• 제목/요약/키워드: Cold Formed Part

검색결과 59건 처리시간 0.025초

한국적 의상디자인에 표현된 자연주의에 관한 연구-1990년 이후의 디자인을 중심으로- (A Study on the Naturalism presented in Korean Fashion Design-Focused on the Design Since 1990-)

  • 강희경
    • 복식
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    • 제38권
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    • pp.213-231
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    • 1998
  • The purpose of this study is to find a root from naturalism to contribute the identity of Korean fashion design in the world which has universality and particularity. The beauty of nature has accumulated in our unconscious-ness, influenced to our unconsciousness, and contributed to make the formative sense. Our consciousness influenced by climate, for example, the sense of softness from soft curve which can feel from the sight of Korean mountain, land the sense of comfort and security from round rock formed by weathering, the sense of thick-ness from cotton to endure cold winter etc. has a tendency to thick and act by nature's law. This tendency made naturalism by Korean climate and linked to the sense of natural-istic beauty and became a important part forming the Korean fashion design. In this study, the researcher found Korean climate is a important factor acting in our consciousness, and influenced the formative sense. The concept of climate which is made our formative sense include topography, climate, soil, plant and so on. This influenced a lot to set up a foundation of Korean fashion design. And the naturalism by Korean climate newly created and developed shape, color, material and design. It is our duty to develope design based on naturalism to secure the competitive power against the world in this period of information and this design is getting important as a high value added method put into Korean culture. Therefore, developing Korean design which shapes the beauty of Korean nature and traditional culture will have a important competitive power in the world. Moreover, it will make a new tradition of Korean fashion culture stagnated by internationally universalized western fashion after the modernization. Also, it will be needed to develop a common design which can be agreed not only us but all the world for the request of these days of international. Therefore, this study contributed to find definite ours and found centripetal point to find the direction of Korean's philosophy and ideology. But this approach, we could secure the competitive power in this period of international and information and determine and develope the Korean fashion as a culture base, leading the world.

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1983년 춘계 제주해협의 해황과 해류 (Hydrography and Sub-tidal Current in the Cheju Strait in Spring, 1983)

  • 장경일;김구;이석우;심태보
    • 한국해양학회지
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    • 제30권3호
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    • pp.203-215
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    • 1995
  • 1983년 4월과 5월에 걸쳐 제주해협에서 부표와 해류계를 이용한 해류관측과 함께 2회에 걸쳐 수온-염분관측을 실시하였다. 관측자료로부터 고온, 고염인 흑조 의 한 지류가 제주도 서쪽을 돌아 제주해협으로 유입됨을 명확히 보였다. 제주도 서쪽을 우회하는 해류는 제주도 서쪽에서는 그 폭이 약 60 km이며 제주 해협내 에서는 20∼30 km 이내에 존재하여 제주도 서쪽에서는 5 cm/s 미만으로 유속이 작은 반면에 제주해협의 서쪽입구와 해협 내에서는 10 cm/s 이상의 큰 유속을 갖는다. 제주해협의 동쪽에는 역시 흑조로부터 기원된 대마난류의 영향이 인지 되었다. 난류수와 연안수 사이에 형성되는 수온, 염분전선의 변화는 제주 해협의 서쪽에서 황해연안수가 남하함을 제시하였다. 난류수역에서는 5월에 수온이 상승 한 반면에 다른 해역에서는 수온이 감소하였다. 5월에 제주해협 중앙부에서는 해 협의 서쪽으로부터 저온, 저염의 해수가 유입되어 4월에 비해 수온과 염분이 급격 히 감소하였다.

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Assessment of geothermal potential in an area of sulfate-rich hot springs, Bugok, southern Korea

