2026-04-17T14:18:32Zhttps://recercat.cat/oai/request

oai:recercat.cat:10256/131352024-06-18T11:53:07Zcom_2072_452955com_2072_2054col_2072_453077

2024-06-18T11:53:07Z urn:hdl:10256/13135 Hot spots for carbon emissions from Mediterranean fluvial networks during summer drought Gómez Gener, Lluís Obrador, Biel von Schiller, Daniel Marcé Romero, Rafael Casas Ruiz, Joan Pere Proia, Lorenzo Acuña i Salazar, Vicenç Catalán, Núria Muñoz Gràcia, Isabel Koschorreck, Matthias Biogeoquímica Biogeochemistry Gasos d'efecte hivernacle Greenhouse gases Metà Methane During summer drought, Mediterranean fluvial networks are transformed into highly heterogeneous landscapes characterized by different environments (i.e., running and impounded waters, isolated river pools and dry beds). This hydrological setting defines novel biogeochemically active areas that could potentially increase the rates of carbon emissions from the fluvial network to the atmosphere. Using chamber methods, we aimed to identify hot spots for carbon dioxide (CO2) and methane (CH4) emissions from two typical Mediterranean fluvial networks during summer drought. The CO2 efflux from dry beds (mean ± SE = 209 ± 10 mmolCO2m-2 d-1) was comparable to that from running waters (120 ± 33 mmol m-2 d-1) and significantly higher than from impounded waters (36.6 ± 8.5 mmol m-2 d-1) and isolated pools (17.2 ± 0.9 mmol m-2 d-1). In contrast, the CH4 efflux did not significantly differ among environments, although the CH4 efflux was notable in some impounded waters (13.9 ± 10.1 mmol CH4 m-2 d-1) and almost negligible in the remaining environments (mean\0.3 mmol m-2 d-1). Diffusion was the only mechanism driving CO2 efflux in all environments and was most likely responsible for CH4 efflux in running waters, isolated pools and dry beds. In contrast, the CH4 efflux in impounded waters was primarily ebullition-based. Using a simple heuristic approach to simulate potential changes in carbon emissions from Mediterranean fluvial networks under future hydrological scenarios, we show that an extreme drying out (i.e., a four-fold increase of the surface area of dry beds) would double the CO2 efflux from the fluvial network. Correspondingly, an extreme transformation of running waters into impounded waters (i.e., a twofold increase of the surface area of impounded waters) would triple the CH4 efflux. Thus, carbon emissions from dry beds and impounded waters should be explicitly considered in carbon assessments of fluvial networks, particularly under predicted global change scenarios, which are expected to increase the spatial and temporal extent of these environments This research was funded by the Spanish Ministry of Economy and Competitiveness through the projects CGL2011-30474-C02-01 and CGL2014-58760-C3-1-R 2024-06-18T11:53:07Z 2024-06-18T11:53:07Z info:eu-repo/date/embargoEnd/2026-01-01 info:eu-repo/date/embargoEnd/2026-01-01 2015 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/10256/13135 info:eu-repo/semantics/altIdentifier/doi/10.1007/s10948-012-1632-z10.1007/s10533-015-0139-7 info:eu-repo/semantics/altIdentifier/issn/0168-2563 info:eu-repo/semantics/altIdentifier/eissn/1573-515X info:eu-repo/grantAgreement/MICINN//CGL2011-30474-C02-01/ES/TRANSPORTE Y PROCESADO DEL CARBONO EN LA RED FLUVIAL: RELEVANCIA DEL CAMBIO GLOBAL/ info:eu-repo/grantAgreement/MINECO//CGL2014-58760-C3-2-R/ES/ECOSISTEMAS FLUVIALES TEMPORALES Y CAMBIO GLOBAL: EFECTOS SOBRE LA ESTRUCTURA Y FUNCION DEL ECOSISTEMA/ Tots els drets reservats info:eu-repo/semantics/embargoedAccess Springer Verlag © Biogeochemistry, 2015, vol. 125, núm. 3, p. 1-18 Articles publicats (ICRA)