Abstract
The construction of dams can increase the emission of greenhouse gases (GHG), mainly methane (CH4) by the anaerobic decomposition of forest residues like twigs, branches, leaves and miscellaneous flooded. The aim of this study was to evaluate the emission of CH4 after the flooding of soil covered with residuals of forests. Experimental units were built with PVC tubes containing soil covered with different combinations of dose (0; 21.2; 42.3 and 64.1 Mg ha-1) and type (branches, leaves and miscellaneous; twigs; and original composition) of forest residues and river water. The experimental design was completely randomized with factorial arrangement and three replications. Rates of CH4 emission were monitored in 19 events during one year (February/2012 to March/2013). Approximately, 75 days after incubation of soil with residue, a significant increase in CH4 emission was observed occurring two emission peaks: at 111 and 249 days. The cumulative emission of CH4 in the first year after flooding was 200 g C m-2 in the dose zero, until above 400 g C m-2 in the 21.2 Mg ha-1 and higher doses, with no effect of type of residues, only the dose as an isolated factor.
Highlights
The construction of dams can increase the emission of greenhouse gases
The aim of this study was to evaluate the emission of CH4 after the flooding
of soil covered with residuals of forests
Summary
Palavras-chave: solo alagado fitomassa decomposição anaeróbica metanogênese gases do efeito estufa. RESUMOA construção de represas pode aumentar a emissão de gases do efeito estufa (GEE), principalmente metano (CH4) pela decomposição anaeróbica dos resíduos florestais, como galhos, ramos, folhas e miscelânea inundados. Unidades experimentais foram construídas com tubos de PVC contendo solo e diferentes combinações de dose (0; 21,2; 42,3 e 64,1 Mg ha-1) e tipo de resíduos (folhas, ramos e miscelânea, galhos e composição original) e água de rio. A emissão acumulada de CH4 no primeiro ano de alagamento foi de 200 g C m-2 na dose zero, passando a valores próximos a 400 g C m-2 nas doses de 21,2 Mg ha-1 e maiores, não havendo efeito do tipo de resíduo, apenas da dose, como fator isolado
Full Text
Topics from this Paper
Rates Of CH4 Emission
Increase In CH4 Emission
Incubation Of Soil
CH4 Emission
Type Of Residues
+ Show 5 more
Create a personalized feed of these topics
Get StartedTalk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Similar Papers
Journal of Geophysical Research: Atmospheres
Nov 20, 1989
Soil Science and Plant Nutrition
Jan 2, 2020
Soil Science and Plant Nutrition
Mar 4, 2014
Atmosphere
Feb 6, 2021
Plant and Soil
Apr 24, 2009
Atmospheric Chemistry and Physics
Jul 28, 2023
Wetlands
Jan 23, 2017
Atmospheric Environment
Jan 1, 2015
Plant and Soil
May 8, 2019
Global Biogeochemical Cycles
Sep 1, 2001
Journal of Environmental Protection
Jan 1, 2011
Water Research
Aug 1, 2022
Atmospheric Chemistry and Physics
Jul 10, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Dec 1, 2023
Revista Brasileira de Engenharia Agrícola e Ambiental
Nov 1, 2023