4.7 Article

Influence of colloids on the attenuation and transport of phosphorus in alluvial gravel aquifer and vadose zone media

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 550, Issue -, Pages 60-68

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2016.01.075

Keywords

Phosphorus; Colloids; Groundwater; Alluvial gravel; Adsorption; Transport

Funding

  1. New Zealand Ministry of Business, Innovation Employment [C03X1001]
  2. German Academic Exchange Service
  3. New Zealand Ministry of Business, Innovation & Employment (MBIE) [C03X1001] Funding Source: New Zealand Ministry of Business, Innovation & Employment (MBIE)

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Phosphorous (P) leaching (e.g., from effluents, fertilizers) and transport in highly permeable subsurface media can be an important pathway that contributes to eutrophication of receiving surface waters as groundwater recharges the base -flow of surface waters. Here we investigated attenuation and transport of orthophosphate -P in gravel aquifer and vadose zone media in the presence and absence of model colloids (Escherichia coli, kaolinite, goethite). Experiments were conducted using repacked aquifer media in a large column (2 m long, 0.19 m in diameter) and intact cores (0.4 m long, 024 m in diameter) of vadose zone media under typical field flow rates. In the absence of the model colloids, P was readily traveled through the aquifer media with little attenuation (up to 100% recovery) and retardation, and P adsorption was highly reversible. Conversely, addition of the model colloids generally resulted in reduced P concentration and mass recovery (clown to 28% recovery), and increased retardation and adsorption irreversibility in both aquifer and vaclose zone media. The degree of P attenuation was most significant in the presence of line material and Fe -containing colloids at low flow rate but was least significant in the presence of coarse gravels and E. col( at high flow rate. Based on the experimental results, setback distances of 49-53 m were estimated to allow a reduction of P concentrations in groundwater to acceptable levels in the receiving water. These estimates were consistent with field observations in the same aquifer media. Colloid -assisted P attenuation can be utilized to develop mitigation strategies to better manage effluent applications in gravelly soils. To efficiently retain P within soil matrix and reduce P leaching to groundwater, it is recommended to select soils that are rich in iron oxides, to periodically disturb soil preferential flow paths by tillage, and to apply a low irrigation rate. (C) 2016 Elsevier B.V. All rights reserved.

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