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Development of temporary subtropical wetlands induces higher gas production

机译:亚热带临时湿地的发展导致天然气产量增加

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摘要

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 (CH4 and CO2) 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 CH4 m−2 d−1 and 1.18 ± 0.30 mg CO2 m−2 d−1 in the soil area with the lower carbon content, and 0.02 ± 0.03 mg CH4 m−2 d−1 and 1.38 ± 0.41 mg CO2 m−2 d−1 in the soil area with higher carbon content. Our results showed that mean rates of CO2 production were higher than those of CH4 in both areas. No statistically significant difference was observed for production of CH4 considering different periods and sites. For carbon dioxide (CO2), 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 CH4 and CO2 production.
机译:临时湿地是通过洪水灌溉水稻种植区而形成的短期替代生态系统。这项研究的目的是描述巴西南部作为临时湿地的稻田的发展周期,评估该过程如何影响碳和有机物含量不同的土壤中的气体产量(CH4和CO2)。在水稻种植周期中使用了巴西南部曼格伊拉湖附近的两个地区。一个地区的土壤含碳量为1.1%,有机质为2.4%,第二个地区的土壤含碳量为2.4%,有机质为4.4%。平均产气速率为0.04±0.02 mg CH4 m −2 d -1 和1.18±0.30 mg CO2 m −2 d <碳含量较低的土壤区域中的sup> -1 ,以及0.02±0.03 mg CH4 m −2 d -1 和1.38±0.41 mg CO2碳含量较高的土壤区域中的m −2 d −1 。我们的结果表明,两个地区的平均CO2产生率均高于CH4。考虑到不同的时期和地点,CH4的生产没有观察到统计学上的显着差异。但是,对于二氧化碳(CO2),考虑到采样时间,双向方差分析显示出统计学上的显着差异(p = 0.05),但区域之间没有差异。所得结果表明,土壤微生物可能以不同的方式利用了水稻种植灌溉区土壤中的碳和有机质,从而导致CH4和CO2的产生变化。

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