Abstract:
Small estuaries often remain neglected while characterizing air-water CO2 flux dynamics. This study reports the seasonal, spatial, and multi-annual variability of carbon biogeochemistry, emphasizing air-water CO2 flux from a small tropical mangrove-dominated estuary (Dhamra Estuary) of the Bay of Bengal, based on the 9-year-long sampling survey (2013 to 2021). The sampling covered twelve pre-fixed locations of this estuary. A suite of biogeochemical parameters was kept within the purview of this study to deliniate the interrelationship between CO2 fluxes and potential factors that can regulate/govern pCO(2)(aq) dynamics. Air water CO2 exchange rates were calculated using five globally accepted empirical gas transfer velocity equations and varied in a range of - 832.5 to 7904 mu mol m(-2) h(-1). The estuary was a sink for CO2 in monsoon season, having the highest average flux rates of - 380.9 +/- 125.5 mu mol m(-2) h(-1), whereas a source in pre-monsoon (38.29 +/- 913.1 mu mol m(-2) h(-1)) and post-monsoon (91.81 +/- 1009.8 mu mol m(-2) h(-1)). The significant factors governing pCO(2) were pH, salinity, total alkalinity and dissolved inorganic carbon (DIC). This long-term seasonal study emphasizes the need to include small regional estuaries for more accurate estimates of global CO2 flux to upscale the global carbon budget and its controlling mechanism.