• 한국해양학회지
• /
• v.22 no.3
• /
• pp.191-206
• /
• 1987

Keum River discharges 6.4billion tons of fresh water annually into the Yellow Sea. More than 60% of the total discharge is concentrated in summer, differentiating distinct low-discharge and high-discharge periods for the estuarine environment. The concentration of SPM(Suspended Particulate Matter) is, in general, very high, except sometime during rainy season, and turbidity maximum is often observed, especially during spring-tides(Lee and Kim, 1987).

• Journal of the Korean Chemical Society
• /
• v.36 no.1
• /
• pp.147-156
• /
• 1992

Supported lead oxide catalysts were prepared by using ${\alpha}-,{\beta}-{\gamma}$-alumina, and MgO as a support. Among the supported lead oxide catalysts, MgO-supported catalyst showed the highest $C_2^+$ hydrocarbon selectivity for the methane conversion into $C_2^+$ hydrocarbons, but ${\gamma}$-alumina-supported PbO catalyst gave the highest $CO_2$ selectivity. And ${\alpha}$-alumina-supported catlyst showed the midium activity, whereas ${\beta}$-alumina-supported catalyst gave little activity. These reaction characteristics seemed to be largely dependent on the acticity of lattice oxygens in supported catalysts, which would be influnto be largely dependent on the activity of lattice oxygens in supported catalysts, which would be influenced in the interaction between the supports and lead oxides and the properties of supports. Especially, much higher ration of (002)/(111) peak intensities for PbO phase on MgO support than on the other supports in X-ray diffraction analysis was considered to be ab evidence that methane oxidative coupling of methane might be so-called structure-sensitive reaction, and this seemed to be an example of surface oxide-support interaction (SOSI) in the oxidative coupling reaction.

• Journal of the Korean Magnetics Society
• /
• v.21 no.1
• /
• pp.1-4
• /
• 2011

We have studied magnetic structure and magnetic anisotropy energy of cubic transition metal mono-oxide cluster FeO and MnO using OpenMX method based on density functional method. The calculation results show that the antiferromagnetic spin arrangement has the lowest energy for FeO and MnO due to the superexchange interactions. The magnetic anisotropy is only found for antiferromagnetically ordered FeO cluster, since occupied electron of 3d down-spin level induces the spin-orbit couplings with <111> directed angular momentum.

• Environmental Analysis Health and Toxicology
• /
• v.20 no.3 s.50
• /
• pp.205-208
• /
• 2005

대표적 간장해 유발 물질인 사염화탄소로 유도된 급성 간독성에 미치는 한국산 부추(Alluim tuberosum) 에탄을 추출물의 효과를 관찰하였다. 사염화탄소 투여로 혈청 AST (aspartate transaminale), ALT (alanine tranlaminase)와 ALP(alkaline phosphatase)활성이 현저히 증가하였으며,부추 에탄을 추출물의 투여(50, 100, 200mg/kg)로 특히 CCl$_{4}$에 의해 유도된 AST와 ALT의 활성이 농도 의존적으로 회복되었다. 사염화탄소 투여로 감소된 SOD (superoxide dismutase)와 catalase 활성은 부추의 에탄을 추출물 투여로 유의성 있는 활성 증가를 나타내어 간장해로 인한 산화적 스트레스가 부추의 항산화작용에 의해 완화되었음을 시사하였다. 결과적으로 부추 ethanol 추출물의 간보호 및 항산화작용으로 사염화탄소로부터의 간장해를 개선시키는 것으로 사료된다.

