• Title/Summary/Keyword: 열속

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Inplementation of a Hydrogen Leakage Simulator with HyRAM+ (HyRAM+를 이용한 수소 누출 시뮬레이터 구현)

  • Sung-Ho Hwang
    • The Journal of the Convergence on Culture Technology
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    • v.10 no.1
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    • pp.551-557
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    • 2024
  • Hydrogen is a renewable energy source with various characteristics such as clean, carbon-free and high-energy, and is internationally recognized as a "future energy". With the rapid development of the hydrogen energy industry, more hydrogen infrastructure is needed to meet the demand for hydrogen. However, hydrogen infrastructure accidents have been occurring frequently, hindering the development of the hydrogen industry. HyRAM+, developed by Sandia National Laboratories, is a software toolkit that integrates data and methods related to hydrogen safety assessments for various storage applications, including hydrogen refueling stations. HyRAM+'s physics mode simulates hydrogen leak results depending on the hydrogen refueling station components, graphing gas plume dispersion, jet frame temperature and trajectory, and radiative heat flux. In this paper, hydrogen leakage data was extracted from a hydrogen refueling station in Samcheok, Gangwon-do, using HyRAM+ software. A hydrogen leakage simulator was developed using data extracted from HyRAM+. It was implemented as a dashboard that shows the data generated by the simulator using a database and Grafana.

한국주식시장(韓國株式市場)에 있어서 반전거래전략(反轉去來戰略) 계속거래전략(繼續去來戰略)의 경제적(經濟的) 유용성(有用性)에 관한 비교연구(比較硏究)

