Soils are large sources of atmospheric greenhouse gases, and the magnitude and composition of gas emissions are both strongly controlled by soil redox conditions. Though the effects of redox dynamics on greenhouse gas emissions have been well studied for flooded soils, oxygen can also be depleted without soil inundation. This can occur when rates of oxygen consumption exceed the rate of atmospheric replenishment. We hypothesized that greenhouse gas emissions may differ under these distinct anaerobic scenarios. We investigated the effects of soil anaerobiosis, generated with and without flooding, on greenhouse gas emissions and a range of redox-sensitive soil characteristics. We collected soil from just above the water table in a periodically flooded peatland pasture and from a clay-rich humid tropical soil in Puerto Rico that never experiences flooding. We produced anaerobic conditions with crossed treatments of flooding and nitrogen headspace, applied to homogenized soil microcosms. Gas fluxes of carbon dioxide, nitrous oxide, and methane were repeatedly measured over the course of a 2 or 3-week incubation. Soil was extracted at the end of the incubation for mineral nitrogen and iron, as indicators of soil redox, both pre-and post-treatment.
Results/Conclusions
We found that anaerobic conditions under a nitrogen headspace, with or without flooding, suppressed carbon dioxide emissions by 50%. Flooding further suppressed carbon dioxide emissions temporarily, but for most of the incubation there was no effect of flooding on soil respiration under a nitrogen headspace. Longer-term impacts of flooding on carbon dioxide emission differed by soil type as under a nitrogen headspace flooding led to greater carbon dioxide emissions than from the tropical forest. The magnitude and temporal trends in nitrous oxide emissions differed greatly across the treatments. Emissions of nitrous oxide were likely sensitive to changes in pore-space diffusivity associated with flooding in addition to the soil redox conditions. Interestingly, only the tropical soil, and not the peatland histosol, produced significant methane effluxes in the anaerobic incubation and this was significantly greater with flooding. Our results indicate that oxygen depletion suppressed carbon dioxide emissions as expected, but that flooding led to greater soil respiration relative to unflooded soils under anaerobic conditions. Flooding also stimulated methanogenesis more than oxygen depletion alone in the tropical soil. We conclude that soil biogeochemistry and greenhouse gas emissions are sensitive to the redox effects of oxygen depletion as a driver of anaerobiosis, but that flooding can have additional effects independent of oxygen depletion.