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Residential catchments to coastal waters: Forms, fluxes, and mechanisms of phosphorus transport

机译:沿海水域的住宅集水区:磷运输的形式,助核和机制

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Controlling phosphorus (P) loss from land to water bodies is of immense scientific and societal interest and scrutiny. We investigated P forms in a longitudinal gradient in three typical urban junctions: stormwater from a residential catchment, pond discharges from a stormwater retention pond, and 13 coastal waters (rivers and estuary). Concentrations of total P (TP) were 122.7 ± 99.1 μg/L in the stormwater, 89.7 ± 35.8 μg/L in the pond discharges, and 212.1 ± 51.2 μg/L in 13 coastal water sites. Lower P concentrations in pond discharges reflect P attenuation in the stormwater pond, and higher P concentrations in surface waters are likely attributed to the additional contributing P sources in the watershed. Dissolved reactive P (DRP) was 38% of TP load in stormwater and 46% of TP concentrations in surface water sites, whereas particulate unreactive P (PUP) was 52% of TP load in pond discharges. The first-flush strength of P forms in the stormwater indicated the dominance of particulate P over dissolved P. More particulate P was transported in the early stages of storms due to the runoff of P associated with sediment, plant materials, and built up on impervious surfaces. Whereas more dissolved P was transported in the later stages of storms likely due to the flushing of P, as exacerbated by greater runoff amounts, from the landscape sources, i.e., grass clippings, tree leaves, and soil. In the pond discharges, DRP was a minor form suggesting its utilization by bacteria and algae in the pond. The high concentration and proportion of DRP in surface waters suggest an abundance of bioavailable P in urban waters. These results imply that treatment designs in urban areas should consider ways to remove P in urban landscapes focusing on attenuating P before the initiation of runoff and discharge to surface waters to protect downstream water quality.
机译:控制磷(P)从土地到水体的损失是巨大的科学和社会兴趣和审查。我们在三个典型的城市连接中调查了P表格:来自住宅集水区的雨水,从雨水保留池塘和13个沿海水域(河流和河口)排出。在雨水中,总P(TP)的浓度为122.7±99.1μg/ L,池塘排放中的89.7±35.8μg/ l,13个沿海水位的212.1±51.2μg/ l。池塘中的较低P浓度反映了雨水池中的P衰减,表面水域中的较高的P浓度可能归因于流域中的其他有助于P源。溶解的反应性P(DRP)为雨水中TP载荷的38%,在地表水位中的TP浓度的46%浓度,而颗粒无反应P(PUP)为池塘排放中的TP载荷的52%。雨水中P形状的第一冲洗强度表明,由于与沉积物,植物材料相关的P的径流,在暴风雨的早期阶段运输颗粒状P溶解的P.颗粒状P的优势。表面。然而,在可能由于P的潮流,从横向源,即草夹,树叶和土壤中加剧,而是由于P的较高径流而在暴风雨的后续阶段被运输。在池塘排放中,DRP是一种轻微的形式,表明它在池塘中的细菌和藻类的利用。表面水域中DRP的高浓度和比例表明了城市水域中的丰富生物可利用的P.这些结果意味着城市地区的治疗设计应考虑在城市景观中删除P的方法,这些景观专注于在径流和放电到地表水中进行衰减,以保护下游水质。

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