The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) Lye
Assays were carried out to evaluate effects of detritus size on the mineralization of an aquatic macrophyte, the Oxycaryum cubense. Samples of plant and water were collected from an oxbow lake, the Infernão lagoon (21° 35' S and 47° 51' W) located at Mogi Guaçu river floodplain. The plants...
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doaj-ca36453ee7814c49b94af7a9c1faa0f72020-11-24T22:23:07ZengInstituto Internacional de EcologiaBrazilian Journal of Biology1678-4375662b64165010.1590/S1519-69842006000400008S1519-69842006000400008The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) LyeI. Bianchini Jr.0M. B. Cunha-Santino1Universidade Federal de São CarlosUniversidade Federal de São CarlosAssays were carried out to evaluate effects of detritus size on the mineralization of an aquatic macrophyte, the Oxycaryum cubense. Samples of plant and water were collected from an oxbow lake, the Infernão lagoon (21° 35' S and 47° 51' W) located at Mogi Guaçu river floodplain. The plants were taken to the laboratory, washed under tap water, dried (50 °C) and fractioned into six groups according to their size, viz. 100, 10, 1.13, 0.78, 0.61 and 0.25 mm. Decomposition chambers were prepared by adding 1.0 g of plant fragments to 4.1 L of water lagoon. In sequence, the incubations were aerated and the concentrations of dissolved oxygen, the pH, the electric conductivity and the temperature were monitored for 120 days. The occurrence of anaerobic processes was avoided by reoxygenating the solutions. The experimental results were fitted to a first order kinetic model and the consumption of dissolved oxygen from mineralization processes was obtained. The physical process of fragmentation of O. cubense detritus is unlikely to promote the consumption of higher quantities of dissolved oxygen in mineralization processes meaning that fragmentation should not interfere in the balance of DO in this aquatic system, however fragmentation processes favored the acidification and increased the liberation of dissolved ions from the Infernão lagoon.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842006000400008&lng=en&tlng=enmineralizationOxycaryum cubenseaquatic macrophytesdetritus size |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
I. Bianchini Jr. M. B. Cunha-Santino |
spellingShingle |
I. Bianchini Jr. M. B. Cunha-Santino The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) Lye Brazilian Journal of Biology mineralization Oxycaryum cubense aquatic macrophytes detritus size |
author_facet |
I. Bianchini Jr. M. B. Cunha-Santino |
author_sort |
I. Bianchini Jr. |
title |
The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) Lye |
title_short |
The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) Lye |
title_full |
The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) Lye |
title_fullStr |
The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) Lye |
title_full_unstemmed |
The effect of the size of particles on mineralization of Oxycaryum cubense (Poepp. & Kunth) Lye |
title_sort |
effect of the size of particles on mineralization of oxycaryum cubense (poepp. & kunth) lye |
publisher |
Instituto Internacional de Ecologia |
series |
Brazilian Journal of Biology |
issn |
1678-4375 |
description |
Assays were carried out to evaluate effects of detritus size on the mineralization of an aquatic macrophyte, the Oxycaryum cubense. Samples of plant and water were collected from an oxbow lake, the Infernão lagoon (21° 35' S and 47° 51' W) located at Mogi Guaçu river floodplain. The plants were taken to the laboratory, washed under tap water, dried (50 °C) and fractioned into six groups according to their size, viz. 100, 10, 1.13, 0.78, 0.61 and 0.25 mm. Decomposition chambers were prepared by adding 1.0 g of plant fragments to 4.1 L of water lagoon. In sequence, the incubations were aerated and the concentrations of dissolved oxygen, the pH, the electric conductivity and the temperature were monitored for 120 days. The occurrence of anaerobic processes was avoided by reoxygenating the solutions. The experimental results were fitted to a first order kinetic model and the consumption of dissolved oxygen from mineralization processes was obtained. The physical process of fragmentation of O. cubense detritus is unlikely to promote the consumption of higher quantities of dissolved oxygen in mineralization processes meaning that fragmentation should not interfere in the balance of DO in this aquatic system, however fragmentation processes favored the acidification and increased the liberation of dissolved ions from the Infernão lagoon. |
topic |
mineralization Oxycaryum cubense aquatic macrophytes detritus size |
url |
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842006000400008&lng=en&tlng=en |
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