MAGNITUDE OF NITRATE REMOVAL IN STREAMBED SEDIMENTS AND THE EFFECT OF PORE-WATER VELOCITY
The drive point device was used to sample streams in both longitudinal and latitudinal directions, and was inserted into streambed sediments from 10 – 60 cm depths. The hydraulic head gradients ranged from -0.108 – 0.164 relative to the overlying stream, and of the 25 gradient measurements collected at ~60 cm depth in the center channel of 7 streams, 72% showed an upward gradient. In general, hydraulic gradient profiles suggest a correlation of decreasing gradient with decreasing depth below the streambed. Dissolved oxygen concentrations of pore water ranged from 0.4 – 7.3 mg/L with the majority of samples <3 mg/L, sufficiently depleted to allow for denitrifying bacteria to be active. Indirect indication of denitrification is provided by measurements of nitrate concentrations in pore water. One vertical profile showed a decrease from 7 mg N/L at 60 cm depth below the streambed to <1 mg N/L at 10 cm depth, greatly reducing the nitrate load carried by the stream. By quantifying the amount of nitrate removal in the streambed sediments for multiple streams on the VAES, we gain insights to the extent and variability of the amelioration of groundwater contaminated by nitrogen-based fertilizers.