Organic Nitrogen
The amount of organic nitrogen in the stream may be increased by the conversion of algal biomass nitrogen to organic nitrogen. Organic nitrogen concentration in the stream may be decreased by the conversion of organic nitrogen to NH or the settling of organic nitrogen with sediment. The change in organic nitrogen for a given day is:
7:3.2.1
where is the change in organic nitrogen concentration (mg N/L), is the fraction of algal biomass that is nitrogen (mg N/mg alg biomass), is the local respiration or death rate of algae (day or hr), is the algal biomass concentration at the beginning of the day (mg alg/L), is the rate constant for hydrolysis of organic nitrogen to ammonia nitrogen (day or hr), is the organic nitrogen concentration at the beginning of the day (mg N/L), is the rate coefficient for organic nitrogen settling (day or hr), and is the flow travel time in the reach segment (day or hr). The fraction of algal biomass that is nitrogen is user-defined. Equation 7:3.1.17 describes the calculation of the local respiration rate of algae. The calculation of travel time is reviewed in Chapter 7:1.
The user defines the local rate constant for hydrolysis of organic nitrogen to NH at 20C. The organic nitrogen hydrolysis rate is adjusted to the local water temperature using the relationship:
7:3.2.2
where is the local rate constant for hydrolysis of organic nitrogen to NH (day or hr), is the local rate constant for hydrolysis of organic nitrogen to NH at 20C (day or hr), and is the average water temperature for the day or hour (C).
The user defines the rate coefficient for organic nitrogen settling at 20C. The organic nitrogen settling rate is adjusted to the local water temperature using the relationship:
7:3.2.3
where is the local settling rate for organic nitrogen (day or hr), is the local settling rate for organic nitrogen at 20C (day or hr), and is the average water temperature for the day or hour (C).
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