 다이버시티 효과로 인해 채널 변화가 없는 상황 대비 검출 방식에 관계없이 오류 성능이 향상되나, 채널 변화 속도가 빠른 경우에는 검출 과정에서의 오류로 인해 특히 준직교 Jafarkhani 적용 시스템에서 STBC 검출 사용 시 ZF 및 MMSE 검출 사용 시와 달리 큰 폭의 성능 열화가 발생함을 관측하였다. 또한 채널 추정 오류 증가 시에는 검출 기법 및 채널 변화 속도에 관계없이 큰 폭의 성능 열화가 발생함을 확인하였다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2007년도 학술발표회 논문집
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• pp.253-257
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• 2007

Channel-aquifer interaction is one of the key hydrological processes that determine water flows in the stream/river channel. Field measurements of channel-aquifer interaction, however, is very difficult and costly, particularly when one intends to understand its variations across a catchment for a long period. Hydrological simulations using a catchment model are a relatively easier and cheaper alternative provided the model structure is appropriate for describing channel-aquifer interaction. In this study, a catchment model called CAMEL (Chemicals from Agricultural Management and Erosion Losses) is used for estimating channel-aquifer interaction over time and space. CAMEL is a distributed catchment model to simulate transformation and transport processes of sediment and pollutants as well as water flows at the catchment scale. In the model, a catchment is represented using a network of square columns each of which is comprised of various storages of water. CAMEL explicitly simulates both surface and subsurface processes including channel-aquifer interaction. This paper presents an application study results of CAMEL for the Tarland Burn Catchment, a small (catchment area $52\;km^2$) rural catchment in Scotland, UK, demonstrating some of the channel-aquifer interaction dynamics across the catchment during a 2-year period.

• 물과 미래
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• 제28권3호
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• pp.197-204
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• 1995

인구의 도시집중으로 인하여 유역의 유출용적이 증대하며 이로 인한 합류부의 수위상승으로 내수배제가 불가능하게 되어 침수피해가 발생하고 있다. 본 실험연구에서는 소유역 하천에서 우수거의 합류로 인한 본류하천의 흐름변화를 실험하였으며, 하천의 수위상승을 소하천(본류)의 유량과 경사, 우수거(지류)의 유량과 경사 및 합류각에 따른 본류의 수위상승을 분석하였다. 실험결과 본류하천의 경사에 대해서는 경사가 급할수록 수심비가 증대하는 것으로 나타났으며, 본류의 유량은 적을수록, 지류의 유량은 많을 수록 수심비는 크게 나타났다. 합류각에 대해서는 합류각이 작을수록 수심비가 작은값을 나타내고 있다. 이와 같이 도시 소하천의 합류시 수심비의 상승영향을 보면 합류각, 지류유량 및 본류유량 등의 순으로 상승영향이 밀접하게 나타났다.

• Fisheries and Aquatic Sciences
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• 제1권1호
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• pp.113-121
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• 1998

A relationship between sea level variations in the Korea Strait (the western and the eastern channels) and the Tokara Strait in the Kuroshio region is examined using daily-mean sea level data from 1966 to 1986. The seasonal variation of the sea level difference (SLD) between Izuhara and Pusan (the western channel) is most periodic: the positive anomalies appear from summer to autumn, and the negative anomalies from winter to spring year to year, whereas SLDs neither between Hakata and Izuhara (the eastern channel) nor between Naze and Nishinoomote (the Tokara Strait) show such a periodic variation. Much similarity has been found between SLDs in the eastern channel and the Tokara Strait, and in particular they were closely correlated in a special event of the Kuroshio region, such as a large meander of the Kuroshio. This paper shows that the periodic seasonal variation of the SLDs in the western channel should be less related to the Kuroshio region. This result also implies that the variation of SLD in the western channel is largely influenced by local factors, such as the bottom cold water in the western channel in summer, rather than from the Kuroshio region.

