• Proceedings of KOSOMES biannual meeting
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• 2007.11a
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• pp.83-86
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• 2007

광양만권 개발에 따른 광양만의 매립과 준설로 인해 광양만의 급격한 지형변화가 일어나고 있다. 또한. 오염에 대한 우려가 있어 해양수산부에서는 특별관리해역으로 지정하여 관리하고 있다. 본 연구는 광양만 중앙의 묘도를 중심으로 5개의 정점을 선정하여 2005년 겨울부터 2007년 8월까지 총 8차례에 걸친 조사를 통해 장기적인 모니터링을 실시하여 환경변화에 따른 오염도를 조사하였다. 광양만의 중금속의 경우 농도의 변동양상으로 볼 때 오염원의 증가에 의한 변동보다는 계절적인 영향에 의한 변동양상으로 판단할 수 있다. 광양만에서 검출되는 중금속의 농도수준은 As를 제외한 전 항목이 US EPA 의 ERL을 초과하지 않은 것으로 조사되었다. 표층퇴적물 중 PAHs의 분석결과를 비교해 보면 지점별 농도변동양상이 뚜렷하지 않으며, 지점별 농도변화도 미약하다. PAHs 오염원의 추정의 결과 조사시기별 전 지점에서 분석한 결과, 몇 지점에서는 유류기원에 의한 오염의 경향이 보이는 반면 그 외의 대부분의 조사지점에서는 연소기원에 의한 PAHs 물질의 분포를 보였다.

• Journal of the Society of Cosmetic Scientists of Korea
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• v.25 no.2
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• pp.45-57
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• 1999

Melanocytes, derived from neural crest, make melanin and protect skin from the hazardous ultraviolet light. Melanocytes with dendritic process has similar morphology with neurogenic cells and share growth factor receptors such as neurotrophin receptors. Melanogenesis can be regulated by ultraviolet light and inflammation of the skin. In addition, several factors such as hormone, cytokines, arachidonic acid can affect the proliferation and melanogenesis of melanocytes. For melanogenesis, melanocytes need expression of various genes including tyrosinase, TRP-1, TRP-2. In addition, melanin need to be transferred from melanocytes to surrounding keratinocytes. The biology of melanocytes is complex and mechanism of melanocytes proliferation and melanogenesis is still under the investigation.

• Proceedings of the Korea Water Resources Association Conference
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• 2022.05a
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• pp.473-473
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• 2022

일차생산은 화학합성 또는 광합성에 의하여 무기탄소가 유기물질로 전환되는 것을 의미한다. 수중의 일차생산자는 광합성을 통하여 유기물을 해당 수역에 공급하는 기능을 수행하며, 이는 수역의 상위 먹이 단계의 총생산력을 결정하는 주요 구성원이다. 한강은 하류로 갈수록 유속이 느리지만 수심이 깊어져 부착조류가 서식하기 쉽지 않은 환경이기에 대부분의 일차생산자는 식물플랑크톤이다. 과거 1994년 이후로 2017년까지 5년 간격으로 총 6회 연구된 결과, 해당 하천의 부영양화가 여름철에 발생하였다. 팔당댐 방류량과 지류의 유입에 의한 유기물 증가로 하천 내 1차 생산의 기여도가 증가하고 있으며, 이는 유기물 근원을 판정하여 수질오염에 대한 처리대책을 위해 지속적으로 연구가 필요하다. 따라서 본 연구는 한강본류에서 식물플랑크톤의 일차생산력을 조사하고, 유기물의 분해속도를 측정하여 당해 유역의 유기물 수지를 추정하여 한강 고유의 특성을 파악하여 부영양화에 의한 유기물 증가로 발생할 수 있는 수질오염을 예측하고자 한다. 조사유역은 한강의 팔당댐 방류구로부터 신곡수중보까지 전 구역 중 총 12개의 지점을 선정하였다. 기간은 2021년 5월부터 2022년 3월까지 계절별 2회로 총 8회 조사를 실시하였으며, 한강본류에서는 식물플랑크톤의 산소소비법을 통해 일차생산력과 유기물 분해속도를 조사하여 내부기원 유기물을 측정하였고, 한강본류로 유입되는 4개의 유입하천에서는 COD를 조사하여 외부기원 유기물을 측정하여 한강에서 발생하는 총유기물량을 산정하였다.

