Effects of rice cultivars on methane fluxes in a paddy soil

Abstract

CH₄ emission and its relevant processes involved (i.e. CH₄ production, rhizospheric CH₄ oxidation and plant-mediated CH₄ transport) were studied simultaneously to comprehensively understand how rice cultivars (Yanxuan, 72031, and 9516) at growth stages (early and late tillering, panicle initiation, ripening, and harvest stage) affect CH₄ emission in a paddy soil. Over the entire rice-growing season, Yanxuan had the highest CH₄ emission flux with 5.98 μg CH₄ m⁻² h⁻¹ followed by 72031 (4.48 μg CH₄ m⁻² h⁻¹) and 9516 (3.41 μg CH₄ m⁻² h⁻¹). The highest CH₄ production rate of paddy soils planted to Yanxuan was observed with 18.0 μg CH₄ kg_{{ (d.w.soil)}} h⁻¹ followed by the soil planted to 9516 (17.5 μg CH₄ kg_{{ (d.w.soil)}} h⁻¹). For each cultivar, both rhizospheric CH₄ oxidation ability and plant-mediated CH₄ transport efficiency varied widely with a range of 9.81–76.8% and 15.5–80.5% over the duration of crop growth, respectively. Multiple regression analyses showed that CH₄ emission flux was positively related with CH₄ production rate and rice plant-mediated CH₄ transport efficiency, but negatively with rhizospheric CH₄ oxidation (R ²=0.425 for Yanxuan, P<0.01; R ²=0.426 for 72031, P<0.01; R ²=0.564 for 9516, P<0.01). The contribution of rice plants to CH₄ production seems to be more important than to rhizospheric CH₄ oxidation and plant-mediated transport in impact of rice plants on CH₄ emission.