• Title/Summary/Keyword: 영하온도

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과학리포트-초전도현상 등 신비 연출하는 극저온의 세계

  • Lee, Gwang-Yeong
    • The Science & Technology
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    • v.28 no.8 s.315
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    • pp.14-15
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    • 1995
  • 온도가 영하로 계속 내려가는 우리들의 주변엔 신비로운 현상들이 나타난다. 온도가 더 이상 내려갈 수 없다는 극저절대온도는 영하 273.15도 그러나 온도가 영하 148도만 돼도 초전도 현상이 일어나 컴퓨터 성능이 수천배 올라가고 전자제품의 잡음이 없어진다. 이렇게 신비로운 극저온의 세계를 열어본다.

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Shooting and Fruiting Characteristics of 'Hachiya' Persimmon Tree Affected by Sub-zero Temperature Treatment at Early Budding Stage (발아 초기에 영하온도 처리에 따른 감나무 '갑주백목' 의 신초 생장과 착과 특성)

  • Kim, Ho Cheol
    • The Journal of the Convergence on Culture Technology
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    • v.5 no.4
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    • pp.395-399
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    • 2019
  • The purpose of this study was to investigate shooting and fruiting characteristics of persimmon 'Hachiya' affected by sub-zero temperature at early budding stage. The number of developed shoots, and the number of shoots with young fruits, and the shooting and fruiting of terminal buds of one-year-old branch (1YOB) were significantly decreased with the sub-zero temperature treatment (SZT). The number of shoots developed in the top of 1YOB decreased 47.2% due to SZT. The number of shoots with fruits was significantly decreased at 50% or higher in non-budding rate of 1-YOB. Especially the number of fruits (Y) at the three terminal buds of 1YOB was significantly affected by SZT and the non-budding rate (X) as Y = -0.145X + 12.950 ($r^2=0.4672^*$). Therefore, in the early budding stage of persimmon, when tree is affected by SZT ($-2^{\circ}C$, 3 hours), shoots growth is reduced and increase of 10% in non-budding rate reduces 1.4 of fruits per the three terminal buds of 1YOB.

Unsaturated Soil Properties of Compacted Soil at Sub-Zero Temperature (영하온도에서 다짐된 지반의 불포화 특성)

  • Lee, Jeonghyeop;Hwang, Bumsik;Cho, Wanjei
    • Journal of the Korean GEO-environmental Society
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    • v.19 no.3
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    • pp.5-13
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    • 2018
  • Recently, construction disasters in thawing season are increasing due to the ground collapse and it is related to the improper compaction during winter season. Compaction at sub-zero temperature reduces the compaction effect and the research of mechanical properties of thawed soil after winter compaction can be used as useful data to understand the behavior of the ground in the thawing season. On the other hand, the research interest in the unsaturated soil mechanics has been increasing in the field of the geotechnical engineering. Therefore, it is expected that the research of unsaturated characteristics under the compaction of sub-zero temperature and freezing & thawing condition provides information to the researchers in the related fields. Therefore, in this research, unsaturated soil-water characteristics test and unsaturated uniaxial compression test were conducted on the specimens compacted at sub-zero temperature and continuous freezing & thawing condition to investigate change of unsaturated characteristics and matric suction. Based on the test results, the change of matric suction and the decrease of strength and stiffness were observed with the freezing & thawing conditions. Especially in case of the weathered soil, the strength and matric suction were significantly reduced with lower temperature and more repetition of freezing & thawing cycles. This result implies that compaction of sub-zero temperature and freezing & thawing cycles will have a considerable influence on the stability of the ground.

Evaluations on the Compaction Energy Effects on the Soil Compaction at Sub-Zero Temperature (영하에서의 다짐에너지에 따른 다짐 효과 평가)

  • Lee, Jeonghyeop;Hwang, Bumsik;Chae, Deokho;Cho, Wanjei
    • Journal of the Korean GEO-environmental Society
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    • v.16 no.8
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    • pp.13-20
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    • 2015
  • Due to the population growth and exhaustion of resource, the development on the harsh environment such as cold weather is emerging as an alternative for new resource development. The permafrost area covers about 14 percent of the world's land area and the global construction market for such area is rapidly expanded. Whereas the developed countries have already recognition of the need for research of coldest place and invested heavily in technology development, the domestic technology for the coldest place development is less developed and related research has rarely been performed. There is not a detailed national specification standard for the strength and deformation properties of the earthworks at sub-zero temperature but simple field directions. Therefore, the D compaction tests were conducted on the sand with fine contents of 0%, 5%, 10% and 15% at room temperature ($18^{\circ}C$), $-3^{\circ}C$ and $-8^{\circ}C$ to investigate the effect of the compaction energy on the compacted soils at sub-zero temperatures. Based on the test results, the larger compaction energy, the larger maximum dry unit weight under sub-zero temperature and D type compaction at $-3^{\circ}C$ show similar max. dry unit weights as those obtained from the compaction at the room temperature. However, compaction at $-8^{\circ}C$ showed significant performance degradation regardless of the compaction energy.

