• 한국지형학회지
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• 제25권2호
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• pp.43-61
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• 2018

Heterogeneous sedimentary deposits with different soil colors and various degree of hardness are exposed in its foredune and tidal zone due to the effects of recently accelerated coastal erosion along the Ujeon Coast in Jeung-do, Shinan-gun. This study was conducted on the assumption that these sedimentary deposits were developed in different timing and environments. Thus, we can infer the geomorphic development processes of the area based on evidences like the physicochemical characteristics of each sedimentary layer. Several analysis of these sedimentary depositssuch as grain size analysis, X-ray Fluorescence Measurement (XRF), and Loss on ignition (LOI) were performed on central (Ujeon A) and southern (Ujeon B) parts of the Ujeon Coast. I found that the foredune sedimentary deposits have four stages of geomorphic development processes. In the initial stage of development, during the peak of the Last Interglacial Period (MIS 5e), basal deposits were accumulated in the low-energy environment of subtidal zones. In the second stage, during the Last Glacial Period (MIS 4~MIS 2), eolian sedimentary layers were developed by terrestrial aeolian processes by which fine materials were transported from the Yellow Sea which became a dry land exposed by lowered sea level. In the third stage, various mechanism existed for the formation of each sedimentary layer. In the region of Ujeon A, sedimentary layers were developed in the littoral zone environment dominated by marine processes during the maximum phase of transgression in the Holocene. Meanwhile, the region of Ujeon B began to form eolian sedimentary layers during MIS 2. In the last stage, thick coastal dune deposits, covered all over the Ujeon Coast. During the late Holocene (0.7~0.6 ka), terrestrial processes kept dominating the region, developing typical eolian sedimentary layers.

• 한국광물학회지
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• 제27권4호
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• pp.169-181
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• 2014

우리나라는 2008년부터 심해저 광물자원 확보를 위하여 남서태평양 통가국 EEZ 내 Tofua arc의 해저 화산열도에서 해저열수광상에 관한 조사를 지속적으로 수행하고 있다. 통가국 라우분지 TA 25 해저산에서 해저 열수 활동에 의하여 형성된 광물들의 특성과 분포를 규명하기 위하여 X선회절분석, 주사전자현미경 관찰, X선형광분석과 유도결합 플라즈마 방출분광분석을 실시하였다. 연구에 사용된 시료는 TA 25 해저산 주변에서 채취된 7개의 코어 시료와 9개의 해저퇴적물 시료이다. 열수분출구 모든 지역에서 중정석, 섬아연석, 클리노클레이스 등이 존재하고, 열수분출구 A 지역에는 석고, 스멕타이트 및 카올린 광물, 열수분출구 B와 C 지역에는 스멕타이트, 카올린 광물, 황동석과 황철석, 열수분출구 D 지역에는 석고, 황동석, 황철석, 침철석 등이 분포한다. 점토부분에 대한 분석 결과 칼데라 중심부 지역을 제외한 모든 지역에서 스멕타이트와 소량의 카올리나이트가 포함되어 있는 것으로 보아 이질변질작용에 해당하는 열수변질이 있었음을 알 수 있다. 열수분출구 B, C, D 지역은 여러가지 종류의 황화광물과 비소화광물이 존재한다. 광물조성, 주성분과 미량성분 분석 결과로 판단할 때 열수분출구 B, C, D 지역이 비교적 강한 고온의 열수변질작용, 열수분출구 A와 칼데라 중심부 지역은 열수의 영향을 적게 받았거나 저온의 열수변질작용을 받은 것으로 판단된다. 추후 열수광상 탐사는 열수분출구 B, C, D 지역에서 수행되어야 할 것으로 여겨진다.