• The Korean Journal of Pharmacology
• /
• v.27 no.1
• /
• pp.69-80
• /
• 1991

Inhibitory effects of quercetin and rutin on lipid peroxidation of microsomes caused by iron(II) were investigated with respect to the scavenging action for oxygen radicals produced during oxidation of iron and the chelating action for iron. Lipid peroxidation by $Fe^{2+}$ alone was markedly inhibited by quercetin or rutin in a dose dependent fashion. Lipid peroxidation by ascorbate or NADPH in the presence of $Fe^{2+}$ was almost completely inhibited by both quercetin and rutin. The peroxidative action of $Fe^{2+}$ was inhibited by SOD and DABCO and slightly inhibited by catalase, DMSO and mannitol. Quercetin and rutin inhibited oxidation of $Fe^{2+}$ which is responsible for DETAPAC and they showed a significant initial chelating effect. Quercetin and rutin effectively inhibited lipid peroxidation by $H_{2}O_{2}$ and decomposed $H_{2}O_{2}$. Both $OH{\cdot}$ production in the presence of $Fe^{2+}$ and $^1O_2$ production by U.V. irradiation were inhibited by quercetin and rutin. Lipid peroxidations by $Cd^{2+},\;Cu^{2+},\;Ni^{2+},\;Pb^{2+}$ and $Zn^{2+}$ were almost completely inhibited by quercetin. Quercetin and rutin significantly prevented the loss of sulfhydryl groups by $Fe^{2+}$. These results suggest that inhibitory effects of quercetin and rutin on the peroxidative action of $Fe^{2+}$ in the presence or absence of ascorbate and NADPH may be attributable to their scavenging action on reactive oxygen species and chelating action on iron.

• The Korean Journal of Food And Nutrition
• /
• v.17 no.3
• /
• pp.294-301
• /
• 2004

Effects of superoxide dismutase(SOD), catalase(CAT), and such other proteins as bovine serum albumin(BSA), ovalbumin, lysozyme, and v-globulin on the autoxidation rates of L-ascorbic acid(AsA) in the absence of heavy metal ions and in the presence of Fe(III) or Cu(II) ions in water were examined. AsA was dissolved in a ultra-refined water at a concentration of 50 ${\mu}$M and 5 ${\mu}$M Fe(III) or 0.1 ${\mu}$M Cu(II) were added, and a oxygen gas was bubbled through the solution at a flow rate of 200 ml/min at 35$^{\circ}C$. The amount of remaining AsA in the reaction mixture was determined by using a UV spectrophotometer(at 265 nm). It was found that the Cu(II) at a concentration of 0.1 ${\mu}$M had a more accelerated for the autoxidation of AsA than Fe(III) at 5 ${\mu}$M. Moreover, it was confirmed that the ratio of remaining AsA was significantly larger in the presence of SOD, CAT, BSA, ovalbumin, lysozyme, and v-globulin than in the absence of proteins. The stabilization of AsA by various proteins were confirmed during the autoxidation of AsA in the presence of Fe(III) or Cu(II) in water. It was suggested that the non-enzymatic effects of SOD, CAT and some other proteins might be involves in the stabilization of AsA.

• Applied Chemistry for Engineering
• /
• v.8 no.3
• /
• pp.395-402
• /
• 1997

The $SiO_2$ films were prepared by ECR(electron cyclotron resonance) plasma diffusion method, Deal-Grove model and Wolters-Zegers-van Duynhoven model were used to estimate the oxidation rate which was correlated with surface morphology for different orientation of Si(100) and Si(111). It was seen the $SiO_2$ thickness increased linearly with initial oxidation time. But oxidation rate slightly decrease with oxidation time. It was also shown that the oxidation process was controlled by the diffusion of the reactive species through the oxide layer rather than by the reaction rate at the oxide interface. The similar time dependency has been observed for thermal and plasma oxidation of silicon. From D-G model and W-Z model, the oxidation rate of Si(111) was 1.13 times greater than Si(100) because Si(111) had higher diffusion and reaction rate, these models more closely fits the experimental data. The $SiO_2$ surface roughness was found to be uniform at experimental conditions without etching although oxidation rate was increased, and to be nonuniform due to etching at experimental condition with higher microwave power and closer substrate distance.

