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Nitrite

The amount of nitrite (NO2βˆ’NO_2^-NO2βˆ’β€‹) in the stream will be increased by the conversion of NH4+NH_4^+NH4+​ to NO2βˆ’NO_2^-NO2βˆ’β€‹ and decreased by the conversion of NO2βˆ’NO_2^-NO2βˆ’β€‹ to NO3βˆ’NO_3^-NO3βˆ’β€‹. The conversion of NO2βˆ’NO_2^-NO2βˆ’β€‹ to NO3βˆ’NO_3^-NO3βˆ’β€‹ occurs more rapidly than the conversion of NH4+NH_4^+NH4+​ to NO2βˆ’NO_2^-NO2βˆ’β€‹, so the amount of nitrite present in the stream is usually very small. The change in nitrite for a given day is:

Ξ”NO2str=(Ξ²N,1βˆ—NH4strβˆ’Ξ²N,2βˆ—NO2str)βˆ—TT\Delta NO2_{str}=(\beta_{N,1}*NH4_{str}-\beta_{N,2}*NO2_{str})*TTΞ”NO2str​=(Ξ²N,1β€‹βˆ—NH4strβ€‹βˆ’Ξ²N,2β€‹βˆ—NO2str​)βˆ—TT 7:3.2.8

where Ξ”NO2str\Delta NO2_{str}Ξ”NO2str​ is the change in nitrite concentration (mg N/L), Ξ²N,1\beta_{N,1}Ξ²N,1​ is the rate constant for biological oxidation of ammonia nitrogen (dayβˆ’1^{-1}βˆ’1 or hrβˆ’1^{-1}βˆ’1), NH4strNH4_{str}NH4str​ is the ammonium concentration at the beginning of the day (mg N/L), Ξ²N,2\beta_{N,2}Ξ²N,2​ is the rate constant for biological oxidation of nitrite to nitrate (dayβˆ’1^{-1}βˆ’1 or hrβˆ’1^{-1}βˆ’1), NO2strNO2_{str}NO2str​ is the nitrite concentration at the beginning of the day (mg N/L), and 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:

7:3.2.9

where is the rate constant for biological oxidation of nitrite to nitrate (day or hr), is the rate constant for biological oxidation of nitrite to nitrate at 20C (day or hr), is the dissolved oxygen concentration in the stream (mg O/L), and is the average water temperature for the day or hour (C). The second term on the right side of equation 7:3.2.9, , is a nitrification inhibition correction factor. This factor inhibits nitrification at low dissolved oxygen concentrations.

TTTTTT
Ξ²N,2=Ξ²N,2,20βˆ—(1βˆ’exp[βˆ’0.6βˆ—Oxstr])βˆ—1.047(Twaterβˆ’20)\beta_{N,2}=\beta_{N,2,20}*(1-exp[-0.6*Ox_{str}])*1.047^{(T_{water}-20)}Ξ²N,2​=Ξ²N,2,20β€‹βˆ—(1βˆ’exp[βˆ’0.6βˆ—Oxstr​])βˆ—1.047(Twaterβ€‹βˆ’20)
Ξ²N,2\beta_{N,2}Ξ²N,2​
βˆ’1^{-1}βˆ’1
βˆ’1^{-1}βˆ’1
Ξ²N,2,20\beta_{N,2,20}Ξ²N,2,20​
Β°\degreeΒ°
βˆ’1^{-1}βˆ’1
βˆ’1^{-1}βˆ’1
OxstrOx_{str}Oxstr​
2_22​
TwaterT_{water}Twater​
Β°\degreeΒ°
(1βˆ’exp[βˆ’0.6βˆ—Oxstr])(1-exp[-0.6*Ox_{str}])(1βˆ’exp[βˆ’0.6βˆ—Oxstr​])