• Ocean and Polar Research
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• 제25권spc3호
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• pp.423-426
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• 2003

The seawater exchange breakwater equipped with an oscillating water channel and water transmitting pipes has a very spectacular function that seawater supply can be greatly increased due to the upsurge of the water surface inside the channel at resonance condition which can be reached when the incident wave period becomes close to the natural period of the channel. The variations of the water level and period inside the channel are very important factors in enhancing the efficiency of sea water exchange, especially when designing the breakwater cross-section in shallow water zone which requires longer resonance period with the elongated horizontal projection of the channel. In the present study, a hydraulic experiment was performed varying the length of the oscillating channel, and the resonance periods and water surface variations are analyzed in terms of water transmission through the pipes.

• IEIE Transactions on Smart Processing and Computing
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• 제6권4호
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• pp.276-280
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• 2017

This paper presents computationally efficient image compression for wireless transmission of high-definition video, to adaptively utilize available channel bandwidth and improve image quality. The method indirectly predicts an unknown available channel bandwidth by monitoring encoder buffer status, and adaptively controls a quantization parameter to fully utilize the bandwidth. Experimental results show that the proposed method is robust to variations in channel bandwidth.

• Journal of Communications and Networks
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• 제15권4호
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• pp.338-351
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• 2013

Multiple-input multiple-output (MIMO) communication may provide high spectral efficiency through the deployment of a very large number of antenna elements at the base stations. The gains from massive MIMO communication come from the use of multi-user MIMO on the uplink and downlink, but with a large excess of antennas at the base station compared to the number of served users. Initial work on massive MIMO did not fully address several practical issues associated with its deployment. This paper considers the impact of channel aging on the performance of massive MIMO systems. The effects of channel variation are characterized as a function of different system parameters assuming a simple model for the channel time variations at the transmitter. Channel prediction is proposed to overcome channel aging effects. The analytical results on aging show how capacity is lost due to time variation in the channel. Numerical results in a multicell network show that massive MIMO works even with some channel variation and that channel prediction could partially overcome channel aging effects.

• 한국정보통신학회논문지
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• 제16권4호
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• pp.785-792
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• 2012

본 연구에서는 고속 및 저전력 스위칭 소자 응용을 위하여 n-채널 무접합 및 반전모드 MuGFET 와 p-채널 무접합 및 축적모드 MuGFET의 기판전압에 따른 전류-전압 특성을 측정하고 비교 분석하였다. 기판전압에 따른 문턱전압과 포화 드레인 전류 변화로부터 n-채널 소자에서는 반전모드 소자가 무접합 소자보다 변화량이 크며 p-채널 소자에서는 무접합 소자가 축적모드 소자보다 변화량이 큰 것을 알 수 있었다. 전달컨덕턴스 변화는 n-채널 소자보다 p-채널 소자의 변화량이 큰 것을 알 수 있었다. 그리고 subthreshold swing 특성으로부터 n-채널 소자와 p-채널 무접합 소자는 기판전압 변화에 따라 S값의 변화가 거의 없지만 p-채널 축적모드 소자는 기판전압이 양의 방향으로 증가할 때 S 값이 증가하는 것으로 관측되었다. 기판전압을 이용한 고속 및 저전력 스위칭 소자 응용 측면에서는 n-채널 소자에서는 반전모드 소자가 p-채널 소자에서는 무접합 소자가 더 좋은 특성을 보였다.

• 한국지구과학회지
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• 제27권7호
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• pp.757-767
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• 2006

Alluvial-plain deposits in the southeastern part of the Eumsung Basin (Cretaceous) are characterized by coarse-grained channel fills encased in purple siltstone beds. It represents distinct channel geometry, infill organization, and variations in facies distribution. The directions of paleocurrent, sedimentary facies changes, and channel-fill geometry can be used to reconstruct a channel network in the alluvial system developed along the southeastern margin of the basin. The channel-fill facies represent downstream changes: 1) down-sizing and well-sorting in clast and martix of channel fills and 2) internal organization of scour fill or gravel lag and overlying cross-stratified, planar-stratified beds. These findings suggest multiple stages of channel-filling processes according to flooding and subsequent stream flows. In the small-scale pull-apart Eumsung Basin (${\sim}7{\times}33km^2$ in area), vertical-stacked alluvial architecture of the coarse-grained channel fills encased in purple siltstone is expected to result from episodic channel shifting under a rapidly subsiding setting.