Ch. 14

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Chapter 14

Fluids

Fluids at Rest

(Fluid = liquid or gas)

Density (

r

)

r  dm dV

• unit: kg/m 3

• we will consider only r

= m / V = constant

• (incompressible fluid)

• we will also assume g = constant

Pressure (

p

)

• A fluid exerts a force dF normal to any area dA you consider in it.

• For a fluid at rest, the force is equal and opposite on each side.

Pressure (

p

)

• Why is there a force?

• Microscopically: the fluid particles are in motion and collide with dA

• Macroscopically: the fluid is at rest

Pressure (

p

)

p

 dF

 dA

• pressure p is a scalar

(no intrinsic direction)

• reason: it acts normal to any surface dA

Pressure (

p

)

p

 dF

 dA

• units used: pascal, millibar, atm

• 1 Pa = 1 N/m 2

1 millibar = 100 Pa

1 atm = 1.013×10 5 Pa

Terminology

• ‘gauge pressure’ = p

– p atm

• (can be > 0 or < 0)

• (e.g., read on a car tire pressure gauge)

• p = absolute pressure (> 0)

= atmospheric pressure + gauge pressure

= p atm

+ gauge pressure

Pressure and depth

• pressure: p coordinate: y

• pressure decreases with ‘elevation’ y : dp

  r g dy

Derive this result and integrate it

Pressure and depth

• coordinate: y distance: h > 0

• p increases with depth for any shape of vessel p

2

 p

1

  r g ( y

2

 y

1

) p

1

 p

2

 r gh

Demonstration: depth and shape of container

Exercise 14-10

• The dangers of a long snorkel tube:

• Find the gauge pressure at the depth shown. Will this cause the snorkeler’s lungs to collapse?

Demonstration: atmospheric pressure

Pascal’s Law

• If any change in pressure

D p is applied at one point, it is transmitted to all points in the fluid and to walls enclosing it.

p

2

 p

1

  r g ( y

2

 y

1

) p

1

 p

2

 r gh

Example: Hydraulic Lift

At equilibrium, p = F

1

/ A

1

= F

2

/ A

2

Demonstration

Two Pressure Gauges

Notes on (b) first Notes on (a) and Exercise 14-9

Homework Hints:

Exercise 14-55

Buoyancy and Buoyant Force

A (fully or partially) submerged object feels an upward force equal to the weight of fluid it displaces

(a) fluid element with weight w fluid

(b) body of same shape feels buoyant force B = w fluid

Demonstration

Surface Tension

• Molecules of liquid attract each other (else no definite volume)

• center: net force = 0

• surface: net force is directed inward

Surface Tension

• So the surface acts like a membrane under tension (like a stretched drumhead)

• The surface resists any change in surface area

• Strength characterized by ‘surface tension’

Demonstration

Surface Tension

g g

= F / d

= cohesive force per unit length

• surface tension force

F = g d

• We can measure g by just balancing F

Notes on measuring g

Do Example 14-23

cohesion: attraction of like molecules example: liquid-liquid forces (surface tension)

adhesion: attraction between unlike molecules example: liquid-glass forces

(a) adhesion > cohesion: water wets glass

(b) adhesion < cohesion: mercury beads up

Capillarity

• For these two cases, the surface tension force F pushes the column of liquid either up or down:

• (a) up for water

• (b) down for mercury

Notes on capillary tubes

Homework Announcements

• Homework Set 5: Correction to hints for

14-55 (handout at front and on webpage)

• Recent changes to classweb access

(see HW 5 sheet at front and webpage)

• Homework Sets 1, 2, 3: returned at front

(scores to be entered on classweb soon)

Midterm Announcements

• Friday:

• review required topics

• practice problems (from class, HW, new?)

• Monday: (midterm)

• you can bring a sheet of notes (both sides)

• you will be given a list of equations

Fluid Flow

(Fluid Dynamics)

Flow Fluid

• Flow line = path of fluid element

Flow tube = bundle of flow lines passing through area A

(just a useful construct)

Simplifying Assumptions

• Steady flow:

• At any given point in the fluid, its properties

( v , r

, p

) don’t change in time

Simplifying Assumptions

• Steady flow:

• different flow lines never cross each other

• fluid entering a flow tube never leaves it

Simplifying Assumptions

• Incompressible fluid: r

= constant

No friciton:

• no ‘viscosity’

Notes

Continuity Equation

A

1 v

1

= A

2 v

2

• the same volume dV of fluid enters and exits tube:

• dV = volume passing through A in dt

= Av dt dV

Av dt

Continuity Equation

A

1 v

1

= A

2 v

2

• along the flow:

A = area of flow tube v = speed of fluid

• if one increases, the other must decrease

Notes and Demonstration: water flow

Continuity Equation

A

1 v

1

= A

2 v

2

• Where the flow lines are crowding together, the fluid speed is increasing

Notes

Bernoulli’s Equation p

1

 r gy

1

1

2 r v

1

2

 p

2

 r gy

2

1

2 r v

2

2

• only valid for: steady flow, incompressible fluid, no viscosity!

Bernoulli’s Equation p

1

 r gy

1

1

2 r v

1

2

 p

2

 r gy

2

1

2 r v

2

2

• if v

1

= v

2

= 0:

• reduces to previous result for fluid at rest

Bernoulli’s Equation p

1

 r gy

1

1

2 r v

1

2

 p

2

 r gy

2

1

2 r v

2

2

• if y

1

= y

2 then for p and v :

• if one increases, the other must decrease

Demonstration

Applications of

Bernoulli’s Equation

Notes

Venturi Meter (Example 14-10) horizontal flow tube

Note: if viscosity is present, then v decreases with distance from tube center

Notes

Venturi Meter:

Homework Problem 14-90 (c)

Demonstration

Wing Lift

Can’t predict flow lines but they indicate low pressure above wing, so net force up

Demonstration: propellor

Notes

Efflux Speed: vertical flow tube

Siphon: flow tube points up, then down

• First: you must fill the tube

• There is a limit:

H + h < 10 m

Warm-up demonstrations

Curve Ball: viscosity makes it possible

Viscosity drags air with spinning ball: low pressure=net force so the ball curves

Demonstration

Homework Announcements

• Homework Set 5: Correction to hints for

14-55 (handout at front and on webpage)

• Recent changes to classweb access

(see HW 5 sheet at front and webpage)

• Homework Sets 1, 2, 3: returned at front

(scores to be entered on classweb soon)

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