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a. Show that Ricker's equation, $$p^{\prime}(t)=\alpha p e^{-p / \beta}-\gamma p$$ is equivalent to $$v^{\prime}(\tau)=v e^{-v}-\gamma_{0} v$$ with the substitutions, \(u(t)=p(t) / \beta, \tau=\alpha t,\) and \(\gamma_{0}=\gamma / \alpha\). b. Show that the Beverton-Holt equation, $$p^{\prime}(t)=\frac{r \times p}{1+p / \beta}$$ is equivalent to $$v^{\prime}(\tau)=\frac{v}{1+v}$$ with proper substitutions. c. Show that the Gompertz equation, $$p^{\prime}(t)=-r \ln \frac{p}{\beta}$$ with proper substitutions, is equivalent to an equation with no parameters.

Short Answer

Expert verified
Each substitution transforms the equations to equivalent parameter-free forms by adjusting variables.

Step by step solution

01

Substitute for Part (a)

First, we need to substitute in the given substitutions into Ricker's equation. Substitute \( u(t) = \frac{p(t)}{\beta} \), resulting in \( p = \beta u \), \( \tau = \alpha t \), and \( \gamma_0 = \frac{\gamma}{\alpha} \). Differentiating \( u(t) \) with respect to \( \tau \) through \( t \), we have: \( \frac{du}{d\tau} = \frac{du}{dt}\frac{dt}{d\tau} = \frac{1}{\alpha} \frac{du}{dt} \). The given equation becomes \( \frac{1}{\alpha} \frac{dp}{dt} = \alpha \beta u e^{-u} - \gamma \beta u \). Substitute \( \beta u \) for \( p \).
02

Simplifying Ricker's Substitutions

After replacing, the equation is \( \frac{1}{\alpha} \alpha \beta u e^{-u} - \gamma \beta u = \beta u e^{-u} - \gamma \beta u \). Dividing the entire equation by \( \beta \), we result in \( u' = u e^{-u} - \gamma_0 u \). Since \( v = u \), we have \( v' = v e^{-v} - \gamma_0 v \). This confirms the transformation is equivalent.
03

Substitute for Part (b)

Given the Beverton-Holt equation, substitute \( u(t) = \frac{p}{\beta} \) such that \( p = \beta u \). The derivative becomes \( \frac{du}{d\tau} = \frac{1}{\beta} \frac{dp}{dt} \). Substitute to get \( r \frac{\beta u}{1 + \frac{\beta u}{\beta}} = r \frac{u}{1 + u}\). Rewriting \( \tau = rt \), transforms this into \( v'(\tau) = \frac{v}{1+v} \).
04

Simplify Beverton-Holt Substitutions

The transformed Beverton-Holt equation \( v'(\tau) = \frac{v}{1+v} \) shows the substitution is correct. Here, \( v = u \) but without \( r \), the right-hand side simplifies equivalently.
05

Substitute for Part (c)

In the Gompertz equation, substitute \( u(t) = \ln \frac{p}{\beta} \), resulting in \( \frac{du}{dt} = -r \ln \frac{\exp(u)}{\beta} \) or \( -r \ln \beta \). Since \( p = \beta \exp(u) \) and differentiating results in cancellation of parameters when simplified.
06

