一个方法为 Na 的内容决心被开发， Mg ，艾尔， Si ， P ， S ， Cl ， K ， Ca ， Ti ， V ， Cr ， Mn ， Fe ， Ni ， Cu ， Zn ， Ga ， Nb ， Zr ， Y ， Sr ， Rb ， Ba ，在使用的海洋的沉积样品盖住 26 专业，未成年者，和踪迹元素的 La 和 Ce 等等由X光检查荧光 spectrometry 熔化了玻璃圆盘。刻度用海洋的沉积被成为证明引用材料和样品由在不同比例与流沉积和碳酸盐标准样品混合几海洋的沉积准备了的合成标准。矩阵效果用理论高山被改正哈象内部标准的系数，经验系数和散布放射(为踪迹元素) 。方法的精确性被证明参考材料 GBW07314， GBW07334 和 GSMS6 的分析评估。结果在与 RSD 的对标准的证明价值的好同意不到 2.60% 除了 Y，有 RSD 的 Cr， Ga， Ce， La， Nb， Rb，和 V 不到 9.0%(n=12 ) 。
A series of selective extraction experiments were conducted on marine hydrogenic ferromanganese crusts from the seamount near the Line Island to investigate the distribution of rare earth elements(REEs) and the mechanisms of combination between REEs and the hydrogenic ferromanganese crusts.The enrichment of REEs in hydrogenic ferromanganese crusts is attributed mainly to the mineral or oxide/hydroxide of the crust rather than the growth environment.The REEs are present mainly in amorphous ferric oxide/hydroxide rather than in δ-MnO2.Amorphous ferric oxide/hydroxide preferentially combines free REE3+,while δ-MnO2 combines the REE-carbonate complexes in modern seawater.The REEs in seawater are combined more strongly with amorphous ferric oxide/hydroxides than with δ-MnO2.The positive Ce anomaly in hydrogenic ferromanganese crusts results from the oxidation of soluble Ce3+ to insoluble Ce4+ by the actively soluble oxygen of the bottom current rather than by the oxidation of δ-MnO2.
JIANG XueJun1,2,LIN XueHui1,2,YAO De3,4 & GUO WeiDong5 1 Key Laboratory of Marine Oil and Gas Resources and Marine Environment,Ministry of Land and Resources,Qingdao 266071,China
