Spatial and temporal variability of pCO₂ and CO₂ efflux in seven Amazonian Rivers
Current estimates of CO₂ outgassing from Amazonian rivers and streams have considerable uncertainty since they are based on limited-time surveys of pCO₂ measurements along the Amazon mainstem and mouths of major tributaries, using conservative estimates of gas exchange velocities. In order to refine...
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description | Current estimates of CO₂ outgassing from Amazonian rivers and streams have considerable uncertainty since they are based on limited-time surveys of pCO₂ measurements along the Amazon mainstem and mouths of major tributaries, using conservative estimates of gas exchange velocities. In order to refine basin-scale CO₂ efflux estimates from Amazonian rivers, we present a long time (5-year) dataset of direct measurements of CO₂ fluxes, gas transfer velocities and pCO₂ measurements in seven representative rivers of the lowland Amazon basin fluvial network, six non-tidal (Negro, Solimões, Teles Pires, Cristalino, Araguaia and Javaés) and one tidal river (Caxiuanã), with sizes ranging from 4th to 9th order. Surveys were conducted from January 2006 to December 2010, in a total of 389 campaigns covering all stages of their hydrographs. CO₂ fluxes and gas transfer velocities (k) were measured using floating chambers and pCO₂ was measured simultaneously by headspace extraction followed by gas chromatography analysis. Results show high CO₂ flux rate variability among rivers and hydrograph stages, ranging from −0.8 to 15.3 μmol CO₂ m⁻² s⁻¹, with unexpected negative fluxes in clear-water rivers during low waters. Non-tidal rivers showed marked seasonal CO₂ flux patterns, with significantly higher exchange during high waters. Seasonality was modulated by pCO₂, which was positive and strongly correlated with discharge. In these rivers k was well correlated with wind speed, which allowed the use of wind data to model k. We estimate a release of 360 ± 60 Tg C year⁻¹ from Amazonian rivers and streams within a 1.47 million km² quadrant in the central lowland Amazon. Extrapolating these values to the basin upstream of Óbidos, results in an outgassing of 0.8 Pg C to the atmosphere each year. Our results are a step forward in achieving more accurate gas emission values for Amazonian rivers and their role in the annual carbon budget of the Amazon basin. |
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L. Rasera, Maria ; Krusche, Alex V. ; Richey, Jeffrey E. ; Ballester, Maria V. R. ; Victória, Reynaldo L.</creator><creatorcontrib>de Fátima F. L. Rasera, Maria ; Krusche, Alex V. ; Richey, Jeffrey E. ; Ballester, Maria V. R. ; Victória, Reynaldo L.</creatorcontrib><description>Current estimates of CO₂ outgassing from Amazonian rivers and streams have considerable uncertainty since they are based on limited-time surveys of pCO₂ measurements along the Amazon mainstem and mouths of major tributaries, using conservative estimates of gas exchange velocities. In order to refine basin-scale CO₂ efflux estimates from Amazonian rivers, we present a long time (5-year) dataset of direct measurements of CO₂ fluxes, gas transfer velocities and pCO₂ measurements in seven representative rivers of the lowland Amazon basin fluvial network, six non-tidal (Negro, Solimões, Teles Pires, Cristalino, Araguaia and Javaés) and one tidal river (Caxiuanã), with sizes ranging from 4th to 9th order. Surveys were conducted from January 2006 to December 2010, in a total of 389 campaigns covering all stages of their hydrographs. CO₂ fluxes and gas transfer velocities (k) were measured using floating chambers and pCO₂ was measured simultaneously by headspace extraction followed by gas chromatography analysis. Results show high CO₂ flux rate variability among rivers and hydrograph stages, ranging from −0.8 to 15.3 μmol CO₂ m⁻² s⁻¹, with unexpected negative fluxes in clear-water rivers during low waters. Non-tidal rivers showed marked seasonal CO₂ flux patterns, with significantly higher exchange during high waters. Seasonality was modulated by pCO₂, which was positive and strongly correlated with discharge. In these rivers k was well correlated with wind speed, which allowed the use of wind data to model k. We estimate a release of 360 ± 60 Tg C year⁻¹ from Amazonian rivers and streams within a 1.47 million km² quadrant in the central lowland Amazon. Extrapolating these values to the basin upstream of Óbidos, results in an outgassing of 0.8 Pg C to the atmosphere each year. Our results are a step forward in achieving more accurate gas emission values for Amazonian rivers and their role in the annual carbon budget of the Amazon basin.