• Journal of the Korean Geographical Society
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• v.42 no.6
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• pp.898-913
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• 2007

We examined soil properties and provenance of loess-paleosol sequences at the Daebo Granite area of Buan, Jeonbuk Province, South Korea. The section consists of the surface layer, Layer 1(paleosol), Layer 2(loess), Layer 3(paleosol), Layer 4(loess), and Layer 5(paleosol), from top to bottom and thickness of the exposed section is approximately 280cm. The magnetic susceptibility values show the distinct variations between the loess- and the paleosol layer. Even though pH, ORP, water content, and soil hardness do not display the obvious differences in the section, the organic content indicates the variation similar to those of the magnetic susceptibility. In the respect of the soil colors measured under 3 conditions, although the variations of the wet soil color exceedingly reflect the difference of the layers, these variations are obscure in some points in the section due to the characteristics of the Munsell color system. Based on the geomorphological properties, sedimentary structure, the difference of the major element composition and the condrite-normalized rare earth element(REE) patterns showing the clear difference from the adjacent bedrocks and stream sediments and the similarity to those of the Chinese Loess Plateau, it is suggested that the section was formed by the material originated from the Chinese Loess Plateau and peripheral areas. However, because the material experienced the alteration after sedimentation under the environment of the sediment area, it has the properties different from the material in the provenance areas. This phenomenon may result in the climatic condition of Korea, especially in precipitation.

• Journal of the Korean earth science society
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• v.25 no.4
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• pp.222-231
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• 2004

The purpose of this study is to analyze the seventh curriculum textbooks and teacher's guides of high school science courses in relation to the generation (mechanism) of magma in subduction boundary and find the incorrect descriptions of the texts and the figures (illustrations) and then suggest some improved schemes. According to the result there are many discrepancies in definition of 'magma' among the textbooks and further little scientific explanations about the formation mechanism of magma in most textbooks, and even no descriptions about that. In addition, the figures are inconsistent with the description of the text and also have some incorrect depiction which might contribute to the forming and reinforcing misconceptions about Plate Tectonics as well as a volcanic activity in subduction boundary. On the basis of the previous researches, therefore, some improved schemes (text descriptions and figures) are suggested. The results of this study should be used as a reference for publishing science textbook, developing science curriculum, and teaching effectively in the high school.

• 사회경제평론
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• v.31 no.3
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• pp.271-305
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• 2018

Today we live in the Hyper-Connected Society. The Hyper-Connected Society is the network society connected with hyper-connectivity. We know that this technical substructure of hyper-connectivity is the 4th industrial revolution. In this paper, I want to find the origin of the Hyper-Connected Society by clarifying the pattern of the staged development of industrial revolution. The variation pattern of technical revolution including industrial revolution can be summarized very simply as follows; (1) technical revolution ${\rightarrow}$ network revolution, (2) network revolution화 ${\rightarrow}$ the variation of social network, material revolution${\rightarrow}$spiritual revolution. The pattern of the staged development of industrial revolution is as follows. Therefore, in the aspects of network revolution, the origin of the Hyper-Connected Society is the railroad revolution in USA after 1840.

• Korean Journal of Agricultural and Forest Meteorology
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• v.9 no.1
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• pp.61-70
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• 2007

This study was conducted to investigate nutrient dynamics and water quantity of throughfall and stemflow in natural oak stands in Korea. The ratio of the total throughfnll and stemflow to the amount of precipitation varied with locations. It was considered that the ratio was affected not only by the characteristics of tree species but also by regional, weather and other environmental conditions. It was, therefore, necessary to set up a water control system to launch a tending project for natural oak stands. Comparisons of nutrient amount in throughfall among regions reflected regional characteristics. $Ca^{2+},\;Mg^{2+}$ and $K^+$ ions were leached from the canopy and yellow sand accumulation. $Na^+$ and $Cl^-$ were marine-borne. $NO_3^-$ and $SO_4^{2-}$ resulted from dry deposition of air pollutants. Nutrient amount in the stemflow was as low as about 10% of that in the total throughfall and stemflow. The pH of stemflow in natural oak stands in urban areas ranged from 3 to 5. Influx of the acidic stemflow to soil could, in the long term, affect pH in soil solution and nutrient dynamics around root zones.

• Journal of Korean Society of Environmental Engineers
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• v.29 no.5
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• pp.540-547
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• 2007

Humic substances(HS) from Han River water was physic-chemically isolated by fractionational methods to investigate the seasonal distribution and to characterize the properties compared with intrinsic humic materials. Various HS samples were analyzed by element, Fourier transform infrared(FT-IR), proton nuclear magnetic resonance$(^1H-NMR)$ and fluorescence analyzers. The portion of HS from Han River water(HRHS) was 47.0% on the average, however it appeared that rainfall event brought about higher fraction of HS in Han River water by the periodic investigation. Aromaticity and humification degree of the HRHS were relatively lower than those of intrinsic humic materials originated from decomposing vegetation. FT-IR, $^1H-NMR$ and fluorescence spectroscopy showed the distinct differences between HRHS and intrinsic humic materials. Commercial humic materials could not represent structural and functional characteristics of local HS. The fluorescence spectroscopy, a relatively simple measurement, was found most useful tool to estimate humification degree for humic materials from particular sources.

