• The Journal of the Petrological Society of Korea
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• v.5 no.2
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• pp.188-199
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• 1996

Boeun granodiorite, which intruded into the metasedimentary rocks of the Ogcheon Group, show chemical natures of metaluminous and calc-alkaline. Generating and emplacing environment of the Boeun granodiorite would have been a active continental margin. Comparing to the contemporaneous Inje-Hongcheon granodiorite in the Gyeonggi massif, the Boeun granodiorite seems likely to have formed under more immature continental arc environment. Compositional changes of major, trace and rare earth elements in granodiorite and felsic dyke are not certain to indicate crystallization differentiation. From this fact, the simple fractional crystallization model would be in question to explain the magma process which controlled the formation of the Boeun granitic mass. The model calculations for Rayleigh fractionation, fractionation with variable major-component composition, assimilation-fractional crystallization (AFC) were carried out to examine the magma process of the mass. The results of former two models do not agree with the compositional variations in the mass. The AFC model can be, however, applied to the magma process. The conditions for AFC process are (1) composition of assimilated wallrock is similar to that of primary magma. (2) assimilating rate is similar to crystallizing rate, and (3) mass of assimilated wallrock is about 10% of that of the magma. These conditions deny a possibility that the assimilated wallrock was the metasedimentary rocks of the Ogcheon Group. This indicates that after having experienced the assimilation process in deeper crust, the granodiorite magma intruded into the Ogcheon group. Every model calculating suggests that the felsic dyke was differentiated not from the granodiorite magma, but from a different source magma.

• Proceedings of the Korean Information Science Society Conference
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• 2006.06a
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• pp.25-27
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• 2006

본 논문에서는 시계열 마이크로어레이데이터 마이닝을 위한 전처리 작업으로 시계열 마이크로어레이 데이터에 특징 추출 방법 및 상관관계 분석을 이용하여 분화 과정에 대해 분별력 있는 유전자들을 선정하기 위한 방법을 제안하고, 줄기세포가 신경세포로 분화하는 과정에서 특이적으로 발현되는 유전자들을 찾기 위한 시계열 마이크로어레이 데이터 분석 과정을 하나의 예로 제시한다. 분석 결과, 제안한 방법이 분화 특이적으로 발현되는 분별력 있는 유전자들, 분화 과정에서 공통적으로 발현되는 유전자들, 그리고 경계선에 존재하는 유전자들을 통해서 줄기세포 신경분화의 특징들을 규명하는데 매우 유용함을 보였다.

• KSBB Journal
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• v.10 no.3
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• pp.257-263
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• 1995

Fractional precipitation of "native" dextran by the method of nonsolvent addition was studied. Precipitational phenomenon of fractioned dextran was characterized with the quantitative determination of the precipitational capacity of nonsolvents with different dielectric constants. Based upon this characterization, the fractional precipitation process for the dextran production was developed. From the precipitational characteristics, a first-order relationship between the molecular weight of fractioned dextran and the content of nonsolvents was formulated. The slopes of the first-order equation were correlated with the dielectric constants of the nonslovents. A modified fractionation process was constructed on the basis of refractionation method and employed to increase the efficiency of the controlled production of dextran.

• Economic and Environmental Geology
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• v.54 no.1
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• pp.61-67
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• 2021

Isotopic compositions of snow or ice have been used to reconstruct paleoclimate and to calculate contribution to streamwater using isotopic hydrograph separation as an end member. During freezing and melting of snow or ice, isotopic fractionation occurs between snow or ice and liquid water. Isotopic evolution during melting process has been studied by field, melting experiments and modeling works, but that during freezing has not been well studied. In this review, isotopic fractionation during equilibrium freezing is discussed using the linear relationship between two stable water isotopes (oxygen and hydrogen) and the Rayleigh fractionation. Snow, evaporated from nearby ocean and condensated, follows the Global Meteoric Water Line (slope of 8), but the melting and freezing of snow affect the linear relationship (slope of 19.5/3.1~6.3). The isotopic evolution of liquid water by freezing observed in the open system during Rayleigh fractionation is also seen in the closed system. The isotopic evolution of snow or ice in the open system where the snow or ice is continuously removed becomes more enriched than the residual liquid water by the fractionation factor. The isotopic evolution of snow or ice in the closed system eventually equals the original isotopic compositions of liquid water. It is expected the understanding of isotopic evolution of snow or ice by freezing to increase the accuracy of the paleoclimate studies and hydrograph separation.

• Journal of the Korean Recycled Construction Resources Institute
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• v.4 no.1
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• pp.101-109
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• 2009

This CW(Construction wastes) are increasing as construction industry is growing, so many countries make efforts to recycle CW. Korea also made a stipulation for recycling CW. But the main content of this stipulation is for using recycled aggregates. Advanced countries try to increase reuse rate of not only recycled aggregate but also other kinds of wastes. So they are adopting SDM(separating dismantlement) method and we are also planning to make the system for SDM. This study is about SDM analysis through construction field investigation and difference analysis between SDM and UDM comparing predictive amount by UDM with real generated amount by SDM. First, the generated amount of construction wastes by SDM is more than estimated amount by UDM, and mixed waste was specially reduced more than UDM. The warehouse is easier than the office building to applicate SDM. But still there is no manual for SDM in the site, so establishment of SDM is demanded.

