Methane Emission from Lowland Rice Cultivation
Flooded rice fields are generally anoxic and thus provide excellent habitat for Methanogenic microorganisms. Methane (CH4) absorbs long-wave radiation and therefore is a green house gas that leads to the warming of the earth’s surface.
Together with CO2 and nitrous oxide, methane traps the thermal radiation from the earth’s surface and influences the atmospheric chemistry of ozone in the troposphere as well as the stratosphere through photochemical reactions. The present estimates of CH4 emissions from wetland rice cultivation are placed around 25-17 Tg CH4 per year.





