• 약학회지
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• 제21권2호
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• pp.110-114
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• 1977

The purified .omicron.-iodobenzoic acid-$^{131}$ I, sodium iodide-$^{131}$I and mixtures of those compounds were applied to radio paper or radio thin layer chromatography to select the developing solvents with useful separation efficiency. The separation efficiencies were checked by radiochromatogram sacnnings. It has been found that the two dimensional radio paper chromatogrphy using the solvent systems of 8% phenol and butanol-glacial acid-water (4:1:1 v/v) and the radio thin layer chromatography using alumina gel plate and butanol- glacial acetic acid- water (4:1:1 v/v) are both efficient. In this method, the Rf value of .omicron.-iodobenzoic acid-$^{131}$ I and the unbound $^{131}$ I is 0.48, 0.85 and 0.15, respectively.

• 한국제4기학회지
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• 제16권2호
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• pp.39-56
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• 2002

The results of geoarchaeological studies of the prehistoric cultural complexes on the Russian Far East (Primorye, or Maritime Province; the Amur River basin; and Sakhalin Island) are presented. Upper Palaeolithic sites are dated to ca. 40,000-10,500 B.P. They existed during the mild climate of the Chernoruchie interstadial (ca. 40,000-21,000 B.P.); during harsh climate at the Last Glacial Maximum, ca. 20,000-18,000 B.P., in several places on the Russian Far East (Primorye, Amur River basin, and Sakhalin); and during climatic amelioration in the Late Glacial time, ca. 16,000-10,500 B.P. The earliest Neolithic sites, represented by Osipovka and Gromatukha cultures, existed at ca. 13,000-10,000 B.P. in the environment of coniferous forests with admixture of broadleaved taxa. Since ca. 8000 B.P., Neolithic cultures appeared in all of the Russian Far East. They existed until ca. 3000 B.P., first during the Holocene Climatic Optimum, ca. 8000-5000 B.P., in the environment of coniferous-broadleaved forests, and later, at ca. 5000-3000 B.P., in the environment of birch-oak and coniferous forests.

• 동굴
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• 제42권2호
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• pp.7-16
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• 1995

Karst in Arctic and Subarctic region in North America contains a wide variety of surficial karst landform characteristics due to not only extensive glacial activities, but also interglacial karst processes during the Pleistocene age.(omitted)

• 한국제4기학회지
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• 제21권2호
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• pp.62-63
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• 2007

• 한국제4기학회지
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• 제21권2호
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• pp.64-67
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• 2007

• Journal of the korean society of oceanography
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• 제33권3호
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• pp.80-89
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• 1998

Three cores were taken from the northwest Pacific Ocean (Shikoku Basin) to determine the accumulation rates of both biogenic and terrigeneous fractions since the last penultimate interglacial period. The sediment is characterized by large amounts of terrigenous materials with low biogenic fractions and intermittent volcanic-ash layers, suggesting a hemipelagic origin. Composition of major elements shows no significant differences among sites. Relatively small variation of TiO$_2$/Al$_2$O$_3$ ratios with respect to SiO$_2$ content is the strong evidence for the common origin of terrigenous materials. The fraction of biogenic carbonates varies from near 0% in ash layers to about 35%, with a gradual increase toward the south (St. 4 through St. 6 to St. 20). However, carbonate contents show step-wise increasing tendency from St. 4 through St. 6 to St. 20, which suggests a southward increase of carbonate production. The color reflectance indicates that the sediment of the southern sites contains relatively higher amounts of biogenic carbonates. The mass accumulation rate of terrigenous fractions during the glacial period was 2-3 times higher than that of interglacial period. This enhanced mass accumulation rate of terrigenous materials was concomitant with the high accumulation rate of biogenic fractions. The total sediment accumulation rate is considered as the most important factor controlling mass accumulation rates of the biogenic and terrigenous materials. The enhanced sediment accumulation during the glacial periods is interpreted as a consequence of climate-induced change in the supply of eolian dust from the Asian continent. Enhanced wind strength during the glacial time may have increased transportation of terrigenous materials to the ocean. Thus, variation of sediment accumulation is highly linked with climatic variations.

• 한국콘텐츠학회논문지
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• 제16권10호
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• pp.701-710
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• 2016

봉준호 감독의 그동안 영화에 나타난 시선이 국내문제에 국한된 내용이었다면 <설국열차>에서는 세계와 인류, 그리고 인간의 미래에 대한 시선으로 바뀌었다. 그의 영화 속에 나타나는 이미지들이 성서와 신화에 있는 이야기와 많은 부분이 그 의미를 같이한다. 영화에 나타난 감독의 철학적 세계를 기독교적 세계관과 동양의 순환사고로 살펴보고 이야기 구조에서 <설국열차>는 빙하기 이전과 열차에서 보낸 17년의 빙하기, 그리고 빙하기 이후로 표현되어 지고 있으며 이 이야기 구조는 이스라엘 민족이 애굽 탈출 이전과 40년의 광야 생활, 그리고 가나안 입성으로 알레고리 되어 있다. 성서에서의 종말은 완전한 파국을 의미하는 것은 아니며 새로운 시대를 열고 하나님과 새로운 언약을 맺으며 영원한 삶을 영위하는 새 하늘과 새 땅에 대한 염원이 담겨져 있다. 봉준호 감독이 인류의 미래에 대한 상상이 그동안과는 전혀 다른 의미로 전개된 <설국열차>를 알레고리로 해석하여 감독이 표층 위에 투사한 이미지 아래에 자리한 또 다른 의미를 설명하고자 한다.