  • 박성숙;윤성택;채기택;소칠섭;고영권;최현수
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2006년도 총회 및 춘계학술발표회
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    • pp.303-306
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    • 2006
  • Using a variety of chemical geothermometers we estimate the temperature of a deep geothermal reservoir in relation to thermal groundwater in the Bugok area, southern Korea, in order to assess the potential use of geothermal energy in South Korea. Thermal water at Bugok has been exploited down to about 400 m below the land surface and shows the highest outflow temperatures (up to $78{\circ}C$) in South Korea. Based on the hydrochemical data and occurrence, groundwater in Bugok can be classified into three groups: $Na-SO_4$ type thermal groundwater (CTGW) occurring in the central part (about 0.24 $km^2$) $Ca-HCO_3$ type cold groundwater (SCGW) occurring in shallow peripheral parts of CTGW; and the intermediate type groundwater (STGW). CTGW waters are typical of thermal water in the area, because they have the highest outflow temperatures and contain very high concentrations of Na, K and $SiO_2$ due to the sufficient reaction with silicate minerals in deep reservoir. Their enriched $SO_4$ was likely formed by gypsum dissolution. The major ion composition of CTGW shows the general approach to a partial equilibrium state with rocks at depth. The application of various alkali ion geothermometers yields temperature estimates in the range of 88 to $198{\circ}C$ for the thermal reservoir. Multiple mineral equilibrium calculation indicates asimilar but narrower temperature range between about 100 and $155{\circ}C$. These temperature estimates are not significantly higher than the measured outflow temperatures for CTGW Considering the heat loss during the ascent- of thermal waters, this fact may suggest that a thermal reservoir in the study area is likely located at relatively shallow depths (possibly close to the depth of preexisting wells). Therefore, we suggest a high potential for geothermal energy development around the Bugok area in southern Korea.

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Tests on composite slabs and evaluation of relevant Eurocode 4 provisions

  • Salonikios, Thomas N.;Sextos, Anastasios G.;Kappos, Andreas J.
    • Steel and Composite Structures
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    • 제13권6호
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    • pp.571-586
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    • 2012
  • The paper addresses some key issues related to the design of composite slabs with cold-formed profiled steel sheets. An experimental programme is first presented, involving six composite slab specimens tested with a view to evaluating Eurocode 4 (EC4) provisions on testing of composite slabs. In four specimens, the EC4-prescribed 5000 load cycles were applied using different load ranges resulting from alternative interpretations of the reference load $W_t$. Although the rationale of the application of cyclic loading is to induce loss of chemical bond between the concrete plate and the steel sheet, no such loss was noted in the tests for either interpretation of the range of load cycles. Using the recorded response of the specimens the values of factors m and k (related to interface shear transfer in the composite slab) were determined for the specific steel sheet used in the tests, on the basis of three alternative interpretations of the related EC4 provisions. The test results confirmed the need for a more unambiguous description of the m-k test and its interpretation in a future edition of the Code, as well as for an increase in the load amplitude range to be used in the cyclic loading tests, to make sure that the intended loss of bond between the concrete slab and the steel sheet is actually reached. The study also included the development of a special-purpose software that facilitates design of composite slabs; a parametric investigation of the importance of m-k values in slab design is presented in the last part of the paper.

정동진 의사글레이층의 입도와 화학 조성에 대한 연구 (A Study on the Granulometry and Chemical Composition of Psudo-Gleized Soil in Jeongdongjin Area)

  • 김종연
    • 한국지형학회지
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    • 제24권3호
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    • pp.27-45
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    • 2017
  • At the upper part of terrace deposits at Jeongdongjin area, there is a structure in which reddish brown and grayish white layers laying horizontally. Previous studies have reported the existence of these structures within the deposits and suggested the theoretical background related to the formation process. However, the analysis of physical properties and chemical composition such as particle size, classification, etc. of the materials constituting the reddish brown and grayish white layers is scarcely done. In this study, the physico - chemical properties of gray - white and reddish brown beds are investigated. The mean grain size of the particles was less than $4{\varphi}$ in both layers and the reddish brown layer was more coarse. The results shows that the sorting of the grayish white layer is better. The chemical composition of both layers shows that the average concentration of $SiO_2$, $Al_2O_3$ and $K_2O$ of the grayish white layer was higher than those of the reddish brown layer. The concentration of $Fe_2O_3$ of reddish brown lyaer was 3 times higher than those of the grayish white layer. The degree of chemical weathering (CIA) is 90 or so in both the reddish brown and grayish white layers, indicating a significant level of chemical weathering. In conclusion, reddish brown layers had been formed by the processes related to the migration of iron and the migration of water that induced aggregation after the formation of sediments (psudo-gleization). In this study area, a vertical layer of grayish white which cuts off horizontal reddish brown and grayish white color was found. The vertical layer or wedge similar to a ice-wedge or columnar structure that in a cold environment, and there is a difference in shape and size. The vertical layer appears to have occurred three or more cycles. The vertical layers begin to form at a certain height within the outcrop and descend downwards, which of course is difficult to see as directing certain times.

