Abstract
Denitrification driven by pyrite oxidation can play a major role in the removal of nitrate from groundwater systems. As yet, limited information is available on the interactions between the micro-organisms and aqueous and mineral phases in aquifers where pyrite oxidation is occurring. In this study, we examine the groundwater and sediment composition along a well-characterized redox gradient in a heavily nitrate-polluted pyritic sandy aquifer in Oostrum (the Netherlands) to identify the sequence of steps involved in denitrification coupled to pyrite oxidation. Multi-isotope analyses (δ
Original language | English |
---|---|
Pages (from-to) | 123-130 |
Number of pages | 8 |
Journal | Chemical Geology |
Volume | 300-301 |
DOIs | |
Publication status | Published - 2012 |