“…However, in the routine analysis of natural samples, the Pb isotope ratios to be measured are different one by one, and inevitably the Pb isotope composition of the remaining Pb signal memory after 5 minute washout should vary significantly. If an analyzed sample has an extreme Pb isotopic composition, the memory may affect the measured value of the next sample like the case of zinc in double-spike analysis (Tanimizu et al, 2002), although we had shown that the level of the Pb memory is less than 0.01% of the sample signal in usual analysis (Fig. 1) Zindler and Hart, 1986).…”