4.7 Article

Seasonal exports and drivers of dissolved inorganic and organic carbon, carbon dioxide, methane and δ13C signatures in a subtropical river network

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 575, Issue -, Pages 545-563

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2016.09.020

Keywords

Aquatic carbon; Radon; Keeling plots; Climate change; Greenhouse gases; Carbon budget

Funding

  1. Northern Rivers Regional Council
  2. Southern Cross University
  3. Australian Research Council [DE140101733, DE150100581, LE120100156, LP130100498]

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Riverine systems act as important aquatic conduits for carbon transportation between atmospheric, terrestrial and oceanic pools, yet the magnitude of these exports remain poorly constrained. Interconnected creek and river sites (n = 28) were sampled on a quarterly basis in three subcatchments of the subtropical Richmond River Catchment (Australia) to investigate spatial and temporal dynamics of dissolved inorganic carbon (DIC), dissolved organic carbon (DOC), carbon dioxide (CO2), methane (CH4), and carbon stable isotope ratios (delta C-13). The study site is an area of high interest due to potential unconventional gas (coal seamgas or coal bed methane) development. DIC exports were driven by groundwater discharge with a small contribution by in situ DOC remineralization. The DIC exports showed seasonal differences ranging from 0.10 to 0.27 mmol m(-2) catchment d(-1) (annual average 0.17 mmol m(-2) catchment d(-1)) and peaked during winter when surface water discharge was highest. DOC exports (sourced from terrestrial organic matter) had an annual average 0.07 mmol m(-2) catchment d(-1) and were 1 to 2 orders of magnitude higher during winter compared to spring and summer. CO2 evasion rates (annual average of 347 mmol m(-2) water area d(-1)) were similar to 2.5 fold higher during winter compared to spring. Methane was always supersaturated (0.19 to 62.13 mu M), resulting from groundwater discharge and stream-bed methanogenesis. Methane evasion was highly variable across the seasons with an annual average of 3.05 mmol m(-2) water area d(-1). During drier conditions, stable isotopes implied enhanced CH4 oxidation. Overall, carbon losses from the catchment were dominated by CO2 evasion (60%) followed by DIC exports (30%), DOC exports (9%) and CH4 evasion (<1%). Our results demonstrated broad catchment scale spatial and temporal variability in carbon dynamics, and that groundwater discharge and rain events controlled carbon exports. (C) 2016 Elsevier B.V. All rights reserved.

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