The Setup
A Tale of Two Fluids
Imagine a classic U-tube experiment. Initially, we have pure water resting peacefully, perfectly balanced in both arms at a height of 0.29m from the bottom. The system is in perfect equilibrium.
Then, we disrupt this peace by pouring kerosene into the left arm until it forms a column of 0.1m. Kerosene is lighter than water (density 800 kg m−3 compared to water's 1000 kg m−3) and immiscible, meaning it floats on top without mixing. The added weight of the kerosene pushes the water down in the left arm, forcing it to rise in the right arm. Our goal is to find the new ratio of the total liquid heights, h2h1.
The Unbreakable Rule
Conservation of Volume
Water is an incompressible fluid. This means the total volume of water in the U-tube cannot change. Because the U-tube has a uniform cross-sectional area, the total length of the water column must also remain constant.
Initially, the total length of the water column was 0.29m+0.29m=0.58m.
In the final state, the total height of the liquid in the left arm is h1. Since the top 0.1m is kerosene, the height of the water in the left arm is (h1−0.1). The height of the water in the right arm is simply h2. Equating the final total water length to the initial total water length gives us our first master equation:
Rearranging this, we get:
Pascal's Law
Balancing the Pressures
Now, let's look at the physics of the fluids at rest. According to Pascal's Law, the pressure at any two points at the same horizontal level in a continuous, stationary fluid must be equal. The easiest place to apply this is at the very bottom of the U-tube.
The pressure at the bottom of the left arm is the sum of atmospheric pressure (P0), the pressure exerted by the kerosene column, and the pressure exerted by the water column:
Pleft=P0+ρkg(0.1)+ρwg(h1−0.1)
The pressure at the bottom of the right arm is the sum of atmospheric pressure and the pressure from its water column:
Equating the two pressures (Pleft=Pright), we notice that atmospheric pressure P0 and the acceleration due to gravity g cancel out beautifully:
ρk(0.1)+ρw(h1−0.1)=ρwh2
Substituting the given densities (ρk=800 and ρw=1000):
800(0.1)+1000(h1−0.1)=1000h2
The Final Calculation
We now have a beautifully simple system of two linear equations:
1. h1+h2=0.68
2. h1−h2=0.02
Adding the two equations eliminates h2:
Subtracting the second equation from the first eliminates h1:
Finally, we find the requested ratio:
The correct option is (B).