  • Kim, Tae-Hyeok;Eom, Cheol-Jun
    • The Korean Journal of Financial Management
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    • v.14 no.3
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    • pp.73-111
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    • 1997
  • 본 논문은 1980년${\sim}$1995년의 16년동안 한국주식시장에 있어서 주식수익률의 시계열자기상관성을 확인하는 행태적 측면과 투자수익률의 경제성을 파악하는 투자성과측면으로 구분된 단계적 검증을 실시함으로써 시장수익률을 평균적으로 초과할 수 있는 거래전략의 존재 및 그 초과수익률의 크기를 연구하였는바 이 연구에서 발견된 중요한 내용은 다음 다섯가지로 요약된다. 첫째, 한국주식시장에 있어서 거래전략의 개발가능성을 평가하기 위하여 특정시점을 기준으로 투자기간수익률과 분석기간수익률간의 시계열자기상관성을 검증한 행태적 측면의 실증결과에 의하면, 시계열속성을 나타내는 베타계수가 유의적인 양(+) 혹은 음(-)을 나타내기 때문에 특정시점 이전의 주식수익률은 목표투자기간동안에 투자할 대상을 선정하는데 중요한 정보원천이 될 수 있으며, 각 투자기간에 있어서 분석기간이 길어질수록 더욱더 유의적인 음(-)의 베타계수를 나타냄에 따라 계속거래전략보다 반전거래전략의 개발가능성이 높음을 알 수 있었다. 둘째, 주식시장에 전후수익률간의 시계열속성을 활용하여 투자를 하는 경우에 시장수익률을 평균적으로 초과할 수 있는 거래전략이 존재하는지를 파악하기 위하여 Loser포트폴리오와 Winner포트폴리오 초과수익률간의 차이로써 측정된 수익률을 이용한 실증결과에 의하면, 행태적 측면의 결과와 일관되게 분석기간수익률의 정보를 이용하여 투자기간에 투자하는 경우에 시장수익률을 평균적으로 초과하는 거래전략이 존재하고, 또한 Loser와 Winner포트폴리오의 수익률차이값 중 유의적인 음(-)의 값보다는 유의적인 양(+)의 값이 보다 많으므로 반전거래 전략의 활용가능성이 높음을 확인하였다. 셋째, 분석기간에 기초한 투자기간에 대한 투자전략상의 유용성을 최대한 발휘할 수 있는 거래전략과 투자기간을 검증한 Loser포트폴리오와 Winner포트폴리오의 수익률차이의 1개월 평균값에 의하면, 반전거래전략을 지지하는 경우가 계속거래전략의 경우보다 약 5배이상 높은 값을 실현하였고, 반전거래전략 중에서 분석기간 4개월에 대한 투자기간 24개월의 거래전략이 가장 높은 경제적 성과를 실현하였다. 넷째, 투자종목의 선택측면에서 각 거래전략의 실질적 유용성을 확인하기 위하여 Loser포트폴리오와 Winner포트폴리오의 고유한 속성을 검증한 결과에 의하면, 각 투자기간에 있어서 분석기간의 길이가 길어질수록 Winner포트폴리오는 유의적인 양(+)의 값을, Winner포트폴리오는 유의적인 음(-)의 값을 나타내었고, 특히 투자기간보다 분석기간의 기간길이가 긴 (투자기간<분석기간)에 이러한 경향이 더욱 뚜렷했다. 따라서, Loser포트폴리오를 매수보유하는 반전거래전략이 Winner포트폴리오를 매수보유하는 계속거래전략보다 적합한 전략임을 알 수 있었다. 다섯째, Loser포트폴리오와 Winner포트폴리오를 각각 투자대상종목으로써 매수보유한 반전거래전략과 계속거래 전략에 대한 유용성을 비교검증한 Loser포트폴리오와 Winner포트폴리오 각각의 1개월 평균초과수익률에 의하면, 반전거래전략의 Loser포트폴리오가 계속거래전략의 Winner포트폴리오보다 약 5배정도의 높은 1개월 평균초과수익률을 실현하였고, 반전거래전략의 유용성을 충분히 발휘하기 위하여 장단기의 투자기간을 설정할 경우에 6개월에서 36개월로 이동함에 따라 6개월부터 24개월까지는 초과수익률이 상승하지만, 이후로는 감소하므로, 반전거래전략을 활용하는 경우 주식투자기간은 24개월이하의 중단기가 적합함을 발견하였다. 이상의 행태적 측면과 투자성과측면의 실증결과를 통하여 한국주식시장에 있어서 시장수익률을 평균적으로 초과할 수 있는 거래전략은 존재하므로 이러한 전략을 개발 및 활용할 수 있으며, 특히, 한국주식시장에 적합한 거래전략은 반전거래전략이고, 이 전략의 유용성은 투자자가 설정한 투자기간보다 더욱 긴 분석기간의 주식가격정보에 의하여 최대한 발휘될 수 있음을 확인하였다.

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Case Study on Characteristics of Heat Flux Exchange between Atmosphere and Ocean in the case of cP Expansion accompanying Snowfall over the Adjacent Sea of Jeju Island (제주연안에 강설을 수반하는 대륙성 한기단 확장 시 대기와 해양간의 열교환 특성 사례 연구)

  • Kim Kyoung-Bo;Pang Ig-Chan;Kim Kil-Yap;Kim Dong-Ho;Lee Jimi
    • Journal of the Korean earth science society
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    • v.26 no.5
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    • pp.395-403
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    • 2005
  • This study is focused on the relationship between snowfall and the Bowen’s Ratio (sensible heat flux/latent heat flux) through calculation of heat exchange between air and sea for snowfall events in Jeju Island from 1993 to 2003. The four weather stations for this study are located at Jeju, Seoguipo, Seongsanpo and Gosan in Jeju Island. In order to improve the reliability of snowfall forecast, the Bowen’s Ratio for snowfall, which includes influences from the atmosphere such as wind, is compared with the temperature difference between air and sea for snowfall. As a results, in the case for fresh snowfall, the minimum temperature differences between air and sea were 10, 12.3, 11.5, and $14.3^{\circ}C$ at Jeju, Seoguipo, Seongsanpo and Gosan, respectively. The probabilities of fresh snowfall were 26, 29, 13, and $23\%$, respectively, when the temperature differences were higher than the previous values. On the other hand, the minimum Bowen ratios were 0.59, 0.60, 0.65 and 0.65 at Jeju, Seoguipo, Seongsanpo and Gosan, respectively. The probabilities of fresh snowfall were 33, 70, 31 and $58\%$ respectively, when the Bowen ratio is higher than those. The reason for this is because the probability of fresh snowfall with the Bowen ratio was higher than the probability with temperature difference between air and sea. This result occurred because heat exchange by wind increased the probability of snowfall, along with the temperature difference between air and sea, and the Bowen ratio. Therefore, snowfall forecast of Jeju Island is significantly influenced by the sea, whereas forecast with Bowen ratio seems to have higher reliability than that with the temperature difference between air and sea. The data analysis for the ten-year period $(1993\~2002)$ showed that when each fresh snowfall was within 0.0 to 0.9cm, the average Bowen’s ratio was 0.63 to 0.67, and when each fresh snowfall was 1.0 to 4.9 cm, the average Bowen’s ratio was over 0.72. Therefore, fresh snowfall shows a proportional relationship with the Bowen’s ratio during snowfall.

