• Economic and Environmental Geology
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• v.57 no.5
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• pp.563-575
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• 2024

In Korea, talc, vermiculite, sepiolite, and serpentine were designated as minerals likely to contain asbestos (MLCA) according to the Ministry of Environment (Asbestos Safety Management Act). The asbestos content in commercial products made of MLCA must not exceed 0.1 %. In this study, mineralogical analyses using PLM, XRD, and TEM-EDS were used to characterize the presence, content, and morphological characteristics of asbestos in MLCA-containing commercial products. A total of 28 samples were analyzed, including 18 cosmetics containing talc, 5 fertilizers containing vermiculite, 2 pet sanitary products containing sepiolite, and 3 accessories containing serpentine. All samples were heated at 450 ℃ for 6 hours to remove organic matter prior to XRD and PLM analyses according to the Ministry of Environment guidelines. Additionally, the presence and morphology of elongated mineral particles (EMPs) were investigated using TEM-EDS analysis according to the recently revised asbestos analysis method (FDA-2020-N-0025) by the US FDA. The analyses showed that no asbestos was detected in both talc-containing cosmetics and sepiolite-containing products, but actinolite asbestos was found (<0.25 %) in vermiculite-containing fertilizers and chrysotile was found (<0.25 %) in decorative serpentine stones. In TEM-EDS analysis, multiple columnar/fibrous particles measuring 0.5 ㎛ or more in length were observed in talc-containing products, and short chrysotile fibers were observed in bracelets containing serpentine. Therefore, these results indicated that the MLCA-containing products that come into direct contact with the human body would require management through precise inspection and continuous monitoring considering EMPs of 5 ㎛ or less. Furthermore, TEM-EDS for asbestos analysis indicated that it could overcome the detection limits of XRD and PLM analyses for short or thin asbestos fibers, thereby improving the precision and accuracy of asbestos analysis.

• Proceedings of the Mineralogical Society of Korea Conference
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• 2001.06a
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• pp.133-133
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• 2001

우리는 괴산 덕평리 지역의 소위 구룡산층과 대전 추부 지역의 창리층 흑색 점판암에 대한 납 동위원소 연대측정 결과를 보고한다. 덕평리 지역의 흑색 점판암은 270 Ma 내외의 Pb-Pb 연대를 보이고 U-Pb 연대는 정의되지 않는다. 그 Pb-Pb 연대는 같은 시료의 22개 uraninite 입자에 대한 CHIME 연대와 오차범위 내에서 일치한다. 이로 보아 uraninite는 형성 또는 변성작용에 의한 동위원소적 재평형 작용 이후 폐쇄계를 잘 유지하였지만 흑색 점판암이 지질학적으로 최근에 지표에 노출된 이후에는 전암 규모에서 개방계로 거동하였음을 알 수 있다. 박편 미조직 관찰에 의하면 흑색 점판암의 1차광물인 uraninite 외에 풍화기원 2차광물인 uranocircite, francevillite가 관찰된다. 덕평리 지역 흑색 점판암의 최고 변성온도 조건은 50$0^{\circ}C$ 내외이므로 (Kim et al., 2000) uraninite CHIME 연대의 폐쇄온도가 50$0^{\circ}C$ 이상이거나 uraninite의 형성시기와 변성시기 사이에 시간차가 거의 없었다고 판단된다. 덕평리 지역의 U 광화작용 시기는 이번 자료에 의해 고생대 말로 정의될 수 있으나 그 연대가 흑색 점판암의 모물질인 해저 흑색 유기질 퇴적물의 초기 속성작용과 관련 있는지 후기의 변성작용과 관련 있는지에 대해서는 광물학적인 연구가 더 진행되어야 한다. 옥천대 변성퇴적암의 일부가 고생대 말에 퇴적되었을 가능성은 황강리층 역의 xenotime 및 monazite에 대한 CHIME 연대측정 결과 (약 367 Ma; Adachi et al., 1996)에 의해서 지지된다. 추부 지역 흑색 점판암의 Pb-Pb 연대는 170 Ma 내외로서 인접한 쥬라기 화강암의 관입시기를 지시하는 것으로 생각된다. 이는 화강암체로부터의 거리로 볼 때 덕평리 지역과 추부 지역의 시료 채취 위치가 유사하지만 지하 천부에 관입한 백악기 속리산 화강암 (91$\pm$6 Ma, Cheong and Chang, 1997)에 의해서는 덕평리 지역 흑색 점판암의 납 동위원소계가 영향받지 않았다는 점과 대조적이다.

