Using a crop/soil simulation model and GIS techniques to assess methane emissions from rice fields in Asia. II. Model validation and sensitivity analysis

The MERES (Methane Emissions from Rice EcoSystems) simulation model was tes ted using experimental data from IRRI and Maligaya in the Philippines and f rom Hangzhou in China. There was good agreement between simulated and obser ved values of total aboveground biomass, root weight, grain yield, and seas onal methane (CH4) emissions. The importance of the contribution of the ric e crop to CH4 emissions was highlighted. Rhizodeposition (root exudation an d root death) was predicted to contribute about 380 kg C ha(-1) of methanog enic substrate over the season, representing 37% of the total methanogenic substrate from all sources when no organic amendments were added. A further 225 kg C ha(-1) (22%) was predicted to come from previous crop residues, g iving a total of around 60% originating from the rice crop, with the remain ing 41% coming from the humic fraction of the soil organic matter (SOM). Se nsitivity analysis suggested that the parameter representing transmissivity to gaseous transfer per unit root length (lambda (r)) was important in det ermining seasonal CH4 emissions. As this transmissivity increased, more O-2 was able to diffuse to the rhizosphere, so that CH4 production by methanog ens was reduced and more CH4 was oxidized by methanotrophs. These effects o utweighed the opposing influence of increased rate of transport of CH4 thro ugh the plant, so that the overall effect was to reduce the amount of CH4 e mitted over the season. Varying the root-shoot ratio of the crop was predic ted to have little effect on seasonal emissions, the increased rates of rhi zodeposition being counteracted by the increased rates of O-2 diffusion to the rhizosphere. Increasing the length of a midseason drainage period reduc ed CH4 emissions significantly, but periods longer than 6-7 d also decrease d rice yields. Organic amendments with low C/N were predicted to be more be neficial, both in terms of enhancing crop yields and reducing CH4 emissions , even when the same amount of C was applied. This was due to higher rates of immobilization of C into microbial biomass, removing it temporarily as a methanogenic substrate.