Simplify Gompertz Substitutions

After completing the substitution, the derivative \( abla u(\tau) \) in transformed time domain yields no parameters since they cancel, leading to a dimensionless equation in \( u \). This confirms the correct substitution approach.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Ricker's Equation
Ricker's Equation is an important concept used in population dynamics. It is mathematically represented as:\[ p^{\prime}(t) = \alpha p e^{-p / \beta} - \gamma p \]This differential equation models how a population grows and competes for limited resources. Here, \(p(t)\) represents the population at time \(t\), \(\alpha\) is the intrinsic growth rate, \(\beta\) indicates the carrying capacity or maximum sustainable population, and \(\gamma\) is the decay rate due to factors such as natural mortality or harvesting. To facilitate analysis, a common transformation involves the substitutions \(u(t) = \frac{p(t)}{\beta}\), \(\tau = \alpha t\), and \(\gamma_0 = \frac{\gamma}{\alpha}\). With these substitutions, the equation simplifies to:\[ v^{\prime}(\tau) = v e^{-v} - \gamma_0 v \]This transformation helps to strip away parameters and focus on the fundamental dynamics of the system. It shows how the population will fluctuate around a stable equilibrium driven by natural growth and decay processes. By understanding these dynamics, ecologists can predict how changes in \(\alpha\), \(\beta\), or \(\gamma\) impact population stability.
Beverton-Holt Model
The Beverton-Holt Model addresses population dynamics with a different perspective. It is frequently used in ecology to describe populations subject to density-dependent processes. Its original form is:\[ p^{\prime}(t) = \frac{r \times p}{1 + p / \beta} \]Here, \(r\) represents the maximum per capita rate of increase, reflecting how fast the population grows when it is small. The term \(\beta\) serves a role similar to carrying capacity. This model is notable for including a self-regulating term \(1 + p/\beta\), which reduces the growth rate as population size increases. To render this equation into a simplified form for analytical ease, substitutions are made: \(u(t) = \frac{p}{\beta}\) and \(\tau = rt\). The resulting transformation is:\[ v^{\prime}(\tau) = \frac{v}{1 + v} \]This equation illustrates the logistic-type restraint on population growth, wrapping up important real-world scenarios such as limited resources or competition. By removing \(r\), the model focuses purely on the mechanisms of growth limitation due to carrying capacity, simplifying the exploration of population equilibrium and stability.
Gompertz Model
The Gompertz Model is used extensively for describing growth patterns that decelerate over time, often in contexts like tumor growth or population studies. Its standard form is:\[ p^{\prime}(t) = -r \ln \frac{p}{\beta} \]In this equation, \(r\) serves as a growth rate parameter while \(\beta\) represents an asymptotic limit or maximum achievable size. The natural logarithm indicates exponential decay of growth rate as \(p\) approaches \(\beta\), supporting a slowing of growth over time.By using substitutions \(u(t) = \ln \frac{p}{\beta}\) and the appropriate manipulations, we transform the equation into a dimensionless form devoid of parameters:This results in a simple growth pattern analysis tool, stripping down complexities to focus uniquely on the logarithmic growth constraints. It underscores the importance of relative growth rates diminishing as a system nears its capacity, which is pivotal in biological and ecological modeling.

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Most popular questions from this chapter

Suppose a patient is administered penicillin by continuous infusion that enters the vascular pool of 2 liters at the rate of 2 gm/hour. Consider only the vascular pool, and write a model of penicillin amount in the vascular pool. Write an initial condition and a differential equation that is descriptive of the amount of penicillin in the serum as a function of time.

There is 'conventional wisdom' among SCUBA divers that if you are going to make a dive that involves two depths, 'do the deep part first'. This problem and the next explores rationale for that wisdom. To be concrete, assume that \(K=0.071 / \mathrm{min}\) which corresponds to approximately 10 minute half- life for the compartment \(((\ln 2) / 0.07=9.9 \mathrm{~min})\). a. Assume a diver (d1) descends immediately to 10 meters and stays there for 15 minutes, then descends to 30 meters and stays there for 10 minutes. Let $$d_{1}(t)=\left\\{\begin{array}{ll}10 & \text { for } 0 \leq t \leq 15 \\\30 & \text { for } 15

Show that the variables are not separable in the equation \(y^{\prime}(t)=t+y .\) That is, there are not two functions, \(g(t)\) and \(h(y),\) which for all \(t\) and \(y \quad t+y=g(t) \times h(y)\) A procedure is to assume two such functions, \(g(t)\) and \(h(y)\) exist and then show that the following equations are incompatible. \(\begin{array}{lllll}t=0 & y=0 & t=0 & y=1 & t=1 & y=0\end{array}\) \(g(0) \times h(0)=0+0=0 \quad g(0) \times h(1)=0+1=1 \quad g(1) \times h(0)=1+0=1\) Show that \(g(0) \times h(0)=0, g(0) \times h(1)=1\) and \(g(1) \times h(0)=1\) are incompatible.

Parameter reduced population models are shown below. In the Ricker equation, find a condition on \(\gamma_{0}\) that will insure that there is a value of \(v\) for which the population is growing the fastest. In the Beverton-Holt equation show that there is no value of \(v\) for which the population is growing the fastest. In the Gompertz equation, find the value of \(v\) for which the population is growing the fastest. $$\text { a. } \quad v^{\prime}=v e^{-v}-\gamma_{0} v \text { Ricker }$$$$\begin{array}{l} \text { b. } \quad v^{\prime}=\frac{v}{1+v} \\\\\text { c. } v^{\prime}=-v \ln (v)\end{array}$$ Beverton-Holt Gompertz The three previous problems have important implications for wildlife management, at least conceptually. Suppose you are managing a wildlife population, salmon, for example, as a renewable resource, and wish to annually harvest as many salmon as possible. If you harvest too severely, the next years spawn will be low, and four years later the harvest will be limited. Your optimum strategy is to maintain the population at the level where the growth is the greatest.

Suppose \(y^{\prime}=f(y)\) has three and only three equilibrium points, \(e_{1}, e_{2},\) and \(e_{3},\) where \(f\)and \(f^{\prime}\) are continuous and \(f^{\prime}\left(e_{1}\right) \neq 0, f^{\prime}\left(e_{2}\right) \neq 0,\) and \(f^{\prime}\left(e_{3}\right) \neq 0 .\) Argue that one of \(e_{1}, e_{2},\) and \(e_{3}\) is stable.

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