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Handout Lesson 10, Equilibrium Solutions and Stability
This lesson is based on Section 2.2 of your textbook by Edwards, Penney, and Calvis.
CITATION: This set of notes contains several slope fields and solution curves sketched in the slope fields. I used the
direction field plotter by Ariel Barton at the Unviersity of Arkansas to create these pictures.
Autonomous Differential Equations, Critical Points, and Equilibrium Solutions.
Definition 62 .
autonomous
\begin{equation*}
\frac{dy}{dx}=f(y)\text{.}
\end{equation*}
Example 63 . Identifying autonomous equations.
\(\frac{dP}{dt}=kP(M-P)\) (This is also a equation.)
\(\displaystyle \frac{dy}{dx}=yx^2\)
With the logistic model
\(\frac{dP}{dt}=kP(M-P)$\) \(P \equiv \fillinmath{XXXXXXXXXXXXXXX}\) and
\(P \equiv \fillinmath{XXXXXXXXXXXXXXX}\) are constant solutions. These constant solutions separate the other solutions into three categories, depending on the value of
\(P_0\text{.}\)
Letβs consider the logistic growth model
\begin{equation*}
\frac{dP}{dt}=P(2-P)
\end{equation*}
The following slope field and solution curves were generated by the direction field plotter by Ariel Barton.
A slope field for
\(\frac{dP}{dt}=P(2-P)\text{.}\)
Definition 64 .
The solutions of \(f(y)=0\) are the critical points of the autonomous differential equation
\begin{gather}
\frac{dy}{dx}=f(y)\tag{βΆβΆ}
\end{gather}
If
\(y=c\) is a critical point of
(βΆβΆ) , then the constant solution
\begin{equation*}
y(x)=c \text{ or } y\equiv c
\end{equation*}
Phase Diagrams and Stability.
Letβs take another look at the slope field diagram that we saw earlier for the logistic model
\(\frac{dP}{dt}=P(2-P)\text{.}\)
A slope field for
\(\frac{dP}{dt}=P(2-P)\text{.}\)
As \(t \rightarrow \infty\text{:}\)
the diagram around
\(P \equiv 0\) looks like a β
β. We call
\(P= 0\) an
critical point of the model.
the diagram around $P \equiv M$ looks like a β
β. We call
\(P= 0\) an
critical point of the model.
We do not need to see the slope field to understand the stability of a critical point. We can analyze the derivative algebraically.
Example 65 . Phase diagrams and stability.
Consider the logistic model
\(\frac{dP}{dt}=kP(M-P)\) where
\(k>0\text{.}\) Use a phase diagram to determine the stability of the critical points of the model.
Example 66 .
Discuss the stability of the critical point(s) of the model.
\(\frac{dx}{dt}=(x-3)^2\text{.}\)
A slope field for
\(\frac{dx}{dt}=(x-3)^2\text{.}\)
The Effect of Parameters - Bifurcation.
Parameters can have a significant effect on the type of solutions you obtain for a differential equation. For example, parameters can affect critical points.
Example 67 . Bifurcation point.
(Based on Number 21 from Section 2.2 of your textbook by Edwards, et.al.)
Consider the model
\begin{gather}
\frac{dx}{dt}=kx-x^3=-x(x^2-k)\tag{β }
\end{gather}
with parameter \(k\text{.}\)
If
\(k>0\text{,}\) then
(β ) has
critical points:
.
If
\(k < 0\text{,}\) then
(β ) has only
critical points:
.
We call
\(k=0\) a
point of the differential equation in
(β ) because it is the point at which the parameter
\(k\) changes the
nature of the solutions.
We can visualize this by plotting all points
\begin{equation*}
(k,c)
\end{equation*}
such that
\(c\) is a critical point of
(β ) for that value of
\(k\text{.}\)
A Cartesian coordinate system with independent variable \(k\) and dependent variable \(c\text{.}\)
Harvesting Logistic Populations.
Consider the logistic model that has been slightly modified to account for harvesting of a population (such as fishing or butchering beef).
\begin{align*}
\frac{dP}{dt} & = kP(M-P)-h \\
& = -kP^2+kMP-h
\end{align*}
where \(k, M, h>0\) and \(h\) represents the rate at which the population is being harvested.
\(kP(M-P)-h\) \(P\text{,}\)
The quadratic equation has 2 distinct real roots \(H\) and \(N\) with \(H<N\text{.}\) Using the quadratic formula, it can be argued that \(0 < H < N < M\text{.}\) (See example 4 in section 2.2 of your textbook by Edwards, et.al.)
There is one distinct real root \(N\text{.}\)
There are no real roots.
\begin{equation*}
\frac{dP}{dt}= -kP^2+kMP-h
\end{equation*}
Letβs consider the harvesting model
\begin{equation*}
\frac{dP}{dt}=P(6-P)-h = -P^2+6P-h
\end{equation*}
where \(k=1\) and \(M=6\text{.}\) Letβs look at what happens for some values of \(h\text{.}\) The direction fields on this page were made Ariel Bartonβs direction field plotter. The graphs of parabolas were created using Desmos.
\(h=0\) (This is just a logistic growth model)
Slope field when harvesting rate is 0.
Graph of
\(y=-P^2+6P-0\text{.}\)
\(h=4\)
Slope field when harvesting rate is 4.
Graph of
\(y=-P^2+6P-4\text{.}\)
\(h=9\)
Slope field when harvesting rate is 9.
Graph of
\(y=-P^2+6P-9\text{.}\)
\(h=10\)
Slope field when harvesting rate is 10.
Graph of
\(y=-P^2+6P-10\text{.}\)