04.08.2013 Views

Fluid Mechanics with teacher's notes

Fluid Mechanics with teacher's notes

Fluid Mechanics with teacher's notes

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

the water pressure pushing up on the bottom of the box is P o + rgh 2. The net<br />

pressure on the box is the sum of these two pressures.<br />

P net = P bottom + P top = (P 0 + rgh 2) – (P 0 + rgh 1) = rg(h 2 − h 1) = rgL<br />

From this result, we can find the net vertical force due to the pressure on the<br />

box as follows:<br />

F net = P netA = rgLA = rgV = m fg<br />

Note that this is an expression of Archimedes’ principle. In general, we can say<br />

that buoyant forces arise from the differences in fluid pressure between the<br />

top and the bottom of an immersed object.<br />

Atmospheric pressure is pressure from above<br />

The weight of the air in the upper portion of Earth’s atmosphere exerts pressure<br />

on the layers of air below. This pressure is called atmospheric pressure; the<br />

force it exerts on our bodies (assuming a body area of 2 m 2 ) is extremely large,<br />

on the order of 200 000 N (40 000 lb). How can we exist under such tremendous<br />

forces <strong>with</strong>out our bodies collapsing? The answer is that our body cavities<br />

and tissues are permeated <strong>with</strong> fluids and gases that are pushing outward<br />

<strong>with</strong> a pressure equal to that of the atmosphere. Consequently, our bodies are<br />

in equilibrium—the force of the atmosphere pushing in equals the internal<br />

force pushing out.<br />

An instrument that is commonly used to measure atmospheric pressure is<br />

the mercury barometer. Figure 9-9 shows a very simple mercury barometer. A<br />

long tube that is open at one end and closed at the other is filled <strong>with</strong> mercury<br />

and then inverted into a dish of mercury. Once inverted, the mercury does not<br />

empty into the bowl; rather, the atmosphere exerts a pressure on the mercury in<br />

the bowl and pushes the mercury in the tube to some height above the bowl. In<br />

this way, the force exerted on the bowl of mercury by the atmosphere is equal to<br />

the weight of the column of mercury in the tube. Any change in the height of<br />

the column of mercury means that the atmosphere’s pressure has changed.<br />

Kinetic theory of gases can describe the origin of gas pressure<br />

Many models of a gas have been developed over the years. Almost all of these<br />

models attempt to explain the macroscopic properties of a gas, such as pressure,<br />

in terms of events occurring in the gas on a microscopic scale. The most<br />

successful model by far is the kinetic theory of gases.<br />

In kinetic theory, gas particles are likened to a collection of billiard balls<br />

that constantly collide <strong>with</strong> one another. This simple model is successful in<br />

explaining many of the macroscopic properties of a gas. For instance, as these<br />

particles strike a wall of a container, they transfer some of their momentum<br />

during the collision. The rate of transfer of momentum to the container wall<br />

is equal to the force exerted by the gas on the container wall (see Chapter 6).<br />

This force per unit area is the gas pressure.<br />

Copyright © by Holt, Rinehart and Winston. All rights reserved.<br />

NSTA<br />

TOPIC: Atmospheric pressure<br />

GO TO: www.scilinks.org<br />

sciLINKS CODE: HF2093<br />

Mercury<br />

<strong>Fluid</strong> <strong>Mechanics</strong><br />

Empty<br />

Figure 9-9<br />

The height of the mercury in the<br />

tube of a barometer indicates the<br />

atmospheric pressure.<br />

329<br />

SECTION 9-2<br />

Demonstration 6<br />

Hydrostatic pressure<br />

Purpose Demonstrate that pressure<br />

increases <strong>with</strong> depth.<br />

Materials 32 oz plastic soda bottle,<br />

tape, water, bucket; optional:<br />

plastic straw or small pieces of<br />

glass or metal tubing and modeling<br />

clay or silicon<br />

Procedure Drill three holes<br />

about 10 cm apart along the side<br />

of the bottle, <strong>with</strong> the lowest hole<br />

close to the bottom, and tape<br />

them. The holes should not be<br />

aligned vertically; they should be<br />

displaced horizontally about 1<br />

cm so that the water streams do<br />

not collide. Put small pieces of<br />

tubing into the holes to improve<br />

the flow. Cover the holes <strong>with</strong><br />

tape, fill the bottle <strong>with</strong> water,<br />

and place it at the edge of a table.<br />

Place it high enough above the<br />

bucket so that the effects of depth<br />

on the range of each stream will<br />

be easily observed. Ask students<br />

to predict how the water streams<br />

will compare. Quickly pull the<br />

tape away from all three holes,<br />

and have students observe the<br />

shape of each stream. Water<br />

shooting out from near the bottom<br />

of the bottle exits the bottle<br />

at a higher speed than water<br />

shooting out from near the top<br />

does. The reason is that the pressure<br />

in the bottle increases <strong>with</strong><br />

depth.<br />

329

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!