• Economic and Environmental Geology
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• v.42 no.4
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• pp.315-333
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• 2009

In this study, the hydrochemical and the isotopic characteristics of major streams in the Daejeon area were investigated during rainy and dry seasons. The stream water shows the electrical conductivity of the range of $37{\sim}527{\mu}s$/cm, and pH $6.21{\sim}9.83$. The chemical composition of stream waters can be grouped as three types: the upper streams of Ca(Mg)-$HCO_3$ type, Ca(Mg)-$SO_4(Cl)$ type of middle streams flowing through urban area, and Na(Ca)-$HCO_3$(Cl, $SO_4$) type of the down streams. Based on in-situ investigation, the high pH of stream waters flowing through urban area is likely to be caused by the inflow of a synthetic detergent discharging from the apartment complex. The electrical conductivity of stream waters at a dry season is higher than those of at a rainy season. We suggest that the hydro-chemical composition of stream waters in the Daejeon area was affected by the discharging water from the sewage treatment facilities and anthropogenic contaminants as well as the interaction with soil and rocks. ${\delta}D$ and ${\delta}^{18}O$ values of the stream waters show the relationship of ${\delta}D=6.45{\delta}^{18}O-7.4$, which is plotted at a lower area than global meteoric water line(GMWL) of Craig(1961). It is likely that this isotopic range results from the evaporation effect of stram waters and the change of an air mass. The isotope value shows an increasing trend from upper stream to lower stream, that reflects the isotopic altitude effect. The relationship between ${\delta}^{13}C$ and $EpCO_2$ indicates that the carbon as bicarbonate in stream water is mainly originated from $CO_2$ in the air and organic materials. The increasing trend of ${\delta}^{13}C$ value from upper stream waters to lower stream waters can be attributed to the following reasons: (1) an increasing dissolution of $CO_2$ gas from a contaminated air in downtown area of the Daejeon, and (2) the increment of an inorganic carbon of groundwater inflowed into stream by base flow. Based on the relationship between ${\delta}^{34}S$ and $SO_4$ of stream waters, the stream waters can be divided into four groups. $SO_4$ content increases as a following order: upper and middle Gab stream${\delta}^{34}S$ value decreases as above order. ${\delta}^{34}S$ value indicates that sulfur of stream waters is mainly originated from atmosphere, and is additionally supplied by pyrite source according to the increase of sulfate content. The sulfur isotope analysis of a synthetic detergent and sewage water as a potential source of the sulfur in stream waters is furtherly needed.

• Economic and Environmental Geology
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• v.28 no.1
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• pp.25-31
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• 1995

In Dongnam area, Cretaceous igneous rocks, such as diorite, porphyritic granite, and quartz porphyry intruded Paleozoic sedimentary rocks, such as Myobong slate and Pungchon limestone. The Dongnam Fe-Mo skarn deposits were imposed on the diorite(endoskarn) and the Myobong slate(exoskarn). The ore deposits consist mainly of magnetite and molybdenite with small amounts of sulfides, such as galena, sphalerite, pyrite, chalcopyrite, and pyrrhotite. The igneous rocks show nearly constant $^{206}Pb/^{204}Pb(18.80{\sim}19.06)$ and $^{207}Pb/^{204}Pb(15.71{\sim}15.72)$ ratios. Their $^{207}Pb/^{204}Pb$ ratios higher than the typical ratios of orogene suggest that the igeneous rocks were formed from lower crust(or mantle) - derived magma excessively contaminated by upper crustal materials such as high radiogenic Precambrian basement rocks. The lead isotopic compositions of the igneous rocks, the Pungchon limestone, and the ore minerals show a well defined linear in $^{206}Pb/^{204}Pb$ - $^{207}Pb/^{204}Pb$ plot. The lead isotopic compositions of the igneous rocks are similar to those of magnetite and galena, which were formed at early skarn stage and significantly lower than those of altered quartz porphyry, molybdenites, and pyrite, which were formed at late epithermal alteration stage. Considering the systematic variation of the lead isotopic compositions in the ore minerals according to hydrothermal stages, the variation may be due to a relative variation in surrounding rock(Pungchon limestone) involvement in hydrothermal ore solution leaching the surrounding rock. Therefore, the variation of the lead isotopic compositions in ore minerals can be modeled in terms of the mixing of the leads derived from the igneous rocks as low radiogenic source and the surrounding rock(Pungchon limestone) as high radiogenic source.