文摘
Silicon isotope ratios in natural waters and several commercial Si standards were determined by online ion exclusion chromatography (IEC) multicollector inductively couple plasma mass spectrometry (MC-ICPMS). As recent studies have shown that mass-independent fractionation (MIF) also exists in MC-ICPMS, e.g., Nd, Ce, W, Sr, Hf, Ge, Hg, and Pb isotopes, the nature of mass bias for Si isotopes was thus investigated. MIF was observed for Si isotopes on both Neptune and Neptune plus MC-ICPMS instruments in this study. Therefore, a standard-sample bracketing (SSB) mass bias correction model, capable of correcting both mass-dependent and mass-independent bias, was employed to obtain accurate Si isotope ratio results in all samples by using NBS28 Si standard as the bracketing standard. Medium resolution was used for all measurements in order to resolve polyatomic interferences on Si isotopes. NBS28 Si standard solutions prepared in nutrient-free seawater and 0.1% NaOH matrix, respectively, were used for the method validation and subjected to the online IEC MC-ICPMS determination of Si isotope ratios. Values of 鈭?.01 卤 0.06 and 0.00 卤 0.06 鈥?(1 SD, n = 10) and 鈭?.01 卤 0.03 and 0.01 卤 0.06 鈥?(1 SD, n = 10) for 未29/28Si and 未30/28Si, respectively, were obtained, confirming accurate results can be obtained using the reported method for natural waters. Significant variations in Si isotope ratios from 鈭?.72 卤 0.09 to 鈭?.24 卤 0.03 鈥?(1 SD, n = 10) and 鈭?.36 卤 0.11 to 鈭?.46 卤 0.04 鈥?(1 SD, n = 10) for 未29/28Si and 未30/28Si, respectively, were found among commercial Si standards of NIST SRM3150, SCP Si, and Sigma-Aldrich Si. Values of 鈭?.06 卤 0.07 and 鈭?.20 卤 0.11 鈥?(1 SD, n = 10) for 未29/28Si and 未30/28Si, respectively, were obtained for the MOOS-3 seawater whereas 0.59 卤 0.11 and 1.19 卤 0.15 鈥?(1SD, n = 10) for 未29/28Si and 未30/28Si, respectively, were obtained for the SLRS-5 river water. To the best of our knowledge this is the first report of an application of online IEC MC-ICPMS for the high accuracy and precision determination of Si isotope ratios in natural waters. The reported method provides for a relatively rapid (10 min per run) and simple online technique that requires no sample pretreatment for the Si isotope ratio measurements.
