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This article in SSSAJ

  1. Vol. 40 No. 4, p. 528-533
     
    Received: June 25, 1975
    Published: July, 1976


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doi:10.2136/sssaj1976.03615995004000040023x

Ammonium Diffusion as a Factor in Nitrogen Loss from Flooded Soils1

  1. K. R. Reddy,
  2. W. H. Patrick and
  3. R. E. Phillips2

Abstract

Abstract

The role of NH4+-N diffusion in a flooded soil on nitrogen (N) loss through the nitrification-denitrification process was investigated under laboratory conditions. The distribution of applied NH4+-N in both the aerobic and anaerobic soil layers of a flooded soil was experimentally determined and compared with the values obtained from theoretical equations. The total loss of NH4+-N from the flooded soil system (15-cm depth) by nitrification-denitrification was equivalent to 12.43 g N/m2 for a 120-day incubation period when the initial concentration of NH4+-N was 44.84 g N/m2. Diffusion of NH4+-N from the anaerobic soil layer to the aerobic soil layer accounted for more than 50% (7.16 g N/m2) of the total NH4+-N loss with the remainder being lost from NH4+-N originally present in the aerobic layer. The NH4+-N that diffused upward into the aerobic soil layer was nitrified to NO3--N, which readily diffused back down into the anaerobic soil layer and was subsequently denitrified. The experimental distributions of NH4+-N were not in close agreement with calculated distributions in the surface aerobic soil layer, but were in close agreement in the anaerobic soil layer. It is possible that the rate constant (k) for NH4+-N oxidation varied considerably with depth in the aerobic soil layer and thus resulted in the disagreement. The total NH4+-N loss calculated from the experimental distributions tended to agree with the values obtained theoretically from rate constant (k) values of 3.18, 5.00, and 6.67 µg cm-3 day-1. The first rate constant value was obtained from an independent experiment (for same soil), the second from matching the concentration of NH4+-N at the aerobic-anaerobic layer interface of the theoretical and experimental distribution at 90 days after flooding, and the third from the NH4+-N disappearance in the aerobic soil layer of the soil columns described in this study. These rate constants indicate that the rate of nitrification is one of the factors controlling N loss from flooded soil.

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