• Journal of Periodontal and Implant Science
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• v.14 no.1
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• pp.79-79
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• 1984

• Proceedings of the Korean Vacuum Society Conference
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• 2011.08a
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• pp.195-195
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• 2011

공기 중 산소를 이용한 다양한 산화반응에 적합한 이종상 촉매 개발이 공업적으로나, 학문적으로 중요한 의미를 갖는다. 우리는 수산화 인회석(hydroxyapatite, HAP)에 Cu이 도입된 새로운 이종상 촉매를 합성하였으며, 이를 이용하여 Mesitylene의 산화반응을 통해 반응성을 관찰하였다. 전이금속 Cu를 이온교환 반응 하는 과정에서 온도와 압력조건의 변화가 촉매의 활성에 미치는 영향에 대해 연구하였다. 반응 후의 생성물질은 GC/MS를 통해 알아내고 Mesitylene 이외에 벤젠고리에 치환된 알킬기의 수가 다른 물질의 산화반응을 수행하였다.

• Economic and Environmental Geology
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• v.44 no.1
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• pp.37-48
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• 2011

Some industrial minerals used in domestic industries such as monazite, apatite, bauxite, and ilmenite belong to NORM (Naturally Occurring Radioactive Materials) because they show a high radioactivity. Products, semi-products, wastes, and by-products which show higher radioactivity than NORM belong to TENORM (Technologically Enhanced Naturally Occurring Radioactive Materials). Apatite used for manufacturing phosphate fertilizer in Namhae Chemical company belongs to NORM, and its by-product, phospo-gypsum, belongs to TENORM. A geological investigation is needed for the future environmental impact assessment of the Namhae Chemical company's site. According to survey results of the Namhae Chemical company's site, soil mineral composition indicated the mixture of minerals derived from the country rock (quartz, feldspar, mica, $l4{\AA}$ mineral, kaolin and amphibole) and minerals from the gypsum open-air storage yard (gypsum and apatite). Soil samples showed average content of U 4.6 ppm and Th 10 ppm, which are similar to average crustal abundances. They also show average contents of $^{40}K$ 191-1,166 Bq/kg, $^{226}Ra$ 15.6-710 Bq/kg, and $^{232}Th$ 17.4-72.7 Bq/kg, which indicate moderate levels of radio nuclide. But $^{226}Ra$ anomaly in the gypsum open storage yard is clearly confirmed and $^{232}Th$ anomaly is also confirmed in the east road side of the factory and nearby mountain areas. Soil external hazard indices ranged 0.24-2.01 with the average 0.54. Although most external hazard indices were lower than 1, which means radiation hazard index to be negligible, 5 samples out of total 40 samples showed higher values than 1, and further detailed investigation is needed.

• Economic and Environmental Geology
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• v.55 no.1
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• pp.77-95
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• 2022

The Gonamsan gabbroic complex in the Pocheon area, northwestern region of South Korea consists of a variety types of gabbroic rocks and associated Fe-Ti oxide deposits caused by magmatic differentiation. Post-magmatic intrusions (i.e., gabbroic pegmatite and pyroxene-apatite-zircon rocks) partly intruded into the gabbroic rocks. The gabbroic pegmatite occurs in monzodiorite and oxide gabbro of the complex, intimately and spatially associated with high-grade lenticular Fe-Ti oxide mineralization. The pegmatite can be subdivided into plagioclase-amphibole and pyroxene-olivine pegmatite, in which the contact surface is sharp. The plagioclase-amphibole pegmatite comprises plagioclase and amphibole, with lesser amount of pyroxene, ilmenite, sphene, apatite, and biotite. The pegmatite shows plagioclase-amphibole intergranular texture, in which the open space formed by large plagioclase laths (An_2-26Ab_72-98Or_0-2) are infilled by amphibole. The pyroxene-olivine pegmatite is dark gray to black in color and also contains magnetite, ilmenite, spinel, apatite, and calcite as a minor component. The pyroxene (En_35-36Fs_8-9Wo₅₅) and olivine (Fo_84-85Fa_15-16) partly show a poikilitic texture defined by smaller euhedral olivine enclosed by coarser clinopyroxene. Fe-Ti oxide minerals consist mainly of magnetite and ilmenite that are found interstitially to earlier formed silicates. Subsequently, they are encompassed by reaction rim (almost of amphibole and biotite) along the boundary with surrounding silicate minerals. Under the microscope, magnetite contains a lot of oxyexsolved ilmenite (trellis type) and spinel, and thereby is weakly enriched in magnetite-compatible elements such as Ti, Al, Mg, and V. The structure and textures at the contact zone as well as mineralogical disequilibrium between gabbroic pegmatite and the host gabbroic rocks suggest that the pegmatite may form as a result of accumulation from Fe-rich melt (or liquid) that occurred somewhere rather than in situ form from the host gabbroic rock during the magmatic differentiation. Consequently, the preliminary study suggests that further study on the post-magmatic activities can not only help us improve our understanding on magmatic fractionation but also provide critical information on Fe-Ti oxide mineralization in gabbroic rocks resulting from the magmatic differentiation.

