The problem of a floating cube undergoing thermal expansion is a beautiful intersection of Archimedes' principle and thermodynamics. It challenges us to think about how multiple physical properties—volume, area, and density—change simultaneously when heat is applied.
The Principle of Flotation
Imagine a solid cube floating peacefully in a liquid bath. For it to remain in equilibrium, the upward buoyant force, commonly known as upthrust, must perfectly balance the downward pull of gravity, which is its weight.
According to Archimedes' principle, the upthrust is equal to the weight of the liquid displaced by the submerged portion of the cube. If we let the cube's cross-sectional area be A and its submerged depth be hi, the immersed volume is Vi=Ahi. Therefore, the initial upthrust FB can be written as:
where ρL is the initial density of the liquid and g is the acceleration due to gravity.
Turning Up the Heat
Now, we introduce thermal energy into the system, raising the temperature by ΔT. This causes both the solid cube and the liquid to expand. However, the problem provides a fascinating constraint: the submerged depth hi remains exactly the same.
Even though the cube has expanded, its mass is conserved, meaning its weight remains constant. Consequently, the new upthrust FB′ must still equal the original weight to maintain flotation:
The Master Equation
Let's determine the new parameters after heating. The cube's cross-sectional area expands according to the laws of superficial expansion. Since the coefficient of linear expansion is αs, the areal expansion coefficient is 2αs. The new area A′ is:
Simultaneously, the liquid expands volumetrically. As its volume increases, its density decreases. The new density ρL′ is given by:
where γl is the coefficient of volume expansion of the liquid. The new upthrust is the product of the new immersed volume (A′hi), the new density, and gravity:
FB′=A(1+2αsΔT)hi(1+γlΔTρL)g
The Elegant Conclusion
Equating the initial and final upthrusts, we get our master equation:
AhiρLg=A(1+2αsΔT)hi(1+γlΔTρL)g
Notice how the physical constants and initial dimensions—A, hi, ρL, and g—appear on both sides. Canceling them out simplifies the equation dramatically:
Cross-multiplying yields:
Subtracting 1 from both sides and dividing by ΔT, we arrive at the final, elegant relation:
This result tells us a profound physical truth: for the submerged depth to remain constant, the volumetric expansion of the liquid must perfectly match the areal expansion of the solid's base!