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a Department for Production Ecology, Faculty of Forestry, P.O. Box 7042, Swedish University of Agricultural Sciences, 750 07, Uppsala, Sweden
b Department of Physical Geography and Ecosystems Analysis, P.O. Box 118, Lund University, 221 00, Lund, Sweden
* Corresponding author (Anders.Lindroth{at}nateko.lu.se)
Comparisons have revealed large discrepancies among the many methods for measuring soil CO2 efflux indicating the need for an absolute calibration of methods. This study presents a calibration system, constructed to imitate an area of soil, and its application to two different chamber systems for the measurement of soil CO2 efflux: one open and one closed dynamic. Air rich in CO2 was allowed to diffuse through a layer of sand on top of a box of known volume. By measuring the decrease in CO2 concentration inside the box, the exact CO2 efflux could be calculated. The CO2efflux rates measured by the chambers could then be compared with the efflux rates calculated from the box. The error of the closed-chamber system ranged from an underestimate of 19% to an overestimate of 21%. The errors were most likely caused by a combination of underestimated chamber volume, causing an underestimation of CO2 efflux, and turbulence within the chamber, which increased the flux by disturbing the boundary layer above the surface. The open-chamber system always overestimated the CO2 efflux. Disturbing the boundary layer alone was believed to cause a 17% increase in efflux. Increasing negative pressure difference caused a mass flow of CO2rich air into the chamber. At a pressure difference of -0.15 Pa, the error was 11 to 40%, depending on air-filled soil volume. Accordingly, soil-water content, a parameter to which soil CO2 efflux is often related, was found to substantially affect the measurements made by both tested systems. These results point to the need of calibrating systems used for measuring soil CO2 efflux is measured against a known flux, to elucidate the limits and applicability of each system.
Abbreviations: DP34, dry sand of 34% porosity DP60, dry sand of 60% porosity IRGA, infrared-gas analyzer Fb, CO2 flux from the calibration box with a chamber on top Fbr, CO2 flux from the calibration box with no chamber on topreference flux Fb-Co, CO2 flux from the calibration box outside the chamber FCc, CO2 efflux measured by a closed-dynamic chamber system FCo, CO2 efflux measured by an open chamber system LOI, loss on ignition WP34, wet sand of 34% porosity
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