• 한국산업보건학회지
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• 제8권1호
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• pp.50-66
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• 1998

This study was conducted to estimate crystalline silica contents in airborne respirable dust from various manufacturing industries and to compare analytical performance of two methods of quantifying crystalline silica, X-ray diffraction(XRD) and Fourie transform infrared spectroscopy (FTIR). For this study, various manufacturing industries with a history of having pneumoconiosis cases and also known to generate dusts containing crystalline silica were investigated. These industries include: foundry, brick, potteries, concrete, and abrasive material, etc. Both personal and area respirable dust samples were collected using 10 mm, Dorr-Oliver nylon cyclone equipped with 37mm, $5{\mu}m$ pore size, polyvinylchloride (PVC) filters as collection media. In addition, total dust samples were collected side-by-side to the respirable samples. All samples were weighed before and after sampling and were pretreated according to the NIOSH sampling and analytical methods 0500, 7500, and 7602 for dust collection and quartz analysis. In addition, bulk samples were collected and analyzed by X-ray fluorescence (XRF) for minerals. In this article, only the results obtained from foundry are reported. The results from various other industries will be published in future articles. The respirable dust concentrations from personal samples by cyclone were $0.46-1.06mg/m^3$ and those from area samples were $0.34-0.73mg/m^3$. Dust concentrations of personal samples were significantly higher than those of area samples. The highest dust concentration was obtained from the personal samples of the finishing operation. Total dust concentration ranged $1.24-3.40mg/m^3$. The mean quartz contents estimated by FTIR and XRD in the personal respirable dust samples were 5.12% and 4.41%, respectively, without significant difference between them. For quartz analyses, the two techniques were highly correlated with $r^2$ ranged 0.803-0.920. But the results by FTIR were mostly higher than those by XRD. In addition, cristobalite was not detected by FTIR. Significant correlations between contents of crystalline silica and such minerals as $Al_2O_3$, CaO, $TiO_2$, and $K_2O$ suggest possible interferences from these minerals.

• 한국수소및신에너지학회논문집
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• 제24권5호
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• pp.359-366
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• 2013

This work is investigated for the catalytic decomposition of hydrogen iodide (HI). Platinum was used as active material by loading on $ZrO_2-SiO_2$ mixed oxide in HI decomposition reaction. To obtain high and stable conversion of hydrogen iodide in severe condition, it was required to improve catalytic activity. For this reason, a method increasing dispersion of platinum was proposed in this study. In order to get high dispersion of platinum, zirconia was incorporated in silica by sol-gel synthesis. Incorporating zirconia influence increasing platinum dispersion and BET surface area as well as decreasing deactivation of catalysts. It should be able to stably product hydrogen for a long time because of inhibitive deactivation. HI decomposition reaction was carried out under the condition of $450^{\circ}C$ and 1 atm in a fixed bed reactor. Catalysts analysis methods such as $N_2$ adsorption/desorption analysis, X-ray diffraction, X-ray fluorescence, ICP-AES and CO gas chemisorption were used to measurement of their physico-chemical properties.

• 헤리티지:역사와 과학
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• 제40권
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• pp.413-430
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• 2007

우리나라 저습지에서 출토되는 목제유물은 대부분 흑갈색을 띠고 있다. 이와 같은 현상은 매장 환경의 주체인 토양성분에 기인한다고 할 수 있다. 예를 들면 광주 동림동 저습지 유적과 창녕 송현동 고분군 내의 토양성분을 비교 분석한 결과 두 유적 모두 Si, AI, Fe 등의 함유량이 높게 나타난 바가 있다. 또한 신안선과 광주 동림동 및 창녕 송현동 고분 출토 목재의 무기물 분석에서도 모두 토양의 주성분인 Si보다 Fe의 함유량이 상대적으로 높은 수치를 나타냈으며, 성분과 함유량에 있어서도 유사함을 보였다. 출토지가 다름에도 불구하고 Fe 함량에서 유사한 결과를 나타내는 것은 일반적으로 매장 환경의 영향을 크게 받는다는 근거자료가 될 수 있는 것이다. 그 중 Fe는 목재의 열화로 생성된 타닌과 반응하여 타닌산 제I철이 되고, 산소와 결합하여 타닌산 제II철이 되므로 흑색을 띠게 된다. 이러한 목재흑화의 주원인이라고 할 수 있는 Fe은 EDTA를 사용하여 킬레이트 화합물을 형성함으로써 제거가 가능하다. EDTA를 통해 흑화된 목재에서 Fe을 제거하는 실험을 한 결과 EDTA-2Na가 가장 효율적이었으며, 72시간 동안 반응 후 용액을 제거하고 다시 EDTA와 반응시켜 Fe을 제거하는 방법이 가장 효과적으로 흑화현상을 제거할 수 있었다.