Estimate of Heat Flux in the East China Sea (동지나해의 열속추정에 관한 연구)

  • KIM Young-Seup
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.29 no.1
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    • pp.84-91
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    • 1996
  • Heat flux of the East China Sea was estimated with the bulk method, the East China mount based on the marine meteorological data and cloud amount data observed by a satellite. Solar radiation is maximum in May and minimum in December. Its amount decreases gradually southward during the winter half year (from October to March), and increases northward during the summer half year (from April to September) due to the influence of Changma (Baiu) front. The spatial difference of long-wave radiation is relatively small, but its temporal difference is quite large, i.e., the value in February is about two times greater than that in July. The spatial patterns of sensible and latent heat fluxes reflect well the effect of current distribution in this region. The heat loss from the ocean surface is more than $830Wm^{-2}$ in winter, which is five times greater than the net radiation amount during the same period, The annual net heat flux is negative, which means heat loss from the sea surface, in the whole region over the East China Sea. The region with the largest loss of more than $400Wm^{-2}$ in January is observed over the southwestern Kyushu. The annual mean value of solar radiation, long-wave radiation, sensible and latent heat fluxes are estimated $187Wm^{-2},\;-52Wm^{-2},\;-30Wm^{-2}\;and\;-137Wm^{-2}$, respectively, consequently the East China Sea losses the energy of $32Wm^{-2}(2.48\times10^{13}W)$. Through the heat exchange between the air and the sea, the heat energy of $0.4\times10^{13}W$ is supplied from the air to the sea in A region (the Yellow Sea), $2.1\times10^{13}W$ in B region (the East China Sea) and $1.7\times10^{13}W$ in C region (the Kuroshio part), respectively.

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Temporal and spatial distributions of heat fluxes in the East Sea(Sea of Japan) (東海熱收支 의 時.空間的인 分布)

  • 박원선;오임상
    • 한국해양학회지
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    • v.30 no.2
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    • pp.91-115
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    • 1995
  • Air-sea heat fluxes in the East Sea were estimated from the various ship's data observed from 1961 to 1990 and the JMA buoy #6 data from 1976 to 1985. The oceanic heat transport in the sea was also determined from the fluxes above and the heat storage rate of the upper layer of 200m from the sea surface. In winter, The incoming solar radiation is almost balanced with the outgoing longwave radiation. but the sea loses her heat through the sea surface mainly due to the latent and sensible heat fluxes. The spatial variation of the net surface heat flux is about 100 Wm/SUP -2/, and the maximum loss of heat is occurred near the Tsugaru Strait. There are also lots of heat losses in the southern part of the East Sea, Korea Strait and Ulleung Basin. Particularly, the heat strong loss in the south-western part of the sea might be concerned with the formation of her Intermediate Homogeneous Water. In summer, the sea is heated up to about 120∼140 Wm/SUP -2/ sue to strong incoming solar radiation and weak turbulent heat fluxes and her spatial variation is only about 20 Wm/SUP -2/. The oceanic heat flux is positive in the southeasten part f the sea and the magnitude of the flux is larger than that of the net surface heat flux. This shows the importance of the area. In the southwestern part of the sea, however, the oceanic heat flux is negative. This fact implies cold water inflow, the North Korean Cold Water. The sigh of net surface heat flux is changed from negative to positive in March and from positive to negative in September. The heat content in the upper surface 200 m from the sea surface reaches its minimum in March and maximum in October. The annual variation of the net surface heat flux is 580 Wm/SUP -2/ in southwestern part of the sea. The annual mean values of net surface heat fluxes are negative, which mean the net heat transfer from the sea to the atmosphere. The magnitude of the flux is about 130 Wm/SUP -2/ near the Tsugaru Strait. The net surface fluxes in the Korea Strait and the Ulleung Basin are relatively larger than those of the rest areas. The spatial mean values of surface heat fluxes from 35$^{\circ}C$ to 39$^{\circ}$N are 129, -90, -58, and -32 Wm/SUP -2/ for the incoming solar radiation, latent hear flux, outgoing longwave radiation, and sensible heat flux, respectively.

