Transient signal isotope analysis using multicollection of ion beams with Faraday cups equipped with 10~(12) Ω and 10~(11) Ω feedback resistors

摘要

To improve the precision of isotope analyses of low ion intensities using the Faraday detection system, amplifiers equipped with 10~(12) Ω resistors (hereafter 10~(12) Ω amplifiers) have been developed. While the behavior of these amplifiers for steady signals has been well investigated, there is no ample evidence regarding the use of 10~(12) Ω amplifiers for transient signal acquisition. In this work, we investigated the simultaneous use of amplifiers equipped with 10~(12) Ω and 10~(11) Ω resistors for transient signal acquisition. Using the equation describing the relationship between the input ion current and the output voltage in the amplifiers, we showed how the transient signal duration influences the accuracy of the isotope ratio measurements. In particular, lead transient signals were investigated using a Neptune Plus MC-ICPMS and ~(204)Pb and ~(206)Pb isotopes were measured using 10~(12) Ω and 10~(11) Ω amplifiers, respectively. The ~(204)Pb/~(206)Pb isotope ratio showed an important drift due to a large time lag between 10~(12) Ω and 10~(11) Ω amplifiers. The time lag was quantified (0.175(3) s) and the isotopic drift was corrected using a method of internal signal synchronization. The ~(204)Pb/~(206)Pb drift corrected data obtained from the 10~(12)-10~(11) Ω amplifier configuration were compared to the data obtained from 10~(11) - 10~(11) Ω amplifiers. Our results point out that for low transient signal intensities (＜10~(13) A), the use of 10~(12) - 10~(11) Ω amplifiers is more beneficial in terms of isotope ratio uncertainty, repeatability and trueness, compared to the 10~(11) - 10~(11) Ω amplifier configuration.