Mechtensimer Sara, Toor Gurpal S
Soil and Water Quality Laboratory, Gulf Coast Research and Education Center, University of Florida, Institute of Food and Agricultural Sciences, 14625 CR 672, Wimauma, FL 33598, USA.
Soil and Water Quality Laboratory, Gulf Coast Research and Education Center, University of Florida, Institute of Food and Agricultural Sciences, 14625 CR 672, Wimauma, FL 33598, USA.
Chemosphere. 2016 Sep;159:153-158. doi: 10.1016/j.chemosphere.2016.05.084. Epub 2016 Jun 9.
Septic systems can be a potential source of phosphorus (P) in shallow groundwater. Our objective was to investigate the fate, mass balance, and transport of P in the drainfield of a drip-dispersal septic system. Drainfields were replicated in lysimeters (152.4 cm long, 91.4 cm wide, and 91.4 cm high). Leachate and effluent samples were collected over 67 events (n = 15 daily; n = 52 weekly flow-weighted) and analyzed for total P (TP), orthophosphate (PO4P), and other P (TP - PO4P). Mean TP was 15 mg L(-1) (84% PO4P; 16% other P) in the effluent and 0.16 mg L(-1) (47% PO4P, 53% other P) in the leachate. After one year, 46.8 g of TP was added with effluent and rainfall to each drainfield, of which, <1% leached, 3.8% was taken up by St. Augustine grass, leaving >95% in the drainfield. Effluent dispersal increased water extractable P (WEP) in the drainfield from <5 to >10 mg kg(-1). Using the P sorption maxima of sand (118 mg kg(-1)) and soil (260 mg kg(-1)), we estimated that ∼18% of the drainfield P sorption capacity was saturated after one year of effluent dispersal. We conclude that despite the low leaching potential of P dispersed with effluent in the first year of drainfield operation, a growing WEP pool in the drainfield and low P sorption capacity of Florida's sandy soils may have the potential to transport P to shallow groundwater in long-running septic systems.
化粪池系统可能是浅层地下水中磷(P)的一个潜在来源。我们的目标是研究滴灌式化粪池系统排水区中磷的归宿、质量平衡和迁移。在渗漏测定仪(长152.4厘米、宽91.4厘米、高91.4厘米)中复制排水区。在67次事件中(每天15次;每周52次流量加权)采集渗滤液和流出液样本,并分析总磷(TP)、正磷酸盐(PO4P)和其他磷(TP - PO4P)。流出液中的平均总磷为15毫克/升(84%为PO4P;16%为其他磷),渗滤液中的平均总磷为0.16毫克/升(47%为PO4P,53%为其他磷)。一年后,每个排水区通过流出液和降雨添加了46.8克总磷,其中<1%被淋溶,3.8%被圣奥古斯丁草吸收,>95%留在排水区。流出液的分散使排水区中可被水提取的磷(WEP)从<5毫克/千克增加到>10毫克/千克。利用沙子(118毫克/千克)和土壤(260毫克/千克)的最大磷吸附量,我们估计在流出液分散一年后约18%的排水区磷吸附能力被饱和。我们得出结论,尽管在排水区运行的第一年,随流出液分散的磷淋溶潜力较低,但排水区中不断增加的WEP库以及佛罗里达州沙质土壤较低的磷吸附能力,可能会使长期运行的化粪池系统中的磷有向浅层地下水迁移的潜力。