Problem 102
Question
The hammer and the feather When Apollo 15 astronaut David Scott dropped a hammer and a feather on the moon to demonstrate that in a vacuum all bodies fall with the same (constant) acceleration, he dropped them from about \(1.2 \mathrm{m}\) above the ground. The television footage of the event shows the hammer and the feather falling more slowly than on Earth, where, in a vacuum, they would have taken only half a second to fall the \(1.2 \mathrm{m}\). How long did it take the hammer and feather to fall \(1.2 \mathrm{m}\) on the moon? To find out, solve the following initial value problem for \(s\) as a function of \(t .\) Then find the value of \(t\) that makes \(s\) equal to \(0 .\). Differential equation: \(\frac{d^{2} s}{d t^{2}}=-1.6 \mathrm{m} / \mathrm{s}^{2}\) Initial conditions: \(\frac{d s}{d t}=0\) and \(s=1.2\) when \(t=0\)
Step-by-Step Solution
VerifiedKey Concepts
Differential Equations
Constant Acceleration
In the problem, due to this constant acceleration, the velocity changes linearly over time. This makes it easier to predict the motion path of the falling objects, using simple integration techniques.
Integration
- **Velocity Function:** By integrating the acceleration function, we derive the velocity function. In our situation: \[ \frac{ds}{dt} = \int -1.6 \, dt = -1.6t + C_1 \] - **Position Function:** Similarly, we integrate the velocity function to calculate the position: \[ s(t) = \int -1.6t \, dt = -0.8t^2 + C_2 \] Applying initial conditions helps determine the constants \(C_1\) and \(C_2\), giving us precise equations for this specific scenario.
Physics Applications
In the Apollo 15 experiment, the differential equation and its solutions allowed us to predict the path and duration of the hammer and feather's fall on the moon, showcasing that mathematical tools can precisely model physical events. This demonstration emphasized how gravity affects objects regardless of their mass, as per Galileo's principle, specifically when no air resistance is present, like on the moon.