• Spatial Information Research
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• v.4 no.1
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• pp.1-11
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• 1996

DRASTIC system developed by U.S.EPA, is widely used for assessing groundwater pollution potential The system can be applied to site selection of well or waste disposal, Ianduse planning for groundwater protection, and monitoring. In this study, GIS(Geographic Information System) was established hydrogeological database of DRASTIC system and cartographic modeling to asre:; regional groundwater pollution potential around Chungju Lake. Hydrogeological factors of the system were depth to water, net recharge, aquifer media, soil media, slope and hydraulic conductivity. Risk of groundwater pollution to non -point source pollution, was also analyzed by incorporation of actual pollution sources(N, P) and DRASTIC system. The GIS data could be very quickly analysed hydrogeological characteristics of the study area by graphic user interface programs devel¬oped with AML(ARC Macro Language) of ARC/INFO.

• Journal of Veterinary Clinics
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• v.27 no.2
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• pp.142-146
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• 2010

The purpose of this study is to establish experimental canine skin barrier disruption model in dog. The study was designed to investigate the predictive properties of acetone damage using as effect parameters transepidermal water loss (TEWL) and stratum corneum (SC) hydration. To compare the structures of SC intercellular lipids in normal and acetone damaged skin, TEM observations were performed. Six clinically normal, male Beagles without dermatological problems were chosen for this study. Acetone damage was performed at 48hrs after clipping. Efficacy measurements for TEWL and skin hydration were performed before ($t_1$) and after ($t_2$) damage in a temperature- and humidity-controlled room ($2{0\sim}22^{\circ}C$, 50-60%). TEWL and SC hydration values were decreased in the acetone damaged model compared with non damaged skin. In TEM observation of acetone damaged sample, the intercellular lipid lamellae exhibit abnormal and incomplete structure compared with those of normal skin. It seems that acetone damage would be one of canine skin epidermal barrier disruption model for the study of canine atopic dermatitis (AD) as well as dry skin in veterinary dermatology research.

• Economic and Environmental Geology
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• v.47 no.5
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• pp.507-515
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• 2014

Asbestos is designated as carcinogen minerals. Detoxification of asbestos is being conducted by physical and chemical treatments that lead the formation of non-fibrous mineral particles or phase transitions. Major researches have been performed on mineralogical properties of asbestos and possibilities of detoxification in Korea. More specific studies are needed to prove the form and crystal structure changes during the detoxification of asbestos via heat treatment. Therefore, we studied thermal effects on mineralogical characteristics of chrysotile and asbestiform tremolite using electron microscopy investigation. Electron microscopy investigation showed chrysotile fibers were fully transformed into rod-shaped forsterite at $850^{\circ}C$ in 2 hours, and asbestiform tremolite fibers were converted into non-fibrous diopside at $1050^{\circ}C$ in 2 hours. Fibrous asbestos were converted into rod-shaped minerals, which are non-asbestiform. However, compositions of both minerals were not changed before and after heat treatment. These results indicate that thermal treatment of asbestos completely broke down asbestos structure due to dehydroxylation and recrystallization. Thus, electron microscopy investigation can provide the useful information of shapes, crystal structure, and chemistries of the asbestos for the detoxification.

• Korean Journal of Mineralogy and Petrology
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• v.36 no.2
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• pp.95-106
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• 2023

Quartz (SiO₂) is among the major rock-forming minerals in the earth's crust. The atomistic structures of SiO₂ may evolve during diverse frictional processes. The reduction of friction of quartz-rock accompanied by its amorphization, hydration, and formation of silica gel provides mineralogical insights into earthquakes and related phenomena. Ball milling, together with rotary shear experiments have been useful to infer the atomic origins of such processes. In this study, optimal experimental conditions for ball milling for amorphization of SiO₂ were determined by taking into account various process variables. The crystallinity of SiO₂ gradually decreased and became amorphous as the ball milling time increased at a high milling speed. The degree of wear of the milling media and its effect on the amorphization of SiO₂ were analyzed using distinct milling materials (zirconia, stainless steel). The amount of ball wear increased with increasing milling time. Furthermore, the worn stainless steel particles from balls tend to interact with amorphized SiO₂ to form Si-O-Cr. These results aid in understanding the process of atomistic structural changes caused by ball milling of divserse materials with relatively high hardness, such as SiO₂, and understanding various geological friction processes.

