Metya, Abirlal, Chakraborty, Supriyo, Bhattacharya, S. K., Datye, Amey, Deb Burman, Pramit K., Dasgupta, Panini, Sarma, Dipankar, Gogoi, Nirmali, and Bora, Abhijit
Among the natural ecosystems, forests and wetlands emit a sizable amount of carbon dioxide (CO2) and methane (CH4) through autotrophic and heterotrophic respiration and bacterial activities. Interestingly, some evidence suggests that a significant amount of CH4 is generated by the trees in forested ecosystems. The net ecosystem exchange (NEE), measured by the eddy covariance (EC) method, typically represents the net CO2 flux arising from the photosynthetic and respiration processes in the biosphere. This flux is subsequently partitioned into two components, the respired carbon and the assimilated carbon. However, the usual method of partitioning introduces significant errors in each of these fluxes. The present study was undertaken to address this issue where the NEE partitioning was constrained by using the carbon isotopic ratios of CO2. We used a real‐time in situ analyzer in a tropical forest in northeast India, the Kaziranga National Park. The greenhouse gas analyzer provided CO2 and CH4 concentrations, as well as their carbon isotopic ratios. The isotopic data were used to partition the EC‐derived NEE values and derive the isoflux values. Additionally, the isotopic data provided evidence of plant‐generated CH4 in conformity with some recent studies, which requires further investigation. Plain Language Summary: The terrestrial vegetation absorbs a vast amount of carbon in the photosynthetic process. They also emit a sizeable amount of carbon through respiration. Eddy‐covariance‐based technique is often employed to quantify these two opposing fluxes. An eddy‐covariance‐based system measures carbon dioxide (CO2) concentrations along with wind speed, and covariance of their fluctuations is used to calculate the net ecosystem exchange (NEE). The NEE is then partitioned into the photosynthetic and respiration components through a series of numerical operations and environmental constraints. Flux measurements in association with carbon isotopic ratios can provide a unique way to partition NEE. We have measured the concentration and isotopic ratio of CO2 and the eddy covariance‐based measurements to obtain the respiratory and photosynthetic fluxes of CO2 in a tropical forest in India. In addition, methane (CH4) concentration and its isotopic ratio have been measured to identify if trees can be considered a CH4 source in this ecosystem. Key Points: The net ecosystem exchange was measured using an eddy‐covariance technique in a forest in IndiaSeparately the greenhouse gases isotopic data were collected and used to determine the "isofluxes"Partitioning of the respiratory and the photosynthetic fluxes was carried out [ABSTRACT FROM AUTHOR]