Internal phoshorus loading potential of a semiarid reservoir: an experimental study

Abstract: Aim To determine the internal P loading potential of semiarid tropical reservoir sediment while verifying the driving factors that affect P release rates. Methods An experiment was performed with water and sediment from the reservoir Boqueirão de Parelhas in Brazil. The effects of three variables on P release were studied: air temperature (region average of 28 °C and 32 °C, simulating an increase of 4 °C), pH (region average of pH 8, more acidic pH 6 and more alkaline pH 10) and oxygen (presence and absence). In addition, P fractionation analysis was performed on the P forms in the sediment. Results It was found that the minimum P release was in an oxic treatment at pH 6 and temperature 28 °C (0.22 mg m-2 d-1 ± 0.13) and the maximum P release in an anoxic treatment at pH 10 and temperature 32 °C (2.1 mg m-2 d-1 ± 0.15). The total P in the sediment was 597 mg kg-1, and the major P form in the sediment was NaOH-rP, the P bound to aluminum, corresponding to 42% of the total P. Conclusion These results allow us to confirm that the sediment of the Boqueirão reservoir is susceptible to the release of P bound to aluminum due to the prevalence of this form in its sediments concomitant with the high temperatures and alkaline pH of the water. This scenario can be aggravated by climate change.

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Main Authors: Cavalcante,Hérika, Araújo,Fabiana, Becker,Vanessa, Barbosa,José Etham de Lucena
Format: Digital revista
Language:English
Published: Associação Brasileira de Limnologia 2021
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2179-975X2021000100703
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spelling oai:scielo:S2179-975X20210001007032021-04-22Internal phoshorus loading potential of a semiarid reservoir: an experimental studyCavalcante,HérikaAraújo,FabianaBecker,VanessaBarbosa,José Etham de Lucena eutrophication phosphorus fractionation internal loading temperature increase Abstract: Aim To determine the internal P loading potential of semiarid tropical reservoir sediment while verifying the driving factors that affect P release rates. Methods An experiment was performed with water and sediment from the reservoir Boqueirão de Parelhas in Brazil. The effects of three variables on P release were studied: air temperature (region average of 28 °C and 32 °C, simulating an increase of 4 °C), pH (region average of pH 8, more acidic pH 6 and more alkaline pH 10) and oxygen (presence and absence). In addition, P fractionation analysis was performed on the P forms in the sediment. Results It was found that the minimum P release was in an oxic treatment at pH 6 and temperature 28 °C (0.22 mg m-2 d-1 ± 0.13) and the maximum P release in an anoxic treatment at pH 10 and temperature 32 °C (2.1 mg m-2 d-1 ± 0.15). The total P in the sediment was 597 mg kg-1, and the major P form in the sediment was NaOH-rP, the P bound to aluminum, corresponding to 42% of the total P. Conclusion These results allow us to confirm that the sediment of the Boqueirão reservoir is susceptible to the release of P bound to aluminum due to the prevalence of this form in its sediments concomitant with the high temperatures and alkaline pH of the water. This scenario can be aggravated by climate change.info:eu-repo/semantics/openAccessAssociação Brasileira de LimnologiaActa Limnologica Brasiliensia v.33 20212021-01-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S2179-975X2021000100703en10.1590/s2179-975x10220
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country Brasil
countrycode BR
component Revista
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databasecode rev-scielo-br
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region America del Sur
libraryname SciELO
language English
format Digital
author Cavalcante,Hérika
Araújo,Fabiana
Becker,Vanessa
Barbosa,José Etham de Lucena
spellingShingle Cavalcante,Hérika
Araújo,Fabiana
Becker,Vanessa
Barbosa,José Etham de Lucena
Internal phoshorus loading potential of a semiarid reservoir: an experimental study
author_facet Cavalcante,Hérika
Araújo,Fabiana
Becker,Vanessa
Barbosa,José Etham de Lucena
author_sort Cavalcante,Hérika
title Internal phoshorus loading potential of a semiarid reservoir: an experimental study
title_short Internal phoshorus loading potential of a semiarid reservoir: an experimental study
title_full Internal phoshorus loading potential of a semiarid reservoir: an experimental study
title_fullStr Internal phoshorus loading potential of a semiarid reservoir: an experimental study
title_full_unstemmed Internal phoshorus loading potential of a semiarid reservoir: an experimental study
title_sort internal phoshorus loading potential of a semiarid reservoir: an experimental study
description Abstract: Aim To determine the internal P loading potential of semiarid tropical reservoir sediment while verifying the driving factors that affect P release rates. Methods An experiment was performed with water and sediment from the reservoir Boqueirão de Parelhas in Brazil. The effects of three variables on P release were studied: air temperature (region average of 28 °C and 32 °C, simulating an increase of 4 °C), pH (region average of pH 8, more acidic pH 6 and more alkaline pH 10) and oxygen (presence and absence). In addition, P fractionation analysis was performed on the P forms in the sediment. Results It was found that the minimum P release was in an oxic treatment at pH 6 and temperature 28 °C (0.22 mg m-2 d-1 ± 0.13) and the maximum P release in an anoxic treatment at pH 10 and temperature 32 °C (2.1 mg m-2 d-1 ± 0.15). The total P in the sediment was 597 mg kg-1, and the major P form in the sediment was NaOH-rP, the P bound to aluminum, corresponding to 42% of the total P. Conclusion These results allow us to confirm that the sediment of the Boqueirão reservoir is susceptible to the release of P bound to aluminum due to the prevalence of this form in its sediments concomitant with the high temperatures and alkaline pH of the water. This scenario can be aggravated by climate change.
publisher Associação Brasileira de Limnologia
publishDate 2021
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2179-975X2021000100703
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