| Reference Type | Journal (article/letter/editorial) |
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| Title | Quantitative determination of water in granites by infra-red analysis |
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| Journal | Mineralogical Magazine |
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| Authors | Aucott, J. W. | Author |
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| Marshall, M. | Author |
| Year | 1969 (June) | Volume | 37 |
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| Issue | 286 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-286-256.pdf+ |
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| DOI | doi:10.1180/minmag.1969.037.286.16Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6265 | Long-form Identifier | mindat:1:5:6265:1 |
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| GUID | 0 |
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| Full Reference | Aucott, J. W., Marshall, M. (1969) Quantitative determination of water in granites by infra-red analysis. Mineralogical Magazine, 37 (286) 256-261 doi:10.1180/minmag.1969.037.286.16 |
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| Plain Text | Aucott, J. W., Marshall, M. (1969) Quantitative determination of water in granites by infra-red analysis. Mineralogical Magazine, 37 (286) 256-261 doi:10.1180/minmag.1969.037.286.16 |
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| In | (1969, June) Mineralogical Magazine Vol. 37 (286) Mineralogical Society |
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| Abstract/Notes | SummaryTwo methods using nujol and hexachloro-butadiene mulls are described to analyse the water content of powdered granite samples. The nujol mull analyses were carried out on a Unicam SP 100 spectrometer using the silica content of the rock as an internal standard. The hexachlorobutadiene mull analyses were done by a twin-path Unicam SP 200 spectrometer, using hexachlorobutadiene as the internal standard. The broader and more pronounced V1 vibrational mode (3450 cm−1) is ratioed to a standard of known composition. Comparisons are also made between absorption due to free water (V1 = 3450 cm−1) and combined water (V3 = 3680 cm−1) in aplites, biotite granite, and chlorite schists. |
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