The Physics of Trapped Air
A Journey Through Boyle's Law and Fluid Statics
Imagine you are in a laboratory, holding a glass tube partially submerged in a pool of shimmering liquid mercury. This classic setup is not just a visual treat; it is a profound demonstration of the invisible forces that govern our atmosphere and the gases around us. Let's dive into the mechanics of this fascinating problem.
Analyzing the Initial State
We start with an open glass tube immersed in mercury, with exactly 8 cm extending above the surface. When we seal the top, we trap a specific amount of air inside. Because the tube was open to the atmosphere just before sealing, the pressure of this trapped air, p1, is perfectly balanced with the outside world.
Therefore, p1=patm=76 cm of Hg.
If we assume the cross-sectional area of the tube is A, the initial volume of this trapped air is simply the area multiplied by the height: V1=8A.
The Upward Pull and Fluid Statics
Now, the plot thickens. We raise the tube vertically by an additional 46 cm. The total length of the tube extending above the outside mercury level is now 8+46=54 cm.
As we pull the tube up, the pressure inside drops, and the atmospheric pressure pushes mercury up into the tube. Let's call the new length of the air column x. This means the mercury has risen inside the tube to a height of (54−x) cm.
How do we find the new pressure, p2, of the trapped air? We rely on the fundamental principle of fluid statics: the pressure at the same horizontal level in a continuous static fluid must be equal.
If we look at the horizontal level of the outside mercury surface, the pressure is patm. Inside the tube at this exact same level, the pressure is the sum of the trapped air's pressure (p2) and the pressure exerted by the column of mercury above it.
Solving for p2, we get a beautiful expression dependent entirely on our unknown x:
Boyle's Law in Action
Because this process happens slowly, the temperature of the trapped air remains constant. This is the perfect scenario to deploy Boyle's Law, which states that for a fixed mass of gas at a constant temperature, the product of pressure and volume is constant.
Let's substitute our knowns and expressions into this master equation:
The Final Calculation
The cross-sectional area A elegantly cancels out from both sides, leaving us with a pure algebraic equation:
Rearranging this into a standard quadratic form, we get:
To solve this, we look for two numbers that multiply to −608 and add to 22. Those numbers are 38 and −16. Factoring the quadratic gives:
This yields two mathematical solutions: x=−38 and x=16. Since a physical length cannot be negative, we discard −38.
Thus, the new length of the air column is exactly 16 cm. By carefully balancing fluid pressures and applying the laws of thermodynamics, we've successfully decoded the hidden mechanics of the trapped air!