2018
DOI: 10.1038/s41561-018-0238-x
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Low buffering capacity and slow recovery of anthropogenic phosphorus pollution in watersheds

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Cited by 113 publications
(70 citation statements)
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References 41 publications
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“…High nutrient loads to streams below WWTP effluent outfalls lead to eutrophication issues, both locally and downstream (Figueroa-Nieves, McDowell, Potter, & Martínez, 2016;Goyette et al, 2018;Haggard et al, 2005;Martí, Aumatell, Gode, Poch, & Sabater, 2004) along with changes to biological communities (Gücker et al, 2006;Price, Ledford, Ryan, Toran, & Sales, 2018;Ribot et al, 2012). A range of impacts of large nutrient loads below WWTP effluent outfalls to nutrient cycling has been observed, requiring more research.…”
Section: Wastewater Treatment Plants As Nutrient Sourcesmentioning
confidence: 99%
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“…High nutrient loads to streams below WWTP effluent outfalls lead to eutrophication issues, both locally and downstream (Figueroa-Nieves, McDowell, Potter, & Martínez, 2016;Goyette et al, 2018;Haggard et al, 2005;Martí, Aumatell, Gode, Poch, & Sabater, 2004) along with changes to biological communities (Gücker et al, 2006;Price, Ledford, Ryan, Toran, & Sales, 2018;Ribot et al, 2012). A range of impacts of large nutrient loads below WWTP effluent outfalls to nutrient cycling has been observed, requiring more research.…”
Section: Wastewater Treatment Plants As Nutrient Sourcesmentioning
confidence: 99%
“…However, the majority of overland runoff is particulate, typically >50% and up to 90% (Withers & Jarvie, 2008). Furthermore, bioavailabilty of sedimentbound P is likely limited and release of accumulated P in sediment could take decades or centuries (Goyette, Bennett, & Maranger, 2018). Both biological uptake and abiotic sorption of SRP occur during baseflow, leading to retention in rivers (Withers & Jarvie, 2008) with rapid SRP uptake in forested streams (Mulholland, Marzolf, Webster, Hart, & Hendricks, 1997).…”
Section: Introductionmentioning
confidence: 99%
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“…In the St. Lawrence Lowlands, runoff accounts for 60% of P transport outside agricultural fields (Beaudet, Beaudin, Michaud, & Giroux, 2008). Goyette, Bennett, and Maranger (2018) showed that legacy P inputs caused a significant acceleration of P loss in runoff from the Quebec agricultural soils. Fertilization decisions should thus avoid elevating or maintaining soil test P above a given threshold (Bergström et al, 2015;Fulford & Culman, 2018;Pellerin et al, 2006aPellerin et al, , 2006b).…”
Section: Environmental Benefitsmentioning
confidence: 99%
“…Due to the inherent lithophilic properties of P (i.e., P is subject to sorption or coprecipitation), excess P has a propensity to accumulate in soils and sediments Chen et al 2018). The accumulated P increases P transfers along the land-freshwater continuum, causing a considerable lag time between anthropogenic P inputs and P delivery to surface waters (Kleinman et al 2011;Goyette et al 2018). For example, global P accumulated in croplands was 815 Tg P between 1965 and 2007 (Sattari et al 2012), which was * 40-fold higher than applied P fertilizer in 2012 (20.3 Tg P year -1 ).…”
Section: Introductionmentioning
confidence: 99%