Abstract. Through model experiments we quantitatively examined fractional methane oxidation and net methane emissions using three model systems which encompass a management gradient from pristine (wetlands) to managed (rice production) to highly engineered (landfills). Fractional methane oxidation is rarely determined in situ; thus our goal was to cross-compare modeling results and major drivers to field and laboratory data for this important parameter in both pristine and managed systems. In the models, management factors are typically introduced as combinations of theoretical relationships, empirical functions, or scaling factors which drive net emissions through forcing of water table variations, availability of degradable organic carbon substrates, input and cycling of major nutrients, variability in plant communities, physical properties for gaseous transport, and indigenous capaci .ty of soils for methane oxidation. The net methane emission and fractional oxidation vary by orders of magnitude within and among the three model systems, yet each model was quite consistent in its predictive ability. This study lays the groundwork for a more unified, modular approach to modeling methane emissions from soil sources where both natural (climatic and ecological) and anthropogenic factors are important drivers.
BackgroundMethane is a radiatively important trace gas whose current atmospheric mixing ratio is 1.8 ppmv,--2.5 times greater than it is important to establish which factors control changes in emissions for specific sources. This can best be done through the application of models which have been validated at appropriate scales for discrete sets of field observations. For all methanogenic-methanotrophic systems, models rely on a mass balance to describe net methane emissions to the atmosphere as a function of (1) methane production rates, (2) methane transport rates through soil, water (ebullition), and plant systems, and (3) processes which reduce the bulk methane available for transport (methanotrophic oxidation and landfill methane recovery). Of particular importance is the role of methanotrophic methane oxidation, which is capable of reducing net emissions to the atmosphere in all terrestrial settings. it is thus necessary to model the opposing rates of methanogenesis and methanotrophy, linked through soil transport processes, to determine the net methane emission to the atmosphere ( Figure 1). In extreme circumstances, methane oxidation capacities in soils can exceed the rate of methane transport from deeper methanogenic zones, resulting in oxidation of atmospheric methane [Yavitt et al., 1988; Bognet et al., 1997a].In this paper, we focus on three field-validated models for net methane emissions from wetlands, rice production, and landfills: (1) wetland model [Walter et al