ND70 Series Basaltic Glass Reference Materials for Volatile Element (H2O, CO2, S, Cl, F) Measurement and the C Ionisation Efficiency Suppression Effect of Water in Silicate Glasses in SIMS

Author:

Moussallam Yves1ORCID,Towbin William Henry2ORCID,Plank Terry1,Bureau Hélène3,Khodja Hicham4,Guan Yunbin5,Ma Chi5,Baker Michael B.5,Stolper Edward M.5,Naab Fabian U.6,Monteleone Brian D.7,Gaetani Glenn A.7,Shimizu Kenji8,Ushikubo Takayuki8,Lee Hyun Joo1,Ding Shuo1,Shi Sarah1ORCID,Rose‐Koga Estelle F.9

Affiliation:

1. Lamont‐Doherty Earth Observatory Columbia University New York USA

2. Gemological Institute of America 50 W. 47th Street New York NY 10036 United States of America

3. IMPMC, Sorbonne Université, CNRS UMR 7590, MNHN, IRD UR 206 4 place Jussieu 75252 Paris Cedex 05 France

4. LEEL, NIMBE, CEA, CNRS, Université Paris−Saclay, CEA Saclay 91191 Gif sur Yvette Cedex France

5. Division of Geological and Planetary Sciences California Institute of Technology Pasadena California 91125 USA

6. Department of Nuclear Engineering and Radiological Sciences University of Michigan Ann Arbor Michigan 48109 USA

7. Department of Geology and Geophysics Woods Hole Oceanographic Institution Woods Hole MA 02543 USA

8. Kochi Institute for Core Sample Research, X‐star Japan Agency for Marine‐Earth Science and Technology Monobe‐otsu 200 Nankoku Kochi 783‐8502 Japan

9. ISTO, UMR 7327, CNRS‐UO‐BRGM 1A rue de la Férollerie 45071 Orléans cedex 2 France

Abstract

We present a new set of reference materials, the ND70‐series, for in situ measurement of volatile elements (H2O, CO2, S, Cl, F) in silicate glass of basaltic composition. The materials were synthesised in piston cylinders at pressures of 1 to 1.5 GPa under volatile‐undersaturated conditions. They span mass fractions from 0 to 6% m/m H2O, from 0 to 1.6% m/m CO2 and from 0 to 1% m/m S, Cl and F. The materials were characterised by elastic recoil detection analysis for H2O, by nuclear reaction analysis for CO2, by elemental analyser for CO2, by Fourier transform infrared spectroscopy for H2O and CO2, by secondary ion mass spectrometry for H2O, CO2, S, Cl and F, and by electron probe microanalysis for CO2, S, Cl and major elements. Comparison between expected and measured volatile amounts across techniques and institutions is excellent. It was found however that SIMS measurements of CO2 mass fractions using either Cs+ or O primary beams are strongly affected by the glass H2O content. Reference materials have been made available to users at ion probe facilities in the US, Europe and Japan. Remaining reference materials are preserved at the Smithsonian National Museum of Natural History where they are freely available on loan to any researcher.

Publisher

Wiley

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