</description><identifier>ISSN: 0168-2563</identifier><identifier>EISSN: 1573-515X</identifier><identifier>DOI: 10.1007/s10533-013-9854-0</identifier><identifier>CODEN: BIOGEP</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Biogeochemistry ; Biogeosciences ; Carbon dioxide ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Ecosystems ; Engineering and environment geology. Geothermics ; Environmental Chemistry ; Estuaries ; Exact sciences and technology ; Gas chromatography ; Gas exchange ; Greenhouse gases ; Groundwater ; Headwaters ; Hydrographs ; Hydrology ; Hydrology. Hydrogeology ; Life Sciences ; Marine and continental quaternary ; Pollution, environment geology ; River basins ; River water ; Rivers ; Seasonal variations ; Soil water ; Streams ; Surface water ; Surficial geology ; Tidal rivers ; Wind speed ; Wind velocity</subject><ispartof>Biogeochemistry, 2013-12, Vol.116 (1-3), p.241-259</ispartof><rights>Springer Science+Business Media Dordrecht 2013</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c368t-797dbd39e9fc0b221c96fd2a191aec8a3751994a65c27b3e776f131b7a5741873</citedby><cites>FETCH-LOGICAL-c368t-797dbd39e9fc0b221c96fd2a191aec8a3751994a65c27b3e776f131b7a5741873</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/24716797$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/24716797$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27924,27925,41488,42557,51319,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28067962$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>de Fátima F. L. Rasera, Maria</creatorcontrib><creatorcontrib>Krusche, Alex V.</creatorcontrib><creatorcontrib>Richey, Jeffrey E.</creatorcontrib><creatorcontrib>Ballester, Maria V. R.</creatorcontrib><creatorcontrib>Victória, Reynaldo L.</creatorcontrib><title>Spatial and temporal variability of pCO₂ and CO₂ efflux in seven Amazonian Rivers</title><title>Biogeochemistry</title><addtitle>Biogeochemistry</addtitle><description>Current estimates of CO₂ outgassing from Amazonian rivers and streams have considerable uncertainty since they are based on limited-time surveys of pCO₂ measurements along the Amazon mainstem and mouths of major tributaries, using conservative estimates of gas exchange velocities. In order to refine basin-scale CO₂ efflux estimates from Amazonian rivers, we present a long time (5-year) dataset of direct measurements of CO₂ fluxes, gas transfer velocities and pCO₂ measurements in seven representative rivers of the lowland Amazon basin fluvial network, six non-tidal (Negro, Solimões, Teles Pires, Cristalino, Araguaia and Javaés) and one tidal river (Caxiuanã), with sizes ranging from 4th to 9th order. Surveys were conducted from January 2006 to December 2010, in a total of 389 campaigns covering all stages of their hydrographs. CO₂ fluxes and gas transfer velocities (k) were measured using floating chambers and pCO₂ was measured simultaneously by headspace extraction followed by gas chromatography analysis. Results show high CO₂ flux rate variability among rivers and hydrograph stages, ranging from −0.8 to 15.3 μmol CO₂ m⁻² s⁻¹, with unexpected negative fluxes in clear-water rivers during low waters. Non-tidal rivers showed marked seasonal CO₂ flux patterns, with significantly higher exchange during high waters. Seasonality was modulated by pCO₂, which was positive and strongly correlated with discharge. In these rivers k was well correlated with wind speed, which allowed the use of wind data to model k. We estimate a release of 360 ± 60 Tg C year⁻¹ from Amazonian rivers and streams within a 1.47 million km² quadrant in the central lowland Amazon. Extrapolating these values to the basin upstream of Óbidos, results in an outgassing of 0.8 Pg C to the atmosphere each year. Our results are a step forward in achieving more accurate gas emission values for Amazonian rivers and their role in the annual carbon budget of the Amazon basin.