Diurnal variation in methane emission from a rice paddy due to ebullition

Abstract

AbstractDiurnal fluctuations in methane (CH4) emission are frequently observed in rice paddy fields, yet the driving mechanisms behind these variations are not fully understood. We posited that the observed diurnal patterns are predominantly due to temperature‐dependent bubbling emissions (ebullition). To investigate this hypothesis, we conducted measurements of CH4 emission in a Japanese rice paddy using static chambers coupled with a high‐time‐resolution CH4 analyzer that allowed us to partition the total flux into its two principal components: plant‐mediated transport and ebullition. Diurnal variation in the total flux was minimal during the early parts of reproductive growth (panicle formation and booting stages), when plant‐mediated emission was dominant. At a later stage (heading period), ebullition accounted for 43%–70% of the total emission, and CH4 emission via both pathways varied diurnally; however, the diurnal range was much greater for bubbling emission (ratio of maximum to minimum = 3.5) than for plant‐mediated emission (ratio of maximum to minimum = 1.4). The magnitude of emissions due to ebullition depended on the temperature, but was greater during the flux‐increasing phase in the morning than the flux‐decreasing phase in the afternoon even at the same temperature, forming a hysteresis in the flux versus temperature relationship. These findings support our hypothesis and indicate that abiotic processes, such as a change in the solubility of gases and the temperature dependence of the gas‐phase volume (Charles's law), may play a central role in shaping the diurnal pattern of the CH4 ebullition.