대기환경영향평가를 위한 대구광역시 상인동 달비골의 봄철 기상관측 사례분석 (A Case Study on the Meteorological Observation in Spring for the Atmospheric Environment Impact Assessment at Sangin-dong Dalbi Valley, Daegu)

  • 박종길;정우식;황수진;윤일희;박길운;김신호;김석철
    • 한국환경과학회지
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    • 제17권9호
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    • pp.1053-1068
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    • 2008
  • This study aims to produce fundamental database for Environment Impact Assessment by monitoring vertical structure of the atmosphere due to the mountain valley wind in spring season. For this, we observed surface and upper meteorological elements in Sangin-dong, Daegu using the rawinsonde and automatic weather system(AWS). In Sangin-dong, the weather condition was largely affected by mountains when compared to city center. The air temperature was low during the night time and day break, and similar to that of city center during the day time. Relative humidity also showed similar trend; high during the night time and day break and similar to that of city center during the day time. Solar radiation was higher than the city, and the daily maximum temperature was observed later than the city. The synoptic wind during the measurement period was west wind. But during the day time, the west wind was joined by the prevailing wind to become stronger than the night time. During the night time and daybreak, the impact of mountain wind lowered the overall temperature, showing strong geographical influence. The vertical structure of the atmosphere in Dalbi valley, Sangin-dong had a sharp change in air temperature, relative humidity, potential temperature and equivalent potential temperature when measured at the upper part of the mixing layer height. The mixing depth was formed at maximum 1896m above the ground, and in the night time, the inversion layer was formed by radiational cooling and cold mountain wind.

한라산 동.서사면 좀꽝꽝나무 아개체군 자생지의 환경 및 생태적 특성 (Environmental and Ecological Characteristics of Ilex crenata var. microphylla Max. Subpopulations Habitats in the East-West Slopes in Mt. Halla National Park)

  • 이동곤;김용식;신현탁
    • 한국환경생태학회지
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    • 제25권4호
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    • pp.562-572
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    • 2011
  • 본 연구는 한라산국립공원의 동 서사면에 자생하는 좀꽝꽝나무 아개체군의 환경특성을 파악하기 위하여 환경요인, 식생 및 토양분석을 실시하였다. 한라산국립공원의 동 서사면 해발고 500m~1600m 내에 설정한 56개 조사지를 대상으로 TWINSPAN 분석결과 주목-산개벚지나무군집, 당단풍나무군집, 개서어나무-굴거리나무군집, 졸참나무군집, 곰솔군집 등 5개의 유형으로 구분되었다. 이 중 좀꽝꽝나무 아개체군의 우점치가 높은 군집은 개서어나무-굴거리나 무군집으로 해발고 600m~1200m 지점에 포함되며, 교목상층의 우점종은 개서어나무(I.P.: 29.82%)이고 아교목층의 우점종은 굴거리나무(I.P.: 26.76%), 관목층은 좀꽝꽝나무(I.P.: 33.08%)이었다. 이곳의 토양은 유기물함량, 유효인산 및 Ca, Mg의 양료가 많은 곳이다. 좀꽝꽝나무 아개체군의 우점치가 높은 곳은 동쪽사면 해발고 600m~800m, 서쪽사면 해발고 800m~1,000m 부근으로 이곳은 냉온삼림대 남부에 해당되는 곳으로 개서어나무의 우점치가 높고 종다양도지수도 0.7427로 낮은 편으로 개서어나무의 극상림을 형성한 안정된 상태로 보인다.

동북(東北)아시아 유의 기원(起源)과 그 교류(交流)에 관(關)한 연구(硏究) -$4{\sim}8$세기(世紀)를 중심(中心)으로- (A study on the origination and Transmission of Yu in Northeast Asia. -from the 4th Century to the 8th Century-)

