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

被引:96
|
作者
Emelko, Monica B. [1 ]
Stone, Micheal [2 ]
Silins, Uldis [3 ]
Allin, Don [2 ]
Collins, Adrian L. [4 ]
Williams, Chris H. S. [3 ]
Martens, Amanda M. [3 ]
Bladon, Kevin D. [5 ]
机构
[1] Univ Waterloo, Dept Civil & Environm Engn, Waterloo, ON N2L 3G1, Canada
[2] Univ Waterloo, Dept Geog & Environm Management, Waterloo, ON N2L 3G1, Canada
[3] Univ Alberta, Dept Renewable Resources, Edmonton, AB T6G 2H1, Canada
[4] Rothamsted Res, Sustainable Soils & Grassland Syst Dept, Wyke EX20 2SB, Okehampton, England
[5] Oregon State Univ, Dept Forest Engn Resources & Management, Corvallis, OR 97331 USA
基金
加拿大自然科学与工程研究理事会;
关键词
climate change; cumulative watershed; effects; eutrophication; land disturbance; phosphorus; sediment; treatability; wildfire; FLUVIAL SUSPENDED SEDIMENT; FINE-GRAINED SEDIMENT; PARTICULATE PHOSPHORUS; LAKE-ERIE; FIRE; TRANSPORT; PHOSPHATE; NITROGEN; STREAM; FOREST;
D O I
10.1111/gcb.13073
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
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 (<125m) were sampled continuously during ice-free conditions over a two-year period (2009-2010), 6 and 7years 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 7years 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.
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页码:1168 / 1184
页数:17
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