Biogenic gases in tropical floodplain river

Analysis of the distribution of biogenic gases in the floodplain of the Mogi-Guaçu River (São Paulo, Brazil) enabled the establishment of a "redox hierarchy", in which the main channel was the most oxidizing environment, followed by Diogo Lake, with Infernão Lake having the most reducing conditions of the subsystems evaluated. Diogo Lake exported about 853.4 g C.m-2.year-1, of which, 14.6% was generated from methanogenesis and 36.7% by aerobic respiration. For Infernão Lake, these values were 2016 g C.m-2.year-1, 1.8 % and 41.5 %, respectively. Carbon export by these systems was predominantly in the form of CO2, which was responsible for the release of 728.78 g C.m-2.year-1 at Diogo Lake and 1979.72 g C.m-2. year-1 at Infernão Lake. Such patterns may result from the nature of the hydrological conditions, the action of the hydroperiod, and morphological characteristics of the environment.

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Main Authors: Ballester,Maria Victória Ramos, Santos,José Eduardo dos
Format: Digital revista
Language:English
Published: Instituto de Tecnologia do Paraná - Tecpar 2001
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-89132001000200006
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spelling oai:scielo:S1516-891320010002000062001-11-07Biogenic gases in tropical floodplain riverBallester,Maria Victória RamosSantos,José Eduardo dos Biogenic gases methanogenesis aerobic respiration CO2 production Analysis of the distribution of biogenic gases in the floodplain of the Mogi-Guaçu River (São Paulo, Brazil) enabled the establishment of a "redox hierarchy", in which the main channel was the most oxidizing environment, followed by Diogo Lake, with Infernão Lake having the most reducing conditions of the subsystems evaluated. Diogo Lake exported about 853.4 g C.m-2.year-1, of which, 14.6% was generated from methanogenesis and 36.7% by aerobic respiration. For Infernão Lake, these values were 2016 g C.m-2.year-1, 1.8 % and 41.5 %, respectively. Carbon export by these systems was predominantly in the form of CO2, which was responsible for the release of 728.78 g C.m-2.year-1 at Diogo Lake and 1979.72 g C.m-2. year-1 at Infernão Lake. Such patterns may result from the nature of the hydrological conditions, the action of the hydroperiod, and morphological characteristics of the environment.info:eu-repo/semantics/openAccessInstituto de Tecnologia do Paraná - TecparBrazilian Archives of Biology and Technology v.44 n.2 20012001-06-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-89132001000200006en10.1590/S1516-89132001000200006
institution SCIELO
collection OJS
country Brasil
countrycode BR
component Revista
access En linea
databasecode rev-scielo-br
tag revista
region America del Sur
libraryname SciELO
language English
format Digital
author Ballester,Maria Victória Ramos
Santos,José Eduardo dos
spellingShingle Ballester,Maria Victória Ramos
Santos,José Eduardo dos
Biogenic gases in tropical floodplain river
author_facet Ballester,Maria Victória Ramos
Santos,José Eduardo dos
author_sort Ballester,Maria Victória Ramos
title Biogenic gases in tropical floodplain river
title_short Biogenic gases in tropical floodplain river
title_full Biogenic gases in tropical floodplain river
title_fullStr Biogenic gases in tropical floodplain river
title_full_unstemmed Biogenic gases in tropical floodplain river
title_sort biogenic gases in tropical floodplain river
description Analysis of the distribution of biogenic gases in the floodplain of the Mogi-Guaçu River (São Paulo, Brazil) enabled the establishment of a "redox hierarchy", in which the main channel was the most oxidizing environment, followed by Diogo Lake, with Infernão Lake having the most reducing conditions of the subsystems evaluated. Diogo Lake exported about 853.4 g C.m-2.year-1, of which, 14.6% was generated from methanogenesis and 36.7% by aerobic respiration. For Infernão Lake, these values were 2016 g C.m-2.year-1, 1.8 % and 41.5 %, respectively. Carbon export by these systems was predominantly in the form of CO2, which was responsible for the release of 728.78 g C.m-2.year-1 at Diogo Lake and 1979.72 g C.m-2. year-1 at Infernão Lake. Such patterns may result from the nature of the hydrological conditions, the action of the hydroperiod, and morphological characteristics of the environment.
publisher Instituto de Tecnologia do Paraná - Tecpar
publishDate 2001
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-89132001000200006
work_keys_str_mv AT ballestermariavictoriaramos biogenicgasesintropicalfloodplainriver
AT santosjoseeduardodos biogenicgasesintropicalfloodplainriver
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