Problem 26
Question
If the temperature of a plate at the point \((x, y)\) is \(T(x, y)=10+x^{2}-y^{2}\), find the path a heat-seeking particle (which always moves in the direction of greatest increase in temperature) would follow if it starts at \((-2,1) .\) Hint: The particle moves in the direction of the gradient $$ \nabla T=2 x \mathbf{i}-2 y \mathbf{j} $$ We may write the path in parametric form as $$ \mathbf{r}(t)=x(t) \mathbf{i}+y(t) \mathbf{j} $$ and we want \(x(0)=-2\) and \(y(0)=1 .\) To move in the required direction means that \(\mathbf{r}^{\prime}(t)\) should be parallel to \(\nabla T\). This will be satisfied if $$ \frac{x^{\prime}(t)}{2 x(t)}=-\frac{y^{\prime}(t)}{2 y(t)} $$ together with the conditions \(x(0)=-2\) and \(y(0)=1\). Now solve this differential equation and evaluate the arbitrary constant of integration.
Step-by-Step Solution
VerifiedKey Concepts
Differential Equations - Nature and Solution
We derive a differential equation to model this path using the condition \( \frac{x^{\prime}(t)}{2x(t)} = -\frac{y^{\prime}(t)}{2y(t)} \). This stems from the need for the derivative of the path, \( \mathbf{r}^{\prime}(t) \), to be parallel to the gradient vector. By solving this differential equation, we set the mathematical foundation for understanding how variables \(x\) and \(y\) evolve in time as the particle moves.
This equation is formulated by assuming a proportional relationship between derivatives of \(x(t)\) and \(y(t)\), captured by a constant \(K\). We then decouple the equation into two simpler differential equations, \( \frac{x^{\prime}(t)}{x(t)} = K \) and \( \frac{y^{\prime}(t)}{y(t)} = -K \), simplifying the integral process. Solving these will yield the parametric functions that describe the particle's trajectory.
Parametric Equations - Expressing the Path
The parametric representation \( \mathbf{r}(t) = x(t) \mathbf{i} + y(t) \mathbf{j} \) encompasses both spatial coordinates \(x(t)\) and \(y(t)\) as functions dependent on \(t\). Each coordinate function can be independently considered, linking changes in \(x\) and \(y\) directly to time progression.
Solving the differential equations gives us exponential functions, \( x(t) = x_0 e^{Kt} \) and \( y(t) = y_0 e^{-Kt} \). These solutions map how exactly the particle travels through the temperature field, consistently adapting to the most significant temperature changes the gradient outlines. As such, each function serves to parameterize not just position, but orientational change–a continuous representation of the particle's movement.
Initial Conditions - Determining Specific Solutions
In this problem, our initial conditions are \( x(0) = -2 \) and \( y(0) = 1 \), which inform us of the particle's position at time \( t = 0 \). Applying these conditions to our parametric solutions \( x(t) = x_0 e^{Kt} \) and \( y(t) = y_0 e^{-Kt} \), we find \( x_0 = -2 \) and \( y_0 = 1 \).
This anchoring in place allows us not only to ensure that our given solution coincides with the particle's known starting point but ultimately dictates the path that will be traced. Without such initial conditions, any number of potential paths could satisfy the differential equation, but specificity integrates practical demands with theoretical solutions.