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温带城市化河口反硝化和一氧化二氮产生的潜在速率和环境控制。

Potential rates and environmental controls of denitrification and nitrous oxide production in a temperate urbanized estuary.

机构信息

Institute of Biomedical Sciences (ICBAS), University of Porto, Laboratory of Hydrobiology, Largo Prof. Abel Salazar 2, 4009-003 Porto, Portugal.

出版信息

Mar Environ Res. 2010 Dec;70(5):336-42. doi: 10.1016/j.marenvres.2010.07.001. Epub 2010 Jul 17.

Abstract

Denitrification may play a major role in inorganic nitrogen removal from estuarine ecosystems, particularly in those subjected to increased nitrate and organic matter loads. The Douro estuary (NW Portugal) suffers from both problems: freshwater input of nitrate and organic load from untreated wastewater discharges. To assess how these factors might control sediment denitrification, a 12-month survey was designed. Denitrification potential and nitrous oxide (N(2)O) production were measured at different locations using the slurry acetylene blockage technique. Denitrification rate ranged from 0.4 to 38 nmol N g⁻¹ h⁻¹, increasing towards the river mouth following an urban pollution gradient. N(2)O production, a powerful greenhouse gas implicated on the destruction of the ozone layer, was significantly related with sediment organic matter and accounted for 0.5-47% of the N gases produced. Additional enrichment experiments were consistent with the results found in the environment, showing that sediments from the upper less urban stretch of the estuary, mostly sandy, respond positively to carbon and, inversely, in organic rich sediments from the lower estuary, the denitrification potential was limited by nitrate availability. The obtained results confirmed denitrification as an important process for the removal of nitrate in estuaries. The presence of wastewater discharges appears to stimulate nitrogen removal but also the production of N(2)O, a powerful greenhouse gas, exacerbating the N(2)O:N(2) ratio and thus should be controlled.

摘要

反硝化作用可能在河口生态系统中无机氮的去除中起着重要作用,特别是在那些受到硝酸盐和有机负荷增加的影响的生态系统中。杜罗河口(葡萄牙西北部)同时存在这两个问题:淡水输入硝酸盐和未经处理的污水排放的有机负荷。为了评估这些因素如何控制沉积物反硝化作用,设计了一项为期 12 个月的调查。使用浆态乙炔阻断技术在不同地点测量了反硝化潜力和氧化亚氮(N 2 O)的产生。反硝化速率范围从 0.4 到 38 nmol N g ⁻¹ h ⁻¹ ,沿河口向河流口方向逐渐增加,遵循城市污染梯度。氧化亚氮(N 2 O)是一种强大的温室气体,被认为是破坏臭氧层的原因之一,它与沉积物中的有机物质有显著的相关性,占产生的 N 气体的 0.5-47%。额外的富集实验与环境中的结果一致,表明来自河口上游污染较少的沙质沉积物的沉积物对碳有积极的响应,而在河口下游富含有机质的沉积物中,反硝化潜力受到硝酸盐供应的限制。所得结果证实了反硝化作用是河口去除硝酸盐的重要过程。污水排放的存在似乎刺激了氮的去除,但也刺激了 N 2 O 的产生,N 2 O 是一种强大的温室气体,加剧了 N 2 O:N 2 的比例,因此应该加以控制。

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