• 한국광물학회지
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• 제32권2호
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• pp.145-150
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• 2019

최근 남북한 사이에 화해의 분위기가 무르익어가고 있으므로, 미래에 발생할 한반도 통일을 대비하는 관점에서 남북한 사이의 광물명을 통일하여 사용하는 것이 절실히 요구되고 있다. 외래어 표기법에 다른 언어에서 빌려온 어휘를 한글로 표기하는 규정이 있음에도 불구하고 광물명의 경우 이를 준수하지 않고 같은 외래어 광물명에 대하여 다양한 용어를 사용하고 있으므로 외래어 표기법에 맞도록 통일해야 한다. 금속광물과 비금속광물 모두에 ${\bigcirc}{\bigcirc}{\bigcirc}$석을 사용하고, 외래어 표기법 용례 찾기에 포함된 약 70개의 광물명은 용례 찾기에 나와 있는 대로 표기하고, 인명이나 지명에서 유래한 광물명은 인명이나 지명 + 석으로 표기할 것을 제안한다.

• 한국환경농학회지
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• 제22권3호
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• pp.177-184
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• 2003

Although clay can sorb significant amounts of inorganic contaminants from soils and wastewater, the hydration of exchangeable cations in clay minerals makes it hydrophilic at the clay mineral surfaces and interlayers. Thus, natural clays are often ineffective in complexing and stabilizing toxic organic contaminants in soils and groundwater environment. But, substituting these hydrated cations with cationic surfactant such as QAC(Quaternary ammonium Compound) can change the natural clay from hydrophilic to hydropobic. Furthermore functionalized organoclay can act as a powerful dual function sorbent for both toxic metals and organic compounds. It also can be used as landfill clay liners, slurry walls, nano-composite materials, petroleum tank farms, waste treatment, and filter systems. To use this modified clay minerals effectively, it is required to understand the fundamental chemistry of organoclay, synthetic procedures, its engineering application, bioavailability of sorbed ion-clay complex, and potential risk of organoclay. In this review, we investigate the use, application and historical background of the organoclay in remediation technology. The state-of-the-art of organoclay research is also discussed. Finally, we suggest some future implications of organoclay in environmental research.

• Asian-Australasian Journal of Animal Sciences
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• 제12권2호
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• pp.189-191
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• 1999

Mineral profile of serum and cerebrospinal fluid (CSF) of 15 Himalayan Yak (adult female, n=8; adult male n=4 and young male,n=3) was studied in their natural habitat at an altitude of 3300 meters above mean sea level at Sangla in north western Himalayas. The macro and micro minerals estimated in serum and CSF were; Sodium, Potassium, Calcium and Magnesium and Zinc, Copper and Iron respectively. The values recorded among different Yak groups did not significantly differ from each other except serum iron and haemoglobin which were significantly higher (p<0.05 ) in young male Yaks compared to the adult male and female Yaks. An observation of great significance was considerably higher potassium and lower sodium level in Yaks compared to other bovine species of plains. The serum potassium values in some adult female Yaks were recorded as high as 10.4 mEq/l and the values varied between 6.6 to 9.8 mEq/l in young male Yaks. The serum Sodium values and Na:K ratios in Yak serum ranged between 117.5 to 122.6 mEq/l and 13.7 to 15.3 respectively. The possible relationship of high serum Potassium value with hypoxic conditions and hostile mountain environment has been discussed.

• 자원환경지질
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• 제25권3호
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• pp.225-232
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• 1992

The hydrothermal alteration is evaluated using multicomponent equilibrium calculations with the program CHILLER for the reactions between hydrothermal water and rhyolite at the temperature of $300^{\circ}C$ and pressure of 500 bars. The chemical-reaction model on the depositional processes of the sericitite confirms that the hydrothermal water-rock interaction(hydrothermal alteration) is the main mechanism of the sericitite formation. The principal change in the aqueous phase during the reaction is the pH increase. Overall trends for the major species are the increase in total molalities of K, Ca, $SiO_2$, Al, Mg, Fe, Na, and sulfide in solid phase with hydrothermal water-rhyolite reaction and the decrease of them in aqeous solution by precipitation of hydrothermal products. Quartz and sericite are the first minerals to form. The sequence of minerals to precipitate following them is chlorite, epidote, pyrite and microcline as water/rock ratio decreases. Although calculated results cannot duplicate the complexities of natural hydrothermal alteration, the calculation provides thermodynamic constraints on the natural process. The calculation results resemble those of experimental studies. Sericitite forms where pH decreases and water/rock ratio increases.

