River outgassing has proven to be an integral part of the carbon cycle. In Southeast Asia, river outgassing quantities are uncertain due to lack of measured data. Here we investigate six rivers in Indonesia and Malaysia, during five expeditions. CO2 fluxes from Southeast Asian rivers amount to 66.9 ± 15.7 Tg C per year, of which Indonesia releases 53.9 ± 12.4 Tg C per year. Malaysian rivers emit 6.2 ± 1.6 Tg C per year. These moderate values show that Southeast Asia is not the river outgassing hotspot as would be expected from the carbon-enriched peat soils. This is due to the relatively short residence time of dissolved organic carbon (DOC) in the river, as the peatlands, being the primary source of DOC, are located near the coast. Limitation of bacterial production, due to low pH, oxygen depletion or the refractory nature of DOC, potentially also contributes to moderate CO2 fluxes as this decelerates decomposition.
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http://dx.doi.org/10.1038/ncomms10155 | DOI Listing |
Sci Total Environ
December 2024
Department of Earth and Environmental Sciences, National Chung Cheng University, Chiayi 621, Taiwan.
Secondary carbonate precipitation plays a crucial role in determining the CO outgassing from carbonate-saturated rivers and influences the short-term terrestrial carbon cycle. The fractionation of stable isotopes has been extensively employed to quantify post-weathering reactions in rivers and assess the quantities of metals removed by secondary carbonates. However, a major challenge is that water isotopic compositions usually reflect both lithological mixing and biogeochemical fractionation, which complicates distinguishing between these signals.
View Article and Find Full Text PDFWater Res
October 2023
College of Eco-Environmental Engineering, Guizhou Minzu University, Guiyang 550025, China.
Environ Sci Technol
May 2024
iES─Institute for Environmental Sciences, University of Kaiserslautern-Landau (RPTU), Landau D-76829, Germany.
Artificial channels, common features of inland waters, have been suggested as significant contributors to methane (CH) and carbon dioxide (CO) dynamics and emissions; however, the magnitude and drivers of their CH and CO emissions (diffusive and ebullitive) remain unclear. They are characterized by reduced flow compared to the donor river, which results in suspended organic matter (OM) accumulation. We propose that in such systems hydrological controls will be reduced and OM accumulation will control emissions by promoting methane production and outgassing.
View Article and Find Full Text PDFSci Total Environ
May 2024
School of Renewable Natural Resources, Louisiana State University, Baton Rouge, LA 70803, USA.
Rivers not only function as a conduit for the delivery of terrestrial constituents to oceans, but they also serve as an essential medium for biogeochemical processing of the constituents. While extensive research has been conducted on carbon transport in many rivers, little is known about carbon transformation in engineered rivers reconnected with their floodplain network. Being the largest distributary of the levee-confined Mississippi River (MR), the Atchafalaya River (AR) carries 25 % of the MR water, flowing through North America's largest freshwater swamp basin and emptying into the Gulf of Mexico.
View Article and Find Full Text PDFSci Total Environ
November 2023
Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China.
It is generally acknowledged that riverine dissolved inorganic carbon (DIC) behaviors play a critical role in global carbon cycling and hence have an impact on climate change. However, little is known about the intricate DIC dynamics under various meteorological conditions in the alpine areas. Here, we investigated DIC biogeochemical processes in the Bailong River catchment, eastern Qinghai-Tibet Plateau (QTP), by combining measurements of major ions, stable and radioactive isotopic compositions of DIC (δC and ΔC), and physiographic parameters in the Bailong River catchment.
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