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Variation of Pressure with Depth in a Fluid

Module by: OpenStax College. E-mail the author

Summary:

  • Define pressure in terms of weight.
  • Explain the variation of pressure with depth in a fluid.
  • Calculate density given pressure and altitude.

If your ears have ever popped on a plane flight or ached during a deep dive in a swimming pool, you have experienced the effect of depth on pressure in a fluid. At the Earth’s surface, the air pressure exerted on you is a result of the weight of air above you. This pressure is reduced as you climb up in altitude and the weight of air above you decreases. Under water, the pressure exerted on you increases with increasing depth. In this case, the pressure being exerted upon you is a result of both the weight of water above you and that of the atmosphere above you. You may notice an air pressure change on an elevator ride that transports you many stories, but you need only dive a meter or so below the surface of a pool to feel a pressure increase. The difference is that water is much denser than air, about 775 times as dense.

Consider the container in Figure 1. Its bottom supports the weight of the fluid in it. Let us calculate the pressure exerted on the bottom by the weight of the fluid. That pressure is the weight of the fluid mgmg size 12{ ital "mg"} {} divided by the area AA size 12{A} {} supporting it (the area of the bottom of the container):

P=mgA.P=mgA. size 12{P= { { ital "mg"} over {A} } } {}
(1)

We can find the mass of the fluid from its volume and density:

m=ρV.m=ρV. size 12{m=ρV} {}
(2)

The volume of the fluid VV size 12{V} {} is related to the dimensions of the container. It is

V=Ah,V=Ah, size 12{V= ital "Ah"} {}
(3)

where AA size 12{A} {} is the cross-sectional area and hh size 12{h} {} is the depth. Combining the last two equations gives

m=ρAh.m=ρAh. size 12{m=ρ ital "Ah"} {}
(4)

If we enter this into the expression for pressure, we obtain

P=ρAhgA.P=ρAhgA. size 12{P= { { left (ρ ital "Ah" right )g} over {A} } } {}
(5)

The area cancels, and rearranging the variables yields

P=hρg.P=hρg. size 12{P=hρg} {}
(6)

This value is the pressure due to the weight of a fluid. The equation has general validity beyond the special conditions under which it is derived here. Even if the container were not there, the surrounding fluid would still exert this pressure, keeping the fluid static. Thus the equation P=hρgP=hρg size 12{P=hρg} {} represents the pressure due to the weight of any fluid of average density ρρ size 12{ρ} {} at any depth hh size 12{h} {} below its surface. For liquids, which are nearly incompressible, this equation holds to great depths. For gases, which are quite compressible, one can apply this equation as long as the density changes are small over the depth considered. Example 2 illustrates this situation.

Figure 1: The bottom of this container supports the entire weight of the fluid in it. The vertical sides cannot exert an upward force on the fluid (since it cannot withstand a shearing force), and so the bottom must support it all.
A container with fluid filled to a depth h. The fluid’s weight w equal to m times g is shown by an arrow pointing downward. A denotes the area of the fluid at the bottom of the container and as well as on the surface.

Example 1: Calculating the Average Pressure and Force Exerted: What Force Must a Dam Withstand?

In (Reference), we calculated the mass of water in a large reservoir. We will now consider the pressure and force acting on the dam retaining water. (See Figure 2.) The dam is 500 m wide, and the water is 80.0 m deep at the dam. (a) What is the average pressure on the dam due to the water? (b) Calculate the force exerted against the dam and compare it with the weight of water in the dam (previously found to be 1.96×1013N1.96×1013N).

Strategy for (a)

The average pressure P ¯ P ¯ due to the weight of the water is the pressure at the average depth h ¯ h ¯ of 40.0 m, since pressure increases linearly with depth.

Solution for (a)

The average pressure due to the weight of a fluid is

P ¯ =h¯ ρg. P ¯ =h¯ ρg. size 12{P=hρg} {}
(7)

Entering the density of water from (Reference) and taking h ¯ h ¯ size 12{h} {} to be the average depth of 40.0 m, we obtain

P ¯ = ( 40.0 m ) 10 3 kg m 3 9.80 m s 2 = 3.92 × 10 5 N m 2 = 392 kPa. P ¯ = ( 40.0 m ) 10 3 kg m 3 9.80 m s 2 = 3.92 × 10 5 N m 2 = 392 kPa.
(8)

Strategy for (b)

The force exerted on the dam by the water is the average pressure times the area of contact:

F=P¯A.F=P¯A. size 12{F= {overline {P}} A} {}
(9)

