• 제목/요약/키워드: 미량 원소

검색결과 710건 처리시간 0.034초

Chemical Characteristics for Hydrothermal Alteration of Surface Sediments from Submarine Volcanoes of the Tonga Arc (통가열도 해저화산 표층 퇴적물 내 열수변질의 화학적 특성)

  • Um, In Kwon;Chun, Jong-Hwa;Choi, Hunsoo;Choi, Man Sik
    • Journal of the Mineralogical Society of Korea
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    • 제26권4호
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    • pp.245-262
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    • 2013
  • We analyzed 29 surface sediment samples in five submarine volcanoes (TA12, TA19, TA22, TA25, and TA26) located in the southern part of the Tonga arc for trace elements and rare earth elements to investigate characteristics of the hydrothermal alteration of surface sediments. Based on analytical results of trace element and rare earth element (REE), surface sediments of TA12, TA19, and TA22 submarine volcanoes, which are located in the northern part of the study area, were very little or not influenced by hydrothermal fluids. In contrast, some stations of TA25 and TA26 submarine volcanoes were strongly affected by hydrothermal fluids. However, these two submarine volcanoes showed different features in element concentration in the sediments. Some stations of TA25 submarine volcano showed enrichment of Ni, Cu, Sn, Zn, Pb, Cr, Cd, Sb, W, Ba, Ta, Rb, Sr, and As, however, those of TA26 submarine volcano showed enrichment of Sn, Zn, Pb, Cd, Sb, Ba, Rb, and Sr. Stations which enriched trace elements were observed, enriched REEs were also observed. Average upper continental crust (UCC)-normalized REE patterns of the surface sediments generally showed low light REE (LREE) abundances and increased heavy REE (HREE) abundances. Eu enrichment was identified at several stations of TA25 and TA26 submarine volcanoes. In addition, enrichment of Ce was found at some stations of TA26 submarine volcano and these enrichment patterns were similar with hydrothermal fluid of near stations. Furthermore, TA25 and TA26 submarine volcanoes showed different enrichment characteristics of trace elements and REE. Trace elements were concentrated at TA25 submarine volcano. TA26 submarine volcano, on the other hand, observed highly enrichment of REE especially, Eu and Ce. As a result of the investigation, the characteristics and concentrations of REEs and trace elements in the surface sediments of each submarine volcano can be applied to identify hydrothermal alteration of sediments during exploration for hydrothermal deposits.

Determination of Trace Elements in $PM_{2.5}/PM_{10}$ of Dsejeon Region using Neutron Activation Analysis(IV) (중성자 방사화분석에 의한 대전지역의 $PM_{2.5}/PM_{10}$ 농도 밀 미량원소의 측정(IV))

  • 문종화;김선하;임종명;정용삼
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 한국대기환경학회 2003년도 춘계학술대회 논문집
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    • pp.259-260
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    • 2003
  • 대기환경에 대한 정보의 파악은 환경연구의 기본이 된다. 유해원소 및 미량원소에 의한 환경오염과 그로 인한 인체건강에 대한 영향은 인간생활에 심각한 문제가 되므로 대기, 수질, 토양등의 환경시료 중의 농도를 정확히 측정하는 것은 매우 중요한 일이다. 중성자방사화분석법은 핵반응을 통해 생성시킨 방사성동위원소로부터 방출되는 방사선을 검색하여 절대적으로 성분원소를 정량하는 핵분석기술(Nuclear Analytical Techniques)중의 하나로서 소량의 시료로부터 미소량원소의 비파괴, 동시다원소분석이 가능하고 분석감도($10^{-3}$ - $10^{-7}$$\mu\textrm{g}$)가 탁월한 분석기술이다. (중략)

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Determination of Trace Elements in $PM_{2.5}/PM_{10}$ of Daejeon Region Using Neutron Activation Analysis(V) (중성자 방사화분석에 의한 대전지역 $PM_{2.5}/PM_{10}$의 미량원소농도의 측정(V))

  • 김선하;문종화;임종명;백성렬;정용삼
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 한국대기환경학회 2003년도 추계학술대회 논문집
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    • pp.376-377
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    • 2003
  • 대기환경에 대한 정보의 파악은 환경연구의 기본이 된다. 유해원소 및 미량원소에 의한 환경오염과 그로 인한 인체건강에 대한 영향은 인간생활에 심각한 문제가 되므로 대기, 수질, 토양등의 환경시료 중의 농도를 정확히 측정하는 것은 매우 중요한 일이다. 중성자 방사화분석법은 핵반응을 통해 생성시킨 방사성동위원소로부터 방출되는 방사선을 검색하여 절대적으로 성분원소를 정량하는 핵분석기술(Nuclear Analytical Techniques)중의 하나로서 소량의 시료로부터 미소량원소의 비파괴, 동시다원소분석이 가능하고 분석감도($10^{-3}$ - $10^{-7}$$\mu\textrm{g}$)가 탁월한 분석기술이다. (중략)

