TIME-INTEGRATED COLLECTION OF CO2 FOR 14C ANALYSIS FROM SOILS

• Published in: Radiocarbon
• Main Authors: Pedron, Shawn, Xu, X, Walker, JC, Ferguson, JC, Jespersen, RG, Welker, JM, Klein, ES, Czimczik, CI
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2021
• Subjects: carbon; mineral soil; molecular sieve; soil respiration; Geochemistry; Physical Geography and Environmental Geoscience; Archaeology; Paleontology; Arctic; Tundra
• Online Access: https://escholarship.org/uc/item/11x2t2tt; https://escholarship.org/content/qt11x2t2tt/qt11x2t2tt.pdf; https://doi.org/10.1017/rdc.2021.42

We developed a passive sampler for time-integrated collection and radiocarbon (14C) analysis of soil respiration, a major flux in the global C cycle. It consists of a permanent access well that controls the CO2 uptake rate and an exchangeable molecular sieve CO2 trap. We tested how access well dimensions and environmental conditions affect collected CO2, and optimized cleaning procedures to minimize 14CO2 memory. We also deployed two generations of the sampler in Arctic tundra for up to two years, collecting CO2 over periods of 3 days-2 months, while monitoring soil temperature, volumetric water content, and CO2 concentration. The sampler collects CO2 at a rate proportional to the length of a silicone tubing inlet (7-26 g CO2-C day-1·m Si-1). With constant sampler dimensions in the field, CO2 recovery is best explained by soil temperature. We retrieved 0.1-5.3 mg C from the 1st and 0.6-13 mg C from the 2nd generation samplers, equivalent to uptake rates of 2-215 (n=17) and 10-247 g CO2-C day-1 (n=20), respectively. The method blank is 8 ± 6 g C (mean ± sd, n=8), with a radiocarbon content (fraction modern) ranging from 0.5875-0.6013 (n=2). The sampler enables more continuous investigations of soil C emission sources and is suitable for Arctic environments.