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Development of temporary subtropical wetlands induces higher gas production

Temporary wetlands are short-term alternative ecosystems formed by flooding for irrigation of areas used for rice farming. The goal of this study is to describe the development cycle of rice fields as temporary wetlands in southern Brazil, evaluating how this process affect the gas production (CH(4)...

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Detalles Bibliográficos
Autores principales: Canterle, Eliete B., da Motta Marques, David, Rodrigues, Lúcia R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2013
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3597979/
https://www.ncbi.nlm.nih.gov/pubmed/23508352
http://dx.doi.org/10.3389/fmicb.2013.00056
Descripción
Sumario:Temporary wetlands are short-term alternative ecosystems formed by flooding for irrigation of areas used for rice farming. The goal of this study is to describe the development cycle of rice fields as temporary wetlands in southern Brazil, evaluating how this process affect the gas production (CH(4) and CO(2)) in soil with difference % carbon and organic matter content. Two areas adjacent to Lake Mangueira in southern Brazil were used during a rice-farming cycle. One area had soil containing 1.1% carbon and 2.4% organic matter, and the second area had soil with 2.4% carbon and 4.4% organic matter. The mean rates of gas production were 0.04 ± 0.02 mg CH(4) m(−2) d(−1) and 1.18 ± 0.30 mg CO(2) m(−2) d(−1) in the soil area with the lower carbon content, and 0.02 ± 0.03 mg CH(4) m(−2) d(−1) and 1.38 ± 0.41 mg CO(2) m(−2) d(−1) in the soil area with higher carbon content. Our results showed that mean rates of CO(2) production were higher than those of CH(4) in both areas. No statistically significant difference was observed for production of CH(4) considering different periods and sites. For carbon dioxide (CO(2)), however, a Two-Way ANOVA showed statistically significant difference (p = 0.05) considering sampling time, but no difference between areas. The results obtained suggest that the carbon and organic matter contents in the soil of irrigated rice cultivation areas may have been used in different ways by soil microorganisms, leading to variations in CH(4) and CO(2) production.