Solution for (b)

We have already found the value for P¯P¯ size 12{ { bar {P}}} {}. The area of the dam is A=80.0 m×500 m=4.00×104 m2A=80.0 m×500 m=4.00×104 m2 size 12{A="80" "." 0`m times "500"`m=4 "." "00" times "10" rSup { size 8{4} } `m rSup { size 8{2} } } {}, so that

F = ( 3.92 × 10 5 N/m 2 ) ( 4.00 × 10 4 m 2 ) = 1.57 × 10 10 N. F = ( 3.92 × 10 5 N/m 2 ) ( 4.00 × 10 4 m 2 ) = 1.57 × 10 10 N. alignl { stack { size 12{F= \( 3 "." "92" times "10" rSup { size 8{5} } `"N/m" rSup { size 8{2} } \) \( 4 "." "00" times "10" rSup { size 8{4} } `m rSup { size 8{2} } \) } {} # " "=1 "." "57" times "10" rSup { size 8{"10"} } `N "." {} } } {}
(10)

Discussion

Although this force seems large, it is small compared with the 1.96×1013N1.96×1013N size 12{1 "." "96" times "10" rSup { size 8{"13"} } `N} {} weight of the water in the reservoir—in fact, it is only 0.0800%0.0800% of the weight. Note that the pressure found in part (a) is completely independent of the width and length of the lake—it depends only on its average depth at the dam. Thus the force depends only on the water’s average depth and the dimensions of the dam, not on the horizontal extent of the reservoir. In the diagram, the thickness of the dam increases with depth to balance the increasing force due to the increasing pressure.epth to balance the increasing force due to the increasing pressure.

Figure 2: The dam must withstand the force exerted against it by the water it retains. This force is small compared with the weight of the water behind the dam.
A two-dimensional view of a dam with dimensions L and h is shown. Force F at h is shown by a horizontal arrow. The force F exerted by water on the dam is F equals average pressure p bar into area A and pressure in turn is average height h bar into density rho into acceleration due to gravity g.

Atmospheric pressure is another example of pressure due to the weight of a fluid, in this case due to the weight of air above a given height. The atmospheric pressure at the Earth’s surface varies a little due to the large-scale flow of the atmosphere induced by the Earth’s rotation (this creates weather “highs” and “lows”). However, the average pressure at sea level is given by the standard atmospheric pressure PatmPatm size 12{P rSub { size 8{"atm"} } } {}, measured to be

1 atmosphere (atm)=Patm=1.01×105 N/m2=101 kPa.1 atmosphere (atm)=Patm=1.01×105 N/m2=101 kPa. size 12{1`"atmosphere"` \( "atm" \) =P rSub { size 8{"atm"} } =1 "." "01" times "10" rSup { size 8{5} } `"N/m" rSup { size 8{2} } ="101"`"kPa"} {}
(11)

This relationship means that, on average, at sea level, a column of air above 1.00m21.00m2 of the Earth’s surface has a weight of 1.01×105 N1.01×105 N size 12{1 "." "01" times "10" rSup { size 8{5} } `N} {}, equivalent to 1 atm1 atm. (See Figure 3.)

Figure 3: Atmospheric pressure at sea level averages 1.01×105 Pa1.01×105 Pa size 12{1 "." "01" times "10" rSup { size 8{5} } `"Pa"} {} (equivalent to 1 atm), since the column of air over this 1 m21 m2 size 12{1`m rSup { size 8{2} } } {}, extending to the top of the atmosphere, weighs 1.01×105 N1.01×105 N size 12{1 "." "01" times "10" rSup { size 8{5} } " N"} {}.
Figure shows a column of air exerting a weight of one point zero one times ten to the power five newtons on a rectangular patch of ground of one square meter cross section.

Example 2: Calculating Average Density: How Dense Is the Air?

Calculate the average density of the atmosphere, given that it extends to an altitude of 120 km. Compare this density with that of air listed in (Reference).

Strategy

If we solve P=hρgP=hρg size 12{P=hρg} {} for density, we see that

ρ¯=Phg.ρ¯=Phg. size 12{ { bar {ρ}}= { {P} over { ital "hg"} } } {}
(12)

We then take PP size 12{P} {} to be atmospheric pressure, hh size 12{h} {} is given, and gg size 12{g} {} is known, and so we can use this to calculate ρ¯ρ¯ size 12{ { bar {ρ}}} {}.

