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Determination of rhizosphere 13 C pulse signals in soil thin sections by laser ablation isotope ratio mass spectrometry
Author(s) -
Bruneau Patricia M.C.,
Ostle Nick,
Davidson Donald A.,
Grieve Ian C.,
Fallick Anthony E.
Publication year - 2002
Publication title -
rapid communications in mass spectrometry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.528
H-Index - 136
eISSN - 1097-0231
pISSN - 0951-4198
DOI - 10.1002/rcm.740
Subject(s) - rhizosphere , chemistry , soil test , mass spectrometry , isotope ratio mass spectrometry , isotopes of carbon , thin section , pulse (music) , soil carbon , tracer , soil science , environmental chemistry , analytical chemistry (journal) , soil water , environmental science , mineralogy , total organic carbon , geology , bacteria , paleontology , physics , engineering , chromatography , detector , electrical engineering , nuclear physics
In grassland ecosystems, soil animals act as key soil engineers and architects. The diversity of soil animals is also a regulator of ecosystem carbon flow. However, our understanding of the link between soil animals, carbon fluxes and soil physical organisation remains poor. An integrated approach based on soil micromorphology and laser ablation stable isotope ratio mass spectrometry (LA‐IRMS) was developed to provide spatially distributed data of pulse‐derived 13 C tracer from roots in the soil environment. This paper describes the development and testing of a LA‐IRMS 13 C/ 12 C analytical method on soil thin sections as a means to determine the fate of root carbon derived from photosynthesis into soil. Results from this work demonstrated (1) that micro‐scale δ 13 C (‰) analysis could be made on targeted features located within a soil thin section and (2) that LA‐IRMS δ 13 C (‰) measurements made on samples obtained from 13 CO 2 pulse labelled plant‐soil blocks confirmed the presence of recent photosynthates in the rhizosphere (1 and 4 weeks post‐pulse). Copyright © 2002 John Wiley & Sons, Ltd.