INGENIA

ENV-03

First-order BOD remaining

Lt = L0 e^{−k t}.

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KineticsPhelps

Governing equation

Lt=L0e−ktL_t = L_0 e^{-kt}

t∈[0.1,20]t \in \left[0.1, 20\right]

where

L_0
Ultimate BOD (mg/L)
k
Rate constant (1/d)
t
Time (d)
L_t
BOD remaining (mg/L)
y_t
BOD exerted (mg/L)

The figure, part by part

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ENV-03 · decay
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①

Governing law — red

Lt=L0e−ktL_t = L_0 e^{-kt}

t∈[0.1,20]t \in \left[0.1, 20\right]

t=0.1t = 0.1Lt=244.3L_t = 244.3

②

Domain of the variable — blue

tmin⁡=0.1,tmax⁡=20t_{\min} = 0.1,\quad t_{\max} = 20

t∈[0.1,20]t \in \left[0.1, 20\right]

t=0.1t = 0.1t=0.1t = 0.1

③

Response curve — green

Lt=L0e−ktL_t = L_0 e^{-kt}

t∈[0.1,20]t \in \left[0.1, 20\right]

t=0.1t = 0.1Lt=244.3L_t = 244.3

④

Rate of change — amber

dLtdt\frac{\mathrm{d}L_t}{\mathrm{d}t}

t∈[0.1,20]t \in \left[0.1, 20\right]

t=0.225t = 0.225Lt′=−54.61L_t^{\prime} = -54.61

Lecture brief

Historical brief

Streeter–Phelps (1925) oxygen sag, settling theory and Guldberg–Waage kinetics made water and air quality a rate problem. The lab computes sag, overflow and a snapshot of reactor mass balance. This sheet (ENV-03 — First-order BOD remaining) is the form associated with Phelps. Working symbols: L0L_0, kk, tt →\rightarrow LtL_t, yty_t. Phelps modelled biochemical oxygen demand as a first-order decay of the remaining carbonaceous load.

Purpose

Purpose: compute LtL_t, yty_t from L0L_0, kk, tt in Environmental via Lt=L0e−ktL_t = L_0 e^{-kt} Lt = L0 e^{−k t}. Use it when a real environmental question must be answered in SI before a code check.

Live realistic example

In symbols

Live case. Given L0=250.000 mg/LL_0 = 250.000\,\mathrm{mg/L}, k=0.230 1/dk = 0.230\,\mathrm{1/d}, t=5.000 dt = 5.000\,\mathrm{d}, the governing relation Lt=L0e−ktL_t = L_0 e^{-kt} yields Lt=79.159 mg/LL_t = 79.159\,\mathrm{mg/L}, yt=170.841 mg/Ly_t = 170.841\,\mathrm{mg/L}. Constant k, no nitrification lag. Move a slider: the numbers are this situation, not a canned story.

Calculator

Inputs

Outputs

  • BOD remaining L_t79.159 mg/L
  • BOD exerted y_t170.841 mg/L
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ENV-03 · decay
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Narration of this film

Constant k, no nitrification lag.

Phelps modelled biochemical oxygen demand as a first-order decay of the remaining carbonaceous load.

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