A model of the production and transport of CO 2 in soil: predicting soil CO 2 concentrations and CO 2 efflux from a forest floor

Abstract

A process-based model of the transport of heat and water in the soil and surface energy balance components is extended to include production of CO 2 from heterotrophic (microbial decomposition) and autotrophic (root) respiration, and transport of the resulting CO 2 in both the gaseous and liquid phases. The production of CO 2 is determined by the amount and type as well as distribution in the soil profile of organic matter and roots, and their respective first-order rate constants. Influences of soil water and temperature are considered through their effects on respiration, CO 2 diffusivities and chemical equilibria among various C species in the soil–solution–air continuum. Also included is CO 2 uptake by plant roots associated with root water uptake. Model calculations, using independently determined parameters, are compared with measurements of soil CO 2 concentrations and chamber-measured forest floor fluxes in a second-growth 54-year-old Douglas-fir forest located on the east coast of Vancouver Island, Canada. Measured and modeled forest floor CO 2 effluxes and soil CO 2 concentration profiles, as well as soil water contents and temperatures showed good agreement. The efflux was most sensitive to soil temperature, and the influence of soil water content was relatively small. In this rapidly draining soil, the CO 2 efflux, at time scales as small as half-hour, was very well approximated by the total production of CO 2 in the soil profile, even during and after rainfall, which significantly increases soil water content. This is because CO 2 diffusion in this forest soil is relatively rapid compared to changes in the rates of CO 2 production. In this podzolic soil ecosystem with low soil pH, liquid-phase diffusion appears to play a minor role in CO 2 transport. High soil CO 2 concentrations, up to 10,000 μmol mol −1 in summer and 6000 μmol mol −1 in winter, and a positive downward gradient at the 1 m depth indicate some CO 2 sources associated with very low CO 2 diffusivity at deeper depths.