• The Journal of the Petrological Society of Korea
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• v.10 no.3
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• pp.190-201
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• 2001

Isotope Dilution Mass Spectrometry(IDMS) is one of the analytical method which uses enriched isotope spikes and analyzes the abundance of element by comparison of the spectrum between spiked mass and non-spike mass. Especially, the Thermal Ion Mass Spectrometry with isotope dilution technique (in general ID-TIMS) is the most accurate method of the chemical analysis, which enables us to obtain the data better than 1% in accuracy and precision. In IDMS, enriched isotope spike is one of the most important factor in order to obtain the best data. For rare earth elements, in general, a mixture of /sup 138/La, /sup 142/Ce, /sup 145/Nd, /sup 149/Sm, /sup 151/Sm, /sup 151/Eu, /sup 157/Gd, /sup 163/Dy, /sup 167/Er, /sup 171/Yb, and /sup 176/Lu is used as composite spike. IDMS is very useful in geochronology and REE geochemistry. Especially, it is very effective in studying the “tetrad effect” of rare earth elements in natural samples.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2003.04a
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• pp.59-62
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• 2003

동위원소희석법에 의한 열이온화 질량분석법 (ID-TIMS)을 이용하여 지하수내 희토류원소의 함량을 측정하였다. 희토류원소의 분리에는 철공침법과 양이온교환수지에 의한 컬름분리법을 이용하였다. 경희토류(La-Eu)와 Gd, Dy, Er의 경우 수-수십 ppt의 수준에서 1%이내의 오차범위를 측정되어졌으며, 중희토류 중 Yb와 Lu은 정확도가 다소 떨어진 10% 전후에서 측정되었다. 지하수내 함량을 운석으로 규격화한 결과, 경희토류가 부화되었고 중희토류는 결핍되었으며 Eu의 이상은 거의 존재하지 않는다. 특히 경희토류에서는 M-type의 테트라드효과, 중희토류에서는 W-type의 테트라드효과가 관찰되었다. 이는 희토류원소의 수화수와 밀접한 관련이 있는 것으로 사료된다.

• Journal of the Korean Chemical Society
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• v.63 no.5
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• pp.387-391
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• 2019

• Analytical Science and Technology
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• v.16 no.6
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• pp.450-457
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• 2003

The determination of uranium and its isotopes in spent nuclear fuels by isotope dilution mass spectrometry (IDMS) has been studied. The spent fuel samples were dissolved in 8 M $HNO_3$ or its mixture with 14 M $HNO_3-0.05M$ HF. The dissolved solutions were filterred on membrane filter with $1.2{\mu}m$ pore size. The uraniums in the spiked and unspiked sample solutions were quantitatively adsorbed by anion exchange resin, AG 1X8 and eluted with 0.1 M HCl. The contents of uranium and its isotopes ($^{234}U$, $^{235}U$, $^{236}U$ 및 $^{238}U$) in the spent fuel samples were determined by isotope dilution mass spectrometric method using $^{233}U$ as spike. The spike reference solution was standarized by reverse isotope dilution mass spectrometry (R-IDMS) using natural and depleted uranium. The results from IDMS were in average relative difference of 0.34% when compared with those by the potentiometric titration method.

• Analytical Science and Technology
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• v.27 no.6
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• pp.269-276
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• 2014

A short study for the uncertainty of post column isotope dilution method has been performed for the analysis of Selenomethionine in HPLC-ICP/MS. Major error sources studied were concentration and the flow rate of Se isotope solution, atomic weights of Se in spike and sample, and isotope ratio measured for the spiked sample. Uncertainties were obtained for each factor and the contribution for the total concentration uncertainty was 54.4% and 0.61%, 0.0072% and 0.018%, and 45.0%, respectively. The biggest contribution factor was concentration of the spike solution and the second was the isotopic ratio measured for the spiked sample solution. The mass flow rate of spike and atomic weights did not show much contribution. The calculated total uncertainty was $1.46ng{\cdot}g^{-1}$ for the standard SeMet ($126.30ng{\cdot}g^{-1}$). The experimental result was $127.09{\pm}1.46ng{\cdot}g^{-1}$ and the relative uncertainty was 1.20%.

• Analytical Science and Technology
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• v.17 no.1
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• pp.29-36
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• 2004

An analytical method of polybrominated diphenyl ethers in soil samples by isotope dilution method using gas chromatography/mass spectrometry (GC/MS)-selected ion monitoring (SIM) was described. PBDEs in soil were extracted with soxhlet extractor and then silica and florisil solid phase extraction (SPE) methods as purification of extract were compared. After clean-up, the extractions were analyzed by GC/MS with SIM mode. Quantitation was performed isotope dilution method using four $^{13}C$ isotopically labeled PBDEs as internal standards. This developed method was validated for eight congeners of PBDEs in the concentration range 0.04~4 ng/g in soil and the average recovery of the analytes ranged 30.8~110.8% for florisil and 44.4~110.7% for silica, respectively. The method detection limits of PBDEs were 0.04~0.3 ng/g.

• Analytical Science and Technology
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• v.27 no.3
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• pp.140-146
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• 2014

An internal standard was used in PCID (post column isotope dilution) to improve the accuracy and precision in quantification of various chemical species. The error occurring in the column was the largest in HPLC-ICP/MS (high performance liquid chromatography-inductively coupled plasma/mass spectrometry) when PCID and other traditional quantification methods were compared with each other. Internal standard was effective in correcting the loss of sample in the column to improve accuracy and precision. When applied to SeMet, using MeSecys or $Se^{4+}$ as an internal standard, relative errors were reduced from 31% and 13% to less than 1%, while standard deviations were reduced from 5.1% and 6.9% to 1.5% and 0.2%, respectively. Positive aspects of using an internal standard in PCID were compared with other quantitative techniques and discussed in detail.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2003.09a
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• pp.210-212
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• 2003

동위원소희석법에 의한 열이온화 질량분석법(ID-TIMS)을 이용하여 한국지질자원연구원과 에너지기술연구 원내 지하수와 강우 희토류원소의 함량을 측정/해석하였다. 분석결과를 토대로 지하수의 희토류원소 함량은 강우의 함량과 비교해 볼 때, 상대적으로 낮은 값을 보여준다. 그리고 굴착 심도가 더 깊은 한국지질자원연구원의 지하수내 희토류원소 함량이 한국에너지기술연구원의 지하수내 함량보다 더 낮은 값을 보여준다. 이는 강우가 지하로 흘러들어 가면서, 희토류원소와 대수층 구성암석과의 흡착반응에 의해 심부로 갈수록 함량이 낮아졌을 가능성이 크다고 판단된다. 뿐만 아니라, 강우의 경우, 희토류원소의 W형-테트라드 효과가 매우 현저하게 나타나고, 지하수에서는 M형과 W형의 테트라드 효과가 동시에 존재하는 특성이 강한데, 이는 희토류원소의 수화수 및 화강암 대수층과의 물-암석 반응에 의한 결과인 것으로 사료된다.

• Proceedings of the Korean Radioactive Waste Society Conference
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• 2006.06a
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• pp.198-198
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• 2006

• Proceedings of the Korean Radioactive Waste Society Conference
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• 2007.11a
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• pp.259-260
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• 2007