快速入渗点的地下水水质

James V. Olson, P. E. Levine, R. Crites
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引用次数: 2

摘要

对30年快速入渗地下12个月的水质进行了研究。该系统接收初级污水,并通过土地处理过程将其处理到非常高的质量。经过处理的水流穿过10米到20米的渗透性砂,然后横向流出场地。这种浅层地下水不用作供水,也不影响更深的、独立的含水层。BOD和TOC去除率达96%。由于BOD / n比值较高,负荷率相对较低(15.4 m/yr),且气候温和,土壤中的氮通过硝化和反硝化作用被去除。平均氮去除率为93%。磷去除率为30%。微量元素的去除率各不相同,但浅层地下水位一般低于无限制灌溉的标准。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ground-Water Quality at Rapid Infiltration Site
The ground water quality beneath a 30-yr old rapid infiltration was studied over a 12-month period. The system receives primary effluent and treats it to a very high quality through the land treatment process. The flow of treated water passes through 10 m to 20 m of permeable sands and then moves laterally off the site. This shallow ground water is not used as a water supply and does not affect the deeper, separate aquifers. A 96% BOD and TOC removal was achieved. Because of the high BOD to nitrogen ratio, the relatively low loading rate of 15.4 m/yr, and the moderate climate, nitrogen was removed by nitrification and denitrification in the soil. The average nitrogen removal was 93%. Phosphorus removal was 30%. Trace element removal varied, but shallow ground-water levels were generally lower than guidelines established for unrestricted irrigation.
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