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Master's Dissertation
DOI
https://doi.org/10.11606/D.18.1998.tde-12062024-091601
Document
Author
Full name
Luiz Fernando Charbel
Institute/School/College
Knowledge Area
Date of Defense
Published
São Carlos, 1998
Supervisor
Committee
Sikar, Bohdan Matvienko (President)
Bianchini Junior, Irineu
Krusche, Alex Vladimir
Title in Portuguese
Contribuições para o balanço de massa do carbono no reservatório do Broa, Itirapina - SP
Keywords in Portuguese
.
Abstract in Portuguese
O balanço de carbono do Broa, foi realizado considerando-o como um sistema "caixa preta", no qual foram considerados apenas os compartimentos de entradas e saídas. As entredas de carbono foram quantificadas, periodicamente, nos compartimentos;afluentes, lençol freático e interface atmosfera-água, contribuindo com 19,93%, 17,38% e 24,05%, respectivamente. Também considerou-se como entrada, as macrófitas do reservatório, contribuindo com: 38,64%. As saídas foram quantificadas noscompartimentos: efluente, sedimento e interface atmosfera-água, contribuindo com 20,04%, 76,94% e 3,02%, respectivamente. Neste trabalho foi desenvolvido um método para determinação da taxa de sedimentação do carbono, usando-se a sílica comotraçador. Como resultado final, obteve-se para entrada de carbono no reservatório o valor de '376,12 mgC.m POT.-2 .d POT.' e para saída, '614,42 mgC.m POT.-2 .d.POT.-1'. Teoricamente, o valor para o balanço deveria ser zero, por se tratar de umacaixa preta imutável. No entanto, obteve-se um saldo negativo de '-238,30 mgC.m POT.-2 .d POT.-1'
Title in English
.
Keywords in English
.
Abstract in English
The carbon budget of Broa reservoir, was established in a "black-box" treatment, in which only the compartments of input and output were considered. Carbons inputs were quantified perodically in the compartments: stream inflow, groundwater and atmosphere-water interface, contributing with 19,93%, 17,38% and 24,05%, respectively. Macrophytes of the reservoir were also tireated as an entry contributing with 38,64%. The outputs were quantified in the compartments: stream outflow, sediment and atmosphere-water interface, contributming with 20,04%, 76,94% and 3,02%, respectively. In this work a method was developed to detemúne the carbon sedúnentation rate, using sílica as a tracer. As a fínal input result 376,12 mg.Cm .d were obtained and for the output 614,42 mg.Cm-2.d-1. Theoretically, the value of the balance should be zero, because an unchangeable "black box" was assumed. In stead of a null balance a deficit of-238,30 mg.Cm-2.d-1 was obtained.
 
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Publishing Date
2024-06-12
 
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