• Title/Summary/Keyword: 극서지역

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광주.전남의 지질 및 지반공학적 특성

  • 장용채
    • Proceedings of the Korean Geotechical Society Conference
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    • 2004.03a
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    • pp.134-145
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    • 2004
  • 전남은 한반도의 서남부를 차지하는 지역으로 동북으로는 높은 산지에 의해 서남으로는 바다에 의해 확연히 구분된 지역이다. 전남의 북부는 전북의 고창, 순창군에 연접해 있으며, 동부는 경남의 하동, 남해군 등과 인접해 있다. 전남의 경위도상 위치를 보면 극동에는 여수시 남면 연도리 작도, 극서에는 신안군 흑산면 소흑산도, 극남에는 완도군 소안면 장수리, 극북에는 장성군 북하면 신성리에 위치해 있다.(중략)

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Property Evaluation of Low-Heat Concrete with Phosphate-PCM Composite (Phosphate-PCM계 복합물질 기반 저발열 콘크리트의 특성 평가)

  • Ki, Jun-Do;Lee, Sang-Hyun;Cho, Hong-Bum;Kim, Young-Sun;Seok, Won-Kyun
    • Proceedings of the Korean Institute of Building Construction Conference
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    • 2020.06a
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    • pp.175-176
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    • 2020
  • This study aims to develop the hydration heat reducing material (powder type) to lower the heat of hydration of mass members in the extremely hot weather condition. In this study, we applied the developed material to the concrete that used two kinds of binders with cement and evaluate the concrete properties with it.

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Climatic Changes and Geographical Characteristics of Solar Term Temperatures in the Korean Peninsula (한반도 절기 기온의 기후적 변화와 지리적 특성)

  • PARK, Sun-Yurp;LEE, Su-Kyung
    • Journal of the Korean Association of Geographic Information Studies
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    • v.22 no.3
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    • pp.65-81
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    • 2019
  • The twenty-four Solar Terms are Chinese traditional astronomical divisions that describe seasonal cycles of the year. Based on the analyses of meteorological data during 1979~2018, study results showed that the temperatures of the Solar Terms had increased in general in the Korean Peninsula. In North Korea, temperature increases were observed on 21 Solar Terms, and their seasonal mean temperatures were increased by $0.87^{\circ}C$, $1.19^{\circ}C$, $1.45^{\circ}C$, and $0.64^{\circ}C$ on average in spring, summer, fall, and winter, respectively. The duration of summer has lengthened due to the temperature rise in fall, and the magnitude of temperature change was greater in summer compared to winter. As for South Korea, increases in temperature were observed on 18 Solar Terms, and the temperature changes were more pronounced in fall and winter than spring and summer. The Great Snow temperature decreased more than any other Solar Terms during the study period, and this temperature change was observed both in North and South Koreas. The Great Cold, which represents the coldest day of the year, showed a significant temperature increase of $3.08^{\circ}C$, while the Slight Heat had a marginal temperature increase of $0.29^{\circ}C$. The hottest day and the first day of frost tended to come later than the Great Heat and the Frost's Decent. By contrast, the coldest day tended to occur later than the Great Cold in the study area. On average over the entire study period, the climatic fitness of the Great Heat and the Frost's Decent was higher in North Korea, and that of the Great Cold was higher in South Korea, respectively.

A Study on Microclimate Change Via Time Series Analysis of Satellite Images -Centered on Dalseo District, Daegu City- (위성영상의 시계열 분석을 통한 미기후변화 분석 -대구시 달서구를 대상으로-)

  • Baek, Sang-Hun;Jung, Eung-Ho
    • Journal of the Korean Association of Geographic Information Studies
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    • v.12 no.2
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    • pp.34-43
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    • 2009
  • Based on previous research on ways of reducing an urban heat island phenomenon via an introduction of wind corridors, I conducted this study to see what influence a change in land cover arising of or going through urbanization has on wind corridors of urban space. As a target place, I chose Daegu city where is a representative extreme heat place in Korea and has been also largely expanded in size by incorporating its neighboring areas since the 1980s, expecially Dalseo District whose surface temperature gap is large. The population of Dalseo District has been sharply increased since its creation as a new administrative district in 1988. I studied on the urban microclimate change for a 20-year period by using satellite images on summer months in 1987, 1997 and 2007 in time frames. The finding of this study found that a reduction of natural land cover and an increase of artificial land cover serves as a disadvantageous factor for cold air creation and flowing and strikingly lowers the amount and height of cold air in the downtown area. It seemed that the cold air creation and flowing functions are influenced by land cover. In order to steadily create cold air and secure its flowing, it is thought that urban development or urban regeneration should be implemented by analysing the characteristics of the space surrounding the city. By doing so, a pleasant and healthy city could be formed.

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