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transform the given initial value problem into an equivalent problem with the initial point at the origin. $$ d y / d t=1-y^{3}, \quad y(-1)=3 $$

Short Answer

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Question: Determine the equivalent problem with the initial point at the origin for the given initial value problem: \(dy/dt = 1 - y^3, y(-1) = 3\). Answer: The equivalent problem with the initial point at the origin is: \(\frac{d y_T}{dt} = 1 - {y_T}^3, y_T(0) = y_0\).

Step by step solution

01

Write down the given initial value problem

The given initial value problem is: $$ \frac{dy}{dt} = 1 - y^3, \quad y(-1) = 3 $$
02

Find the general solution of the differential equation

Let's first find the general solution of the given differential equation, ignoring the initial condition for now. To do this, we need to solve: $$ \frac{dy}{dt} = 1 - y^3 $$ This is a first-order separable differential equation. To solve it, we will separate the variables and then integrate both sides. Separate the variables as follows: $$ \frac{dy}{1 - y^3} = dt $$ Now integrate both sides with respect to their respective variables: $$ \int \frac{dy}{1 - y^3} = \int dt $$ Integrating gives us: $$ \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y}{\sqrt[3]{2}}\right) = t + C $$ where C is the constant of integration.
03

Determine the constant of integration C given the original initial condition

Now we will use the initial condition given in the problem \(y(-1) = 3\). Plugging this into our general solution, we get: $$ \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) = -1 + C $$ Solving for C, we get: $$ C = \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) + 1 $$
04

Write down the complete solution with the determined constant

Substituting C into our solution from Step 2, the complete solution for our given initial value problem becomes: $$ \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y}{\sqrt[3]{2}}\right) = t + \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) + 1 $$
05

Transform the solution to have the initial point at the origin

Let's denote the transformed function as \(y_T(t)\) and the initial value of this function as \(y_T(0) = y_0\). We want to find a function \(y_T(t)\) that has the same shape as our original solution but is shifted so that its initial point is at the origin. To do this, we can simply replace \(t\) with \((t-T)\) in our solution and use the new initial condition \(y_T(0) = y_0\) to find \(T\): $$ \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y_T}{\sqrt[3]{2}}\right) = (t - T) + \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) + 1 $$ Now, plug in the new initial condition \(y_T(0) = y_0\): $$ \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y_0}{\sqrt[3]{2}}\right) = - T + \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) + 1 $$ Solve for \(T\): $$ T = \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) - \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y_0}{\sqrt[3]{2}}\right) + 1 $$
06

Write down the transformed initial value problem

The equivalent problem with the initial point at the origin is: $$ \frac{d y_T}{dt} = 1 - {y_T}^3, \quad y_T(0) = y_0 $$ and the transformed solution is: $$ \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y_T}{\sqrt[3]{2}}\right) = (t - T) + \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) + 1 $$ with $$ T = \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{3}{\sqrt[3]{2}}\right) - \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y_0}{\sqrt[3]{2}}\right) + 1 $$

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Key Concepts

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

Differential Equations
When students tackle differential equations, they are dealing with a fundamental topic in mathematics that describes the rate of change of a variable in relation to another variable. Imagine you are observing how fast water is draining from a tub; a differential equation would allow you to represent the rate at which the water's level is dropping as a function of time. In the context of the given exercise, the rate at which the function y changes with respect to time t is expressed by the equation \( \frac{dy}{dt} = 1 - y^3 \).

The solution to this kind of equation usually involves finding a function that satisfies the rate of change specified. But when an additional piece of information such as an initial value is provided, like \( y(-1) = 3 \), you’re dealing with an initial value problem. This means you’re not just looking for any solution to the differential equation - you're looking for the specific solution that lines up with the initial conditions given.
Separable Variables
The technique of separable variables is like finding the right dance steps that allow both partners, y and t, to move smoothly across the dance floor - or in more mathematical terms, to isolate variables on each side of the equation. The key move here is to rearrange the equation so that all the y terms are on one side and all the t terms are on the other. For our problem, this led to \( \frac{dy}{1 - y^3} = dt \).

