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Nutrient Retention Performance of Advanced Bioretention Systems Results from Three Years of Mesocosm Studies

机译:先进的生物保留系统的营养保留性能来自三年的中观研究结果

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Current bioretention designs are not very effective at nutrient retention for a variety of reasons. Negatively charged organic amendments compete for the few phosphorus (P) binding sites available in the sand matrix. The rapid rate of flow through the systems does not permit enough time for effective nitrogen (N) retention to occur. To improve bioretention designs for nutrient retention, it is necessary to understand the processes involved in nutrient transformations. Given this understanding, it is then possible to develop approaches that improve nutrient retentions. Our mesocosm studies have shown that advances in bioretention system design substantially improve retention of N and P from runoff. Using advanced media, our research over three years has confirmed our initial findings on P retention trends. After accumulating 190 g-m~2 P (the equivalent of nearly five decades of stormwater runoff), the advanced media had a median TP discharge concentration of 0.077 mg/1. The median Ortho-phosphate discharge concentration was 0.015 mg/1. N retention by the outlet regulated treatment was 66% in even quite large (~6 month ARI) events, and 62% for oxides of N. The corresponding free discharge treatment was significantly less effective, at 27% and 19% retention respectively. A year later, total N retention in small storm events exceeded 70%, while nitrate retention exceeded 90%. These results confirm how advanced media combined with outlet controls substantially raise the bar for treating runoff nutrients. This is become ever more important with the adoption of strict numeric criteria in TMDLs in affected waterbodies throughout the US.
机译:由于多种原因,当前的生物保留设计在营养保留方面不是很有效。带负电荷的有机改性剂争夺砂基质中可用的少量磷(P)结合位点。通过系统的快速流速无法为有效的氮(N)保留留出足够的时间。为了改善用于养分保留的生物保留设计,有必要了解养分转化所涉及的过程。有了这种了解,便有可能开发出改善养分保留的方法。我们的中观研究表明,生物滞留系统设计的进步大大提高了径流中氮和磷的保留能力。使用先进的媒体,我们三年来的研究证实了我们对磷保留趋势的初步发现。在积累了190 g-m〜2 P(相当于近五十年的雨水径流)之后,高级培养基的TP排放中位数浓度为0.077 mg / 1。正磷酸盐排放浓度的中位数为0.015 mg / 1。即使在相当大的事件(约6个月ARI)中,出口调节处理的氮保留量也为66%,氮氧化物的保留率为62%。相应的自由放电处理效果明显较差,分别为27%和19%。一年后,小风暴事件中的总氮保留量超过70%,而硝酸盐保留量超过90%。这些结果证实了先进的培养基与出口控制相结合如何显着提高了处理径流养分的标准。在整个美国受影响的水体中,通过在TMDL中采用严格的数字标准,这一点变得越来越重要。

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