Soil cores from river marginal wetlands in the UK, France and Ireland, sampled and contained within PVC piping, were flooded with nitrate‐N enriched water. Half of the cores were sterilized prior to flooding to destroy the denitrifying bacteria. The change in nitrate‐N concentration in the floodwater was measured over time. It is argued that the observed nitrate depletion rates (from 0.4 to 2.3 kg/ha per day) may be identified With microbially‐mediated denitrification. The results show the method to be a simple and direct procedure for the assessment of spatial variation in nitrate‐sink capacity. The depth of the denitrifying layer at the soil‐water interface was confirmed to be of the order of a few mm.
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Maltby et al. (1998) studied this question.
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