• Korean Journal of Environmental Agriculture
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• v.1 no.2
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• pp.116-122
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• 1982

Investigation on the water quality of Hwangguji River and experiment on the effects of nitrogen and soil improvements were carried out in the paddy field irrigated with polluted water of the river. The obtained results are as follows: 1) Amount of COD and $NH_4-N$ in water of the river were 54 ppm, 65 ppm, during the seeding time, and were 52 ppm, 512 ppm during the transplanting time respectively. Their concentrations were over the standard levels. It seemed that the water pollution was mainly caused by organic waste matters. 2) It seemed that the effective nitrogen level was $7{\sim}8$kg/10a in the paddy field irrigated with polluted water of the river. 3) The rice yields of potassium twice quantity application plot with N.P.K. fertilizer, the calcium application plot with N.P.K. fertilizer and the combined plot with potassium, wallarstonite, calcium and fresh straw, were increased 4, 5 and 8%, respectively, than that of the N.P.K. fertilizer standard level plot.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.183-184
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• 2002

악취현상 평가방법은 냄새유발물질의 농도를 정량적으로 분석하는 화학성분분석법과 복합취기물질에 의란 감각수준을 다수의 악취판정인이 평가하는 관능측정법으로 대별할 수 있다. 특히, 관능측정법의 경우 자극의 세기를 표현하는 직접관능법과 최소냄새감지한계회석배수를 구하는 간접관능법으로 구분할 수 있으며, 환경악취현상을 객관적으로 평가하기 위해서는 성분분석과 감각수준을 평가하는 두 방법에 의한 측정결과를 종합적으로 고려하는 것이 타당한 것으로 알려져 있다. (중략)

• Korean Journal of Mineralogy and Petrology
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• v.35 no.3
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• pp.283-298
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• 2022

In this study, we investigated the mineral geochemistry of the albite-spodumene pegmatite, associated exogreisen, and wall rock from the Boam Li deposit, Wangpiri, Uljin, Gyeongsangbuk-do, South Korea. The paragenesis of the Boam Li deposit consists of two stages; the magmatic and endogreisen stages. In the magmatic stage, pegmatite dikes mainly composed of spodumene, albite, quartz, and K-feldspar intruded into the Janggun limestone formation. In the following endogreisen stage, the secondary fine-grained albite along with muscovite, apatite, beryl, CGM(columbite group mineral), microlite, and cassiterite were precipitated and partly replaced the magmatic stage minerals. Exogreisen composed of tourmaline, quartz, and muscovite develops along the contact between the pegmatite dike and wall rock. The Cs contents of beryl and muscovite and Ta/(Nb+Ta) ratio of CGM are higher in the endogreisen stage than the magmatic stage, suggesting the involvement of the more evolved melts in the greisenization than in the magmatic stage. Florine-rich and Cl-poor apatite infer that the parental magma is likely derived from metasedimentary rock (S-type granite). P₂O₅ contents of albite in the endogreisen stage are below the detection limit of EDS while those of albite in the magmatic stage are 0.28 wt.% on average. The lower P₂O₅ contents of the former albite can be attributed to apatite and microlite precipitation during the endogreisen stage. Calcium introduced from the adjacent Janggun formation may have induced apatite crystallization. The interaction between the pegmatite and Janggun limestone is consistent with the gradual increase in Ca and other divalent cations and decrease in Al from the core to the rim of tourmaline in the exogreisen.

