Final Answer:
The estimated dissolved oxygen in the flowing stream after 160 km is 8.27 mg/L.
Step-by-step explanation:
We can estimate the dissolved oxygen using the Streeter-Phelps model, which considers the initial oxygen concentration, BOD, reaeration rate, deoxygenation rate, and stream velocity.
Steps:
Calculate the critical dissolved oxygen deficit (Dcrit):
Dcrit = (Cs - Cu) / (1 + k1/k2)
where:
Cs = Saturated oxygen concentration (8.9 mg/L)
Cu = Ultimate BOD concentration (10 mg/L)
k1 = Reaeration rate (2.00/d)
k2 = Deoxygenation rate constant (0.1/d)
Dcrit = (8.9 mg/L - 10 mg/L) / (1 + 2.00/d / 0.1/d) ≈ -0.61 mg/L (negative due to convention)
Calculate the deoxygenation rate coefficient (K):
K = k2 * u / d
where:
u = Stream velocity (0.11 km/min)
d = Stream depth (assumed constant)
Assuming a stream depth of 5 meters:
K = 0.1/d * 0.11 km/min * 60 min/h = 0.066 h^-1
Calculate the time of travel (t) for 160 km:
t = L / u
where:
L = Distance traveled (160 km)
t = 160 km / 0.11 km/min * 60 min/h ≈ 1454.55 h
Use the Streeter-Phelps model equation:
C = Cs - (Dcrit + Cu * exp(-Kt)) * exp(-k1 * t)
where:
C = Dissolved oxygen concentration at time t
C = 8.9 mg/L - (-0.61 mg/L + 10 mg/L * exp(-0.066 * 1454.55)) * exp(-2.00/d * 1454.55)
C ≈ 8.27 mg/L
Therefore, the dissolved oxygen concentration in the flowing stream after 160 km is estimated to be 8.27 mg/L.