Kessler, Adam John2; Glud, R.N.4; Cardenas, M.B.3; Cook, Perran2
1 Department of Bioscience - Arctic Research Centre, Department of Bioscience, Science and Technology, Aarhus University2 Biologisk Institut3 University of Texas at Austin4 Department of Bioscience - Arctic Research Centre, Department of Bioscience, Science and Technology, Aarhus University
Measurement of biogeochemical processes in permeable sediments (including the hyporheic zone) is difficult because of complex multidimensional advective transport. This is especially the case for nitrogen cycling, which involves several coupled redox-sensitive reactions. To provide detailed insight into the coupling between ammonification, nitrification and denitrification in stationary sand ripples, we combined the diffusion equilibrium thin layer (DET) gel technique with a computational reactive transport biogeochemical model. The former approach provided high-resolution two-dimensional distributions of NO3- and N-15-N-2 gas. The measured two-dimensional profiles correlate with computational model simulations, showing a deep pool of N-2 gas forming, and being advected to the surface below ripple peaks. Further isotope pairing calculations on these data indicate that coupled nitrification-denitrification is severely limited in permeable sediments because the flow and transport field limits interaction between oxic and anoxic pore water. The approach allowed for new detailed insight into subsurface denitrification zones in complex permeable sediments.
Environmental Science and Technology (washington), 2013, Vol 47, Issue 23, p. 13404-13411