University of Birmingham , School of Geography, Earth and Environmental Sciences , Edgbaston, Birmingham B15 2TT , United Kingdom.
Environ Sci Technol. 2019 Mar 5;53(5):2364-2374. doi: 10.1021/acs.est.8b04243. Epub 2019 Feb 15.
Greenhouse gas (GHG) emissions of carbon dioxide (CO) and methane (CH) from streambeds are currently understudied. There is a paucity of research exploring organic matter (OM) controls on GHG production by microbial metabolic activity in streambeds, which is a major knowledge gap given the increased inputs of allochthonous carbon to streams, especially in agricultural catchments. This study aims to contribute to closing this knowledge gap by quantifying how contrasting OM contents in different sediments affect streambed GHG production and associated microbial metabolic activity. We demonstrate, by means of an incubation experiment, that streambed sediments have the potential to produce substantial amounts of GHG, controlled by sediment OM quantity and quality. We observed streambed CO production rates that can account for 35% of total stream evasion estimated in previous studies, ranging between 1.4 and 86% under optimal conditions. Methane production varied stronger than CO between different geologic backgrounds, suggesting OM quality controls between streambed sediments. Moreover, our results indicate that streambed sediments may produce much more CO than quantified to date, depending on the quantity and quality of the organic matter, which has direct implications for global estimates of C fluxes in stream ecosystems.
温室气体(GHG)排放的二氧化碳(CO)和甲烷(CH)从河床目前研究不足。有一个缺乏研究探索有机物质(OM)对温室气体生产的微生物代谢活动在河床中的控制,这是一个主要的知识差距,因为所有的异源碳的输入增加到溪流,特别是在农业流域。本研究旨在通过量化不同沉积物中不同 OM 含量如何影响河床 GHG 产量和相关微生物代谢活性来填补这一知识空白。我们通过一项培养实验证明,河床沉积物具有产生大量温室气体的潜力,受沉积物 OM 数量和质量的控制。我们观察到河床 CO 产生率可占先前研究中估计的总溪流逸出量的 35%,在最佳条件下范围为 1.4%至 86%。甲烷的产生比 CO 在不同地质背景下变化更大,这表明河床沉积物之间的 OM 质量控制。此外,我们的结果表明,河床沉积物可能产生比目前定量更多的 CO,这取决于有机物质的数量和质量,这对溪流生态系统中 C 通量的全球估计有直接影响。