For the measurement of 143 Nd/ 144 Nd ratios, Nd must be separated from the major matrix and isobaric interfering elements before mass spectrometry measurements are performed. We report an improved technique for the separation of Nd from the other rare earth elements (REE), in particular Ce and Sm, in geological samples. This method uses Ln resin chromatography, combining oxidative and conventional "Ln-resin" procedures in order to remove Ce and Sm, respectively, from the Nd fraction. Repeated analyses of 143 Nd/ 144 Nd in standard JNdi-1 prepared using the newly developed technique are in good agreement with the values measured by direct analysis. The procedural Nd blanks are extremely small. The recovery yield of Nd after the entire separation process was always better than 90%, which is better than the recovery realized in previous studies owing to the collection of wider Nd elution points by the effective removal of neighbour elution elements (Ce and Sm). The Ln resin column (e.g., Peppard et al., 1957;Rehkämper et al., 1996).This method can also be used to purify Ce for Ce isotope ratio measurement (Tazoe et al., 2007). However, further purification of Ce is necessary before the Ce isotope ratio measurements can be conducted; this will be described in a separate paper. Tazoe et al. (2007) Nd ratios were measured in four igneous rock standards (JB-1a, JB-2, JA-1, and JR-1) provided by the Geological Survey of Japan (GSJ). These standards cover the range of major element compositions found in naturally occurring igneous rocks.They comprise an alkali basalt from Myojin-toge, NagasakiPrefecture (JB-1a), an oceanic island arc basalt from Izu Oshima volcano, Tokyo Metropolis (JB-2), an andesite from Hakone volcano, Kanagawa Prefecture (JA-1), and a rhyolite (obsidian)from Wada-toge, Nagano Prefecture (JR-1).Samples were prepared and analysed at the Institute for was weighed into a 7-ml Teflon perfluoroalkoxy (PFA) screw-cap vial (Savillex Co. Laboratory Products). A 1:1 mixture of 20 M HF and 11.6 M HClO 4 (2 ml) was added to the sample, and the mixture was heated at 100 ど overnight in a closed vial. The dissolved sample was subsequently dried and re-dissolved in a 1:1 binary solution of 6 M HCl and 11.6 M HClO 4 (2 ml), and then heated at 100 ど overnight in a closed vial. The re-decomposed sample was again evaporated to dryness. The dried sample was dissolved in 1 ml of 6 M HCl, and then heated overnight on a hotplate at 100 ど in a closed vial. Subsequently, the dissolved sample was dried, and finally dissolved in 1 ml of 2.5 M HCl. Although the analysed standards do not contain un-dissolved minerals such as garnet and zircon for the acid digestion, they do not need to be transferred to bombs (Krogh, 1969). Nd was separated from the other elements using ion-exchange column chemistry, as described in Section 3 ( Figure 3).
Mass spectrometryPrior to mass spectrometry, Nd fraction was evaporated to dryness.
Column preparation and chemical purificationThe column designs for each of the separation pr...