Analyzing the Setup
Imagine you are standing on the surface of a solid iron ball with a radius of 10 cm. You are watching a layer of ice, with a uniform thickness x, slowly melt away.
The total radius of the sphere, including the ice, is R=10+x. The volume of the ice is the difference between the total volume and the volume of the iron core:
This equation serves as our foundation for the problem.
The Power of Calculus
To understand how this volume changes over time, we differentiate our volume equation with respect to time t. Using the chain rule, the derivative of the first term is 34π⋅3(10+x)2⋅dtdx, and the derivative of the constant term is zero.
This simplifies beautifully to the following master equation:
This equation links the rate of volume change to the rate of thickness change. Notice how the 3s cancel out, leaving us with a clean, elegant expression.
The Final Calculation
We know the ice is melting at 50 cm3/min, so dtdV=−50. We want to find dtdx when x=5.
Substituting these values into our master equation, we get:
Simplifying the bracket, we have −50=4π(15)2dtdx, which becomes:
Multiplying the constants, we get −50=900πdtdx. Finally, isolating dtdx, we find:
Simplifying this fraction, we get the final result:
The negative sign confirms the thickness is decreasing, and the magnitude of the rate is 18π1 cm/min. We have successfully navigated the geometry and the calculus to find the answer!