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Determination of Trace Elements in $PM_{2.}5/PM_{10}$ of Daejeon Region using Neutron Activation Analysis(II) (중성자 방사화분석에 의한 대전지역의 $PM_{2.}5/PM_{10}$ 농도 및 미량원소의 측정(II))

  • 문종화;박광원;김선하;정용삼
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 한국대기환경학회 2002년도 춘계학술대회 논문집
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    • pp.219-220
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    • 2002
  • 대기환경에 대한 정보의 파악은 환경연구의 기본이 된다. 유해원소 및 미량원소에 의한 환경오염과 그로 인한 인체건강에 대한 영향은 인간생활에 심각한 문제가 되므로 대기, 수질, 토양 등의 환경시료 중의 농도를 정확히 측정하는 것은 매우 중요한 일이다. 중성자방사화분석법은 핵반응을 통해 생성시킨 방사성동위원소로부터 방출되는 방사선을 검색하여 절대적으로 성분원소를 정량하는 핵분석기술(Nuclear Analytical Techniques)중의 하나로서 소량의 시료로부터 미소량원소의 비파괴, 동시다원소분석이 가능하고 분석감도($10^{-3}$-$10^{-7}$$\mu\textrm{m}$)가 탁월한 분석기술이다. (중략)

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Determination of Trace Elements in $PM_{2.5}/PM_{10}$ of Daejeon Region using Neutron Activation Analysis(III) (중성자 방사화분석에 의한 대전지역의 $PM_{2.5}/PM_{10}$ 농도 및 미량원소의 측정(III))

  • 문종화;김선하;박광원;임종명;정용삼
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 한국대기환경학회 2002년도 추계학술대회 논문집
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    • pp.328-329
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    • 2002
  • 대기환경에 대한 정보의 파악은 환경연구의 기본이 된다. 유해원소 및 미량원소에 의한 환경오염과 그로 인한 인체건강에 대한 영향은 인간생활에 심각한 문제가 되므로 대기, 수질, 토양 등의 환경시료 중의 농도를 정확히 측정하는 것은 매우 중요한 일이다. 중성자방사화분석법은 핵반응을 통해 생성시킨 방사성동위원소로부터 방출되는 방사선론 검색하여 절대적으로 성분원소를 정량하는 핵분석기술(Nuclear Analytical Techniques)중의 하나로서 소량의 시료로부터 미소량원소의 비파괴, 동시다원소분석이 가능하고 분석감도가 탁월한 분석기술이다. (중략)

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Geochemical Characteristics and Pollution Level of Heavy Metals of Asian Dust in Daejeon Area, 2007 (spring season) (2007년 봄철 대전지역에서 발생한 황사 및 대기부유물의 지구화학적 특성 및 중 금속의 오염도)

  • Lee, Pyeong-Koo;Youm, Seung-Jun;Bae, Beob-Geun
    • Economic and Environmental Geology
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    • 제45권3호
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    • pp.217-235
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    • 2012
  • We evaluated the geochemical characteristics and their potential pollution of Asian Dusts in Daejeon, Korea during spring 2007. Compared with the chemical compositions of soils in source area of Asian Dust, those of aerosols in Daejeon were enriched with trace elements (ten to hundred fold), inferring that pollutants from China have affected on local environment in adjoining country such as Korea. Chemical analysis of aerosols during Asian dust showed that fine particles ($PM_{2.5}$) contained high contents of trace elements such as Cr, Cu, Pb, Zn, V, S, As, Cd, Co, Ni, Mo, Sb, Cs, Rb, Th, Sc and Y. In the case of TSP (Total Suspended Particle), Zr, Sr, Ba, Li, Th and U were contained much more than other trace elements. The contents of some elements (i.e. Li, Cs, Co, U, Cr, Ni, Rb, V, Th, Y, Sr and Sc) in aerosols collected in Asian Dust period, which are not likely enriched by air pollutants, were higher (2 - 4.2 fold) than those in Non Asian Dust period, indicating that these elements could be used as indicator elements for determining the occurrence of Asian Dust phenomena (especially, Sr, V, Cr & Li). In the case of Asian Dust coming through the big cities and/or industrial areas of China, the domestic aerosols had higher contents of trace elements (such as S, Cd, Zn, Pb, Cu, Mo and As) than those from Northeastern China via North Korea, indicating that the transportation courses of air mass are very important to determine the pollution degrees. Using the enrichment factors of trace elements in aerosols during Asian Dust and Non Asian Dust, we identified that some elements (i.e. S, Zn, Cu, Pb, As, Mo and Cd) were most problematic in terms of environmental hazard aspects, and these elements could affect adverse effects on human health as well as ecosystem and surface environment (soil and water) through long-lived precipitation.

