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泥沙-磷动态变化可能会改变大型河流系统中的水生态,并在野火后造成下游的遗留效应。

Sediment-phosphorus dynamics can shift aquatic ecology and cause downstream legacy effects after wildfire in large river systems.

机构信息

Department of Civil and Environmental Engineering, University of Waterloo, Waterloo, ON, N2L 3G1, Canada.

Department of Geography and Environmental Management, University of Waterloo, Waterloo, ON, N2L 3G1, Canada.

出版信息

Glob Chang Biol. 2016 Mar;22(3):1168-84. doi: 10.1111/gcb.13073. Epub 2015 Dec 26.

Abstract

Global increases in the occurrence of large, severe wildfires in forested watersheds threaten drinking water supplies and aquatic ecology. Wildfire effects on water quality, particularly nutrient levels and forms, can be significant. The longevity and downstream propagation of these effects as well as the geochemical mechanisms regulating them remain largely undocumented at larger river basin scales. Here, phosphorus (P) speciation and sorption behavior of suspended sediment were examined in two river basins impacted by a severe wildfire in southern Alberta, Canada. Fine-grained suspended sediments (<125 μm) were sampled continuously during ice-free conditions over a two-year period (2009-2010), 6 and 7 years after the wildfire. Suspended sediment samples were collected from upstream reference (unburned) river reaches, multiple tributaries within the burned areas, and from reaches downstream of the burned areas, in the Crowsnest and Castle River basins. Total particulate phosphorus (TPP) and particulate phosphorus forms (nonapatite inorganic P, apatite P, organic P), and the equilibrium phosphorus concentration (EPC0 ) of suspended sediment were assessed. Concentrations of TPP and the EPC0 were significantly higher downstream of wildfire-impacted areas compared to reference (unburned) upstream river reaches. Sediments from the burned tributary inputs contained higher levels of bioavailable particulate P (NAIP) - these effects were also observed downstream at larger river basin scales. The release of bioavailable P from postfire, P-enriched fine sediment is a key mechanism causing these effects in gravel-bed rivers at larger basin scales. Wildfire-associated increases in NAIP and the EPC0 persisted 6 and 7 years after wildfire. Accordingly, this work demonstrated that fine sediment in gravel-bed rivers is a significant, long-term source of in-stream bioavailable P that contributes to a legacy of wildfire impacts on downstream water quality, aquatic ecology, and drinking water treatability.

摘要

全球范围内,森林流域中大型、剧烈野火的发生频次增加,威胁着饮用水供应和水生生态系统。野火对水质的影响,特别是营养物水平和形态,可能非常显著。这些影响的持续时间和下游传播,以及调节这些影响的地球化学机制,在较大的河流流域尺度上,在很大程度上仍未被记录。在此,我们研究了加拿大艾伯塔省南部剧烈野火影响的两个流域中,磷(P)的形态和悬浮泥沙的吸附行为。在两年(2009-2010 年)无冰期内,连续采集了细粒悬浮泥沙(<125μm),并在野火发生后 6 年和 7 年采集了这些样本。悬浮泥沙样品分别来自上游参考(未燃烧)河段、燃烧区多个支流以及燃烧区下游河段,这些样品取自克罗斯内斯特和卡斯尔河流域。我们评估了总颗粒磷(TPP)和颗粒磷形态(非磷灰石无机磷、磷灰石磷、有机磷)以及悬浮泥沙的平衡磷浓度(EPC0)。与上游参考(未燃烧)河段相比,野火影响区下游的 TPP 和 EPC0 浓度显著更高。来自燃烧支流输入的泥沙含有更高水平的生物可利用颗粒磷(NAIP)——这些影响在更大的河流流域尺度上也在下游观察到。火后富含 P 的细颗粒泥沙中释放的生物可利用 P 是导致砾石床河流在更大流域尺度上产生这些影响的关键机制。野火后 6 年和 7 年,NAIP 和 EPC0 仍持续增加。因此,这项工作表明,砾石床河流中的细颗粒泥沙是河流中生物可利用 P 的重要、长期来源,这会对下游水质、水生生态系统和饮用水处理能力产生野火影响的遗留问题。

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