The deep ocean is a fascinating and extreme environment. As you dive deeper, the weight of the water above you increases, leading to immense pressure. But it's not just the water pushing down on you; the Earth's atmosphere is also pressing down on the ocean's surface. This problem perfectly illustrates how these two pressures combine and how they scale with depth.
Analyzing the Setup
Imagine a submarine cruising at a certain depth h in the ocean. The problem states that the total pressure acting on it at this depth is 3×105 Pa. We are also given the atmospheric pressure, p0=1×105 Pa.
Our goal is to find out what happens to the pressure when the submarine dives to twice its original depth, 2h, and specifically, to calculate the percentage increase in that pressure.
The Master Equation
To solve this, we need the fundamental equation for absolute pressure in a fluid:
Here, p is the total (absolute) pressure, p0 is the atmospheric pressure at the surface, ρ is the density of the fluid, g is the acceleration due to gravity, and h is the depth.
The term ρgh represents the gauge pressure—the pressure exerted solely by the weight of the water column above the submarine.
Finding the Gauge Pressure
Let's apply our master equation to the initial state of the submarine. We know the initial pressure pi is 3×105 Pa:
By subtracting the atmospheric pressure from the total pressure, we can isolate the gauge pressure:
This tells us that at depth h, the water alone exerts a pressure of 2×105 Pa. Notice that we didn't even need to use the given values for the density of water (ρ) or gravity (g)! Treating ρgh as a single variable simplifies the math tremendously.
Diving Deeper
The New Pressure
Now, the submarine dives to a new depth of 2h. Let's write the pressure equation for this new depth. The final pressure pf will be:
We can rearrange this to make use of the gauge pressure we just found:
Now, we simply substitute our known values back into the equation. We know p0=1×105 Pa and ρgh=2×105 Pa:
So, at twice the depth, the total pressure is 5×105 Pa. Notice that the pressure didn't simply double from 3×105 to 6×105. This is a common trap! The pressure doesn't double because the atmospheric pressure p0 is a constant addition that doesn't scale with depth.
Final Calculation
Percentage Increase
Finally, we need to find the percentage increase in pressure. The formula for percentage increase is:
% Increase=Initial ValueFinal Value−Initial Value×100
Substituting our pressure values:
% Increase=pipf−pi×100
% Increase=3×1055×105−3×105×100
% Increase=3×1052×105×100
The 105 terms cancel out beautifully, leaving us with:
% Increase=32×100=3200%
And there we have it! The pressure increases by 3200%, which corresponds to option (a). This problem is a fantastic reminder to always account for atmospheric pressure when dealing with absolute pressure in fluids.