Infrared spectroscopy of hydrous glasses of arc magma compositions.
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- Yamashita Shigeru
- Institute for Study of the Earth's Interior, Okayama University
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- Kitamura Toshihiro
- Institute for Study of the Earth's Interior, Okayama University
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- Kusakabe Minoru
- Institute for Study of the Earth's Interior, Okayama University
Bibliographic Information
- Other Title
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- Infrared spectroscopy of hydrous glasse
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Abstract
Molar absorption coefficients of water in glasses of arc magma compositions have been determined for ∼2.8 μm, ∼2.2 μm, and ∼1.9 μm bands. Excellent agreement was found between the water contents calculated from the absorption peak heights and those determined by H2 manometry when the following molar absorption coefficients (m3/mol m) are used for different glass compositions: ε2.8μm=6.4±0.1, ε2.2μm=0.085±0.007, and ε1.9μm=0.084±0.006 for tholeiite and high-Al basalt glasses; ε2.8μm=6.8±0.1, ε2.2μm=0.094±0.006, and ε1.9μm=0.16±0.03 for dacite glass. With IR spectroscopy using these coefficients, water concentrations up to ∼3 wt.% in the arc basalt and dacite glasses can be determined accurately.
Journal
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- GEOCHEMICAL JOURNAL
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GEOCHEMICAL JOURNAL 31 (3), 169-174, 1997
GEOCHEMICAL SOCIETY OF JAPAN
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Details 詳細情報について
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- CRID
- 1390001204550642560
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- NII Article ID
- 130003904579
- 10008801613
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- NII Book ID
- AA00654975
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- COI
- 1:CAS:528:DyaK2sXjvV2ksL0%3D
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- ISSN
- 18805973
- 00167002
- http://id.crossref.org/issn/00167002
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- NDL BIB ID
- 4231176
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed