Carbon dioxide emissions from Tucurui reservoir (Amazon biome): New findings based on three-dimensional ecological model simulations
We used a three-dimensional model to assess the dynamics of diffusive carbon dioxide flux (F-CO2) from a hydroelectric reservoir located at Amazon rainforest. Our results showed that for the studied periods (2013 summer/wet and winter/dry seasons) the surface averaged F-CO2 presented similar behavio...
| Autores: | , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2016 |
| País: | Brasil |
| Institución: | Universidade Estadual Paulista (UNESP) |
| Repositorio: | Repositório Institucional da UNESP |
| Idioma: | inglés |
| OAI Identifier: | oai:repositorio.unesp.br:11449/161342 |
| Acceso en línea: | http://dx.doi.org/10.1016/j.scitotenv.2016.02.001 http://hdl.handle.net/11449/161342 |
| Access Level: | acceso abierto |
| Palabra clave: | Numerical modeling Greenhouse gases emission Carbon dioxide Hydroelectric reservoirs Amazon biome |
| Sumario: | We used a three-dimensional model to assess the dynamics of diffusive carbon dioxide flux (F-CO2) from a hydroelectric reservoir located at Amazon rainforest. Our results showed that for the studied periods (2013 summer/wet and winter/dry seasons) the surface averaged F-CO2 presented similar behaviors, with regular emissions peaks. The mean daily surface averaged F-CO2 showed no significant difference between the seasons (p > 0.01), with values around - 1338 mg C m - 2 day - 1 (summer/wet) and - 1395 mg C m - 2 day - 1 (winter/dry). At diel scale, the F-CO2 was large during the night and morning and low during the afternoon in both seasons. Regarding its spatial distribution, the F-CO2 showed to be more heterogeneous during the summer/wet than during the winter/dry season. The highest F-CO2 were observed at transition zone (-300 mg C m - 2 h - 1) during summer and at littoral zone (-55 mg C m - 2 h - 1) during the winter. The total CO2 emitted by the reservoir along 2013 year was estimated to be 1.1 Tg C year - 1. By extrapolating our results we found that the total carbon emitted by all Amazonian reservoirs can be around 7 Tg C year - 1, which is 22% lower than the previous published estimate. This significant difference should not be neglected in the carbon inventories since the carbon emission is a key factor when comparing the environmental impacts of different sources of electricity generation and can influences decision makers in the selection of the more appropriate source of electricity and, in case of hydroelectricity, the geographical position of the reservoirs. (C) 2016 Elsevier B.V. All rights reserved. |
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