• 암석학회지
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• 제8권1호
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• pp.1-13
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• 1999

The Latite Ridge Latite in the East Tintic volcanic field, Utah in USA occurs as a welded ash-flow tuff, has 63.7-66 wt% $SiO_2$ on an anhydrous basis, and shows calc-alkaline affinities. The rocks fall in the trachyte field of IUGS classification. It is characterized by unusally high $K_2O$ content (5.9-7.6 wt%), relatively high equilibration temperature (950-973$^{\circ}C$), and biotites with high $TiO_2$ content (7.4-8.2wt%). Various differentiation processes were tested using the XLFRAC program to infer the origin of the Latite Ridge Latite. The results suggests that crystal fractionation from shoshonite is one possible process to generate the Latite Ridge Latite. Shoshonite of the East Tintic volcanic field was possibly formed by crystal fractionation from a subduction-related K-, Mg-rich mafic magma.

• 자원환경지질
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• 제31권3호
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• pp.249-264
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• 1998

The Creataceous volcanic rocks distributed in the southeastern part (Kyeongsang basin) of Korea peninsula are composed of basalt, basaltic andesite, andesite, dacite and rhyolite. The variation of major elements show that contents of MgO, CaO, $FeO^T$, $Al_2O_3$, $TiO_2$ and $P_2O_5$ decrease with increasing of $SiO_2$, but $K_2O$ contents are increased slightly, $Na_2O$ widely dispersed. We can show slightly inflection point and low frequency of dacites in range between 63-65 wt.% $SiO_2$, while continuous trend exit in variation diagram. Variation trends in Harker diagrams for the major, minor, trace and REEs suggest that the BAV (basaltic to andesitic volcanics) and DRV (dacitic to rhyolitic volcanics) are not related to a simple crystal fractionation process. In the regime of under 65 wt. % in silica content, fractionation of olivine and clinopyroxene is predominant, while that of plagioclase happens strongly higher than 65 wt.% (e.g., $SiO_2$, vs. Eu and Sr, MgO vs. $Al_2O_3$ and CaO). The latter means low-pressure fractional crystallization for DRV. On the discriminant diagram, DRV are located in more mature environment than BAV. The $(Ce/Sm)_N$ vs. CeN digram shows that these two classes cannot be related to crystal fractionation. If they had been produced by fractionation, although they plotted in a slightly elongate cluster along the same horizontal trend, DRV should lie to the right of these primitive compositions. These diagrams clearly rule out a simple fractionation throughout from BAV to DRV. BAV had been influenced greatly subductiong slab as shown by K/Yb vs. Ta/Yb. We suggest that BAV primitive magma generated higher degree of partial melting than DRV primitive magma. LILE (K, Ba, $Rb{\pm}Th$) enriched characteristics as shown in BAV are inherited from subducting slab fluids and/or higher degree of partial melting of mantle material. However, lower degree of partial melting of mantle relative to BA V and contamination at high-level magma reservoir caused LILE enrichment to DRV.

• 약학회지
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• 제40권2호
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• pp.225-229
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• 1996

The cytotoixic effect of Pylorae Herba (Pyrola japonica Klenze) against L1210 and K-562 cells was studied in vitro. The methanolic extract of Pylorae Radix was add ed to the culture of L1210 cells and K-562 cells for the cytotoxic activity and the ED50 values of hexane, ethylacetate, buthanol and water fractions from methanolic extract were determined using MTT (3-[4,5-dimethylthiazol-2-yl]-2,5-diphenyltetrazoliumbromide) assay. The active constituent isolated by bioassay guided fractionation followed by purification gave rise to a yellow needle crystal and was clarified to be chimaphilline by the comparison with the published data. The average life spans with it were not prolonged significantly on tumor growth in hybrid female mouse (BDF1-KIST) inoculated subcutaneously with P388 cells.

• 자원환경지질
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• 제25권1호
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• pp.51-60
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• 1992