Temperature Sensitivity Analysis of TDR Moisture Content Sensor for Road Pavement (도로하부 함수비 계측을 위한 TDR 방식 함수비 센서 온도 민감도 분석)

  • Cho, Myunghwan;Lee, Yoonhan;Kim, Nakseok;Jee, Keehwan
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.33 no.1
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    • pp.329-336
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    • 2013
  • The infrastructure of flexible pavement is composed of aggregate subbase, anti-frost layer, and subgrade. In particular, the subgrade performance is affected by climates such as frost action and precipitation. The method of TDR(Time Domain Reflectometry) sensors to measure moisture contents in subgrade layer has been used in the research. Due to the TDR method using dielectric permitivity of soil and water, the sensors can be affected by the low subgrade temperatures. The air temperatures frequently drops below $-20^{\circ}C$ in the winter in Korea. As a result, it is necessary to estimate the accuracy of the TDR moisture sensors in the range of below zero temperatures. In this study, the subgrade temperatures of lower than $-2^{\circ}C$ were extended to evaluate temperature sensitivity of the TDR moisture sensors. The test results revealed that the moisture contents around the sensors were reduced while those of the upper part of specimen showed a tendency to increase as the specimen surface temperature drops below zero under the volumetric moisture contents(VMC) of 20% and 30%. However, the impact of temperature on the function of the sensor at lower water contents was found to be negligible if any.

손상 핵연료의 온도 및 산소대 금속 비율의 변화 모형 연구

  • 서영하;박광헌;호광일
    • Proceedings of the Korean Nuclear Society Conference
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    • 1996.05c
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    • pp.329-334
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    • 1996
  • 손상 핵연료의 온도 및 산소대 금속 비율의 변화모형을 연구하였다. 열역학적 분석과 산화과정에 대한 분석을 통해 손상핵연료에서의 핵연료 온도와 핵연료내 O/U값 변화를 기술함으로써 결함발생에 의한 핵연료내 냉각수 침투는 Gap conductance를 떨어뜨리고 소결체 산화에 따른 O/U값 증가로 열전달특성의 저하를 가져와 핵연료의 온도를 상승시킨다는 결과를 얻어냈다.

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Evaluation on Thermal Performance of Thermosyphon by Numerical Analysis (열사이펀의 열성능 산정을 위한 수치해석 연구)

  • Jang, Changkyu;Choi, Changho;Lee, Jangguen;Lee, Chulho
    • Journal of the Korean Geotechnical Society
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    • v.30 no.9
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    • pp.57-66
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    • 2014
  • The ground in cold region consists of active and permafrost layers. The active layer at the unstable state may cause ground corrosion and uplift, when the temperature of frozen ground increases due to seasonal changes. The thermosyphon is one of the stabilization methods to maintain the ground stability in the frozen ground. The thermosyphon is a closed two-phase convection device that extracts heat from the ground and discharges it into the atmosphere. In this study, ground freezing experiment using a thermosyphon and simulated ground with the isolation material was conducted to evaluate the thermal performance of the thermosyphon. In order to consider the thermal performance of the thermosyphon, commercial numerical program (TEMP/W) was adopted. Likewise, the thermal performance of thermosyphon and thermal properties of ground were applied in the numerical model. In a series of comparisons with experiment results and numerical study, thermal performance of thermosyphon can be evaluated.

Experimental and Numerical Investigation of the Performance of Vertical Thermosyphon for Frozen Ground Stabilization (실험과 수치해석을 통한 동토지반 안정화용 수직형 열사이펀의 성능평가)

  • Lee, Jangguen;Lee, Chulho;Jang, Changkyu;Choi, Changho
    • Journal of the Korean Geosynthetics Society
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    • v.13 no.4
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    • pp.45-56
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    • 2014
  • Frozen ground in cold region consists of an upper active layer and lower permafrost which is permanently frozen land. During the summer season, the air temperature is high enough to make the frozen ground melt, which causes the reduction of soil strength and thaw settlement. These phenomena result in structural instability, so it is necessary to apply frozen ground stability techniques. Thermosyphon is a closed natural two-phase convection device to maintain the ground temperature below $0^{\circ}C$ by extracting heat from the ground and discharges it into the atmosphere. Experimental and numerical investigation has been performed to estimate the effect of the refrigerant filling ratio in thermosyphon using R-134a refrigerant and the thermal conductance of the thermosyphon.

A Study of the Development of a Korea Wind Chill Temperature Index (I) - Focusing on the Distribution of Existing Wind Chill Temperature Index and Sensitivity Analysis of Model - (한국형 체감온도지수 개발연구(I) -기존 체감온도지수 분포 및 민감도 분석 -)

  • Park, Jong-Kil;Jung, Woo-Sik;Kim, Eun-Byul;Park, Gil-Un
    • Journal of the Korean earth science society
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    • v.28 no.7
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    • pp.878-890
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    • 2007
  • This study aimed to provide a fundamental basis for the development and promotion of a Korea windchill temperature index model in the field of human biometeorology. For this, a sensitivity model currently being used by KMA (Korea Meteorological Administration) was analyzed. The results of the analysis showed that the Korean peninsula could be divided into the urban area, the coastal/island area, the inland area, and the mountain area. The average temperature was highest in the coastal/island area, while it was lowest in the mountain regions. The lowest temperature in the urban and coastal/island areas was 20 degrees below zero and that in the inland and mountain regions were 30 degrees below zero. As for wind speed, both average and maximum wind speed were highest in the coastal/island area. The distribution of temperature and wind speed in winter was similar to that of the entire period. The results of the JAG/Tl and Missenard model sensitivity showed that temperature tends to have more influence on sensitivity than any other factors. In sub-zero temperature, however, the influence of wind speed tends to increase.