摘要
基性、超基性岩中的稀土元素含量极少,尤其后者,比花岗岩低1至2个数量级。文献用中子活化法测定两个超基性岩标样报出11项稀土元素含量。据此估算稀土总量约Xppm,其分量达ppb级,属超微痕量级,给富集和检测带来困难。目前,除中子活化分析外未见到其它方法测定的报导。
REE in basic and ultra basic rocks were seperated and preconcentrated by chemical pre-treatment.The samples were delivered by a desolution system,the torch was positioned horizentally and the spectra were viewed at the top of the ICP-torch.The detection limits were o.x-x ppb.RSD were 1.4-4.7%.The optimum pH value of P507 resin adsorbing the REE and the conditions of leaching them off were studied also.
作者
张立行
张成恕
Zhang Li-xiang;Zhang Chen-shu
出处
《岩矿测试》
CAS
1986年第2期113-117,共5页
Rock and Mineral Analysis