Geochemical Studies of the Trace Element of the Basalt in the Kilauea, Hawaii (킬라우에아 현무암의 미량원소에 대한 지구화학적 연구)

  • Park, Byeong-Jun;Jang, Yun-Deuk;Kwon, Suk-Bom;Kim, Jeong-Jin
    • Economic and Environmental Geology
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    • 제40권5호
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    • pp.675-689
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    • 2007
  • Kilauea volcano's summit area was formed by continuous ind/or sporadic eruption activities for several hundreds years. In this study, we mainly focused on the trace elements characteristics through systematic sample rocks erupted from 1790 to September of 1982. Under the microscope it can be observed some main minerals such as olivine, clinopyroxene. and plagioclase with minor opaque minerals including Cr-spinel and ilmenite. Zr, V, Y, Ti elements show incompatible activities with MgO while Ni, Cr, Co elements show highly compatible properties. Elements like as Ba, Rb, Th, Sr, Nd are highly incompatible to show positive trends with $K_2O$. In the REE diagram LREE is more enriched than HREE suggesting typical Oceanic Island Basalt(OIB) type. It can be suggested that Sr have an effect on the fractionation of plagioclase from the kink in the $K_2O$ variation diagram. Y/Ho ratio diagram shows there was no fluids effect in the historical Kilauea volcano but Zr/Hf ratio diagram shows a significant difference between Kilauea lavas and PuuOo lavas. There are distinctive changes of trace element contents showing in particular abrupt changes of temporal variations between 1924 and 1954. Moreover, PuuOo lavas which had been erupted since 1983 follow these decreasing trends of trace element variation. Therefore, it is strongly suggested that these abrupt changes of trace elements trends result from the huge collapse geological event which formed Halemaumau crater in 1924 causing contamination effects of crustal contents into magma chamber and from the changes of parental magma composition injected into Kilauea volcano's summit magma reservoir.

Preparation and Dissolution Properties of the Trace Elements doped ${K_2}O$-CaO-${P_2}{O_5}$ Glasses (미량원소함유 ${K_2}O$-CaO-${P_2}{O_5}$유리의 제조 및 용출 특성)

  • Lee, Hoi-Kwan;Kang, Won-Ho
    • Journal of the Korea Academia-Industrial cooperation Society
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    • 제6권2호
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    • pp.144-148
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    • 2005
  • At the previous papers, we showed that ${K_2}O$-CaO-${P_2}{O_5}$ glasses had a solubility in air so that they could be used for glass fertilizer. In this work, we fabricated the Eco-glass fertilizer containing trace elements of B, Mg, Zn, Fe, Cu, Co, Mo, the needed micronutrients for plants to grow, by a melt-quenching process. The dissolution properties in these glasses were investigated with a pH meter and an ICP analyzer. The trace elements doped glasses showed similar behavior in dissolutions and stability properties with the mother glass without containing trace elements. In addition, the dissolution amount of each trace elements depends on the mother glass composition and the quantity of each trace elements, which determine the dissolving velocity of chemical elements.

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Trace Element Compositions and Optically Stimulated Luminescence Characteristics of Sedimentary Quartz (퇴적물 내 석영의 광여기 루미네선스 특성과 미량원소 조성)

  • Jeon, Gi-Young;Choi, Jeong-Heon;Kil, Young-Woo
    • Journal of the Mineralogical Society of Korea
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    • 제23권4호
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    • pp.357-365
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    • 2010
  • Optically stimulated luminescence (OSL) of quartz is commonly applied to the age dating of Quaternary sediments. However, one of the issues is that some of the quartz samples are not suitable to OSL dating. Mineralogical analysis of the quartz samples with diverse OSL signals are required to strengthen the reliability and applicability of the OSL dating. We analysed the OSL signal characteristics of sedimentary quartz samples from diverse geological environments and measured their trace element contents using laser-ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). Quartz samples could be grouped into ones suitable to OSL dating and ones unsuitable on the basis of their OSL signal characteristics. The average trace element contents ranged from 73 to 260 ppm (Al), and from 61 to 248 ppm (Ti) with minor Li, Mg, Cr, Mn, and Fe contents below 40 ppm. We did not find any significant variation of trace element contents of quartz samples consistent with their OSL signal characteristics. This indicates unknown mineralogical factors causing diverse OSL characteristics which should be confirmed by further analysis of sufficient set of samples.