Nitrite
The amount of nitrite (NO2−) in the stream will be increased by the conversion of NH4+ to NO2− and decreased by the conversion of NO2− to NO3−. The conversion of NO2− to NO3− occurs more rapidly than the conversion of NH4+ to NO2−, so the amount of nitrite present in the stream is usually very small. The change in nitrite for a given day is:
ΔNO2str=(βN,1∗NH4str−βN,2∗NO2str)∗TT 7:3.2.8
where ΔNO2str is the change in nitrite concentration (mg N/L), βN,1 is the rate constant for biological oxidation of ammonia nitrogen (day−1 or hr−1), NH4str is the ammonium concentration at the beginning of the day (mg N/L), βN,2 is the rate constant for biological oxidation of nitrite to nitrate (day−1 or hr−1), NO2str is the nitrite concentration at the beginning of the day (mg N/L), and TT is the flow travel time in the reach segment (day or hr). The local rate constant for biological oxidation of ammonia nitrogen is calculated with equation 7:3.2.5. The calculation of travel time is reviewed in Chapter 7:1.
The rate constant for biological oxidation of nitrite to nitrate will vary as a function of in-stream oxygen concentration and temperature. The rate constant is calculated:
βN,2=βN,2,20∗(1−exp[−0.6∗Oxstr])∗1.047(Twater−20) 7:3.2.9
where βN,2 is the rate constant for biological oxidation of nitrite to nitrate (day−1 or hr−1), βN,2,20 is the rate constant for biological oxidation of nitrite to nitrate at 20°C (day−1 or hr−1),Oxstr is the dissolved oxygen concentration in the stream (mg O2/L), and Twater is the average water temperature for the day or hour (°C). The second term on the right side of equation 7:3.2.9, (1−exp[−0.6∗Oxstr]), is a nitrification inhibition correction factor. This factor inhibits nitrification at low dissolved oxygen concentrations.
Last updated