Biochar influences on soil CO(2) and CH(4) fluxes in response to wetting and drying cycles for a forest soil

Biochar has been the focus of significant research efforts in agriculture, but little research has been conducted in forested ecosystems. Here, we assess CO(2) and CH(4) fluxes from a forest soil in response to biochar additions using a before-after-control-intervention experimental design. Soil CO(2) and CH(4) fluxes were measured over a series of wetting cycles by coupling soil mesocosms equipped with auto-chambers to a laser-based spectrometer for high-frequency measurements of gas fluxes and related soil processes. We found that soil CO(2) fluxes were higher and CH(4) fluxes were less negative (e.g. reduced CH(4) uptake) for the biochar-amended soil compared to the no biochar condition. Furthermore, biochar improved soil infiltrability under wet conditions, and enhanced soil moisture levels under dry conditions. Biochar additions shifted the point of maximum soil respiration (i.e. soil CO(2) efflux) to a slightly wetter soil moisture level. The point of maximum CH(4) uptake was also shifted to a slightly wetter moisture level for soil with biochar. Overall differences in soil gas fluxes were found to be minor compared to the increase in soil carbon resulting from the biochar addition. Biochar may thus contribute to improved forest management through increases to soil carbon stocks and improved soil moisture levels.