Ch 2.5 Lake Pollution Models

Lake Erie and Lake Ontario

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Lake Burley Griffin

Lake Burley Griffin

Background

  • Pollution in our lakes and rivers has become a major problem, particularly over the past 50 years.

  • In order to improve this situation in the future, it is necessary to gain a good understanding of the processes involved.

  • Some way of predicting how the situation might improve (or decline) as a result of current management practices is vital.

  • To this end we need to be able to predict how pollutant amounts or concentrations vary over time and under different management strategies.

General compartmental model

  • This problem can be considered as a compartmental model with a single compartment, the lake.

  • Applying the balance law there is an input of polluted water from the river(s) flowing into the lake, or due to a pollution dump into the lake, and an output as water flows from the lake carrying some pollution with it.

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Word Equation

  • Use compartment model to express word equation for mass of pollutant in lake.

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Example 2.5: Salt Solution in Tank

  • Before developing the differential equation describing this process for a lake, let's consider the simpler case of a salt solution in a tank.
  • We are interested in modeling amount \( S(t) \) kg of salt (the solute) dissolved in a tank of water (the solution).

Background

  • Suppose that the tank contains 100 liters of salt water.
  • Initially \( s_0 \) kg of salt are dissolved in tank.
  • Salt water flows into the tank at a rate of 10 liters per minute.
  • The concentration \( c_{in}(t) \) kg/liter of salt in this incoming flow of salt water varies with time.
  • The tank is well-mixed and salt solution flows out at same rate that it flows in (tank volume remains constant).

Compartment Diagram & Word Equation

  • Shown below is the input-output compartmental diagram for salt solution in tank.

  • From the compartment diagram, we can write the word equation as

Word Equation: Entering Tank

  • The rate at which salt enters tank is the product of flow rate in and concentration of salt in the incoming mixture:

\[ \left(10 \frac{L}{min}\right) \left(c_{in}(t) \frac{kg}{L}\right) = 10 c_{in}(t) \frac{kg}{min} \]

Word Equation: Leaving Tank

  • The rate at which salt leaves tank is the product of flow rate out and concentration of salt in the outgoing mixture:

\[ \left( 10 \frac{L}{min}\right) \left(\frac{S(t)}{100} \frac{kg}{L} \right) = \frac{S(t)}{10} \frac{kg}{min} \]

Differential Equation

  • We can now write the word equation as a differential equation (IVP):

\[ \frac{dS}{dt}= 10 c_{in}(t) - \frac{S(t)}{10}, \,\, S(0) = s_0 \]

Initial Value Problem

  • Linear first order ODE

\[ \frac{dS}{dt} = 10 c_{in}(t) - \frac{1}{10}S(t), \,\, S(0)= s_0 \]

  • Normal form

\[ \frac{dS}{dt} + \frac{1}{10}S(t) = 10 c_{in}(t) , \,\, S(0)= s_0 \]

  • Solve using method of integrating factors.

Example 2.6: Solve Salt IVP

  • Normal form

\[ \frac{dS}{dt} + \frac{1}{10}S(t) = 10 c_{in}(t) , \,\, S(0)= s_0 \]

  • Solve using method of integrating factors

\[ \begin{align*} \mu(t) & = e^{\int \frac{1}{10} dt } = e^{\frac{t}{10} }\\ S(t) & = e^{-\frac{t}{10} } \int 10 e^{\frac{s}{10} }c_{in}(s) ds + s_0 e^{-\frac{t}{10} } \end{align*} \]

  • Response due to initial condition goes to zero as t gets large.

\[ \lim_{t \rightarrow \infty} s_0 e^{-\frac{t}{10}} = 0 \]

Example 2.6: Salt Solution

  • Normal form for IVP

\[ \frac{dS}{dt} + \frac{1}{10}S(t) = 10 c_{in}(t) , \,\, S(0)= s_0 \]

