A spatial study of denitrification potential of sediments in Belfast and Strangford Loughs and its significance.

The C2H2 inhibition technique was employed to study seasonal denitrification potential rates in sediment slurries from tidal and subtidal sites in Belfast and Strangford Loughs, Northern Ireland. A comparison of denitrification rates obtained from this method with those obtained from the 15N-gas flux method generally showed good agreement. Depth profiles measured up to 1 m showed that denitrification decreased with depth, with highest values in the 0-5-cm fraction. For the Belfast Lough tidal system a multiple regression model was developed which explained 83% of the variation in denitrification potential. The independent variables were water content, sediment temperature, total oxidizable N in porewater and total organic N. The highest rate of denitrification potential, 2100 micromol N m(-2) h(-1), was found in areas where there was a high anthropogenic input of nutrients. Denitrification in sediments in both loughs can play a potentially significant role in removal of NO3- from the overlying water. In Belfast Lough the overall denitrification potential rate matched the external NO3-N inputs, whilst in Strangford Lough it exceeded it by sixfold, which suggests a potential to remove future additional anthropogenic inputs to the Lough.