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Department of Chemistry, Technical University of Denmark, Kemitorvet, DK-2800, Kgs. Lyngby

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Methane concentration in soil gas is measured by gas-chromatography in various depths. The isotopic composition (d(13C)) is determined by isotope ratio mass spectrometry. The results are analyzed in a model describing the soil as a methane sink with a narrow layer of methane producing material.
StatusCompleted
Period01/01/9801/01/99
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ID: 2273011