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중국 복건성(福建省) 토루(土樓) 커뮤니티 가치의 1인 가구 공간에의 융합 가능성에 대한 연구
김규랑(Kim, Gyu rang),정미선(Chung, Mi sun) 한국전시산업융합연구원 2020 한국과학예술융합학회 Vol.38 No.3
본 연구는 1인 가구의 커뮤니티 부재를 해소하고자 시작되었다. 본 연구는 중국 복건성(福建省) 토루(土樓)의 커뮤니티를 분석하여 해결 방향을 찾는 것이다. 1인 가구는 2019년 기준 전체 가구 2천11만6천 중 598만7천(29.8%)으로 우리 사회에서 가장 보편적인 가구 형태로 볼 수 있다. 1인 가구에는 다양한 문제가 있지만, 그중 심리적 불안감에 주목하였다. 아무리 혼자 사는 것을 택했다 하더라도, 심리 문제는 다른 사람과 커뮤니티를 맺어야 해소되는 문제라 할 수 있다. 따라서 본 논문은 그 해소 방법으로 커뮤니티를 제시하고자 시도하였다. 1인 가구의 문제에 관한 연구는 꾸준히 진행되었으나, 과거에서부터 그 해답을 찾고자 하는 접근으로 연구한 사례는 부족하다고 볼 수 있다. 중국 복건성(福建省) 토루(土樓) 600년째 커뮤니티가 유지되고 있는 공간이며, 1인 가구가 필요로 하는 개인적인 공간과 다수 커뮤니티 공간의 조화를 유지 하고 있다. 따라서 본 연구의 목적은 복건토루의 커뮤니티 요소를 현대 공간의 커뮤니티에 적용할 수 있는 요소를 분석하는 것이다. 첫째, 토루에 대해 기본적인 배경지식을 조사한다. 둘째, 토루의 커뮤니티 요소를 알아보고 실제 공간의 쓰임새와 방법에 대해 분석한다. 셋째, 토루의 커뮤니티 요소가 현대 공간에 적용될 수 있는 방안에 관해 연구한다. 이러한 연구 결과를 바탕으로 복건토루의 개념과 커뮤니티를 현대적 공간 시각에서 어떻게 적용될 것인지에 대해 연구, 분석하여 1인 가구의 문제를 완화하는데 적용되기를 기대한다. This study was conducted to find a solution direction by analyzing the community of Fujian(福建省) Tulou (土樓) in order to resolve the lack of community of single households. According to 2019 based living arrangement statistics, single households in Korea account for 5,987,000 of 20,116,000 (29.8%). So, that is the most common form in nowadays. Most single households has many problems, I paid attention to psychological anxiety. No matter how much people choose to live alone, it is a problem that needs to be resolved by forming a community. So ‘community’ is needed to alleviate the psychological problems of a single households. They are a lot of thesis exist on the problem of single households, but there are not enough cases that looking for answers in the past cases. The Fujian Tulou is a space that has been maintained for 600 years, maintaining the harmony between the personal space and community space. Therefore, In this thesis, the transition was made focusing on Fujian Tulou. I research and analyze what is Fujian Tulou"s main concept and how their community are applied from the perspective of modern space. And search for direction of potential to the problem that single households. First, I will investigate the basic background knowledge of Fujian Tulou. Second, I analyze Fujian Tulou"s community elements. Thirdly, I will study a method in which Fujian Tulou"s community element can be applied to contemporary space. Based on the results of these studies, I study and analyze how Fujian Tulou"s concept and community are applied from the perspective of modern space. And I also expect that alleviate the psychological problems that single households has.