• Economic and Environmental Geology
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• v.43 no.4
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• pp.371-379
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• 2010

Fresh water injection test in a fractured bedrock aquifer was applied as an efficient approach to lower saline concentrations in the saltwater-freshwater transition zone formed by seawater intrusion in a coastal area. The methodology and effectiveness of fresh water injection for hydraulically controlling seawater intrusion is overwhelmingly site dependent, and there is an urgent need to characterize the permeable fractures or unconsolidated porous formations which can allow for seawater flow and transport. Considering aquifer characteristics, injection and monitoring boreholes were optimally designed and completed to inject fresh water through sand layer and fractured bedrock, respectively. We devised and used the injection system using double packer for easy field operation and maintenance. Overall fracture distribution was systematically identified from borehole image logs, and the section of fresh water injection was decided from injection test and monitoring. With fresh water injection, the fluid electrical conductivity of the monitoring well started to be lowered by the inflow of fresh water at the specific depth. And this inflow leaded to the replacement of the fluid in the upper parts of the borehole with fresh water. Furthermore, the injection effect lasted more than several months, which means that fresh water injection may contribute to the mitigation of seawater intrusion in a coastal area.

• Journal of Conservation Science
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• v.7 no.1
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• pp.9-18
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• 1998

There are about 1470 stone-cultural properties in Korea which have been registered and protected by the government. Representative of them are pagoda, stupa, stone-buddha, stele support of banner pole and stone-lanterns. Most of them have been exposed to and weathered by natural environments. Stone-cultural properties are destroyed and/or destructed mostly by weathering and its related features of rocks. Therefore, it is necessary to conduct geological studies on the weathering phenomena and related features as well as characteristics of the rock itself must be done for the conservation. Thus geological investigation should include detail measurements, rock varieties and phases, structural lineaments of the rock, cause and degree of weathering, degree and patterns of crack development structural stability, identification of reusable parts for restoration, geomorphological characteristics of the site, and etc. The interaction among these factors must be investigated and analyzed, which must be used as basic data to establish the guideline of conservation and to plan for repair and/or restoration. The conservation plan should involve parts to be repaired, method of repair, type of cementing material, the characteristics of rock phases to be supplemented, method for maintaining structural stability, and method to delay or to prevent the rock weathering.

• The Journal of Engineering Geology
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• v.26 no.2
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• pp.277-290
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• 2016

Deep geological cross-sectional data is generally not common nor easy to construct, because it is expensive and requires a great deal of time. As a result, geological interpretations at depth are limited. Many scientists attempt to construct geological cross-sections at depth using geological surface data and geophysical data. In this paper, we suggest a method for constructing cross-sections from limited geological surface data in a target area. The reason for this study is to construct and interpret geological cros-sections at depth to evaluate heat flow anomaly along the Yangsan fault. The Yangsan Fault passes through the south-eastern part of the Korean Peninsula. The cross-section is constructed from Sangbukmyeon to Unchonmyeon passing perpendicularly through the Yangsan Fault System trending NW-SE direction. The geological cross-section is constructed using the following data: (1) Lithologic distributions and main structural elements. (2) Extensity of sedimentary rock and igneous rock, from field mapping. (3) Fault dimension calculated based on geometry of exposed surface rupture, and (4) Seismic and core logging data. The Yangsan Fault System is composed of the Jain fault, Milyang fault, Moryang fault, Yangsan fault, Dongnae fault, and Ingwang fault which strike NNE-SSW. According to field observation, the western section of the Yangsan fault bounded by igneous rocks and in the eastern section sedimentary rocks are dominant. Using surface fault length we infer that the Yangsan Fault System has developed to a depth of kilometers beneath the surface. According to seismic data, sedimentary rocks that are adjacent to the Yangsan fault are thin and getting thicker towards the east of the section. In this study we also suggest a new method to recognize faults using core loggings. This analysis could be used to estimate fault locations at different scales.

• Journal of Food Hygiene and Safety
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• v.13 no.3
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• pp.258-267
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• 1998

The acetaminophen (AP AP), an antipyretic and analgesic agent, induces the hepatotoxicity by increasing influx of calcium and destabilizing the cellular membrane which can be caused by N-acetyl-p-benzoquinoneimine generated by cytochrome P-450 (CYF-450) when it is overdosed. Diltiazem (DIL), a calcium channel blocking agent, has been known to suppress the CYF-450 activities. To study the effect of DIL in APAP treated rats, the serum biotransformational enzyme analyses and the liver histopathologic examination were conducted on the rats which had been administered DIL at 3, 6, 9 and 12 hours after the 3,000 mg/kg of APAP administration. Following a single dose of DIL administered 12 hours after AP AP administration, serum alanine aminotransferase (ALT) and aspartate aminotransferase (AST) activities, malondialdehyde and calcium contents of liver and microsome were significantly reduced. Glutathione S-transferase (GST) activity was significantly increased. Histopathologic studies showed that DIL had prevented the development of centrilobular necrosis induced by AP AP in liver tissue. Our results suggested that diltiazem could inhibit the formation of free radical and the influx of calcium and could increase GST activity. Therefore, diltiazem can be administered at the time of 12 hours after overdosed AP AP to diminish the liver damage.