Solution

Entering known values into the expression for ρ¯ρ¯ size 12{ { bar {ρ}}} {} yields

ρ¯=1.01×105 N/m2(120×103 m)(9.80 m/s2)=8.59×102 kg/m3.ρ¯=1.01×105 N/m2(120×103 m)(9.80 m/s2)=8.59×102 kg/m3. size 12{ { bar {ρ}}= { {1 "." "01" times "10" rSup { size 8{5} } `"N/m" rSup { size 8{2} } } over { \( "120" times "10" rSup { size 8{3} } `m \) \( 9 "." "80"`"m/s" rSup { size 8{2} } \) } } =8 "." "59" times "10" rSup { size 8{ - 2} } `"kg/m" rSup { size 8{3} } } {}
(13)

Discussion

This result is the average density of air between the Earth’s surface and the top of the Earth’s atmosphere, which essentially ends at 120 km. The density of air at sea level is given in (Reference) as 1.29 kg/m31.29 kg/m3 size 12{1 "." "29"`"kg/m" rSup { size 8{3} } } {} —about 15 times its average value. Because air is so compressible, its density has its highest value near the Earth’s surface and declines rapidly with altitude.

Example 3: Calculating Depth Below the Surface of Water: What Depth of Water Creates the Same Pressure as the Entire Atmosphere?

Calculate the depth below the surface of water at which the pressure due to the weight of the water equals 1.00 atm.

Strategy

We begin by solving the equation P=hρgP=hρg size 12{P=hρg} {} for depth hh size 12{h} {}:

h=Pρg.h=Pρg. size 12{h= { {P} over {ρg} } } {}
(14)

Then we take PP size 12{P} {} to be 1.00 atm and ρρ size 12{ρ} {} to be the density of the water that creates the pressure.

Solution

Entering the known values into the expression for hh size 12{h} {} gives

h=1.01×105 N/m2(1.00×103 kg/m3)(9.80 m/s2)=10.3 m.h=1.01×105 N/m2(1.00×103 kg/m3)(9.80 m/s2)=10.3 m. size 12{h= { {1 "." "01" times "10" rSup { size 8{5} } `"N/m" rSup { size 8{2} } } over { \( 1 "." "00" times "10" rSup { size 8{3} } `"kg/m" rSup { size 8{3} } \) \( 9 "." "80"`"m/s" rSup { size 8{2} } \) } } ="10" "." 3`m} {}
(15)

Discussion

Just 10.3 m of water creates the same pressure as 120 km of air. Since water is nearly incompressible, we can neglect any change in its density over this depth.

What do you suppose is the total pressure at a depth of 10.3 m in a swimming pool? Does the atmospheric pressure on the water’s surface affect the pressure below? The answer is yes. This seems only logical, since both the water’s weight and the atmosphere’s weight must be supported. So the total pressure at a depth of 10.3 m is 2 atm—half from the water above and half from the air above. We shall see in Pascal’s Principle that fluid pressures always add in this way.

Section Summary

  • Pressure is the weight of the fluid mgmg size 12{ ital "mg"} {} divided by the area AA size 12{A} {} supporting it (the area of the bottom of the container):
    P=mgA.P=mgA. size 12{P= { { ital "mg"} over {A} } } {}
    (16)
  • Pressure due to the weight of a liquid is given by
    P=hρg,P=hρg, size 12{P=hρg} {}
    (17)

    where PP size 12{P} {} is the pressure, hh size 12{h} {} is the height of the liquid, ρρ size 12{ρ} {} is the density of the liquid, and gg size 12{g} {} is the acceleration due to gravity.

Conceptual Questions

Exercise 1

Atmospheric pressure exerts a large force (equal to the weight of the atmosphere above your body—about 10 tons) on the top of your body when you are lying on the beach sunbathing. Why are you able to get up?

Exercise 2

Why does atmospheric pressure decrease more rapidly than linearly with altitude?

Exercise 3

What are two reasons why mercury rather than water is used in barometers?

Exercise 4

Figure 4 shows how sandbags placed around a leak outside a river levee can effectively stop the flow of water under the levee. Explain how the small amount of water inside the column formed by the sandbags is able to balance the much larger body of water behind the levee.

Figure 4: Because the river level is very high, it has started to leak under the levee. Sandbags are placed around the leak, and the water held by them rises until it is the same level as the river, at which point the water there stops rising.
The figure shows a flooding river on the extreme right, with a levee set up on its left, and sandbags are stacked on the left of the levee. The height of the levee and that of the stacked sandbags is greater than the water level of the flooding river, so the water does not flow over their tops, but a leak under the levee allows some water to flow under it and reach the sandbags.

