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Organic Phosphorus

The amount of organic phosphorus in the stream may be increased by the conversion of algal biomass phosphorus to organic phosphorus. Organic phosphorus concentration in the stream may be decreased by the conversion of organic phosphorus to soluble inorganic phosphorus or the settling of organic phosphorus with sediment. The change in organic phosphorus for a given day is:

Ξ”orgPstr=(Ξ±2βˆ—Οaβˆ—algaeβˆ’Ξ²P,4βˆ—orgPstrβˆ’Οƒ5βˆ—orgPstr)βˆ—TT\Delta orgP_{str}=(\alpha_2*\rho_a*algae-\beta_{P,4}*orgP_{str}-\sigma_5*orgP_{str})*TTΞ”orgPstr​=(Ξ±2β€‹βˆ—Οaβ€‹βˆ—algaeβˆ’Ξ²P,4β€‹βˆ—orgPstrβ€‹βˆ’Οƒ5β€‹βˆ—orgPstr​)βˆ—TT 7:3.3.1

where Ξ”orgPstr\Delta orgP_{str}Ξ”orgPstr​ is the change in organic phosphorus concentration (mg P/L), Ξ±2\alpha_2Ξ±2​ is the fraction of algal biomass that is phosphorus (mg P/mg alg biomass), ρa\rho_aρa​ is the local respiration or death rate of algae (dayβˆ’1^{-1}βˆ’1 or hrβˆ’1^{-1}βˆ’1), algaealgaealgae is the algal biomass concentration at the beginning of the day (mg alg/L), Ξ²P,4\beta_{P,4}Ξ²P,4​ is the rate constant for mineralization of organic phosphorus (dayβˆ’1^{-1}βˆ’1 or hrβˆ’1^{-1}βˆ’1), orgPstrorgP_{str}orgPstr​ is the organic phosphorus concentration at the beginning of the day (mg P/L), Ξ±5\alpha_5Ξ±5​ is the rate coefficient for organic phosphorus settling (dayβˆ’1^{-1}βˆ’1 or hrβˆ’1^{-1}βˆ’1), and is the flow travel time in the reach segment (day or hr). The fraction of algal biomass that is phosphorus 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 mineralization of organic phosphorus at 20C. The organic phosphorus mineralization rate is adjusted to the local water temperature using the relationship:

7:3.3.2

where is the local rate constant for organic phosphorus mineralization (day or hr), is the local rate constant for organic phosphorus mineralization 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 phosphorus settling at 20C. The organic phosphorus settling rate is adjusted to the local water temperature using the relationship:

7:3.3.3

where is the local settling rate for organic phosphorus (day or hr), is the local settling rate for organic phosphorus at 20C (day or hr), and is the average water temperature for the day or hour (C).

TTTTTT
Β°\degreeΒ°
Ξ²P,4=Ξ²P,4,20βˆ—1.047(Twaterβˆ’20)\beta_{P,4}=\beta_{P,4,20}*1.047^{(T_{water}-20)}Ξ²P,4​=Ξ²P,4,20β€‹βˆ—1.047(Twaterβ€‹βˆ’20)
Ξ²P,4\beta_{P,4}Ξ²P,4​
βˆ’1^{-1}βˆ’1
βˆ’1^{-1}βˆ’1
Ξ²P,4,20\beta_{P,4,20}Ξ²P,4,20​
Β°\degreeΒ°
βˆ’1^{-1}βˆ’1
βˆ’1^{-1}βˆ’1
TwaterT_{water}Twater​
Β°\degreeΒ°
Β°\degreeΒ°
Οƒ5=Οƒ5,20βˆ—1.024(Twaterβˆ’20)\sigma_5=\sigma_{5,20}*1.024^{(T_{water}-20)}Οƒ5​=Οƒ5,20β€‹βˆ—1.024(Twaterβ€‹βˆ’20)
Οƒ5\sigma_5Οƒ5​
βˆ’1^{-1}βˆ’1
βˆ’1^{-1}βˆ’1
Οƒ5,20\sigma_{5,20}Οƒ5,20​
Β°\degreeΒ°
βˆ’1^{-1}βˆ’1
βˆ’1^{-1}βˆ’1
TwaterT_{water}Twater​
Β°\degreeΒ°