• 박물관보존과학
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• 제31권
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• pp.1-20
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• 2024

국립중앙박물관이 소장하고 있는 부석사 괘불(浮石寺 掛佛, 1684년, K969)은 사찰의 야외 행사에 사용하기 위해 제작한 대형 불화이다. 하단에 석가모니불을 중심으로 비로자나불, 약사불, 아미타불의 부처가 그려져 있으며 현존하는 괘불 중에서 가장 복잡한 구성을 보여준다. 본 연구는 부석사 괘불에 대해 바탕직물의 특성과 괘불 제작방법을 조사하고 채색에 사용된 재료를 판별하기 위한 비파괴 조사 결과를 종합하여 채색기법의 특징을 연구한 것이다. 부석사 괘불은 좌·우로 11폭, 상·하단으로 각 1폭씩 연결되어 총 13폭이며 중심 부분의 9폭은 생초(生綃), 사면을 두르는 4폭은 주(紬)를 사용하여 그림의 바탕을 만들었다. 그림을 그리는 데 사용된 채색 재료는 엑스선형광분석 방법으로 조사하였고 적색, 황색, 녹색, 청색, 흰색의 무기안료이며 황색과 청색의 일부에서는 연백을 먼저 칠하고 그 위에 유기안료로 색상을 표현했음을 확인하였다. 또한 검은 선은 먹, 가사의 문양에는 금박이 사용되었다. 엑스선조사는 안료의 주성분과 안료층의 두께에 따라 밝고 어둡게 보이는 차이를 판독하는 것으로 안료의 색상에 따른 채색 위치와 기법을 확인할 수 있었다.

• Environmental Analysis Health and Toxicology
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• 제31권
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• pp.6.1-6.10
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• 2016

Objectives This study examined the spatial distribution and the extent of soil contamination by heavy metals resulting from primitive, unconventional informal electronic waste recycling in the Agbogbloshie e-waste processing site (AEPS) in Ghana. Methods A total of 132 samples were collected at 100 m intervals, with a handheld global position system used in taking the location data of the soil sample points. Observing all procedural and quality assurance measures, the samples were analyzed for barium (Ba), cadmium (Cd), cobalt (Co), chromium (Cr), copper (Cu), mercury (Hg), nickel (Ni), lead (Pb), and zinc (Zn), using X-ray fluorescence. Using environmental risk indices of contamination factor and degree of contamination ($C_{deg}$), we analyzed the individual contribution of each heavy metal contamination and the overall $C_{deg}$. We further used geostatistical techniques of spatial autocorrelation and variability to examine spatial distribution and extent of heavy metal contamination. Results Results from soil analysis showed that heavy metal concentrations were significantly higher than the Canadian Environmental Protection Agency and Dutch environmental standards. In an increasing order, Pb>Cd>Hg>Cu>Zn>Cr>Co>Ba>Ni contributed significantly to the overall $C_{deg}$. Contamination was highest in the main working areas of burning and dismantling sites, indicating the influence of recycling activities. Geostatistical analysis also revealed that heavy metal contamination spreads beyond the main working areas to residential, recreational, farming, and commercial areas. Conclusions Our results show that the studied heavy metals are ubiquitous within AEPS and the significantly high concentration of these metals reflect the contamination factor and $C_{deg}$, indicating soil contamination in AEPS with the nine heavy metals studied.

• 한국대기환경학회지
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• 제21권6호
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• pp.699-708
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• 2005

To characterize the elemental composition of fine particles in urban area, $PM_{2.5}$ was collected by a 3-stage DRUM impactor at Gwangju during spring and summer. Time and size resolved concentrations for 19 trace elements were obtained by synchrotron X-Ray fluorescence analysis. Trace elements in summer were distributed in smaller size range compared to those in spring. Almost trace element concentrations in fine particles were highly increased during the Asian dust. In spring, soil elements such as Si, K, Ca, Ti and Fe had low enrichment factors indicating the dominant influence of soil dust. However, all elements had high enrichment factors in summer implying that these elements could be emitted from the anthropogenic sources. Factor analysis was conducted with the elemental composition data in order to identify anthropogenic sources of aerosols in urban area during spring and summer. Fine particles in spring have several sources such as soil dust originating from China continental region, coal and oil combustion, biomass burning, sea salt, ferrous and nonferrous metal sources. On the other hand, fine particles in summer were influenced by road dust, gasoline vehicle as well as coal and oil combustion, sea salt, ferrous and nonferrous metal sources.

