6533b86efe1ef96bd12cc0af
RESEARCH PRODUCT
δ30Si and δ29Si Determinations on USGS BHVO-1 and BHVO-2 Reference Materials with a New Configuration on a Nu Plasma Multi-Collector ICP-MS
Sophie OpfergeltKathrin AbrahamStephen F. FoleyDamien CardinalFrançois FripiatLuc AndréJeroen De JongA. J. Cavagnasubject
DeltaAnalytical chemistryMineralogyGeologyPlasmaOcean island basaltMedium resolutionGeochemistry and PetrologyChondriteIsotopes of siliconMC-ICP-MSQuartzInductively coupled plasma mass spectrometryGeologydescription
We report silicon isotopic determinations for USGS rock reference materials BHVO-1 and BHVO-2 using a Nu Plasma multi-collector (MC)-ICP-MS, upgraded with a new adjustable entrance slit, to obtain medium resolution, as well as a stronger primary pump and newly designed sampler and skimmer cones ("B" cones). These settings, combined with the use of collector slits, allowed a resolution to be reached that was sufficient to overcome the (NO)-N-14-O-16 and N-14(2) interferences overlying the Si-30 and the Si-28 peaks, respectively, in an earlier set-up. This enabled accurate measurement of both delta Si-30 and delta Si-29. The delta value is expressed in per mil variation relative to the NBS 28 quartz reference material. Based on data acquired from numerous sessions spread over a period of six months, we propose a recommended average delta Si-30 of -0.33 +/- 0.05 parts per thousand and -0.29 +/- 0.11 parts per thousand (2se) for BHVO-1 and BHVO-2, respectively. Our BHVO grand mean silicon isotope composition (delta Si-30 = -0.31 +/- 0.06 parts per thousand) is significantly more negative than the only published value for BHVO-2, but is in very good agreement with the recently established average value of ocean island basalts (OIB), confirming the conclusion that the OIB reservoir has a distinct isotopic composition from the solar reservoir as sampled by chondrites.
year | journal | country | edition | language |
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2008-06-01 |