JpGU-AGU Joint Meeting 2020

Presentation information

[E] Poster

S (Solid Earth Sciences ) » S-GC Geochemistry

[S-GC48] Volatiles in the Earth - from Surface to Deep Mantle

convener:Takeshi Hanyu(Japan Agency for Marine-Earth Science and Technology, Research Institute for Marine Geodynamics), Gray E Bebout(Lehigh University), Hirochika Sumino(Department of Basic Science, Graduate School of Arts and Sciences, The University of Tokyo), Yuji Sano(Division of Ocean and Earth Systems, Atmosphere and Ocean Research Institute, University of Tokyo)

[SGC48-P07] SIMS sensitivity factors of 2H and 16O2H relative to 18O in spinel-structured oxides

*Georg F Zellmer1, Naoya Sakamoto2, Minami Kuroda3, Isao Sakaguchi4, Hisayoshi Yurimoto2,5 (1.Massey University, 2.Hokkaido University, 3.AIST, 4.National Institute of Material Sciences, 5.Japan Aerospace Exploration Agency)

Keywords:spinel-structured oxides, relative sensitivity factors, secondary ion mass spectrometry, hydrogen analysis, nominally anhydrous minerals

Spinel-structured oxides ("spinels") are a group of nominally anhydrous minerals characterized by a wide range of solid solution. To allow the analysis of hydrogen in spinels by ion microprobe, Relative Sensitivity Factors (RSFs), which are typically matrix-dependent, need to be determined. For this work, we have selected five natural spinels from the Mg-Al-Fe-Ti-Cr-Mn-Zn compositional space. We present an approach to estimate spinel density on basis of bulk chemical composition determined by electron microprobe. Densities in our samples range from 3.7 to 5.1 g cm-3. Samples were implanted with a fixed dose of deuterium (1 x 1015 atoms cm-2) using an ion energy of 40 keV. Subsequently, we performed depth profiling using a Cs+ primary beam on the Cameca ims-1270 ion microprobe at Hokkaido University, monitoring secondary ion counts of 2H and 18O, and at high mass-resolution 16O2H, 17O1H, and 18O, until the implanted ion counts dropped below background levels. From the reduced data, we calculated the RSFs for secondary ions of atomic 2H and molecular 16O2H relative to 18O as matrix element. RSFs for 2H are similar for all spinels at 1.11 ±0.32 (2σ) x 1022 atoms cm-3, indicating a small matrix effect for 2H despite the large compositional range of spinels studied. In contrast, RSFs for 16O2H relative to 18O decrease with spinel density from 2.65 ±0.36 (2σ) x 1021 atoms cm-3 at 3.7 g cm-3 to 3.41 ±0.73 (2σ) x 1020 atoms cm-3 at > 4.5 g cm-3, indicating a strong matrix effect on secondary dimer production during processes of ion sputtering and secondary ionization. Our data imply that the analysis of water in natural spinels may be undertaken through measurement of H or OH, but that spinel densities must be well-determined in the case of OH measurement. Mineral density effects on RSF values will have to be evaluated prior to analysis of water in other nominally anhydrous solid solution minerals.