> A procedure is described for the determination of thirty‐seven minor and trace elements'/> Determination of Trace Element Mass Fractions in Ultramafic Rocks by <fc xmlns='http://www.wiley.com/namespaces/wiley'>HR</fc>HR ‐ <fc xmlns='http://www.wiley.com/namespaces/wiley'>ICP</fc>ICP ‐ <fc xmlns='http://www.wiley.com/namespaces/wiley'>MS</fc>MS : A Combined Approach Using a Direct Digestion/Dilution Method and Preconcentration by Coprecipitation
首页> 外文期刊>Geostandards and geoanalytical research >Determination of Trace Element Mass Fractions in Ultramafic Rocks by HRHR ‐ ICPICP ‐ MSMS : A Combined Approach Using a Direct Digestion/Dilution Method and Preconcentration by Coprecipitation
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Determination of Trace Element Mass Fractions in Ultramafic Rocks by HRHR ‐ ICPICP ‐ MSMS : A Combined Approach Using a Direct Digestion/Dilution Method and Preconcentration by Coprecipitation

机译: hr ht - ICP ICP - ms ms:使用直接消化/稀释的组合方法 CopRecipitation的方法和预征

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> A procedure is described for the determination of thirty‐seven minor and trace elements ( LILE , REE , HFSE , U, Th, Pb, transition elements and Ga) in ultramafic rocks. After Tm addition and acid sample digestion, compositions were determined both following a direct digestion/dilution method (without element separation) and after a preconcentration procedure using a double coprecipitation process. Four ultramafic reference materials were investigated to test and validate our procedure ( UB ‐N, MGLGAS [Geo PT 12], JP ‐1 and DTS ‐2B). Results obtained following the preconcentration procedure are in good agreement with previously published work on REE , HFSE , U, Th, Pb and some of the transition elements (Sc, Ti, V). This procedure has two major advantages: (a) it avoids any matrix effect resulting from the high Mg content of peridotite, and (b) it allows the preconcentration of a larger trace element set than with previous methods. Other elements ( LILE , other transition elements Cr, Mn, Co, Ni, Cu, Zn, as well as Ga) were not fully coprecipitated with the preconcentration method and could only be accurately determined through the direct digestion/dilution method.
机译: >一个过程用于确定三十七个次要和跟踪元素( Lile REE HFSE ,U,TH,PB,转换元件和GA)在超空地岩石中。在加法和酸样品消化后,通过使用双共沉淀方法进行直接消化/稀释方法(无元素分离)和在预浓缩过程之后确定组合物。研究了四种超空地参考材料以测试和验证我们的程序( UB -N, MGL - 气体 [Geo Pt 12], JP -1和 DTS -2B)。预浓缩过程中获得的结果与先前公布的 REE HFSE ,U,TH,PB和一些过渡元素(SC,TI,V. )。该程序具有两个主要优点:(a)它避免了由恒星岩的高mg含量产生的任何基质效应,并且(b)它允许较大的痕量元素集的前浓度而不是先前的方法。其他元素(乳绒>,其他过渡元件Cr,Mn,Co,Ni,Cu,Zn以及Ga)没有用前浓缩方法完全共沉淀,只能通过直接消化准确地确定/稀释法。

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