  • 박경자;조선희
    • 복식
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    • 제17권
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    • pp.29-43
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    • 1991
  • Yu was a type of dress worn on the upper part of the body which was commonly used in Northeast Asia. It was originally used by the Northern race for the need of courtesy as well as protecting cold. It was believed that Yu in Northeast Asia, which was called Kaftan, was came from Scythai lived in North Eurasian land around the Black sea. Scythians were the first-formed horse-riding race in the world and their civilization influenced those of far Asiatic sector along the steppe route. As their power expanded, their costume culture transmitted to the East(China, Korea, Japan). The upper garment, Yu, was characterized by the left-sided collars, narrow sleeves belted at the waist to the length of the hip line and the tight trouser on the lower part, which we commonly called HoBok(胡服) style. 1. Yu in Northeast Asia was originated from the Eurasians, Scythian Culture. Being exchanged, active style costumes were widely used among Chinese, Koreans and Japanese throughout centuries' including $4{\sim}8$ century. 2. Chinese Yu had a style of wide-sleeves and right-sided collars. The traditional costumes of Han race are consisted of wide-sleeved Yu on the upper and long-skirt on the lower part of the body. Before the adoptation of HoBok during reign of King Jo Mooryung in 307. B.C., HoBok style had already found in the remains since the Sang period. There were various names among Yu during the Han period. Seup, Sean Eui, Kye, Kyu were one of the styles and several names were meant for collar and sleeves. During $4{\sim}8$ centuries, clothes of right-sided collar were found, superior to that of left-sided and narrow sleeves were widely used both the royal and the humble. Various styles of decoration were seen in Yu around neck, back and sleeves comparing other nations. 3. Yu, in Korea, was typical style of Northern-bound HoBok. Both men and women had similarity in Yu style, narrow sleeves, left-sided collar, belted at the waist and to the length of hip line. Influenced by Han race, in the $4th{\sim}8th$ centuries, dual system of collar was found. But we cannot see major change in Yu and finally was connected to the present. 4. The original design of the Japanese costumes was not similar to that of Northern nomadic hunting race, which was suitable for horse-riding activities. Owing to the climates along the island, we could see various conditions ranging from the cold and to the warm. Influenced by the climates, pulling over the neck(Pancho style) were major design in Japan. As Korea was advanced earlier than Japan, Korean landed Japanese territory showing clothes. So primitive costumes had changes in style. During the $4th{\sim}8th$ period. The Korean mode was found in Haniwa (which was built to make sacrifices to the dead King) and costumes in Jeong Chang Won. Among the costumes in Jeong Chang Won, we put 3 or more costumes to the category of Yu characterizing elements of Korea and Tang period. From the $4th{\sim}8th$ century, China, Korea, Japan fell into the same cultural category, Scythai. Styles in Yu among three nations, we saw little differences, basically along times. Originated from the West Asia, Yu was transmitted to the far East changing Chinese costumes, Koreans melted it into the traditional elements and then influenced Japan.

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동북아세아(東北亞細亞) 고(袴)의 발생(發生) 및 전파(傳播)에 관(關)한 연구(硏究) - $4{\sim}7$세기(世紀) 중심으로 - (A study on the origination and transmission of Koh(袴) in Northeast Asia-from the 4th century to 7th century)

  • 박경자;이진경
    • 복식
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    • 제15권
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    • pp.177-194
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    • 1990
  • Koh(袴) was a type of dress worn on the lower part of the body which was commonly used in the Northeast Asia. It was originally used by the Northern race for the need of nomadism or hunting. The origin of the Koh which appeared in the area would be found from the trousers of the Huns who influenced in the Northeast Asia, and became in the part of the Scythian culture. The Scythians are the nomadizing race inhabited in the Northern Caucasas on the wast of the Black Sea and influenced on the inland Eurasian steppe as the first typical horse-riding race. The objectives of Koh which had been worn in the Scythian, Mongolia, Korea as well as Japan as a part of Dongho dress and ornaments and to contemplate the transmission process by cultural exchange among different races for the period from 4th century to 7th century. 1. The Origination of the Koh The Koh was originated by the environmental factor to protect the cold in the North but also from the heat in the South, and was changed and developed as gradually satisfying to the needs of the times. In the Northeast Asia the Koh was in the class of the Northern Chinese garment, and was used widely by the horse riding Scythians who moved widely from the Eurasian inland to Japan. The oldest original which could reflect the type of the Northern clothes was a pair of trousers discovered in the Huns remains of Noin Ula. This showed the exact form of hunting clothes and had a similar form with the Korean female tro-users. Since the same form of trousers drawn on the wall painting of which was excavated 4-5th century ancient Koguryo(高句麗) tomb was the same form the trousers of Noin Ula seemed to be the original form of Koh in the Northeast Asia. 2. The Chinese Trousers It was the time of the King Mooryung(武靈王) in the Cho(趙) Dynasty B.C. 3th century that the trousers used regularly in China. However, the Koh had been used as undergarment which functioned for the protection of the cold not the horseriding garment. The trousers seemed to be not very obviously shown off since the Poh (袍) was long, but mainly used by the people from lower class. As people learned the adapted the trousers. It was essential for the times of war and quarrel. The king himself started wearing the Koh. The Chinese trousers were influenced by the Huns, the Northern clothes of the Scythian culture, and similar to the Korean clothes. 3. The Korean Trousers Korean was a race bared from the Eastern foreign group. It was obvious that the clothes was Baji-Jeogori(바지 저고리), the garment of the Northern people. This had the same form of the Scythian dress and ornaments which was excavated from the Mongolian Noin Ula. The Scythian dress and ornaments were influenced from the Ancient West Asia Empire and transmitted to the Northeast Koguryu by the horseriding Scythian. The trousers were kept in the traditional style by the common people in Korea were transmitted to Japan which were for behind in cultural aspect, as well as got used to the Chinese as the efficient clothes though active cultural exchange. 4. The Japanese Trousers The ancient Japanese clothes were influenced by the Southern factor but not the form of the Koh. As the Korean people group was moving towards Japan and conquer the Japanese in the 4-5th century, however, North Altaic culture was formed and at the same time the clothes were also developed. The most influenced clothes at this time were those of Baekge(百濟) and the trousers form called Euigon became the main form. Because of the climatic regional factor, it was tied not at the ankle but under the knee. From the view the ancient Japanese clothes disappeard about that time, it could be due to the conquest of the culturally superior race but not the transmission of the culture. In the latest 7th century both the Chinese and Japanese dress forms were present, but the Dongho(東胡) dress and its ornament from Korea was still the basic of the Japanese dress form.

