Water Quality Example Calculations

This example illustrates how WEAP calculates instream water quality. The section of the river modeled is 100 km, with a water temperature throughout of 15 °C. The river headflow of 500 units contains initial concentrations of BOD ( = 5 mg/l), DO (= 8 mg/l), Salt (2 mg/l) and TSS (20 mg/l). Salt is a conservative

constituent, so it will not decay. TSS follow first-order decay, with a decay rate of 0.25 (/day). The demand site withdraws 100 units, consumes 50%, and returns 50% (50 units) to the wastewater treatment plant, with the following concentrations: BOD (20 mg/l), DO (3 mg/l), Salt (10 mg/l) and TSS (5 mg/l). The wastewater treatment plant removes 90% of the BOD, 0% of salt and TSS, and the outflow concentration of DO is 4 mg/l. 10% of the water evaporates in processing, so 90% of the inflow (45 units) returns to the river.

Reach Below Headflow

The initial concentrations of non-conservative pollutants will decay along the reach below the headflow. If the reach is 38.8 km long, and the water velocity is 15.61 m/s, it will take 25 seconds to traverse the reach.

Salinity

Salt is conservative, so it will not decay. Therefore, the concentration at the end of the first reach will be the same as at the beginning: 2 mg/l.

TSS

TSS is simulated with first-order decay. In Eqn. 3, if c0 = 20 mg/l, k = 0.25/day, L = 38.8 km, and U = 196.36 km/day; then c = 19.036 mg/l.

DO

In Eqn. 4, if T = 15; then OS = 10.94.

It follows from Eqn. 5 that if kd=0.4/day, ka = 0.95/day, kr = 0.4/day, L = 38.8 km, U = 196.36 km/day, = 5 mg/l, and DOIN = 8 mg/l; then DO = 8.157 mg/l.

BOD

Using Eqn. 7 with = 0.25, H = 4m (i.e., = 0.3), and T = 15C; krBOD = 0.288

Then, using Eqn. 6 with = 0.288, L = 38.8 km, U = 196.36 km/day, and = 5 mg/l; then BOD = 4.72 mg/l

Withdrawal Node

Removing water from the river does not change the concentration of the water, it just reduces the volume. Therefore, the concentrations immediately below this node will be the same as flowed into the node from the reach above.

Salinity

Salt is conservative, so it will not decay. Therefore, the concentration at the end of the reach will be the same as at the beginning: 2 mg/l.

TSS

Using Eqn. 3, with c0 = 19.036 mg/l, k = 0.25/day, L = 20.4 km, and U = 180 km/day; then c = 18.504 mg/l

DO

Using Eqn. 4 with T = 15; OS = 10.94

Then, using Eqn. 5 with kd = 0.4/day; ka = 0.95/day, kr = 0.4/day, L = 20.4 km, U = 180 km/day, = 4.72 mg/l, DOIN = 8.157 mg/l; then DO = 8.243 mg/l

BOD

Using Eqn. 7 with = 0.25, H = 3.6 m (i.e., = 0.3), T = 15C; then krBOD = 0.288.

Demand Site

Concentrations of pollution in demand site return flows does not depend on concentrations of inflows to the demand site. Therefore, the concentration of the river water supply is irrelevant.

In this example, demand site pollution generation is specified as the concentration in the return flow. The demand site withdraws 100 units, consumes 50%, and returns 50% (50 units) to the wastewater treatment plant with the following concentrations: BOD (20 mg/l), DO (3 mg/l), Salt (10 mg/l) and TSS (5 mg/l).

