Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoir

This study aimed at describing kinetic aspects of aerobic and anaerobic mineralization of Eicchornia azurea. The samples of aquatic macrophyte and water were collected in the Monjolinho Reservoir (22° 00′ S and 47° 54′ W). To determine the leachate potential, dried plant fragments were added to rese...

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Main Authors: I Bianchini Junior, MB Cunha-Santino, JU Ribeiro, DGB Penteado
Format: Article
Language:English
Published: Instituto Internacional de Ecologia
Series:Brazilian Journal of Biology
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842014000100013&lng=en&tlng=en
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author I Bianchini Junior
MB Cunha-Santino
JU Ribeiro
DGB Penteado
author_facet I Bianchini Junior
MB Cunha-Santino
JU Ribeiro
DGB Penteado
author_sort I Bianchini Junior
collection DOAJ
description This study aimed at describing kinetic aspects of aerobic and anaerobic mineralization of Eicchornia azurea. The samples of aquatic macrophyte and water were collected in the Monjolinho Reservoir (22° 00′ S and 47° 54′ W). To determine the leachate potential, dried plant fragments were added to reservoir water, with sampling lasting for 4 months, where the particulate and dissolved organic carbon concentrations were measured. The kinetics of mass loss was obtained with 10 mineralization chambers for both aerobic and anaerobic conditions, with the plant fragments and reservoir water. Two additional chambers were used to monitor the volume of gases produced from anaerobic mineralization, with bioassays to determine oxygen uptake. The results were fitted to a first-order kinetic model, from which 27.21% of detritus corresponded to labile/soluble fractions and 72.62% to the refractory fractions. The decay rates for the global mass losses of the labile/soluble components were 2.07 day–1. DOC mineralization was not verified for either condition. Under aerobic condition, the mass loss constant rate (0.0029 day–1) for the refractory fractions was 2.4 the value for the anaerobic one. Under anaerobic condition, the gases formation occurred in three phases. Based on these results, in the Monjolinho Reservoir, the decomposition of E. azurea that undergo within the water column and in upper layers of sediment is a faster process, favoring the mineralization. In contrast, in the lower layers of sediment the diagenetic processes (i.e. humus production and accumulation of organic matter) are favored.
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spelling doaj.art-97b88e0232214426b5a76d3dfabee8a12022-12-22T03:52:35ZengInstituto Internacional de EcologiaBrazilian Journal of Biology1678-437574110011010.1590/1519-6984.17912S1519-69842014000100013Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoirI Bianchini JuniorMB Cunha-SantinoJU RibeiroDGB PenteadoThis study aimed at describing kinetic aspects of aerobic and anaerobic mineralization of Eicchornia azurea. The samples of aquatic macrophyte and water were collected in the Monjolinho Reservoir (22° 00′ S and 47° 54′ W). To determine the leachate potential, dried plant fragments were added to reservoir water, with sampling lasting for 4 months, where the particulate and dissolved organic carbon concentrations were measured. The kinetics of mass loss was obtained with 10 mineralization chambers for both aerobic and anaerobic conditions, with the plant fragments and reservoir water. Two additional chambers were used to monitor the volume of gases produced from anaerobic mineralization, with bioassays to determine oxygen uptake. The results were fitted to a first-order kinetic model, from which 27.21% of detritus corresponded to labile/soluble fractions and 72.62% to the refractory fractions. The decay rates for the global mass losses of the labile/soluble components were 2.07 day–1. DOC mineralization was not verified for either condition. Under aerobic condition, the mass loss constant rate (0.0029 day–1) for the refractory fractions was 2.4 the value for the anaerobic one. Under anaerobic condition, the gases formation occurred in three phases. Based on these results, in the Monjolinho Reservoir, the decomposition of E. azurea that undergo within the water column and in upper layers of sediment is a faster process, favoring the mineralization. In contrast, in the lower layers of sediment the diagenetic processes (i.e. humus production and accumulation of organic matter) are favored.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842014000100013&lng=en&tlng=endecayoxygen consumptiongases formationaquatic macrophyteMonjolinho Reservoir
spellingShingle I Bianchini Junior
MB Cunha-Santino
JU Ribeiro
DGB Penteado
Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoir
Brazilian Journal of Biology
decay
oxygen consumption
gases formation
aquatic macrophyte
Monjolinho Reservoir
title Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoir
title_full Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoir
title_fullStr Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoir
title_full_unstemmed Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoir
title_short Implication of anaerobic and aerobic decomposition of Eichhornia azurea (Sw.) Kunth. on the carbon cycling in a subtropical reservoir
title_sort implication of anaerobic and aerobic decomposition of eichhornia azurea sw kunth on the carbon cycling in a subtropical reservoir
topic decay
oxygen consumption
gases formation
aquatic macrophyte
Monjolinho Reservoir
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842014000100013&lng=en&tlng=en
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AT juribeiro implicationofanaerobicandaerobicdecompositionofeichhorniaazureaswkunthonthecarboncyclinginasubtropicalreservoir
AT dgbpenteado implicationofanaerobicandaerobicdecompositionofeichhorniaazureaswkunthonthecarboncyclinginasubtropicalreservoir