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Ohmic Heating Characteristics of Fermented Soybean Paste and Kochujang (된장 및 고추장의 Ohmic heating 특성)

  • Cho, Won-Il;Kim, Do-Un;Kim, Young-Suk;Pyun, Yu-Ryang
    • Korean Journal of Food Science and Technology
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    • v.26 no.6
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    • pp.791-798
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    • 1994
  • Ohmic heating is a food processing operation in which heat is internally generated within foods by the passage of alternating electric current. The process enables highly viscous paste foods such as Kochujang, and fermented soybean paste to be heated very fast. In order to develope the novel pasteurization process of paste foods, static Ohmic heating system was built, and heating characteristic during Ohmic heating under various conditions were studied. Electric conductivities of Kochujang and fermented soybean paste at room temperature were 1.865 S/m and 2.510 S/m, respectively and increased linearly with increasing temperature. Specific heating rate was highly dependent on the frequency. The highest heating rate was achieved at 5 KHz for Kochujang and 20 KHz for fermented soybean paste. Uniform heating throughout the sample was achieved during Ohmic heating with low frequency electrical currents, however above 5 KHz frequency, surface temperature was several degrees higher than the bulk.

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Determination of Inherent Strain Regions to Estimate Plate Deformation by Line Heating (선상가열 판변형 해석을 위한 고유변형도 영역의 결정법)

  • Chang-Doo Jang;Yun-Sok Yun;Dae-Eun Ko;Sung-Choon Moon
    • Journal of the Society of Naval Architects of Korea
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    • v.39 no.1
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    • pp.82-89
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    • 2002
  • The inherent strain method is known to be very effective in predicting the plate deformation by line heating. Traditionally the inherent strain regions have been determined from the temperature distribution and the phase transformation regions(Ac3) of welding experiments. Since the phenomena of line heating are similar to those of welding, the experimental results under the same welding conditions have been applied directly to line heating analysis. The results cannot, however, reflect the effect of heating pattern and plate thickness. Besides, water-cooling in the actual heating process can alter the steel's phase to martensite and shear plastic deformation occurs during the transformation. In this study, the experimental measurement of temperature distribution was substituted with a transient heat transfer analysis using FEM so that we could obtain the temperature distribution according to heat flux models of the heating pass. In order to consider plastic strains occurring additionally under phase transformation, inherent strain regions were assumed to be limited to the eutectoid temperature(Ac1). Using the regions, plate deformations could be predicted to validate our method and the results were in good agreement with the experimental ones

Combustion Characteristics of the Quercus variabilis and Zelkova Serrata Dried at Room Temperature (자연 건조된 굴참나무와 느티나무의 연소특성)