The pluton rocks in Kwangyang-Seungju area consist of two mica granite, hornblende diorite, Rimunri quartz diorite, grnodiorite porphyry and granophyre. The analysis of the geochronological data by the methods of K-Ar for the hornblende from Rimunri quartz diorite and hornblende diorite show that the ages are found to be $86{\pm}3.3$ Ma and $108{\pm}4$ Ma, respectively, and K-Ar age for chlorite from the altered two mica granite which intruded by the hornblende diorite of the Bonjeong mine shows $108{\pm}4$ Ma; K-Ar age for sericite from the greisenized hornblende diorite, which is closely associated with the Bonjeong ore deposits, is dated as $94.2{\pm}2.4$ Ma. They correspond to the igneous activity of the Bulgugsa Disturbance periods in the area. In chemical feature for oxides versus silica and AFM triagular diagrams of the pluton rocks in the study area, there is a suggestion of the possibility that these rock facies area a Calc-alkali series of differentiated products by low-pressure crystal fractionation processes in $SiO_2$-undersaturated suites. Compared with hornblende diorite, andesite and granodiorite porphyry, two mica granite, Rimunri quartz diorite and granophyre exhibit a wider range of normalized REE abundance and negative Eu anomalies. Such anomalies imply more extensive feldspar fractionation during crystallization. The Rimunri quartz diorite and hornblende diorite occurring in the margin of four mines(Bonjeong, Okdong, Soungchei and Saungyeul) of this area have high contents of As, Sb, Cu and Zn which have been shown as the best indicators in hypogene gold deposits and low contents of Ba, Cr served as more sensitive indicators. And the granitoids are regarded as the rocks associated with gold and sulfide mineralization of the area.

• 한국식품과학회지
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• 제23권1호
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• pp.76-80
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• 1991

미강유 정제 부산물로부터 오리자놀을 분리하기위해, dark oil과 dark oil의 증류잔류물인 pitch로부터 용매분리법 이용하여 오리자놀을 분리하였다. 분리과정 중 방해물질인 왁스분은 dark oil과 acetone을 1 : 1(w/v)로 혼합하여, $0^{\circ}C$에서 침전시켜 제거하였고, 여기에서 얻어진 dewaxed dark oil에 8 part의 hexane을 섞어 저온분리하여 오리자놀함량이 51.3%인 농축물을 얻었다. 이 농축물에 methanol 20 part를 가하고 재결성하여 98.3%의 오리자놀결정물을 얻었다. Dark oil로부터 pitch를 제조하는 적정조건은$180^{\circ}C$와 $0.2{\sim}0.4torr$의 진공상태에서 2%(w/w)의 steam을 가하는 증류조건이 오리자놀의 파괴를 최소화 하였다. 이로부터 얻어진 pitch의 오리자놀순도와 회수율은 27.3%와 82.3%였다. Pitch에 hexane을 가하고 저온분리하여 오리자놀순도가 75.4%인 오리자놀결정물을 얻었으며 이 농축물에 methanol을 가한 후 재결정하여 순도가 99%인 결정물을 얻었다. 이상과 같은 저온윤리법을 이용하였을 때 오리자놀의 회수율은 dark oil 9.5%, pitch 28.5%로 나타났다.

• 암석학회지
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• 제16권2호
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• pp.59-72
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• 2007

하와이 제도 남단에 위치한 하와이섬의 킬라우에아 화산은 16세기 이래로 1982년 9월까지 계속적이고 간헐적인 분출로 형성된 화산체이다. 킬라우에아 화산 정상부 분화구 지역을 중심으로 야외지질조사, 체계적인 시료채취, 암석기재학 및 지구화학적인 특성분석을 수행하였다. 구성광물로는 주요 반정광물인 감람석을 비롯하여, 단사휘석, 사장석, 불투명광물등의 반정광물과 유리질 기질로 구성된다. 단사휘석과 사장석에서는 취반상조직, 사장석 반정에는 누대구조가 간간히 관찰되었다. 주원소 함량에서 $K_2O$, $P_2O_5$, $TiO_2$는 MgO 함량이 감소할 때 증가하는 경향을 보이고 $Al_2O_3$와 CaO는 변곡점을 보이는데 Al은 사장석, Ca는 사장석과 단사휘석의 결정화와 각각 밀접한 관련이 있는 것으로 해석된다. 감람석의 Fo%값은 60에서 90까지 넓은 변화폭을 가지고 Fo%에 대한 감람석 주원소 값에서 MnO와 FeO는 감소하며 반대로 $SiO_2$, MgO와 NiO는 증가한다. 킬라우에아 화산 현무암의 Ni함량의 변화는 감람석의 모드 함량과 감람석 결정 내의 Ni함량의 변화에 의하여 규제되는 것으로 생각된다.

• 분석과학
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• 제28권1호
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• pp.33-39
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• 2015

