The Setup
A Submerged Oscillator
Imagine a block of mass m attached to a spring of constant k, completely submerged in a container of water. We stretch the spring by a distance xm and let it go.
It begins to oscillate, but this isn't an ideal, frictionless world. The water provides a viscous drag, a damping force that opposes the motion of the block.
The Fate of Mechanical Energy
Because of this damping, the amplitude of the oscillations gradually decreases until the block comes to a complete stop. But where does the energy go?
The First Law of Thermodynamics tells us that energy cannot be destroyed. The initial mechanical energy of the system, which was entirely stored as elastic potential energy in the stretched spring, is dissipated as heat.
This heat doesn't just vanish; it is absorbed by the water and the block, causing their temperature to rise.
Calculating the Energy
Let's quantify this. The initial mechanical energy Emech is given by the potential energy of the stretched spring:
Emech=21kxm2
Substituting the given values (k=800 N/m and xm=2 cm=0.02 m):
Emech=21(800)(0.02)2=0.16 J
The Thermal Response
Now, this 0.16 J of heat energy is absorbed by the block and the water. To find the temperature rise ΔT, we need the total heat capacity C of the system.
The heat capacity is the sum of the heat capacities of the individual components:
C=mblocksblock+mwaterswater
Plugging in the masses and specific heats:
C=(0.5 kg)(400 J/kg K)+(1 kg)(4184 J/kg K)
C=200+4184=4384 J/K
The Final Temperature Rise
Equating the mechanical energy to the thermal energy (Q=CΔT):
0.16=4384×ΔT
ΔT=43840.16≈3.65×10−5 K
This is an incredibly tiny temperature rise! Looking at our options, the order of magnitude is clearly 10−5 K.
This problem beautifully illustrates how macroscopic mechanical energy transforms into microscopic thermal energy, bridging the gap between mechanics and thermodynamics.