• Geosciences Journal
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• 제22권6호
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• pp.989-1000
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• 2018

The provenance of the Central Yellow Sea Mud (CYSM) in the Yellow Sea has been attracted a great deal of attention over the last three decades, but a consensus is not yet reached. In this study, 101 surface sediment samples collected from the CYSM were investigated to determine provenance and transport mechanisms in the area using the clay minerals and major element components. The Huanghe sediments are characterized by higher smectite, but the Changjiang sediments are more abundant illite contents. Western Korean rivers contain more kaolinite and chlorite than do Chinese rivers. The Chinese rivers have higher $Fe_2O_3$, MgO, and CaO than the Korean rivers at the same $Al_2O_3$ concentration. Therefore, the clay minerals and major element concentrations can be useful indicator for the source. Based on our results, we suggest that the surface sediments in CYSM were composed mainly of Changjiang sediments, mixed a partly with sediments from the Huanghe and the western Korean rivers. Although the northwestern part of CYSM is proximate to the Huanghe, the contents of smectite and CaO were extremely low. It could be evidence that the Huanghe materials do not enter directly into the CYSM due to the Shandong Peninsula Front. Considering the oceanic circulation in the Yellow Sea, the Changjiang sediments could be transported eastward with the Changjiang Diluted Water and then mixed in CYSM via the Yellow Sea Warm Current (YSWC). Huanghe sediments could be provided by coastal currents (Shandong Coastal Current and Yellow Sea Coastal Current) and the YSWC. In addition, sediments from western Korean rivers might be supplied into the CYSM deposit via the Korean Coastal Current, Transversal Current, and YSWC.

• 대한건축학회논문집:구조계
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• 제35권12호
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• pp.149-156
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• 2019

Recently, skyscraper building and apartment fires, which were rapidly spread out from a low floor to a rooftop, have become a frequent occurrence in mass media. This fire problems have a fatal disadvantage that the exterior wall finish of the building emits toxic gas in case of fire by using dry bit method or organic insulating material. Therefore, in order to remedy these problems, many exterior wall finishing construction methods have been proposed, but the current trend is to use existing construction methods due to problems such as economy, weight, and durability. On the other hand, in countries such as Germany and Japan, ceramic sidings are used as exterior finishing material for buildings, which is environmentally friendly, excellent natural beauty, long life, easy maintenance and high-quality exterior materials. However, those ceramic sidings have still the problems such as manufacturing cost and weight problem because of boosting the sintering temperature up to 1,350℃ or more. Also, conventional CRC, MgO, FRP sidings which are composed of pulp, glass fiber and organic materials, have been reports of deformation due to ultraviolet rays, discoloration, corrosion and scattering, surface rupture, lifting and peeling. Therefore, in this study as an alternative to solve this problem, halosite nano kaolin produced in Sancheong in Korea and frit flux were used to satisfy the required properties as ceramic siding using low temperature sintering (below 1,000℃) and lightweight materials such as pearlite. This study aims to design the optimal formulation and process of materials and to study the characteristics of nano-coated ceramic siding material development and to present relevant basic data. The findings show that ceramic siding for nanocoated building materials is excellent as a natural ceramic siding building material. The fire resistance of natural minerals and nano particle refining technology satisfy the bending strength of 80kgf / cm2, the volume ratio of 2.0 and the absorption rate of less than 10.0%.

• 대한화학회지
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• 제50권4호
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• pp.321-327
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• 2006

M78과 일본산 KJ, 2개의 점토를 사용하여 계면활성제 CTMA(M-1, KJ-1), DSDMA(M-2, KJ-2) 그리고 TMSA(M-3, KJ-3)를 이용하여 변성된 점토광물을 합성하였다. 이러한 변성된 점토광물을 사용하여 염색 폐수의 주원인인 염료 중의 하나이며 대구 염색 공단 등에서 많이 사용되고 있는 염료인 acid blue 92와 acid red 1의 흡착 제거 실험을 통해 M-1, M-3, KJ-1 KJ-3의 경우 아주 좋은 흡착능력을 보인다는 결과를 얻었으며 이러한 결과는 점토 M과 KJ의 거의 0%에 가까운 흡착능력과 아주 좋은 비교가 될 수 있을 것이다. 또한 M-1과 KJ-3의 경우에는 이러한 염료 제거율이 거의 100%에 근접해 이러한 변성 점토가 실제 염색공단에서 배출되는 유해성 잔류 유기 염료 성분의 제거 방법으로 사용될 수 있는 충분한 가능성을 보였다고 할 수 있겠다.

