The Physics of the Empty Space
Imagine you are holding a sturdy bakelite beaker in your hands. It has a total volume capacity of 500 cc. Now, you pour a small amount of liquid mercury into it. The mercury settles at the bottom, occupying a volume Vm.
The space that remains empty above the mercury is what we call the unfilled volume. Mathematically, this is simply the difference between the total capacity of the beaker and the volume of the mercury inside it.
This equation is our visual anchor. It perfectly describes the physical reality of the setup at any given temperature.
The Balancing Act of Thermal Expansion
Now, the problem introduces a fascinating constraint: as we heat the system and the temperature varies, this unfilled volume remains absolutely constant.
Let's think about what happens when we increase the temperature. The bakelite beaker will undergo thermal expansion, increasing its total capacity. If the mercury didn't expand, the empty space would simply get larger. However, the mercury also expands, and it does so quite aggressively!
For the empty space to remain exactly the same, the extra volume created by the expanding beaker must be perfectly filled by the expanding mercury. This is a beautiful balancing act of thermal physics.
This tells us that the absolute change in volume for both the beaker and the mercury must be identical.
The Master Equation
To proceed, we need to bring in the fundamental law of volumetric thermal expansion. The change in volume ΔV of any substance is proportional to its initial volume V, its coefficient of volume expansion γ, and the change in temperature ΔT.
We can substitute this powerful tool into our balancing equation for both the beaker and the mercury.
Notice how the temperature change ΔT appears on both sides of the equation. Because the beaker and the mercury are in thermal equilibrium and experience the same temperature change, we can elegantly cancel ΔT out.
Crunching the Numbers
We have now isolated the core relationship. Our goal is to find the initial volume of the mercury, Vm. Let's rearrange the equation to solve for it.
Now, we carefully substitute the numerical values provided in the problem. The volume of the beaker Vb is 500 cc. The expansion coefficient of the bakelite beaker γb is 6×10−6∘C−1, and for the mercury γm is 1.5×10−4∘C−1.
Let's simplify the numerator first. Multiplying 500 by 6 gives 3000, which can be written as 3×103.
Vm=1.5×10−43×103×10−6=1.5×10−43×10−3
Finally, we divide the coefficients and the powers of ten. 3 divided by 1.5 is exactly 2. And 10−3 divided by 10−4 leaves us with 101, or 10.
The Real-World Application
The required volume of mercury is exactly 20 cc.
Take a moment to appreciate this result. The mercury's volume is only 4% of the beaker's total volume. Yet, because mercury's expansion coefficient is 25 times larger than that of bakelite, this tiny puddle of liquid expands just enough to perfectly match the expansion of the entire massive beaker!
This exact principle—balancing different rates of thermal expansion—is the foundational engineering concept behind designing accurate liquid-in-glass thermometers and compensating pendulums in grandfather clocks.