The mass of each pollutant is calculated as,

MonthlyPollutionGeneratedDS,p,m = DemandSiteReturnFlowDS,m x ReturnFlowConcentrationDS,m,p

Salinity

Mass = 50 * 10 = 500

TSS

Mass = 50 * 5 = 250

DO

Mass = 50 * 3 = 150

BOD

Mass = 50 * 20 = 1000

Wastewater Treatment Plant

The wastewater treatment plant removes 90% of the BOD, 0% of salt and TSS, and the outflow concentration of DO is 4 mg/l. 10% of the water evaporates in processing, so 90% of the inflow (45 units) returns to the river. Evaporation concentrates the pollutants somewhat, causing the concentrations to be higher (by 11% in this case) than they would with no evaporation. The removal rate (e.g., 90% of BOD) refers to the mass of pollutant, not the concentration.

Salinity

TreatmentPlantPollOutflowTP,p = (1 - RemovalRateTP,p)x TreatmentPlantPollInflowTP,p

Mass outflow = (1 - 0) * 500 = 500

TSS

Mass outflow = (1 - 0) * 250 = 250

BOD

Mass outflow = (1 - 0.9) * 1000 = 100

DO

DO is specified as a concentration, rather than a removal rate. Therefore, the inflow of DO is not used.

TreatmentPlantPollOutflowTP,p = OutflowConcentrationTP,p x TreatmentPlantReturnFlowTP,p

Mass outflow = 4 * 45 = 180

Reach below Withdrawal Node

Salinity

Salt is conservative, so it will not decay. Therefore, the concentration at the end of the reach will be the same as at the beginning: 2 mg/l.

TSS

Using Eqn. 3, with c0 = 19.036 mg/l, k = 0.25/day, L = 20.4 km, U = 180 km/day; then c = 18.504 mg/l.

DO

Using Eqn. 4, with T = 15; then OS = 10.94.

Using Eqn. 5 with kd = 0.4/day, ka = 0.95/day, kr = 0.4/day, L = 20.4 km, U = 180 km/day, = 4.72 mg/l, and DOIN = 8.157 mg/l; then DO = 8.243 mg/l

BOD

Using Eqn. 7 with = 0.25, H = 3.6 m (i.e., = 0.3), T = 15C; then krBOD = 0.288.

Using Eqn. 6 with = 0.288, L = 20.4 km, U = 180 km/day, = 4.72 mg/l; then BOD = 4.57 mg/l

Return Flow Node

Treated effluent from the wastewater treatment plant mixes with the river water, using the following weighted average:

Eqn. 8

c is the new concentration (mg/l)

Qw is the inflow of wastewater = 45

Qr is the flow from upstream = 400

Cw is the concentration of pollutant in the wastewater

Cr is the concentration of pollutant in the flow from upstream

Mw = Qw Cw, the mass of pollutant in wastewater

Salinity

With Mw = 500 and Cr = 2 mg/l; then c = 2.92 mg/l in Eqn. 8.

TSS

With Mw = 250 and Cr = 18.5 mg/l; then c = 17.2 mg/l

DO

With Mw = 180 and Cr = 8.24 mg/l; then c = 7.81 mg/l

BOD

With Mw = 100 and Cr = 4.57 mg/l; then c = 4.33 mg/l

Reach below Return Flow Node

Salinity

Salt is conservative, so it will not decay. Therefore, the concentration at the end of the reach will be the same as at the beginning: 2.92 mg/l.

TSS

TSS uses first-order decay. Using Eqn. 3 with c0 = 17.2 mg/l, k = 0.25/day, L = 40.8 km, and U = 187.92 km/day; then c = 16.29 mg/l

DO

Using Eqn. 4 with T = 15; then OS = 10.94

Using Eqn. 5 with kd = 0.4/day, ka = 0.95/day, kr = 0.4/day, L = 40.8 km, U = 187.92 km/day, = 4.33 mg/l, and DOIN = 7.81 mg/l; then DO = 8.07 mg/l

BOD

Using Eqn. 7 with = 0.25, H = 3.78m (i.e., = 0.3), and T = 15C; then krBOD = 0.291

Using Eqn. 6 with krBOD = 0.288, L = 40.8 km, U = 187.92 km/day, and = 4.33 mg/l; then BOD = 4.066 mg/l

Here is a summary of surface water quality: