희토류원소와 동위원소의 환경지화학에의 응용을 위한 기초연구
자료유형 | KIGAM 보고서 |
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서명 | 희토류원소와 동위원소의 환경지화학에의 응용을 위한 기초연구 |
저자 | 이승구 |
언어 | KOR |
청구기호 | KR-2001-[B]-07-2001-R |
발행사항 | 한국지질자원연구원, 2001 |
초록 | : 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 138La, 142Ce, 145Nd, 149Sm, 151Eu, 157Gd, 163Dy, 167Er, 171Yb, and 176Lu 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. As a result of repeated experiment in order to estimate REE abundance for some gneiss sample, we found that there are some difference in their REE abundance and, nevertheless, existed some regularities in chondrite-normalized REE pattern. Therefore, our results confirm that rare earth elements are very usefiul tool for solving various kinds of geochemical problems in earth environment |
페이지 | 55 p. |
키워드 | 희토류원소, 동위원소, 환경지화학, 원소, 응용 |
원문 | 다운로드 |
유형별 보고서
이승구. (2001). 희토류원소와 동위원소의 환경지화학에의 응용을 위한 기초연구. 한국지질자원연구원.