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EXPLORING THE INFLUENCE OF DISSOLVED ORGANIC MATTER ON PHOSPHORUS MOBILITY IN GROUNDWATER

机译:探讨溶解有机物对地下水磷迁移率的影响

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Phosphorus (P) concentrations in the shallow, unconfined aquifer at Pineview Reservoir, Utah indicate increased phosphorus transport is occurring in groundwater. Because of known septic system influence in shallow groundwater, a set of sorption experiments was completed to determine whether the presence of dissolved organic matter (DOM) influences P sorption and increases P mobility. A P only and a P + DOM isotherm were completed for two types of aquifer sediments. Initial P concentrations of 0, 1, 2, 5, 7, and 10 mg PO4-P/L were chosen to simulate environmentally relevant conditions. For the P + DOM isotherm, 15 mg C/L was spiked into the DOM artificial groundwater solution.
机译:PineView储层浅不合适的含水层中的磷(P)浓度,犹他州表明地下水中发生了增加的磷输送。由于浅地下水中已知的化粪池系统影响,完成了一组吸附实验以确定溶解有机物(DOM)是否存在影响P吸附并增加P流动性。仅为两种类型的含水层沉积物完成了P仅和P + DOM等温线。选择初始P浓度为0,1,2,5,7和10mgPO4-P / L以模拟环境相关的条件。对于P + DOM等温线,将15mg C / L掺入DOM人造地下水溶液中。

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