  • Chung, Yeong-Jin;Kwon, In-Kyu
    • Journal of Korean Society of Forest Science
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    • v.99 no.1
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    • pp.96-101
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    • 2010
  • One of the restriction of wood as building material is its combustibility. The purpose of this paper is to examine the combustion properties of the quercus variabilis and zelkova serrata which are dried at room temperature and meet the desirable characteristics for use of construction materials. The cone calorimeter (ISO 5660-1) was used to determine the heat release rate (HRR) and fire smoke index, as well as CO production and smoke obscuration. The $HRR_{mean}$ 77.94 kW/$m^2$ of the quercus variabilis at 50 kW/$m^2$ was high in comparison with $HRR_{mean}$ 13.06 kW/$m^2$ for the zelkova serrata. Furthermore, the quercus variabilis has high specific extinction area ($SEA_{mean}$), 41.11 $m^2$/kg compared with $SEA_{mean}$ 9.23 $m^2$/kg of zelkova serrata. Thease results are depend on the density of tested wood species. In addition, the quercus variabilis has high CO production rate compared with that of zelkova serrata. Also, zelkova serrata showed an increase of retardant properties attributed to char formation compared with that of quercus variabilis.

A Study on the Estimation of Air-Sea Heat Fluxes and the Wave Characteristics using Chilbaldo Buoy Data (칠발도 Buoy자료를 이용한 해양-대기 열교환량 산출 및 파랑 특성에 관한 연구)

  • Youn, Yong-Hoon;Hong, Sung-Gil;Hong, Yoon;Lee, Ji-Yeon
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.3 no.1
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    • pp.9-15
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    • 1998
  • Hourly meteorological data from a marine buoy ($34^{\circ}49'00"N$, $125^{\circ}46'00"E$) operated by the Korean Meteorological Agency were obtained from July, 1996 to February, 1997. From the data air-sea heat fluxes and marine meteorological characteristics around the area are estimated. The maximum outflux of sensible heat from the sea surface occurred in January (monthly mean value, 12.6 $Wm^{-2}$ and the maximum influx to the sea occurred in July (monthly mean value, 5.5 $Wm^{-2}$). This means that the sea is heated in summer while it loses its heat in winter, and that there is inequality between the absolute values of the two seasons. The outflux of the maximum latent heat occurred in November (monthly mean value, 86.5 $Wm^{-2}$) and reach a value of 300 $Wm^{-2}$, and the maximum influx occurred in July (monthly mean value, 4.6 $Wm^{-2}$). Big difference is shown in their absolute values when the wind becomes strong. The outgoing latent heat flux reaches its maximum in autumn, and it maintains the high value through the whole winter. According to the wave data analysis, the significant wave heights are larger in winter than in summer. The periods of the significant waves are 4~6 sec. In winter, waves propagated from north and northeast are dominant because of the winter monsoon, while in summer waves from south, southwest, and west are relatively frequent.

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A Relationship between Oceanic Conditions and Meteorological Factors in the Western Sea of Korea in Winter (동계 서해의 해황과 기상인자와의 관계)

  • Go Woo-Jin;Kim Sang-Woo;Kim Dong-Sun
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.12 no.1 s.24
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    • pp.23-32
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    • 2006
  • This study was conducted to find out the effects of meterological factors on oceanic conditions when cold and dry continental air mass passes through the western sea of Korea The change of ocean conditions during the winter season were more obvious in coastal area than open sea And sea surface temperature (SST) during February is lower by $3^{\circ}C$ than December but in coastal area SST dropped by $3^{\circ}C$. As for the salinity, there was not much difference between areas except southern area of Mokpo. In the coastal regions, air temperature(AT) and SST showed a positive correlation; as the air temperature goes up with the increase of SST and when the former goes down the latter decrease. SST of open sea seems to be changed by latent (Qe) and sensible heat (Qs), when the open sea lose its heat by Qe and Qs then SST goes down And when they get the heat then the SST goes up. 1here was a positive correlation between the AT of the coastal region and sea surface salinity (SSS), when the AT goes up then SSS increase and when the former goes down the latter decrease. Precipitation during the summer seasons (June$\sim$September) appeared to the more closely related with salinity of February of the following year than those of October and December.

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