• Korean Chemical Engineering Research
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• v.60 no.3
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• pp.414-422
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• 2022

The objective of this work was to investigate the feasibility of acid-catalyzed hydrothermal fractionation for maximum solubilization of the hemicellulosic portion of two typical agricultural residues. The fractionation conditions converted into combined reaction severity (CS) in the range of 1.2-2.9 was used to establish a simple reaction criteria at glance. The hemicellulosic sugar yield of 56.6% was shown when rice straw was fractionated at the conditions at the conditions; 160 ℃ of temperature 0.75% (w/v) of H₂SO₄, 20 min of reaction time, 1:15 solid/liquid ratio. The hemicellulosic sugar yield of 83.0%, however, was achieved when barley straw was fractionated at the conditions at the conditions; 150 ℃ of temperature 0.75% (w/v) of H₂SO₄, and 15 min of reaction time, 1:10 solid/liquid ratio. For barley straw, acid-catalyzed hydrothermal fractionation could be effectively performed. After the fractionation process, the remaining fractionated solids were 48.5% and 57.5% from raw rice and barley straws, respectively. The XMG contents in the solid residues decreased from 17.3% and 17.6% to 6.0% and 2.6%, which corresponded to 16.7% and 8.5% on the basis of the raw straws, respectively. In another way, only 5.6% of cellulose and 8.5% of XMG were lost due to excessive decomposition during the acid-catalyzed hydrothermal fractionation of barley straw, compared to cellulose and XMG losses of 6.4% and 26.6% in rice straw. Hemicellulosic sugars from the rice straw were considered more over-decomposed due to the somewhat higher reaction severity at the acid-catalyzed hydrothermal fractionation.

• Korean Chemical Engineering Research
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• v.53 no.6
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• pp.831-835
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• 2015

This study evaluated the influence of the zeta potential of silica-alumina on the behavior in terms of purity, yield, and precipitate shape and size of fractional precipitation in the fractional precipitation process for the purification of (+)-dihydromyricetin. The optimal silica-alumina amount (surface area per working volume of reacting solution) for zeta potential control was $100mm^{-1}$. As the zeta potential value of silica-alumina increased, (+)-dihydromyricetin yield and precipitate size were increased. The use of silica with the highest value of the zeta potential (+4.99 mV) as a zeta potential-controlling material increased the (+)-dihydromyricetin yield by 2-fold compared with that of the use of alumina with the lowest value of the zeta potential (-19.00 mV). In addition, the (+)-dihydromyricetin yield and precipitate size was inversely correlated with the absolute value of the zeta potential. On the other hand, the purity of (+)-dihydromyricetin had almost no effect on changes in the zeta potential of silica-alumina.

• Journal of the Mineralogical Society of Korea
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• v.18 no.3 s.45
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• pp.165-181
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• 2005

The granitic rocks distributed in the southern part of the Yangsan Fault are classified into five distinct rock facies based on the field relation, petrography and geochemical characteristics. These five different rock facies can be grouped into two considering their origins. Group I, which reveals various evidences of magma mixing, includes three rock facies of granodiorite, enclave-rich porphyritic granite, and enclave-poor porphyritic granite. Group H intruding Croup I includes equigranular granite and micrographic granite with no evidence of magma mixing. It is suggested that the distinctively different trace element and isotopic chemistries between group I and II, support evolution from the different parental magma. It is suggested that the three rock facies in group I were generated by different degrees of magma mixing in addition to fractionation of plagioclase. MMEs experienced fractionation of biotite. The two facies in group H seem to have been generated from different parent magma from group I and evolved by fractionation of K-feldspar. The Rb-Sr whole-rock ages of the group I rocks yield $59.2\~58.9Ma$, and those of the group II rocks give 53. $3\~51.7Ma$, regardless of their distribution whether they occur in the eastern or western parts of the Yangsan Fault. Based on Sm-Nd isotope compositions, depleted mantle model ages $(T_2DM)$ of the group I range $0.8\~0.9Ga$, while those of the group II$0.6\~0.7Ga$.

• Proceedings of the Korea Information Processing Society Conference
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• 2000.04a
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• pp.83-88
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• 2000

본 논문은 mobile agent 시스템 설계의 예를 보인다. 본 시스템 설계에서 구축될 시스템의 사양은 자연어로 묘사되어 있다고 가정한다. 본 시스템 설계 과정은 다음과 같다. 첫째, 시스템 사양으로부터 필요한 사이트들을 분별하고, 둘째, 사이트간에 송수신 되는 정보들을 분별해, 이들 정보 개체들을 각각 한 개의 agent로 구현한다. 셋째, 각 Agent가 수행할 과업을 Petri net으로 정확히 표현한다. Agent가 정의되는 위치에 따라 필요한 통신량이 좌우됨으로 통신량을 최소화시키는 관점에서 Agent 정의의 위치를 결정한다.

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.1254-1258
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• 2008

본 연구에서는 대표적인 준분포 장기유출모형으로 널리 쓰이는 SWAT-K와 HSPF를 이용하여 충주댐유역을 대상으로 2000년부터 2006년까지의 총유출량 산정을 산정하고, 두 모형간의 총 유출량 차이를 분석하기 위해 증발산량, 지표유출량, 중간유출량, 기저유출량 등 각 수문성분별 모의결과를 비교하고, 모형별 유출특성을 분석하였다. 모의기간 연평균 유출량은 SWAT-K는 관측치에 비해 약 2%과다, HSPF는 약 3% 과소하게 모의되었고 모형의 적용 타당성을 가늠할 수 있는 결정계수는 SWAT-K가 0.78, HSPF가 0.88로 나타났다. 수문성분별로 모의치를 비교한 결과 중간 유출은 SWAT-K가, 지하수유출은 HSPF가 크게 산정되는 등 수문성분별 크기에 차이를 드러냄에 따라, 각 모형에서 수문성분을 도출하는 구조의 차이와 계산과정 등의 상세한 비교분석이 필요한 것으로 판단된다.