• The Journal of Engineering Geology
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• v.6 no.2
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• pp.65-81
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• 1996

Friar Tuck, an Abandoned Mine Lands (AML) site, is located on the Greene-Sullivan county line in southwest Indiana. Prior to the on-going reclamation, Friar Tuck was one of the Indiana's largest and most environmentally adverse abandoned mine lands. The direct vegetation method was used to reclaim tailing ponds. Grading, capping, and revegetalon using agricultural limestone, fertilizer, mulch and seed were applied to the gob piles to abate acid mine drainage (AMD) and off-side sedimentaion. Erosion control structures such as terrace, diversion ditch, and gabion structures were also constructed to minimize erosion at slopes. A new method for treatment of AMD using apatite was tested in the laboratory and field. Apatite effectively removed iron, aluminum and sulfate while maintaining an almost constant pH. Apparently, this method can be applied to control AMD from mining refuse materials, even those containing high concentrations of iron and aluminum ions.

• Journal of the Mineralogical Society of Korea
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• v.8 no.2
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• pp.108-117
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• 1995

옥천층군의 상부 이질암에 속하는 구룡산층내의 함흑연질셰일층준에서 흑연단괴가 산출된다. 이들 중 덕평과 조곡지역에서 산출되는 흑연질단괴는 두 지역 모두 장경 2cm 이하의 타원체가 주이며, 조곡지역의 단괴가 덕평지역의 단괴에 비하여 더욱 신장되어 있다. 덕평지역에서는 단괴가 초기 속성기간 중에 생성된 것임을 지시해 주는 조직이 단괴와 모암의 접촉부에서 관찰되는 반면 조곡지역에서는 이러한 조직이 관찰되지 않는다. 덕평지역 단괴의 주구성 광물은흑연, 인회석, 석영, 운모이고 조곡지역 단괴의 구성광물은 흑연, 석영, 운모이다. 덕평 및 조곡지역에서 산출되는 단괴내의 총탄소함량은 각각 40%, 5% 내외의 값을 갖는다. 덕평 및 조곡지역의 탄질물의 d002는 동인한 3.356~3.360$\AA$의 범위의 값을 가진다. 이는 고진화된 흑연의 저면간격에 해당되는 것으로, 두 지역의 변성상이 동일함을 의미한다.

• Proceedings of the Korean Vacuum Society Conference
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• 2011.02a
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• pp.330-330
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• 2011

공기 중 산소를 이용한 다양한 산화반응에 적합한 이종상 촉매 개발이 공업적으로나, 학문적으로 중요한 의미를 갖는다. 우리는 수산화 인회석(hydroxyapatite, HAP)에 Ru이 도입된 새로운 이종상 촉매를 합성하였으며, 이를 이용하여 알콜 산화 반응을 통해 반응성을 관찰하였다. 우리는 다양한 형태의 결정구조와 표면구조를 가지는 HAP를 합성하였으며, 이를 AFM, ICP, XRD, SEM를 통하여 결정구조를 분석하였다. 각각에 대해서 수용액상에서 Ion exchange 반응을 통하여 Ru를 HAP 표면에 치환하여 여러 종류의 RuHAP를 합성하였다. 특히, 알콜 산화반응을 통해 HAP의 결정 형태에 따라서 반응성의 차이를 가짐을 알 수 있었다. HAP는 Molten salt synthesis 방법을 이용하여 합성한 일정한 형태의 단결정과 무정형의 다결정 즉, 두 가지 다른 형태를 이용하여 각각에 대해 칼슘이 부족한 형태로써, Ca과 Ru과의 Ion exchange 반응을 통해 다양한 종류의 HAP를 합성하여 알콜 산화반응의 촉매로서 가지는 반응성을 연구하였다.