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남해 및 동중국해의 하계 수질 및 저질 환경평가 (Summer Environmental Evaluation of Water and Sediment Quality in the South Sea and East China Sea)

  • 이대인;조현서;윤양호;최영찬;이정훈
    • 한국해양환경ㆍ에너지학회지
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    • 제8권2호
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    • pp.83-99
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    • 2005
  • 본 연구는 남해 근해 및 동중국해의 효율적 이용과 관리를 위한 기초연구로서 2001-2003년 6월에 수질과 저질환경 특성을 평가하였다. 연구해역 상층의 수괴는 북상하는 고온 고염의 쿠로시오 난류기원의 영향을 많이 받았고, 25 m 및 50 m층은 황해냉수의 영향을 받는 저온수가 동남향으로 확장하였고, 그리고 양자강 하구역에 인접한 정점들의 표층에서는 29.0 psu이하의 낮은 염분분포를 보였다. 수온약층은 대략 10 m층에서 형성되었고, 양자강 하구쪽으로 갈수록 얕아지고, 멀어질수록 깊어지는 경향을 나타내었다. COD(화학적 산소요구량)와 TN(총질소) 및 TP(총인)는 대부분 해역의 표층에서 해역환경기준 II등급이하를 나타내었으나, 양자강 하구역에 근접한 정점들에서는 TSS(총부유물질)농도가 급증하였고, COD근 해역환경기준 III등급을 초과하였을 뿐만아니라 영양염류도 적조발생 가능농도를 초과하는 분포를 보였다. Redfield ratio(무기질소대 무기인 비)는 2002년과 2003년에는 전 수층 평균값이 대부분 16이하의 값을 나타내었으나, 육상쪽으로 갈수록 16이상의 값을 보였다. Chl. a는 상층에서 양자강 영향지역과 남해 근해에서 상대적 고농도를, 대만난류해역에서 저농도를 보여주었고, 클로로필농도 극대층은 대략 수온과 밀도 약층 수심이나 그 하부에서 형성되었다. 대상해역으로의 영양염류 공급기구는 양자강을 포함한 담수에 의한 공급이 매우 중요한 기여를 하는 것으로 나타났고, 표층의 염분과 Chl. a는 매우 뚜렷한 음의 상관성을 나타내 어서 높은 식물플랑크톤 생물량은 영양염류의 공급과정과 직결되는 것으로 판단되었다. 또한, 이러한 Chl. a는 무기질소에 비해서 무기인과 상관성이 더 좋은 것으로 나타났고, 대상해역의 유기물질 분포에 식물플랑크톤에 의한 자생적인 기여가 큰 것으로 평가되었다. 퇴적물은 공간적으로 다소 불규칙한 변동이 있지만, 저질조성과 관련해서 양자강 하구쪽으로 갈수록 오염도가 낮고, 조사해역의 동쪽부분에서 유기오염의 정도가 상대적으로 크게 나타났지만, 그 오염도는 심하지 않는 것으로 분석되었다. 향후 본 대상해역에 있어서 산샤댐 건설과 관련된 양자강 유량의 변화, 그리고 어업활동과 관련된 폐기물에 의한 해양환경의 영향평가 및 대책 연구가 수행되어져야 할 것이다.

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