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Elementary Differential Equations and Boundary Value Problems - Boyce W.E.

Boyce W.E. Elementary Differential Equations and Boundary Value Problems - John Wiley & Sons, 2001. - 1310 p.
Download (direct link): elementarydifferentialequations2001.pdf
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3. Take another look at the ODEs of the coupled springs model in Module 6. Use ODE Architect for the system of four ODEs given in Experiment 1 of that section (use c = 0.05). Make 3D plots of any three of the five variables x1, x!1, x2, x2, and t. What do the plots tell you about the corresponding motions of the springs? Now use the Tool to find the eigenvalues of the Jacobian matrix of the system at the equilibrium point. What do the eigenvalues tell you about the motions?
134 Exploration 7.3
4. Modify the coupled springs model from Module 6 (where coupled linear springs move on a frictionless horizontal surface) by making one of the springs hard or soft: add a term like ±x3 to the restoring force. Does this change the long-term behavior of the system? Make and interpret graphs as in Problem 3.
5. Chaos in three dimensions.
Some nonlinear 3D systems seem to behave chaotically. Orbits stay bounded as time advances, but the slightest change in the initial data leads to an orbit that eventually seems to be completely uncorrelated with the original orbit. This is thought to be one feature of chaotic dynamics. Choose one of the following three Library files located in the folder “Higher Dimensional Systems”:
• “The Scroll Circuit: Organized Chaos”
• “The Lorenz System: Chaos and Sensitivity”
• “The Roessler System: A Strange Attractor”
Change parameters until you see an example of this kind of chaos. You may want to look at Chapter 12 for additional insight into the meaning of chaos.
Compartment Models
Oscillating chemical reactions on a wineglass?
Overview A salt solution is pumped through a series of tanks. We'll use the balance law to model the rate of change of the amount of salt in each tank:
{Net rate of change of I I Rate into I I Rate out of I amount of salt in tank tank tank
If we know the initial amount of salt and the inflow and outflow rates of the solution in each tank, then we can set up an IVP that models the physical system. We'll use this "balance law" approach to model the pollution level in a lake; the flow of a medication; the movement of lead among the blood, tissues, and bones of a body; and an autocatalytic chemical reaction.
Key words Compartment model; balance law; lake pollution; pharmacokinetics; chemical reactions; chemical law of mass action; autocatalysis; Hopf bifurcation
See also Chapter 9 for the SIR compartment model, and Chapter 6 for linear systems and flow through interconnected tanks.
136
Chapter 8
¦ Lake Pollution
Modeling how pollutants move through an environment is important in the prediction of harmful effects, as well as the formulation of environmental policies and regulations. The simplest situation has a single source of pollution that contaminates a well-defined habitat, such as a lake. To build a model of this system, we picture the lake as a compartment; pollutants in the water flow into and out of the compartment. The rates of flow determine the amount of build-up or dissipation of pollutants. It is useful to represent this conceptual model with a compartment diagram, where a box represents a compartment and an arrow represents a flow rate. Here is a compartment diagram for a simple model of lake pollution:
You can get the volume V(t) of water in the lake by solving the IVP V = sin - $out, V(0) = Vo.
The amount of pollutant in the lake at time t is L(t), while rin is the rate of flow of pollutant into the lake and rout is the rate of flow of pollutant out of the lake. To obtain the equation for the rate of change of the amount of pollutant in the lake, we apply the balance law: the net rate of change of the amount of a substance in a compartment is the difference between the rate of flow into the compartment and the rate of flow out of the compartment:
dL
~J~ — Ëï ^out dt
This ODE is sufficient when we know the rates rin and rout, but these rates are usually not constant: they depend on the rate of flow of water into the lake, the rate of flow of water out of the lake, and the pollutant concentration in the inflowing water. Let sin and sout represent the volume rates of flow of water into and out of the lake, V the volume of water in the lake, and pin the concentration of pollutant in the incoming water. Now we can calculate the rates shown in the compartment diagram:
rm = pinsir
_ L
^out — "j^5out
The ODE for the amount of pollutant in the lake is now
dL
L
(1)
So we need to know V(0), L(0), pin, sin, and sout in order to determine L(t) and V(t).
Take a look at Screen 1.4 in Module 8 for on-off inflow concentrations.
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