• 한국산업보건학회지
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• 제11권3호
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• pp.229-234
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• 2001

The EDXRF(Energy Dispersive X-ray Fluorescence Spectrometer) technique was applied to the determination of heavy metals in welding fume. The EDXRF method designed in this study was a non-destructive analysis method. Samples were analyzed directly by EDXRF without any pre-treatment such as digestion and dilution. The samples used to evaluate this method were laboratory samples exposed in a chamber connected with a welding fume generator. The samples were first analyzed using a non-destructive EDXRF method. The samples subsequently were analyzed using AAS method to verify accuray of the EDXRF method. The purpose of this study was to evaluate the possibility of the non-destructive analysis of heavy metals in welding fume by EDXRF. The results of this study were as follow: 1.When the samples were collected under the open-face sampling condition, a surface distribution of welding fume particles on sample filters was uniform, which made non-destructive analysis possible. 2. The method was statistically evaluated according to the NIOSH(National Institute for Occupational Safety and Health) and HSE(Health and Safety Executive) method. 3. The overall precision of the EDXRF method Was calculated at 3.45 % for Cr, 2.57 % for Fe and 3.78 % for Mn as relative standard deviation(RSD), respectively. The limits of detection were calculated at $0.46{\mu}g$/sample for Cr, $0.20{\mu}g$/sample for Fe and $1.14{\mu}g$/sample for Mn, respectively. 4. A comparison between the results of Cr, Fe, Mn analyzed by EDXRF and AAS was made in order to assess the accuracy of EDXRF method. The correlation coefficient between the results of EDXRF and AAS was 0.9985 for Cr, 0.9995 for Fe and 0.9982 for Mn, respectively. The overall uncertainty was determined to be ${\pm}12.31%$, 8.64 % and 11.91 % for Cr, Fe and Mn, respectively. In conclusion, this study showed that Cr, Fe, Mn in welding fume were successfully analyzed by the EDXRF without any sample pre-treatment such as digestion and dilution and a good correlation between the results of EDXRF and AAS was obtained. It was thus possible to use the EDXRF technique as an analysis method of working environment samples. The EDXRF method was an efficient method in a non-destructive analysis of heavy metals in welding fume.

• 지질공학
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• 제27권1호
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• pp.67-79
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• 2017

암석내 화학종의 함량을 이용한 풍화지수는 암석의 풍화 정도와 2차 광물의 생성을 예측하는데 매우 효과적이다. 풍화의 과정은 암석의 종류에 따라 다르게 나타나는데 국내의 경우 화강암의 분포 면적이 넓은 이유로 풍화지수의 연구는 산성질 화성암에 편중되어 왔다. 이 연구는 쇄설성 퇴적암에 속하는 사암, 이암, 셰일의 전암분석(X-선 형광분석)을 이용하여 풍화지수들을 산정하고, 상관성 분석을 통해 지수들의 유의성을 검토하였다. 쇄설성 퇴적암 중 장석의 비중이 높게 나타나는 사암과 셰일의 경우 장석의 풍화를 나타내주는 Wp, CIA, CIW, PIA 풍화지수가 높은 유의성을 보였다. 화학적 변질지수(CIA)는 풍화경로와 변질점토의 생성을 예측할 수 있는 장점이 있으나 풍화 정도의 변별력을 높이기 위해 화학적 풍화지수를 동시에 고려하는 것이 효과적이다. 탄산염 계열의 광물이 포함된 경우 이에 대한 효과를 산정식을 통해 제거하지 못하였고 정확한 풍화지수 산정을 위해 X-선 회절분석 등을 통해 탄산염 물질의 함량이 높은 시료는 분석과정에서 배제해야 한다.