• 한국제4기학회지
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• 제17권2호
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• pp.33-38
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• 2003

This study is conducted to examine the data of climate or environmental change in the northeastern Asia during the last glacial maximum. A remarkable feature of the 18,000 BP biome reconstructions for China is the mid-latitude extention of steppe and desert biomes to the modem eastern coast. Terrestrial deposits of glacial maximum age from the northern part of Yellow Sea suggest that this region of the continental shelf was occupied by desert and steppe vegetation. And the shift from temperate forest to steppe and desert implies conditions very much drier than present in eastern Asia. Dry conditions might be explained by a strong winter monsoon and/or a weak summer monsoon. A very strong depression of winter temperatures at LGM. has in the center of continent has influenced in northeast Asia similarly. The vegetation of Hokkaido at LGM was subarctic thin forest distributed on the northern area of middle Honshu and cool and temperate mixed forest at southern area of middle Honshu in Japan. The vegetation landscape of mountain- and East coast region of Korea was composed of herbaceous plants with sparse arctic or subarctic trees. The climate of yellow sea surface and west region of Korea was much drier and temperate steppe landscape was extended broadly. It is supposed that a temperate desert appeared on the west coast area of Pyeongan-Do and Cheolla-Do of Korea. The reconstruction of year-round conditions much colder than today right across China, Korea and Japan is consistent with biome reconstruction at the LGM.

• 한국지역지리학회지
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• 제15권2호
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• pp.192-203
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• 2009

본 연구에서는 남강 최상류부의 지우천 유역을 대상으로 침식분지 내 퇴적지형의 형성과정을 고찰하였다. 퇴적 지형의 형태적 특성과 퇴적상 분석을 통하여 밝혀진 형성과정을 요약하면 다음과 같다. 첫째, 사평, 응암, 내동뒷들 지점의 고위퇴적지는 최종빙기 동안의 한랭한 주빙하 환경하에서 젤리플럭션 작용으로 퇴적되었으며, 상류에서 하류방향으로 하상비고가 낮아진다. 고위퇴적지의 범위는 지우천과 남강이 합류하는 곳에서 하류방향 약 1km지점인 것으로 추정된다. 둘째, 장승불들 지점에 분포하는 완경사면의 퇴적물은 심층풍화된 기반암이 완만한 사면을 형성한 이후 최종 빙기 동안 젤리플럭션 작용으로 운반된 것이다. 셋째, 사평, 용추사, 등방들 지점의 저위퇴적지는 후빙기의 온난습윤한 환경하에서 고위퇴적지가 개석되는 동안 퇴적물의 일부가 하상에 남겨지고, 이후 고위퇴적지의 개석이 완료됨에 따라 하천의 저항(퇴적물양)보다 하천의 운반력이 초과함으로써 하상이 다시 침식되어 형성된 것으로 사료된다.

• 약학회지
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• 제52권1호
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• pp.20-26
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• 2008

2-Aminothiazole ring as a bioisoster of catechol in dopamine has provided with good oral availability and lipophilic property. Selenium was reported to have an improved antioxidant ability and to reduce the loss of dopamine. 2-Aminoindan, is a rigid form of dopamine, was evaluated as a dopamine agonist with low neurotoxocity. In order to develop a novel dopamine agonist, we tried to synthesize the selenazoloaminoindan derivative that is a hybrid structure of aminoindan and aminoselenazole instead of aminothiazole. 2-Indanone-2-oxime was reduced with $TiCl_4$ and $NaBH_4$ to form 2-aminoindan, which was reacted with propionyl chloride to give 2-N-n-propionylaminoindan (2). Compound 2 was reduced with $TiCl_4$ and $NaBH_4$ to afford 2-N-n-propylaminoindan (3) and it was nitrated and reduced to form 5-amino-2-N-n-propylaminoindan (5), which was reacted with KSeCN, $Br_2$, and glacial acetic acid to give 4,6-dibromo-5- amino-2-N-n-propylaminoindan (7) instead of selenazole ring formation. Otherwise, compound 2 was nitrated and hydrogenated to form 5-amino-2-N-n-propionylaminoindan (9), which was treated with KSeCN, $Br_2$, and glacial acetic acid to give 4,6-dibromo-5-amino-2-N-n-propionylaminoindan (10). Compound 9 was cyc1ized with KSeCN and glacial acetic acid in the absence of $Br_2$ to give 6-amino-2-N-(n-propionylamino)selenazolo[4,5-f]indan (11).