  • Solution for \( c_{in}(t) = c_1 \):

\[ S(t) = s_0 e^{-t/10} + 100c_1(1-e^{-t/10}) \]

  • Solution for \( c_{in}(t) = 0.2 - 0.1\sin(t) \):

\[ S(t) = s_0 e^{-t/10} + 20 + \frac{10}{101}(\sin(t) - 10\cos(t) - 192e^{-t/10}) \]

Lake Pollution Model: Assumptions

  • Lake is continuously well mixed
  • Pollution is uniform throughout
  • Lake has a constant volume V
  • Lake has constant flow F

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Lake Pollution Model: Constants

  • \( c_0 \) = initial concentration of pollution in lake.
  • Concentration \( c_{in} \) of pollutant in the flow entering lake is constant:

\[ c_{in}\, \frac{g}{m^3} = \mathrm{constant} \]

  • Rate \( F \) at which water flows in and out of the lake is constant:

\[ F \, \frac{m^3}{day} = \mathrm{constant} \]

Lake Pollution Model: Variables

  • Let \( C(t) \) = concentration of pollutant in lake at time t.
  • Let \( M(t) \) = mass of pollutant at time t.
  • We are interested in finding an IVP for \( C(t) \).

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Lake Pollution Model: Model for Mass

  • Apply balance law for mass \( M(t) \) to obtain word equation:

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  • Translate into ODE:

\[ M'(t) = F c_{in} - F \frac{M(t)}{V} \]

Lake Pollution Model: Model for Concentration

  • For the mass \( M(t) \), we have:

\[ M'(t) = F c_{in} - F \frac{M(t)}{V} \]

  • Since \( C(t) = M(t)/V \) and \( C'(t) = M'(t)/V \), we have:

\[ C'(t) = \frac{F}{V} c_{in} - \frac{F}{V}C \]

Example 2.7 Solve Lake Pollution IVP

\[ \begin{align*} \frac{dC}{dt} & = \frac{F}{V}c_{in} - \frac{F}{V}C(t) , \,\, C(0)= c_0 \\ & = \frac{F}{V}\left(c_{in} - C(t)\right) \end{align*} \]

  • Solve using separation of variables (see text)

\[ \begin{align*} C(t) & = c_{in} - (c_{in} - c_0) e^{-Ft/V } \\ & = c_{in}\left(1 - e^{-Ft/V }\right) + c_0e^{-Ft/V } \end{align*} \]

Example 2.7 Lake Pollution Model

  • Solution

\[ \begin{align*} C(t) & = c_{in} - (c_{in} - c_0) e^{-Ft/V } \\ & = c_{in}\left(1 - e^{-Ft/V }\right) + c_0e^{-Ft/V } \end{align*} \]

  • Concentration of \( C(t) \) as \( t \) gets large.

\[ \lim_{t \rightarrow \infty} \left(c_{in} - (c_{in} - c_0) e^{-Ft/V }\right) = c_{in} \]

Example 2.8 Lake Pollution Model

  • How long will it take for the lake's pollution level to reach 5% of its initial level if only fresh water flows into the lake?
  • From previous slide, with \( c_{in} = 0 \):

\[ C(t) = c_{in} - (c_{in} - c_0) e^{-Ft/V } = c_0 e^{-Ft/V } \]

  • Solve for \( t \), and then use \( C = 0.05c_0 \):

\[ t = \frac{V}{F} \ln \left( \frac{C}{c_0} \right) = - \frac{V}{F}\ln(0.05) \cong \frac{3F}{V} \]

Lake Erie and Lake Ontario

  • From previous slide with \( C = 0.05c_0, \,c_{in} = 0 \):

\[ t \cong \frac{3F}{V} \]

  • For Lake Erie, we can plug in values for \( F \) and \( V \)

\[ t \cong 7.8 \, \mathrm{years} \]

  • For Lake Ontario:

\[ t \cong 23.5 \, \mathrm{years} \]

Lake Erie and Lake Ontario