Analysis of extraterrestrial particles using monochromated electron energy-loss spectroscopy

被引:14
作者
Erni, R
Browning, ND
Dai, ZR
Bradley, JP
机构
[1] Univ Calif Berkeley, Lawrence Berkeley Lab, Natl Ctr Electron Microscopy, Berkeley, CA 94720 USA
[2] Univ Calif Davis, Dept Chem Engn & Mat Sci, Davis, CA 95616 USA
[3] Lawrence Livermore Natl Lab, Inst Geophys & Planetary Phys, Livermore, CA 94551 USA
关键词
EELS; VEELS; interplanetary dust particles; silicate; molecular oxygen; iron oxide; magnetite;
D O I
10.1016/j.micron.2004.12.011
中图分类号
TH742 [显微镜];
学科分类号
摘要
A monochromated (scanning) transmission electron microscope was used to analyze individual sub-micron grains within interplanetary dust particles (IDP). Using low-loss and core-loss electron energy-loss spectroscopy, we analyzed fluid and gas inclusions within vesiculated alumosilicate grains. It is shown that nanometer-sized vesicles contain predominantly molecular oxygen (02) beside a small fraction of H2O, Low-loss spectra reveal the Schumann-Runge continuum peaking at 8.6 eV and absorption bands reflecting vibrational excitation states of 02 molecules between the first (12.1 eV) and second (16.1 eV) ionization energy. The presence of oxygen gas is supported by the corresponding oxygen K-edge fine structure. The valence state of Fe in iron-oxide within the IDP was also studied. Low-loss spectra provide qualitative information about the oxidation state of iron consistent with the Fe2+/Fe3+ ratio quantitatively derived from the Fe L-2,L-3 edge. Published by Elsevier Ltd.
引用
收藏
页码:369 / 379
页数:11
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