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DO deficit 50 km downstream, 1.9 m³/s stream

Short answer

Using Streeter-Phelps with O'Connor-Dobbins reaeration: mixed flow 2.5 m³/s, initial deficit 1.769 mg/L, ultimate BOD 52.30 mg/L, K₁=0.1 day⁻¹, K₂=0.396 day⁻¹, travel time 3.858 days. DO deficit at 50 km = 6.80 mg/L (DO = 2.37 mg/L).

A stream saturated with DO has a flow of 1.9 m³/s, BOD of 2.5 mg/l and rate constant (K to base 10) of 0.1 per day. It receives an effluent discharge of 0.6 m³/s having BOD of 210 mg/l and DO of 1.8 mg/l. The average velocity of stream is 0.15 m/s and average depth of stream is 1.4 m. Calculate DO deficit 50 km downstream of outfall. Assume temperature of 20°C throughout and saturation DO at 20°C is 9.17 mg/l.

Assumptions

Streeter-Phelps equation with rate constants to base 10; the BOD values given are taken as the ultimate (first-stage) BODs, so L0L_0 is the BOD of the mixture; K1=0.1K_1=0.1 day⁻¹; the reaeration constant is found from the O'Connor-Dobbins formula (base ee, 20°C):

K2(e)=3.9 v0.5H1.5 day−1(v in m/s, H in m),K2(base 10)=K2(e)2.303K_{2(e)}=\frac{3.9\,v^{0.5}}{H^{1.5}}\ \text{day}^{-1}\quad(v\text{ in m/s},\ H\text{ in m}),\qquad K_2(\text{base }10)=\frac{K_{2(e)}}{2.303}

Step 1: Mixing at the outfall

Qmix=1.9+0.6=2.5 m3/sDOmix=1.9(9.17)+0.6(1.8)2.5=7.401 mg/LD0=9.17−7.401=1.769 mg/LL0=1.9(2.5)+0.6(210)2.5=52.30 mg/L\begin{aligned} Q_{mix}&=1.9+0.6=2.5\ \text{m}^3/\text{s}\\ DO_{mix}&=\frac{1.9(9.17)+0.6(1.8)}{2.5}=7.401\ \text{mg/L}\\ D_0&=9.17-7.401=1.769\ \text{mg/L}\\ L_0&=\frac{1.9(2.5)+0.6(210)}{2.5}=52.30\ \text{mg/L} \end{aligned}

Step 2: Reaeration constant and time of flow

K2(e)=3.9×0.150.51.41.5=0.912 day−1⇒K2=0.396 day−1 (base 10)t=xv=50000 m0.15 m/s=333333 s=3.858 days\begin{aligned} K_{2(e)}&=\frac{3.9\times0.15^{0.5}}{1.4^{1.5}}=0.912\ \text{day}^{-1}\Rightarrow K_2=0.396\ \text{day}^{-1}\ (\text{base }10)\\ t&=\frac{x}{v}=\frac{50000\ \text{m}}{0.15\ \text{m/s}}=333333\ \text{s}=3.858\ \text{days} \end{aligned}

Step 3: Deficit at the section

Dt=K1L0K2−K1(10−K1t−10−K2t)+D010−K2tD_t=\frac{K_1L_0}{K_2-K_1}\left(10^{-K_1t}-10^{-K_2t}\right)+D_010^{-K_2t} Dt=0.1×52.300.396−0.1(10−0.3858−10−1.5278)+1.769×10−1.5278=6.80 mg/L\begin{aligned} D_t&=\frac{0.1\times52.30}{0.396-0.1}\left(10^{-0.3858}-10^{-1.5278}\right)+1.769\times10^{-1.5278}\\ &=6.80\ \text{mg/L} \end{aligned}

Answer: DO deficit 50 km downstream = 6.80 mg/L (DO = 2.37 mg/L).

Note: if the given BODs were 5-day values, L0L_0 would be 76.576.5 mg/L, and the deficit would rise further (to about 9.9 mg/L, which is more than the saturation value, so the stream would turn septic).

✓ Answer checked by Claude Opus 5.5 (high effort)

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