• Title/Summary/Keyword: 원소분석

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Silicon Isotope Measurement of Giant Diatoms Using MC-ICP-MS (다검출기 유도결합 플라즈마 질량분석기를 이용한 대형 규조류 규소 동위원소 분석법)

  • Choi, Ah Yeong;Ryu, Jong-Sik;Hyeong, Kiseong;Kim, Mun Gi;Ra, Kongtae;Jeong, Hyeryeong;Lim, Hyoun Soo
    • Journal of the Korean earth science society
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    • v.42 no.1
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    • pp.1-10
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    • 2021
  • Silicon (Si) is the second most abundant element in the crust and consists of three stable isotopes, 28Si (92.23%), 29Si (4.67%), and 30Si (3.10%). Si isotopes are widely studied worldwide as a proxy for the biogeochemical cycle of Si to reconstruct the paleoenvironment and paleoclimate. However, in Korea, there have been no studies on biogenic silica using Si isotopes. In this study, we carried out Si isotope measurements of giant diatoms, summarizing the previously reported alkali fusion methods and establishing the best Si separation method for biogenic silica. Samples were completely digested using alkali fusion at high temperatures, effectively separating Si using an AG® 50W-X8 cation exchange resin. To evaluate the precision and accuracy of our measurements, Si isotope standard material (NBS-28) and USGS reference materials (AGV-2, GSP-2, BHVO-2) were analyzed. The results are in excellent agreement with the reported values within the acceptable error. The Si isotope measurement method developed in this study is expected to help in understanding the paleoclimate and paleoenvironment by tracing the Si cycle.

Comparison of Ambient Concentration of Heavy Metals in Taejon Area (대전지역 대기 분진중 중금속의 농도 비교)

  • 구부미;임종명;장미숙;이진홍
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 2000.11a
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    • pp.63-64
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    • 2000
  • 본 연구는 대전 1,2공단 지역을 대상으로 22개의 원소를 선정하여 ICP-MS를 이용하여 분석한 농도와 도로변 지역인 충남대학교 정문 지역을 대상으로 31개의 원소를 선정하여 NAA를 이용하여 분석한 농도를 가지고 두 가지의 분석방법에서 공통적으로 분석된 원소들을 통해 대전의 대표적인 공단지역과 도로변 지역의 농도를 비교 평가해 보고자 한다. (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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    • 2003.11a
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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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A STUDY ON KOREAN ANTHRACITE BY INSTRUMENTAL NEUTRON ACTIVATION ANALYSIS

  • Kim, N.B.;Woo, H.J.;Lee, K.Y.;Hong, W.;Chun, S.K.;Park, K.S.
    • Analytical Science and Technology
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    • v.7 no.4
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    • pp.477-482
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    • 1994
  • By the instrumental neutron activation analysis using two comparators of gold and cobalt, 31 elements have been anlalyzed in anthracites collected from two main coal-fields in Korea. The average concentrations and ranges of the elements were obtained with the elemental difference between two coal-fields. The trends of rare-earth elemental distribution and vertical elemental distribution are also given.

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A Study on Three-Dimensional Performance Analysis of Antenna Array Appling LMS Adaptive Algorithm (LMS 적응 알고리즘을 적용한 안테나 배열의 성능분석에 관한 연구)

  • 김원균;박지영;나상동
    • Proceedings of the Korean Institute of Information and Commucation Sciences Conference
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    • 1998.05a
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    • pp.400-404
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    • 1998
  • 본 논문에서는 도심지 이동 통신에서 SINR 성능을 향상시키기 위해 기존의 배열 안테나에 최소 평균 자승(LMS) 알고리즘을 적용하여 실제 배열 출력과 이상적 출력간의 최소 평균 오차(MSE)를 최소화하고 안테나의 배열로부터 가중치를 결합한 신호에 의해 방향성을 적절히 제어하여 간섭신호를 효과적으로 제거한다. 배열 출력 신호 대 간섭에 추가된 잡음비(SINR) 성능 분석에 적합한 삼차원적 분석을 사용하여 적응 배열 원소를 사용한 성능과 모노폴 안테나 원소에서 배열의 성능을 비교한다. 또한, SINR 패턴 각 비(PAR)를 사용하여 적응 배열 원소 방위, 내부 원소간의 간격들 그리고 입사 신호 방향들과 같은 다른 배열 매개 변수들에서 배열 성능을 계산하고 SINR 패턴의 양적 평가를 한다. 결과로서, 적응 배열 원소가 가정된 신호 환경에 있어 4상파형(quarterwave) 모노폴(monopole) 안테나 배열보다 더 바람직하다.