옥천변성대내(沃川變成帶內)에 분포(分布)하는 우라늄광상(鑛床)의 동위원소(同位元素) 지구화학적(地球化學的) 연구(硏究)
김규한,Kim, Kyu Han 대한자원환경지질학회 1986 자원환경지질 Vol.19 No.no.spc
Black and graphite slates from the Okcheon metamorphic belt contain enriched values of uranium (average 200~250ppm) and molybdenum (average 150~200ppm). Uranium mineralization is closely associated with quartz and sulfide veinlets which are formed diagenetically in graphite slate. The uranium minerals were concentrated in outer part of graphite nodules. The ${\delta}^{13}C$ values of organic carbon from the metasediments including uranium bearing graphite slate range from -15.2 to -26.1‰ with a mean of -23.5‰. Meanwhile, ${\delta}^{13}C$ values of coal and coaly shale from some Paleozoic coal fields of South Korea vary from -19.4 to -23.9‰ with an average of -22.5‰. Isotopic compositions of vein calcite in uranium bearing slate range from -13.4 to -15.4‰ in ${\delta}^{13}C$ and +11.3 to +15.1‰ in ${\delta}^{18}O$ could indicate a reduced organic carbon source isotopically exchanged with a graphite of biogenic origin. Metamorphic temperature determined by a calcite-graphite isotope geothermometer was 383~$433^{\circ}C$ which corresponded to greenschist facies by Miyashiro (1973) and is consistent with metamorphic facies estimated by mineral assemblages (Lee, et al., 1981, and Kim, 1971). The fixation of uranyl species by carbonaceous matter in marine epicontinental environment, and remobilization of organouranium by diagenetic processes have attributed to the enrichment of uranium and heavy metals in the graphite slate of Okcheon metamorphic belt.
추가령(標哥嶺) 지구대(地構帶)의 지질구조(地質構造), 고지자기(古地磁氣) 및 암석학적(岩石學的) 연구(硏究)
김규한,김옥준,민경덕,이윤수,Kim, Kyu Han,Kim, Ok Joon,Min, Kyung Duck,Lee, Youn Soo 대한자원환경지질학회 1984 자원환경지질 Vol.17 No.3
Petrological, paleomagnetic, geomorphological and structural studies on the southern part of, so called, Chugaryeong rift valley, have been carried out in order to clarify the nature of the rift valley. Three stages of volcanic activities characterized by Jijangbong acidic volcanic rocks and tholeiitic and andesitic basalt of Cretaceous age(?), and Jongok Quaternary olivine basalt occurred along the Dongducheon fault line. Jijangbong acidic volcanic rocks distributed in the central part of the studied area consist of rhyodacite, acidic tuff and tuff breccia, which are bounded by Dongsong fault on the east and Daegwangri fault on the west. The Jongok basalt differs from those of Ulrung and Jeju islands in mineralogy, chemical composition and differentiation. Jongok basalt distributed along the Hantan river dilineates the vesicles curved toward downstream direction and increment of numbers and thickness of lava flow toward upstream direction. These facts suggest that lava flowed from upstream side of the river. Rectangular drainage patterns also support the presence of the Dongducheon, Pocheon, Wangsukcheon and Kyonggang faults which were previously known. LANDSAT image, however, does not show any lineaments which could be counted as a graben or rift valley. Displacement of Precambrian quartzite and Jurassic Daedong supergroup along the southwestern extension of the Dongducheon fault shows the right lateral movement. The Paleomagnetic study of the tholeiitic and andesitic basalts from Baegeuri, Jangtanri and Tonghyeonri located at 2. 3km east, 0km east, and 1.5km west of Dongducheon fault respectively shows that their VGP(Virtual Geomagnetic Pole) being to intermediate geomagnetic field of short duration which suggests that they formed in almost same period. Mean VGP of Jongok basalt is located 82.4N and 80.6E. This is in good coincidence with worldwide VGP of Plio-Pleistocene indicating that Jongok basalt was extruded during Plio-Pleistocene epoch, and suggesting that the studied area has been tectonically stable since then. From the present study, the tectonic episode of the region is concluded as following three stages. 1. The 1st period is worked by the Daebo orogeny of Jurassic during which granodiorite was intruded in Precambrian basement. 2. The 2nd period is the time when right lateral strike-slip fault of NNE-SSW direction was formed probably during late Cretaceous to Paleogene and the Jijangbong acidic volcanic rocks and the older basalts were extruded. 3. The 3rd period is the time when the fault was rejuvenated during Pliocene or Pleistocene accompanied by the eruption of Jongok basalt. As a conclusion, geologic structure of the studied area is rather fault line valley than graben or rift valley, which is formed by differential erosion along the Dongducheon fault suggesting a continuation of the Sikhote-Alin fault. The volcanic rocks including the Jijangbong acidic rocks, tholeiitic-andesitic basalt and olivine basalt are associated with this fault line.