| Stable Isotope Facility Bayreuth | Established: 04.12.01
Last update: 04.12.01 |
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Dr. Bruno Glaser
PD Dr. Georg Guggenberger
Dr. Wulf Amelung
Prof. Dr. Wolfgang Zech (project coordinator) Jochen Schmitt
Tanja Gonter
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| Determination
of compound specific isotope ratios in humic substances
Bruno Glaser, Wulf Amelung, Georg Guggenberger und Wolfgang Zech Lehrstuhl Bodenkunde, Universität Bayreuth, D-95440 Bayreuth. Email: bruno.glaser@uni-bayreuth.de Rationale The motivation for the determination of compound specific isotope ratios in humic substances is based on the fact that in soils and their chemical and physical fractions many different organic substrates for microbes exist. The analysis of stable carbon isotopes (12C, 13C) of such bulk samples results in a mean isotopic signal (d13C) which does not allow a differentiation between labile and stable carbon in organic compounds. To differentiate between differently available C-sources or to recognize specific pathways for the heterotrophic use of these sources, the compound specific analysis of the d13C-signal by means of gas chromatography - combustion - isotope ratio mass spectrometry (GC-C-IRMS) is necessary. Our approach is based on the analysis of the d13C-singal of biomarkers such as lignin phenols, amino acids, amino sugars and benzenecarboxylic acids in soil samples and their physical fractions. In the past two years we adapted methods developed at our institute for the quantification of the above mentioned biomarkers for the analysis of compound specific isotope ratios by means of GC-C-IRMS and identified and eliminated method induced isotope discriminations. |
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| Picture gallery | |
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The Isotope Ratio Mass Spectrometer (in our case a Thermo Finnigan Delta plus) is the heart of stable isotope ratio mass spectrometers. It serves as a simultaneaous detector for various species of stable isotopes (e.g. masses 44, 45 and 46 for CO2). |
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Molecules of interest can
be separated by gas chromatography and subsequently oxidized quantitatively
to CO2 via a combustion interface before entering the IRMS.
Peak identity can be checked by splitting the GC-effluent and a part entering an Ion-Trap MS. |
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The stable isotope composition of bulk samples or physical soil fractions can be determinedd by connecting an elemental analyser (Thermo Finnigan NA 2500) with the IRMS |
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