4.4 Article

Collection and storage of CO2 for C-13 analysis: an application to separate soil CO2 efflux into root- and soil-derived components

Journal

RAPID COMMUNICATIONS IN MASS SPECTROMETRY
Volume 20, Issue 22, Pages 3379-3384

Publisher

JOHN WILEY & SONS LTD
DOI: 10.1002/rcm.2749

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Soil surface CO2 efflux is comprised of CO2 from (i) root respiration and rhizosphere microbes and GO heterotrophic respiration from the breakdown of soil organic matter (SOM). This efflux may be partitioned between these sources using delta C-13 Measurements. To achieve this, continuous flow isotope ratio mass spectrometry can be used and, in conjunction with 10 mL septum-capped vials, large numbers of samples may be analysed using a Finnigan MAT Delta(plus)XP interfaced to a Gas Bench II. Here we describe a number of advances to facilitate such work, including: W a technique for monitoring mass spectrometer performance, (ii) improvements to sample storage, and (iii) a gas-handling system for incubating and sampling the CO2 derived from roots and soils. Mass spectrometer performance was monitored using an automated refillable vial. Compressed air analysed with this system had mean delta C-13 of -9.61 +/- 0.16% (+/- 1 sigma, n = 28) collected over four runs. Heating the butyl rubber septa used to seal the vials at 105 degrees C for 12 h improved the sample storage. After air transportation over 12 days, the isotope composition of the CO2 at ambient concentrations was unchanged (before: -35.2 +/- 0.10%, n = 4; after: -35.3 +/- 0.10%, n = 15); without heat treatment of the septa the CO2 became slightly enriched (-35.0 +/- 0.14%, n = 15). The linearity of the Gas Bench II was found to decline above 8000 mu mol CO2 mol(-1). To stay within a linear range and to allow the incubation of soil and root material we describe a gas-handling system based around a peristaltic pump. Finally, we demonstrate these methods by growing a C-4 grass (Guinea grass, Panicum maximum Jacq.) in a C-3 soil. Root respiration was found to contribute between 5 and 22% to the soil surface CO2 efflux. These methodologies will facilitate experiments aimed at measuring the isotopic composition of soil-derived CO2 across a range of ecological applications. Copyright (c) 2006 John Wiley & Sons, Ltd.

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