4.7 Article

Pathways and efficiency of nitrogen attenuation in wastewater effluent through soil aquifer treatment

Journal

JOURNAL OF ENVIRONMENTAL MANAGEMENT
Volume 321, Issue -, Pages -

Publisher

ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jenvman.2022.115927

Keywords

Isotopic fractionation; Enhanced biological denitrification; Permeable reactive barrier; Soil aquifer treatment; Nitrification; Denitrification

Funding

  1. EU [PCIN-2015-239, AQU-2017 SGR 1485]
  2. PACE-ISOTEC - Spanish Government [MARadentro-PCI2019-103603]
  3. AEI/FEDER from the UE
  4. Water JPI [CA210/18/00040]
  5. RESTORA from the Catalan Water Agency [2017-SGR-1733]
  6. Consolidated Research Group MAG [CEX2018-000794-S]
  7. Catalan Government
  8. Center of Excellence Severo Ochoa (Spanish Ministry of Science and Innovation) [ACA210/18/00040]
  9. Catalan Research Project RESTORA
  10. AGAUR
  11. [PCI2019-103603-WW2017]
  12. [CGL2017-87216-C4-1-R]

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This study evaluates the treatment effectiveness of Soil Aquifer Treatment (SAT) systems for nitrogen compounds using chemical and isotopic tools. The results show that coupled nitrification-denitrification is the main mechanism responsible for nitrogen migration and distribution. The study also reveals that the addition of a permeable reactive barrier can enhance the removal of nitrogen compounds in the SAT system.
Soil Aquifer Treatment (SAT) is used to increase groundwater resources and enhance the water quality of wastewater treatment plant (WWTP) effluents. The resulting water quality needs to be assessed. In this study, we investigate attenuation pathways of nitrogen (N) compounds (predominantly NH4+) from a secondary treatment effluent in pilot SAT systems: both a conventional one (SAT-Control system) and one operating with a permeable reactive barrier (PRB) to provide extra dissolved organic carbon to the recharged water. The goal is to evaluate the effectiveness of the two systems regarding N compounds by means of chemical and isotopic tools. Water chemistry (NO3-, NH4+, Non-Purgeable Dissolved Organic Carbon (NPDOC), and O2) and isotopic composition of NO3? (?15N-NO3- and ?18O-NO3-) and NH4+ (?15N-NH4+) were monitored in the inflow and at three different sections and depths along the aquifer flow path. Chemical and isotopic results suggest that coupled nitrification-denitrification were the principal mechanisms responsible for the migration and distribution of inorganic N in the systems and that nitrification rate decreased with depth. At the end of the study period, 66% of the total N in the solution was removed in the SAT-PRB system and 69% in the SAT-Control system, measured at the outlet of the systems. The residual N in solution in the SAT-PRB system had an approximately equal proportion of N-NH4+ and N-NO3- while in the SAT-Control system, the residual N in solution was primarily N-NO3-. Isotopic data also confirmed complete NO3? degradation in the systems from July to September with the possibility of mixing newly generated NO3? with the residual NO3? in the substrate pool.

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