• Journal of The Geomorphological Association of Korea
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• v.21 no.4
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• pp.19-40
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• 2014

Rock rebound values and chemical compositions of Gamak island at Sangha, Gochang, Jeollabuk do are analysed as a part of geomorphic survey of that area. Some corestones are formed by deep weathering found from the summit of rock mass of Gamak island, while the rocks a part of weathering front are exposed at the foot of the island. Rebound values of rock increase toward coastal plain, so summit would be weak in resistance to erosion. It can be assumed that chemical weathering is more active at the summit by the chemical index of alteration and changes in chemical composition ratio. However it should be mentioned that the samples are taken from the surface of the rock mass that more fresh part will be exposed when the weathered parts are removed. The chemical composition and CIA values of the polygonal cracks found from on the surface of weathering rind showed that this part has values between those of the summit and the footslope. The bottom of weathering rind with polygonal cracks has higher CIA value than those of the surface. Though it supports the result from the Bisul Mt., there also difference in the ratio of SiO2. It looks caused by the difference in weathering environment and chemical difference in parent rock. In summary Gamak island is the remnants of weathering front after removal of weathered material. The removal processes are more active at the footslope where the coastal processes are stronger than the summit.

• The Journal of the Petrological Society of Korea
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• v.19 no.3
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• pp.181-197
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• 2010

This study is for finding a geoscientific factor for clarifying the source soil of the ancient earthenware finding. The used samples were the earthenware, soil and rocks, which were collected at the Gyeongju, Gyeongsan and Haman area. The chemical and mineralogical study for the samples were carried out for understanding the change of mineralogical and chemical composition among them. The mineralogical compositions of the earthenware are different from those of the soils from the surrounding area, which suggests that the mineralogical approach for clarifying the source soil of the earthenware should be difficult. Major element compositions of the earthenware also are different from those of the surrounding soils, which suggests that the comparison of the chemical composition using the major elements might be difficult for deducing the source soil of the earthenware. However, PAAS-normalized rare earth element (REE) patterns and Nd model ages among the rock, soils and earthenware from the same sampling sites show similar characteristics one another compared to those of the major element compositions. Nd-Sr isotopic systematics among the earthenware, soils and rocks also show a close relationship. Our results suggest that REE and Nd-Sr isotope geochemistry might be more useful than the other geochemical technique in clarifying the source soils of the ancient earthenware.

• Proceedings of the Korean Vacuum Society Conference
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• 2010.02a
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• pp.71-71
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• 2010

최근 나노선의 우수한 전기적, 광학적 특성을 다양한 종류의 전자소자, 광소자, 그리고 센서에 응용하는 연구가 활발히 진행되고 있다. 그 중 $SnO_2$ 나노선은 n-type의 전기특성과 우수한 광 특성을 보이며, 전자소자, 광소자 뿐 아니라 다양한 종류의 가스 센서 제작에 널리 사용되고 있다. 본 연구에서는 화학기상증착법 (Chemical Vapor Deposition)으로 $SnO_2$ 나노선을 성장하여 전계방출효과 트랜지스터 (field effect transistor: FET)를 제작하여 전기적 특성을 측정하였다. 나노선의 성장 조건 (온도와 산소 유량) 에 따른 나노선의 구조, 화학조성, 전기적 특성을 체계적으로 조사하였다. 산소의 유량이 낮을 때는 온도에 따라 나노선의 크기와 전기 특성에 변화가 없었으나, 산소의 유량을 높이면 온도에 따라 나노선의 두께와 전기적 특성이 크게 변화하였다. 본 연구에서는 특히, FET 구조에서 on/off current ratio 가 $10^5$ 이상으로 매우 높은 나노선 제작이 가능하였다. 전기적 특성과 나노선의 결정구조, 화학적 조성을 함께 비교하여 성장 메커니즘을 이해하고자 한다.

• Bulletin of Korea Environmental Preservation Association
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• v.15 no.6
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• pp.33-38
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• 1993

• Bulletin of Korea Environmental Preservation Association
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• v.15 no.5
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• pp.15-19
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• 1993

• Bulletin of Korea Environmental Preservation Association
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• v.15 no.4
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• pp.21-24
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• 1993

• Bulletin of Korea Environmental Preservation Association
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• v.15 no.3
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• pp.18-22
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• 1993

• Monthly Duck's Village
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• s.34
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• pp.31-35
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• 2005

• The Journal of Engineering Geology
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• v.27 no.1
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• pp.1-7
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• 2017

Seawater intrusion was evaluated using electrical conductivity, chemical proxies, and oxygen isotopic compositions in coastal area. It seems that groundwater in the area where the electrical conductivity is over $3,000{\mu}S/cm$ is influenced by seawater. However, it is very difficult that seawater intrusion is distinguished from other contaminants using the electrical conductivity. The chemical proxies and oxygen and hydrogen isotopic compositions can quantitatively estimate seawater intrusion. However, these method is a costly disadvantage. Therefore, firstly, groundwater contamination by seawater intrusion was evaluated using electrical conductivity and then the additional chemical and isotopic analysis were conducted in areas where possibility of contamination by seawater intrusion is high. These systematic analytical method can reduce analytical cost to quantitatively evaluate influence of seawater intrusion on coastal groundwater and may improve efficiency of analytical method for seawater intrusion.

• The Bulletin of The Korean Astronomical Society
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• v.44 no.1
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• pp.73.1-73.1
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• 2019

성간 물질의 분광선 관측을 통해 측정된 분자들의 기둥 밀도 사이에 상관 관계가 존재하는 것이 알려져 있다. 가령 같은 시선 방향을 따라 측정된 H2, CO, CH 분자의 기둥 밀도가 서로 선형 상관 관계를 갖고 있음이 최근 밝혀졌다. 이러한 분자들의 상관 관계는 분자 구름의 물리, 화학적 기원 및 성질과 관련이 있을 것으로 추측되지만 아직까지 상관 관계를 설명하기 위한 연구는 활발히 이루어지지 않고 있다. 본 연구에서는 성간 물질 혹은 구름 모형의 전산 모사를 통해 이러한 상관 관계를 재현함으로써 성간분자 구름의 물리적 특성, 화학적 조성, 그리고 환경 변수들을 영향을 이해하려고 한다. 성간 분자 구름의 화학적 조성이 시간에 따라 변화하는 것을 계산하기 위해 Astrochem을 이용하였다.