• Journal of the Mineralogical Society of Korea
• /
• v.32 no.3
• /
• pp.223-234
• /
• 2019

The geology of the Samdeok Mo deposit consists of Paleozoic Hwajeonri formation, Kowoonri formation, Suchangri formation, Iwonri formation, Hwanggangri formation, Cretaceous, leucocratic porphyritic granite and granitic porphyry. This deposit consists of three quartz veins that filled NS oriented fractured zones in Suchangri formation. Quartz veins vary from 0.05 m to 0.3 m in thickness and extend to about 400 m in strike length. Quartz veins occur as massive, breccia, and cavity textures. Wallrock alteration has silicification, sericitization, argillitization and chloritization. The mineralogy of the quartz veins consists of quartz, fluorite, white mica, biotite, apatite, monazite, rutile, ilmenite, molybdenite, chalcopyrite, Fe-Mg-Mn oxide and Fe oxide. White mica from Samdeok Mo deposit occurs as fine or coarse grains in quartz vein and hostrock and has four mineral assemblages (I type: quartz, molybdenite, Fe oxide and Fe-Mg-Mn oxide, II type: quartz, Fe oxide and Fe-Mg-Mn oxide, III type: quartz and biotite, and IV type: quartz). The structural formular of white mica from quartz vein is $(K_{0.89-0.60}Na_{0.05-0.00}Ca_{0.01-0.00}Sr_{0.02-0.00})_{0.94-0.62}(Al_{1.54-1.12}Mg_{0.36-0.18}Fe_{0.26-0.09}Mn_{0.04-0.00}Ti_{0.02-0.00}Cr_{0.02-0.00}Zn_{0.01-0.00})_{1.91-1.72}(Si_{3.40-3.11}Al_{0.92-0.60})_{4.00}O_{10}(OH_{1.68-1.42}F_{0.58-0.32})_{2.00}$, but white mica of I type has higher FeO content, and lower $SiO_2$ and MgO contents than white micas of other types. Also, compositional variations in white mica from the Samdeok Mo deposit are caused by phengitic or Tschermark substitution ($(Al^{3+})^{VI}+(Al^{3+})^{IV}{\leftrightarrow}(Fe^{2+}{\text{ or }}Mg^{2+})^{VI}+(Si^{4+})^{IV}$) and direct $(Fe^{3+})^{VI}{\leftrightarrow}(Al^{3+})^{VI}$ substitution.

• Economic and Environmental Geology
• /
• v.44 no.1
• /
• pp.11-20
• /
• 2011

Geological survey on the occurrence of copper oxide in Suparaura area around Abancay in the south-central part of Peru had been carried out. Geology of the area is composed of granitoids such as granodiorite, tonalite and andesitic porphyry related to Tertiary igneous activity, Ferrobamba formation with Cretaceous limestone and sandstone in descending order. Red sandstone is widely distributed and emplaced with their attitude of $N70^{\circ}W$ strike and $60^{\circ}NE$ dip. Copper oxides were mineralized along the bedding plane of red sandstone with maximum width of 30 cm. Ore-body structure bounding red sandstone strata have different occurrence characteristics with generally known porphyry system in terms of alteration, mineral assemblage and occurrence mode. Therefore, it is thought to be stratiform sediment-hosted copper (SSC) deposits genetically corresponding to Mississippi-valley type from preliminary study.

• Journal of the Mineralogical Society of Korea
• /
• v.16 no.2
• /
• pp.181-189
• /
• 2003

Diverse microtextures and secondary minerals formed by chemical weathering were observed in the glacial debris of King George Island. Weathering rind was observed in the block of basaltic andesite tuff due to dissolution of calcite producing voids. Eolian volcanic glass altered to mixtrure of allophane-like materials and iron oxyhydroxides at grain edges with relative concentration of Al. Fe, and Ti. Biotite in granodiorite area was transfarmed to vermiculite and interstratified biotite-vermiculite or very rarely to kaolinite and gibbsite. Pyrite in the hydrothermal alteration zone was repalced by iron oxides, resulting in sulfuric acid which locally accelerated alteration of chlorite to expandable clay minerals. Weathering of plagiociase and K-feldspar was negligible. Although glacial debris of the Barton Peninsula has undergone weak chemical weathering with formation of some secondary minerals, massive formation of smectite, abundant in nearby marine sediments, didn't occur.