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Determination of Cadmium, Copper, Lead, Nickel, and Zinc in Sediments by ID-ICP/MS (동위원소희석 질량분석법에 의한 저니토 중의 카드뮴, 구리, 납, 니켈, 아연의 정량)

  • Cho, Kyung-Haeng;Park, Chang-Joon;Suh, Jung-Kee;Han, Myoung-Sub
    • Analytical Science and Technology
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    • v.13 no.3
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    • pp.297-303
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    • 2000
  • Isotope-dilution inductively coupled plasma mass spectrometry was used to determine trace amounts of Cd, Cu, Pb, Ni and Zn in sediment. Sediment samples were dissolved by microwave digestion with addition of mixed acid ($HNO_3$, HF and $HClO_4$). Lead was determined after separation of alkaline and alkaline earth metals by an ammonium pyrrolidenedithiocarbarmate (APDC) solvent extraction. The other elements were determined after separation of iron, tin and titanium by hydroxide precipitation. Recovery efficiency of the analyte elements was not satisfactory, but most of matrix elements causing the isobaric interference could be effectively eliminated by the separation. Good agreement was achieved with the certified values in the analysis of the two sediment reference materials.

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pH Effect for the Separation of Lanthanides with Pyromellitic Acid and Oxalic Acid (Pyromellitic Acid와 Oxialic Acid 용리액에 의한 란탄족 원소의 분리에서 pH의 영향)

  • Lee, Kyung-Ae;Kim, Chae-Kyun;Sung, Hak-Je;Chang, Choo-Wan
    • Analytical Science and Technology
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    • v.6 no.1
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    • pp.121-129
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    • 1993
  • UV/VIS spectrophotometer interfaced with HPIC(High Performance Ion Chromatography) has been applied to the determination of lanthanide elements. The separation of lanthanide elements with HPIC helped to avoid erroneous analytical results due to interferences. Individual lanthanide elements at ppm level were separated on a HPIC CS5 column using pyromellitic acid and oxalic acid. The individual lanthanide elements were detected at 520nm following post-column reaction with PAR. Sm, Eu, Gd, Y, Tb, Dy, Ho, Er, Tm, Tb, and Lu were separated by pyromellitic acid. La, Ce, Pr and Nd were separated by oxalic acid. Appropriate pH of pyromellitic acid for separation was at pH 2.99.

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Low Dilution Glass Bead Digestion Technique for the Trace Element Analysis of Rock Samples (저희석 유리구 용해법에 의한 암석시료 미량원소 분석법)

  • Park, Chan-Soo;Shin, Hyung-Seon;Oh, Hae-Young;Moon, Jong-Hwa;Cheong, Chang-Sik
    • The Journal of the Petrological Society of Korea
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    • v.20 no.3
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    • pp.161-172
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    • 2011
  • Open beaker digestion method is routinely used as the sample preparation technique for trace element determination of rock samples by inductively coupled plasma mass spectrometry, With this method, however, dissolution of Zr and Hf is not always guaranteed especially when the samples contain refractory minerals. In this study, glass bead digestion technique was compared with conventional open beaker digestion technique for the sample preparation of three USGS rock standards such as AGV-2, BHVO-2, and G-3. Thirty trace elements including rare earth elements were analysed by ICP-MS and ICP-AES. There were no clear differences in analytical results for the AGV-2 and BHVO-2 standards between the two techniques, but Zr, Hf, Y, and middle- to heavy- rare earth element concentrations of the G-3 standard prepared by open beaker digestion technique were significantly lower than the recommended values. This can be attributed to the presence of refractory mineral zircon. On the contrary, all the analytical results of the G-3 standard prepared by glass bead digestion technique were in good agreement with the recommended values, indicating complete dissolution of zircon. The analytical results show that the volatile elements such as Pb and Zn were not lost during the preparation of glass bead. Low dilution glass bead digestion technique described here will be very helpful to enhance precision and accuracy of trace element analysis for geological samples containing refractory minerals.