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Elucidating phosphorus removal dynamics in a denitrifying woodchip bioreactor.
Perera, Gimhani N; Rojas, Dorisel Torres; Rivas, Aldrin; Barkle, Greg; Moorhead, Brian; Schipper, Louis A; Craggs, Rupert; Hartland, Adam.
Afiliación
  • Perera GN; Environmental Research Institute, School of Science, Faculty of Science and Engineering, University of Waikato, Kirikirioa Hamilton, New Zealand; National Institute of Water and Atmospheric Research Ltd (NIWA), PO Box 11115, Kirikirioa Hamilton 3251, New Zealand.
  • Rojas DT; Environmental Research Institute, School of Science, Faculty of Science and Engineering, University of Waikato, Kirikirioa Hamilton, New Zealand.
  • Rivas A; Lincoln Agritech Ltd, Ruakura, Kirikirioa Hamilton 3214, New Zealand.
  • Barkle G; Land and Water Research Ltd, Kirikirioa Hamilton 3217, New Zealand.
  • Moorhead B; Lincoln Agritech Ltd, Ruakura, Kirikirioa Hamilton 3214, New Zealand.
  • Schipper LA; Environmental Research Institute, School of Science, Faculty of Science and Engineering, University of Waikato, Kirikirioa Hamilton, New Zealand.
  • Craggs R; National Institute of Water and Atmospheric Research Ltd (NIWA), PO Box 11115, Kirikirioa Hamilton 3251, New Zealand.
  • Hartland A; Environmental Research Institute, School of Science, Faculty of Science and Engineering, University of Waikato, Kirikirioa Hamilton, New Zealand; Lincoln Agritech Ltd, Ruakura, Kirikirioa Hamilton 3214, New Zealand. Electronic address: adam.hartland@waikato.ac.nz.
Sci Total Environ ; 917: 170478, 2024 Mar 20.
Article en En | MEDLINE | ID: mdl-38301780
ABSTRACT
Denitrifying woodchip bioreactors (DBRs) are an established nitrate mitigation technology, but uncertainty remains on their viability for phosphorus (P) removal due to inconsistent source-sink behaviour in field trials. We investigated whether iron (Fe) redox cycling could be the missing link needed to explain P dynamics in these systems. A pilot-scale DBR (Aotearoa New Zealand) was monitored for the first two drainage seasons (2017-2018), with supplemental in-field measurements of reduced solutes (Fe2+, HS-/H2S) and their conjugate oxidised species (Fe3+/SO42-) made in 2021 to constrain within-reactor redox gradients. Consistent with thermodynamics, the dissolution of Fe3+(s) to Fe2+(aq) within the DBR sequentially followed O2, NO3- and MnO2(s) reduction, but occurred before SO42- reduction. Monitoring of inlet and outlet chemistry revealed tight coupling between Fe and P (inlet R2 0.94, outlet R2 0.85), but distinct dynamics between drainage seasons. In season one, outlet P exceeded inlet P (net P source), and coincided with elevated outlet Fe2+, but at ⁓50 % lower P concentrations relative to inlet FeP ratios. In season 2 the reactor became a net P sink, coinciding with declining outlet Fe2+ concentrations (indicating exhaustion of Fe3+(s) hydroxides and associated P). In order to characterize P removal under varying source dynamics (i.e. inflows vs in-situ P releases), we used the inlet Fe vs P relationship to estimate P binding to colloidal Fe (hydr)oxide surfaces under oxic conditions, and the outlet Fe2+ concentration to estimate in-situ P releases associated with Fe (hydr)oxide reduction. Inferred P-removal rates were highest early in season 1 (k = 0.60 g P m3 d-1; 75-100 % removal), declining significantly thereafter (k = 0.01 ± 0.02 g P m3 d-1; ca. 3-67 % removal). These calculations suggest that microbiological P removal in DBRs can occur at comparable magnitudes to nitrate removal by denitrification, depending mainly on P availability and hydraulic retention efficiency.
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Texto completo: 1 Bases de datos: MEDLINE Asunto principal: Fósforo / Nitratos Idioma: En Revista: Sci Total Environ Año: 2024 Tipo del documento: Article País de afiliación: Nueva Zelanda

Texto completo: 1 Bases de datos: MEDLINE Asunto principal: Fósforo / Nitratos Idioma: En Revista: Sci Total Environ Año: 2024 Tipo del documento: Article País de afiliación: Nueva Zelanda