Exercise 5

Why is it difficult to swim under water in the Great Salt Lake?

Exercise 6

Is there a net force on a dam due to atmospheric pressure? Explain your answer.

Exercise 7

Does atmospheric pressure add to the gas pressure in a rigid tank? In a toy balloon? When, in general, does atmospheric pressure not affect the total pressure in a fluid?

Exercise 8

You can break a strong wine bottle by pounding a cork into it with your fist, but the cork must press directly against the liquid filling the bottle—there can be no air between the cork and liquid. Explain why the bottle breaks, and why it will not if there is air between the cork and liquid.

Problems & Exercises

Exercise 1

What depth of mercury creates a pressure of 1.00 atm?

Solution

0.760 m

Exercise 2

The greatest ocean depths on the Earth are found in the Marianas Trench near the Philippines. Calculate the pressure due to the ocean at the bottom of this trench, given its depth is 11.0 km and assuming the density of seawater is constant all the way down.

Exercise 3

Verify that the SI unit of hρghρg size 12{hρg} {} is N/m2N/m2 size 12{"N/m" rSup { size 8{2} } } {}.

Solution

hρ g units = ( m ) kg/m 3 m/s 2 = kg m 2 / m 3 s 2 = kg m/s 2 1/m 2 = N/m 2 hρ g units = ( m ) kg/m 3 m/s 2 = kg m 2 / m 3 s 2 = kg m/s 2 1/m 2 = N/m 2
(18)

Exercise 4

Water towers store water above the level of consumers for times of heavy use, eliminating the need for high-speed pumps. How high above a user must the water level be to create a gauge pressure of 3.00×105 N/m23.00×105 N/m2 size 12{3 "." "00" times "10" rSup { size 8{5} } `"N/m" rSup { size 8{2} } } {}?

Exercise 5

The aqueous humor in a person’s eye is exerting a force of 0.300 N on the 1.10-cm21.10-cm2 size 12{1 "." "10""-cm" rSup { size 8{2} } } {} area of the cornea. (a) What pressure is this in mm Hg? (b) Is this value within the normal range for pressures in the eye?

Solution

(a) 20.5 mm Hg

(b) The range of pressures in the eye is 12–24 mm Hg, so the result in part (a) is within that range

Exercise 6

How much force is exerted on one side of an 8.50 cm by 11.0 cm sheet of paper by the atmosphere? How can the paper withstand such a force?

Exercise 7

What pressure is exerted on the bottom of a 0.500-m-wide by 0.900-m-long gas tank that can hold 50.0 kg of gasoline by the weight of the gasoline in it when it is full?

Solution

1 . 09 × 10 3 N/m 2 1 . 09 × 10 3 N/m 2 size 12{1 "." "09" times "10" rSup { size 8{3} } `"N/m" rSup { size 8{2} } } {}

Exercise 8

Calculate the average pressure exerted on the palm of a shot-putter’s hand by the shot if the area of contact is 50.0 cm250.0 cm2 size 12{"50" "." 0`"cm" rSup { size 8{2} } } {} and he exerts a force of 800 N on it. Express the pressure in N/m2N/m2 and compare it with the 1.00×106 Pa1.00×106 Pa pressures sometimes encountered in the skeletal system.

Exercise 9

The left side of the heart creates a pressure of 120 mm Hg by exerting a force directly on the blood over an effective area of 15.0 cm2.15.0 cm2. size 12{"15" "." 0`"cm" rSup { size 8{2} } } {} What force does it exert to accomplish this?

Solution

24.0 N

Exercise 10

Show that the total force on a rectangular dam due to the water behind it increases with the square of the water depth. In particular, show that this force is given by F=ρgh2L/2F=ρgh2L/2 size 12{F=ρ ital "gh" rSup { size 8{2} } L/2} {}, where ρρ size 12{ρ} {} is the density of water, hh size 12{h} {} is its depth at the dam, and LL size 12{L} {} is the length of the dam. You may assume the face of the dam is vertical. (Hint: Calculate the average pressure exerted and multiply this by the area in contact with the water. (See Figure 5.)

Figure 5
A two-dimensional view of a dam with dimensions L and h is shown. Force F at h is shown by a horizontal arrow. The force F exerted by water on the dam is F equals average pressure p bar into area A and pressure in turn is average height h bar into density rho into acceleration due to gravity g.

Glossary

pressure:
the weight of the fluid divided by the area supporting it

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