</description><subject>Biogeochemistry</subject><subject>Biogeosciences</subject><subject>Carbon dioxide</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Ecosystems</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Environmental Chemistry</subject><subject>Estuaries</subject><subject>Exact sciences and technology</subject><subject>Gas chromatography</subject><subject>Gas exchange</subject><subject>Greenhouse gases</subject><subject>Groundwater</subject><subject>Headwaters</subject><subject>Hydrographs</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Life Sciences</subject><subject>Marine and continental quaternary</subject><subject>Pollution, environment geology</subject><subject>River basins</subject><subject>River water</subject><subject>Rivers</subject><subject>Seasonal variations</subject><subject>Soil water</subject><subject>Streams</subject><subject>Surface water</subject><subject>Surficial geology</subject><subject>Tidal rivers</subject><subject>Wind speed</subject><subject>Wind velocity</subject><issn>0168-2563</issn><issn>1573-515X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kF1LwzAUhoMoOKc_wAuhIF5Wc5omaS7H8AsGA3XgXTjtEsno2pp0w3m5n-ovsbOiXnmVE87zPgkvIadAL4FSeRWAcsZiCixWGU9jukcGwCWLOfDnfTKgILI44YIdkqMQFpRSJSkbkNljg63DMsJqHrVm2dS-u6zRO8xd6dpNVNuoGU8_ttsvpJ-MteXqLXJVFMzaVNFoie915bCKHtza-HBMDiyWwZx8n0Myu7l-Gt_Fk-nt_Xg0iQsmsjaWSs7zOVNG2YLmSQKFEnaeIChAU2TIJAelUhS8SGTOjJTCAoNcIpcpZJINyXnvbXz9ujKh1Yt65avuSQ2p4MAUZayjoKcKX4fgjdWNd0v0Gw1U79rTfXu6a0_v2tO0y1x8mzEUWFqPVeHCTzDJqJBKJB2X9FzoVtWL8X9-8I_8rA8tQlv7X2kqobNK9gkLn4kC</recordid><startdate>20131201</startdate><enddate>20131201</enddate><creator>de Fátima F. 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L. Rasera, Maria</au><au>Krusche, Alex V.</au><au>Richey, Jeffrey E.</au><au>Ballester, Maria V. R.</au><au>Victória, Reynaldo L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial and temporal variability of pCO₂ and CO₂ efflux in seven Amazonian Rivers</atitle><jtitle>Biogeochemistry</jtitle><stitle>Biogeochemistry</stitle><date>2013-12-01</date><risdate>2013</risdate><volume>116</volume><issue>1-3</issue><spage>241</spage><epage>259</epage><pages>241-259</pages><issn>0168-2563</issn><eissn>1573-515X</eissn><coden>BIOGEP</coden><abstract>Current estimates of CO₂ outgassing from Amazonian rivers and streams have considerable uncertainty since they are based on limited-time surveys of pCO₂ measurements along the Amazon mainstem and mouths of major tributaries, using conservative estimates of gas exchange velocities. In order to refine basin-scale CO₂ efflux estimates from Amazonian rivers, we present a long time (5-year) dataset of direct measurements of CO₂ fluxes, gas transfer velocities and pCO₂ measurements in seven representative rivers of the lowland Amazon basin fluvial network, six non-tidal (Negro, Solimões, Teles Pires, Cristalino, Araguaia and Javaés) and one tidal river (Caxiuanã), with sizes ranging from 4th to 9th order. Surveys were conducted from January 2006 to December 2010, in a total of 389 campaigns covering all stages of their hydrographs. CO₂ fluxes and gas transfer velocities (k) were measured using floating chambers and pCO₂ was measured simultaneously by headspace extraction followed by gas chromatography analysis. Results show high CO₂ flux rate variability among rivers and hydrograph stages, ranging from −0.8 to 15.3 μmol CO₂ m⁻² s⁻¹, with unexpected negative fluxes in clear-water rivers during low waters. Non-tidal rivers showed marked seasonal CO₂ flux patterns, with significantly higher exchange during high waters. Seasonality was modulated by pCO₂, which was positive and strongly correlated with discharge. In these rivers k was well correlated with wind speed, which allowed the use of wind data to model k. We estimate a release of 360 ± 60 Tg C year⁻¹ from Amazonian rivers and streams within a 1.47 million km² quadrant in the central lowland Amazon. Extrapolating these values to the basin upstream of Óbidos, results in an outgassing of 0.8 Pg C to the atmosphere each year. Our results are a step forward in achieving more accurate gas emission values for Amazonian rivers and their role in the annual carbon budget of the Amazon basin.</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1007/s10533-013-9854-0</doi><tpages>19</tpages></addata></record> |
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subjects | Biogeochemistry Biogeosciences Carbon dioxide Earth and Environmental Science Earth Sciences Earth, ocean, space Ecosystems Engineering and environment geology. Geothermics Environmental Chemistry Estuaries Exact sciences and technology Gas chromatography Gas exchange Greenhouse gases Groundwater Headwaters Hydrographs Hydrology Hydrology. Hydrogeology Life Sciences Marine and continental quaternary Pollution, environment geology River basins River water Rivers Seasonal variations Soil water Streams Surface water Surficial geology Tidal rivers Wind speed Wind velocity |
title | Spatial and temporal variability of pCO₂ and CO₂ efflux in seven Amazonian Rivers |
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