地球化学
地毬化學
지구화학
GEOCHIMICA
2013年
1期
46-52
,共7页
离子交换分离%Fe同位素%地质标样
離子交換分離%Fe同位素%地質標樣
리자교환분리%Fe동위소%지질표양
ion exchange chromatography%iron isotopes%geological reference materials
报道了利用少量 AG1-X4阴离子交换树脂分离地质样品中 Fe 及测定 Fe 同位素的方法.对少量AG1-X4和AG MP-1树脂的分离效果进行了比较,测定了经过AG1-X4分离后的地质标样BCR-2、BHVO-2、BIR-1a、AGV-2、W-2、GSP-2、COQ-1、DTS-2b、JB-2、Jsd-1、GBW07105和 GBW07267的 Fe 同位素组成,其结果与文献参考值在误差范围内一致.这些数据的发表对于地质样品Fe的化学分离和同位素测定提供了参考依据.此方法可以大大减少化学试剂用量,是一种快速有效分离铁的方法.
報道瞭利用少量 AG1-X4陰離子交換樹脂分離地質樣品中 Fe 及測定 Fe 同位素的方法.對少量AG1-X4和AG MP-1樹脂的分離效果進行瞭比較,測定瞭經過AG1-X4分離後的地質標樣BCR-2、BHVO-2、BIR-1a、AGV-2、W-2、GSP-2、COQ-1、DTS-2b、JB-2、Jsd-1、GBW07105和 GBW07267的 Fe 同位素組成,其結果與文獻參攷值在誤差範圍內一緻.這些數據的髮錶對于地質樣品Fe的化學分離和同位素測定提供瞭參攷依據.此方法可以大大減少化學試劑用量,是一種快速有效分離鐵的方法.
보도료이용소량 AG1-X4음리자교환수지분리지질양품중 Fe 급측정 Fe 동위소적방법.대소량AG1-X4화AG MP-1수지적분리효과진행료비교,측정료경과AG1-X4분리후적지질표양BCR-2、BHVO-2、BIR-1a、AGV-2、W-2、GSP-2、COQ-1、DTS-2b、JB-2、Jsd-1、GBW07105화 GBW07267적 Fe 동위소조성,기결과여문헌삼고치재오차범위내일치.저사수거적발표대우지질양품Fe적화학분리화동위소측정제공료삼고의거.차방법가이대대감소화학시제용량,시일충쾌속유효분리철적방법.
AG MP-1 anion exchange resin has been reported to be an effective chromatographic technique choice for the complete separation of Cu, Fe and Zn in geological samples. In the cases of Fe being the only interested element, AG1-X4 showed better separation efficiencies. In this work, an effective Fe separation procedure has been successfully established using small amount of AG1-X4 anion exchange resin, aiming to speed up separation, to reduce consumption of regents and to lower down the regent background. Comparison with AG MP-1 has been also made. Fe isotope compositions have been measured on geological reference materials, namely BCR-2, BHVO-2, BIR-1a, AGV-2, W-2, GSP-2, COQ-1, DTS-2b from USGS (United States Geological Survey), JB-2, Jsd-1 from GSJ (Geological Survey of Japan) as well as GBW07105 and GBW07267 from RMRC (National standard reference materials research center). With the analytical results being identical with those reported values within analytical errors, the described separation method and reported data set may serve as valuable references for iron isotopic studies.