Once the variables are separated, the path forward is to integrate each side with respect to its own variable, almost like honoring the personal space of each dancer. This method transforms the differential equation into a solvable problem, as we've observed in the given solution steps. Remember, the integration might introduce a constant of integration, which can be determined later by your initial conditions.
Integration of Differential Equations
The step of integrating differential equations can be equated to charting a course on a map. You know where you’re starting from, thanks to the initial values, and you want to find how your variables will behave on the entire journey. To integrate a term like \( \frac{dy}{1 - y^3} \), you may need to recall methods from calculus involving inverse trigonometric functions or partial fraction decomposition.

In our textbook example, integration leads to the expression \( \frac{1}{\sqrt[3]{2}}\operatorname{arctanh}\left(\frac{y}{\sqrt[3]{2}}\right) = t + C \), which still contains an unknown constant C. This is where the initial conditions come into play, allowing you to pin down the value of C and complete the map that describes the relationship between y and t throughout their journey. Understanding the integration process is crucial because it transitions us from the generalized family of solutions to the unique solution that fits our problem.

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Most popular questions from this chapter

Determine whether or not each of the equations is exact. If it is exact, find the solution. $$ \left(2 x y^{2}+2 y\right)+\left(2 x^{2} y+2 x\right) y^{\prime}=0 $$

Harvesting a Renewable Resource. Suppose that the population \(y\) of a certain species of fish (for example, tuna or halibut) in a given area of the ocean is described by the logistic equation $$ d y / d t=r(1-y / K) y . $$ While it is desirable to utilize this source of food, it is intuitively clear that if too many fish are caught, then the fish population may be reduced below a useful level, and possibly even driven to extinction. Problems 20 and 21 explore some of the questions involved in formulating a rational strategy for managing the fishery. At a given level of effort, it is reasonable to assume that the rate at which fish are caught depends on the population \(y:\) The more fish there are, the easier it is to catch them. Thus we assume that the rate at which fish are caught is given by \(E y,\) where \(E\) is a positive constant, with units of \(1 /\) time, that measures the total effort made to harvest the given species of fish. To include this effect, the logistic equation is replaced by $$ d y / d t=r(1-y / K) y-E y $$ This equation is known as the Schaefer model after the biologist, M. B. Schaefer, who applied it to fish populations. (a) Show that if \(E0 .\) (b) Show that \(y=y_{1}\) is unstable and \(y=y_{2}\) is asymptotically stable. (c) A sustainable yield \(Y\) of the fishery is a rate at which fish can be caught indefinitely. It is the product of the effort \(E\) and the asymptotically stable population \(y_{2} .\) Find \(Y\) as a function of the effort \(E ;\) the graph of this function is known as the yield-effort curve. (d) Determine \(E\) so as to maximize \(Y\) and thereby find the maximum sustainable yield \(Y_{m}\).

Involve equations of the form \(d y / d t=f(y)\). In each problem sketch the graph of \(f(y)\) versus \(y,\) determine the critical (equilibrium) points, and classify each one as asymptotically stable or unstable. $$ d y / d t=-2(\arctan y) /\left(1+y^{2}\right), \quad-\infty

draw a direction field and plot (or sketch) several solutions of the given differential equation. Describe how solutions appear to behave as \(t\) increases, and how their behavior depends on the initial value \(y_{0}\) when \(t=0\). $$ y^{\prime}=t-1-y^{2} $$

(a) Verify that both \(y_{1}(t)=1-t\) and \(y_{2}(t)=-t^{2} / 4\) are solutions of the initial value problem $$ y^{\prime}=\frac{-t+\left(t^{2}+4 y\right)^{1 / 2}}{2}, \quad y(2)=-1 $$ Where are these solutions valid? (b) Explain why the existence of two solutions of the given problem does not contradict the uniqueness part of Theorem 2.4 .2 (c) Show that \(y=c t+c^{2},\) where \(c\) is an arbitrary constant, satisfies the differential equation in part (a) for \(t \geq-2 c .\) If \(c=-1,\) the initial condition is also satisfied, and the solution \(y=y_{1}(t)\) is obtained. Show that there is no choice of \(c\) that gives the second solution \(y=y_{2}(t) .\)

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