CdS 양자점 입자는 특정 파장의 빛을 방출하는 반도체 나노 결정으로 이러한 광학적 특성 때문에 질병 진단 시약, 광학기술, 미디어 산업 및 태양전지와 같은 다양한 분야에서 응용되는 물질이다. 방출하는 빛의 색은 입자의 크기에 의존하기 때문에 CdS 양자점 입자의 크기 및 크기분포를 정확하게 분석하는 것이 필요하다. 본 연구에서는 CdS 양자점 입자를 감마-선 조사법(${\gamma}$-ray irradiation method)을 이용하여 합성하고, 크기 및 크기 분포도를 결정하기 위하여 침강 장-흐름 분획법 (SdFFF)를 이용하였다. 침강 장-흐름 분획법을 이용한 CdS 양자점 입자의 정확한 분석을 위하여 분석조건의 최적화(유속, 외부장 세기, field-programming)에 대하여 조사되었다. 투과 전자 현미경(transmission electron microscopy, TEM)으로 확인된 단일 입자의 크기는 ~4 nm 였으며, 단일 입자의 응집으로 생성된 2차 입자 크기의 평균은 159 nm로 확인되었다. 첨가된 입자 안정제의 농도가 증가할수록 CdS 양자점 입자의 크기가 감소하는 경향성을 확인하였다. 침강 장-흐름 분획법, 투과 전자 현미경, 그리고 동적 광 산란법(dynamic light scattering, DLS)으로 결정된 CdS 양자점 크기는 각각 126, 159, 그리고 152 nm 였다. 본 연구의 결과로 침강 장-흐름 분획법은 비교적 넓은 크기분포를 갖는 다양한 종류의 무기입자의 크기 및 크기 분포도를 결정하는데 유용한 방법임을 확인하였다.

• Natural Product Sciences
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• 제2권2호
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• pp.130-136
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• 1996

Evaluation of plant extracts that might inhibit hepatitis B virus (HBV) replication was performed to find potent anti-HBV agents. Eighty-five species of plants from forty-three families were tested for their anti-HBV activities using HBV-producing HepG2-derived 2.2.15 cells. The anti-HBV activity of plant extracts was measured by slot blot hybridization technique and cytotoxicity was determined by crystal violet staining procedure. All plants were extracted with methanol and the extracts were partitioned into n-hexane, ethyl acetate and aqueous layer. The ethyl acetate fractions of Rhus verniciflua $(stem:\;EC_{50},\;8.2{\mu}g/ml;\;CC_{50},\;9.4{\mu}g/ml)$, Gastrodia elata $(root:\;EC_{50},\;17.7{\mu}g/ml;\;CC_{50},\;>20{\mu}g/ml)$, Raphanus sativus $(seeds:\;EC_{50},\;17.3{\mu}g/ml;\;CC_{50},\;>20{\mu}g/ml)$, and Angelica gigas $(root:\;EC_{50},\;8.3{\mu}g/ml;\;CC_{50},\;15.6{\mu}g/ml)$ revealed the anti-HBV activity in 2.2.15 cell culture system and these fractions are under the process of further sequential fractionation by column chromatography to find the active principles against HBV.

• Environmental Sciences Bulletin of The Korean Environmental Sciences Society
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• 제2권1호
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• pp.69-78
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• 1998

Contents of heavy metals (Cr, Cu, Zn, Cd, and Pb) in the sediments of Ulsan Bay were investigated by the sequential extraction methods that classifies heavy metals into five types of chemical forms: exchangeable, bound to carbonates, bound to Fe-Mn oxides, bound to organic matter and residual. The analytes were determined by using an ICP-MS. Total Cr concentrations in the sediments were in the range of 41.6-96.4, Cu 60.7-680, Zn 189-1954, Cd 33.1-83.4, and Pb 138-567 mg/kg. Results of sequential fractionation indicates that relatively high proportion $(\~44\%)$ of Cu is associated with organic matter A large proportion of Pb is associated with three types of chemical forms: Fe-Mn oxides, organic matter, and residual. There were significant correlation in concentrations between the exchangeable components and total organic carbons. The heavy metals in the residual phase cannot be easily released to the environment since these are bound to the crystal lattice. But, reducible and organic Phases cfn a significant amount of most heavy metals. Therefore. there is potential danger of a substantial amount of metals becoming chemically mobile with environmental changes.

• 한국환경과학회지
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• 제2권1호
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• pp.69-78
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• 1993

Contents of heavy metals (Cr, Cu, Zn, Cd, and Pb) in the sediments of Ulsan Bay were investigated by the sequential extraction methods that classifies heavy metals into five types of chemical forms: exchangeable, bound to carbonates, bound to Fe-Mn oxides, bound to organic matter and residual. The analyses were determined by using an ICP-MS. Total Cr concentrations in the sediments were in the range of 41.6-96.4, Cu 60.7-680, Zn 189-1954, Cd 33.1-83.4, and Pb 138-567 mg/kg. Results of sequential fractionation indicates that relatively high proportion ( ~44%) of Cu is associated with organic matter. A large proportion of Pb is associated with three types of chemical forms: Fe-Mn oxides, organic matter, and residual. There were significant correlation in concentrations between the exchangeable components and total organic carbons. The heavy metals In the residual phase cannot be easily released to the environment since these are bound to the crystal lattice. But, reducible and organic Phases con a significant amount of most heavy metals. Therefore, there is Potential dancer of a substantial amount of metals becoming chemically mobile with environmental changes.