• 대한한의학회지
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• 제21권2호
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• pp.43-51
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• 2000

Objectives : It is well known that vegetables and fruits contain minerals, including potassium, sodium and phosphorus etc. Though most oriental herbal medications are made of natural plants, western scientists suppose that they also contain certain amounts of minerals and so are injurious to kidney disease such as chronic renal disease. However, by the reason of the limitation of western medical treatment on kidney disease, many patients depend on oriental medical treatment, which includes taking oriental herbal medicine. So, in order to find out the mineral contents in oriental herbal medicine, and to establish the oriental herbal medication's safety in kidney disease, studies were performed. Methods : In this study, we analyzed 42 oriental herbs commonly used in kidney disease by the Inductively Coupled Plasma(ICP) method. Results : 1. The potassium and sodium contents of oriental herbs were 3-10 times as much as of food. 2. The mineral contents of a daily dose of oriental herbal medicine satisfied the restriction of dietary mineral in CRF, though the amount of mineral intakes by food was considered. Conclusions : The mineral contents of oriental herbal medicine are less than the limits of mineral restriction in renal failure. The yielded results, we carefully suggest that oriental herbal medicine does not induce accumulation of minerals or damage in kidney disease patients.

• 한국자기공명학회논문지
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• 제22권4호
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• pp.82-90
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• 2018

The term "hangover" refers to symptoms such as headache, heartburn, nausea, and dizziness caused by acetaldehyde created through alcohol decomposition in the body after alcohol intake. Many scientists have conducted research on diverse drugs, foods, and medicinal herbs aimed at eliminating hangovers. However, research on metabolism to objectively verify or measure their effects on hangover symptoms has been lacking. Accordingly, in this study, deep sea water minerals were administered orally at varying concentrations to rats that consumed alcohol, and changes in the levels of amino acids in their bodies were measured using nuclear magnetic resonance spectroscopy to gauge the minerals' effects on hangover symptoms. Thus far, biochemical research on hangover cures has been confined to basic research measuring changes in the levels of alcohol dehydrogenase and acetaldehyde dehydrogenase as well as in the concentrations of ethanol, acetaldehyde, and acetate using spectroscopes such as enzyme-linked immunosorbent assay kits or gas chromatography-mass spectrometers. In comparison, this study presents pharmacokinetic research that simultaneously tracked biomaterials including amino acids and organic acids, metabolites associated with hangover, to clarify hangover mechanisms more specifically. In addition, this study examined hangover mechanisms without an external supply of tracked materials not overlapping with alcohol metabolism-related materials, such as external amino acids and sugars.

• 자원환경지질
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• 제51권6호
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• pp.473-483
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• 2018

경남 밀양시에 소재한 납-아연 스카른 광상인 국전광산의 갱내 벽면을 따라 지하수로부터 침전된 청-녹색의 광물들이 암반을 피복하고 있는데, 이 광물들은 과거 문헌에서 남동석과 공작석으로 기재되어 왔으나, 최근 연구를 통해 녹색의 광물은 데빌린(devilline), 청색의 광물은 수화구리아연황산염 광물들로 보고되었다. 그러나 자세한 연구가 이루어지지 않아 정확한 동정이나 광물학적 특성은 알려지지 않았다. 본 연구에서는 청-녹색 이차 광물들을 외형적 특징에 따라 5개 그룹으로 구분하고, X-선회절분석와 주사전자현미분석을 실시하여 정확한 광물 동정과 광물학적 특성을 규명하였다. GJG-1은 밝은 청록색을 띠는 그룹으로 브로칸타이트(brochantite)와 석영, GJG-2는 연두색을 띠며 쉽게 부스러지는 특징을 가지는 그룹으로 슐럼버가이트(schulenbergite)와 소량의 석고(gypsum)로 확인되었다. 연한 청색의 GJG-3와 유리광택을 가지는 청록색의 GJG-4는 외형적 특징은 달랐지만 구성 광물은 서피어라이트(serpierite)와 석고로 동일하고, 석고의 함량이 달라 특징이 다르게 나타난다. GJG-5는 연한 청색과 진한 청색의 광물들이 혼합된 겔(gel)상으로 하이드로우드워다이트(hydrowoodwardite), 글로코세리나이트(glaucocerinite), 베체러라이트(bechererite), 서피어라이트와 석고로 구성된다. 국전광산에서 산출되는 6가지의 녹-청색 광물들은 Cu:Zn 비, (Si+Al) 함량 및 Si:Al 비, Ca 함량 등에 의해 구분될 수 있으며, 각 광물들의 형성 환경은 주변 유체 내에서 이와 같은 지화학적 요인들에 의하여 조절된 것으로 사료되고, 추가적인 연구를 통해 정확한 형성 환경을 밝혀낼 수 있을 것으로 기대된다. 본 연구에서 확인된 서피어라이트, 글로코세리나이트, 베체러라이트 등의 수화황산염 광물들은 국내에서 최초로 보고되며, 해외에서도 보고된 사례가 매우 적어 광물학적으로 큰 의의가 있다.