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I Introduction 2014

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Southern Methodist University Bobby B. Lyle School of Engineering CEE 2342/ME 2342 Fluid Mechanics Roger O. Dickey, Ph.D., P.E. I. INTRODUCTION B. Physical Characteristics of Fluids C. The Science of Fluid Mechanics
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Page 1: I Introduction 2014

Southern Methodist UniversityBobby B. Lyle School of EngineeringCEE 2342/ME 2342 Fluid Mechanics

Roger O. Dickey, Ph.D., P.E.

I. INTRODUCTIONB. Physical Characteristics of FluidsC. The Science of Fluid MechanicsD. Units and DimensionsE. Fluid Properties

Page 2: I Introduction 2014

Reading Assignment:

Chapter 1, following along with daily lecture material.

Page 3: I Introduction 2014

B. Physical Characteristics of Fluids

In engineering applications, matter exists in one of three physical states:

• Solid

• Liquid

• Gas

The term fluid encompasses both liquids and gases.

Fluids

Page 4: I Introduction 2014

Qualitative characteristics of a solid:

• Essentially has constant volume

• Maintains a fixed shape

• Molecules are held in a more less “rigid”

structure

Page 5: I Introduction 2014

Qualitative characteristics of a liquid:

• Molecules are relatively free to change

their positions with respect to each other

but they are restricted by cohesive forces

to a practically constant volume

• Assumes the shape of a container

Page 6: I Introduction 2014

Qualitative characteristics of a gas:

• Molecules are unrestricted by cohesive

forces

• Has no definite volume

• Expands to fill a container

Page 7: I Introduction 2014

Definitions of shear force/shear stress and

normal force/normal stress (pressure):

(i) A shear force on a surface is the

component of the total applied force that is

tangent to the surface. Shear stress is the

shear force per unit area of the surface.

Page 8: I Introduction 2014

(ii) A normal force on a surface is the

component of the total applied force that is

perpendicular to the surface. Normal stress

or pressure is the normal force per unit

area of the surface.

Page 9: I Introduction 2014

Consider a solid subjected to shear forces,

Initial solid shape in static equilibrium

Apply shear force

Page 10: I Introduction 2014

Deformation of the solid takes place until internal forces (spring-like forces due to molecular cohesion) build up to resist further deformation resulting in a deformed solid shape in static equilibrium

Page 11: I Introduction 2014

A fluid can be defined as follows:

Fluid a substance that continuously

deforms (i.e., flows) under the action of a

shear stress.

Page 12: I Introduction 2014

Consider a fluid element subjected to shear forces,

Initial fluid element shape in static equilibrium

Apply shear force

Page 13: I Introduction 2014

Continuous deformation occurs until the shear stress is removed

Page 14: I Introduction 2014

Fluid as a Continuum -

It is virtually impossible to evaluate the forces

acting on, and the behavior of individual

molecules when studying the behavior of fluids

because the number of molecules in a tiny

volume is astronomical (approximately 1021

molecules/mm3 for liquids and 1018

molecules/mm3 for gases).

Page 15: I Introduction 2014

In the fluid sciences, behavior of fluids is

characterized by considering the average, or

macroscopic value of physical quantities of

interest where the average is taken for an

extremely large number of molecules. These

macroscopic fluid properties can be perceived

by human senses, and measured by instruments.

Page 16: I Introduction 2014

In essence, the derivation and application of the

basic principles of fluid mechanics requires that

the actual molecular structure of fluids be

replaced by a hypothetical continuous medium

called the continuum.

Page 17: I Introduction 2014

C. The Science of Fluid Mechanics

The sub-disciplines of the science of fluid

mechanics are summarized on the following

flow chart:

Page 18: I Introduction 2014

Fluid Mechanics

Fluid Dynamics(Flow of Fluids)

Fluid Statics(Fluids at Rest)

Hydrodynamics(Incompressible Flow - liquids and low speed flow of gases)

Gas Dynamics(Compressible Flow - gases)

Aerodynamics

Hydraulics(Flow of Liquids in Pipes and Channels)

Page 19: I Introduction 2014

Examples of the practical importance of fluid

mechanics:

(1) Hydrology

• Flow of groundwater

• Flow of water in streams and lakes

• Ocean currents and tides

• Weather (flow of air in the atmosphere)

Page 20: I Introduction 2014
Page 21: I Introduction 2014

(2) Closed Conduit Flow

• Water supply transmission pipelines

• Water distribution networks

• Cold and hot water plumbing for buildings

• Oil and gas pipelines

• Air and oxygen distribution piping (e.g., in waste treatment systems, hospitals, etc.)

• Blood flow in human circulatory system

Page 22: I Introduction 2014
Page 23: I Introduction 2014

(3) Open Channel Flow

• Storm sewer networks and channels

• Sanitary sewer networks

• Wastewater plumbing in buildings (e.g.,

industrial wastewater and sewage

collection networks)

• Irrigation networks

Page 24: I Introduction 2014
Page 25: I Introduction 2014

(4) Turbomachinery

• Turbines (power generation)

• Pumps

• Compressors and blowers

Page 26: I Introduction 2014
Page 27: I Introduction 2014

(5) Aerodynamics

• Airframe design (lift and drag)

• Propulsion systems (propellers, jet

engines, rocket engines)

Page 29: I Introduction 2014

(6) Naval Architecture – design of boats and

ships

Page 30: I Introduction 2014

Consider the example of an automobile:

• Pneumatic tires

• Gasoline and engine coolant pumped through closed conduits

• Hydraulic shock absorbers

• Hydraulic brakes

• Aerodynamic body shapes increase fuel efficiency by reducing drag

Page 31: I Introduction 2014

Interest in fluid behavior dates back to ancient

civilizations based on the necessity for

development of water supply and irrigation

systems, design of boats and ships, and

propelling projectiles through the air (e.g., the

addition of feathers at the tail of an arrow,

creating drag to true the flight of the arrow).

Page 32: I Introduction 2014

The beginnings of the formalization of the

science of fluid mechanics began with the need

to control water in large irrigation systems in

ancient Egypt, Mesopotamia (Iraq), and India as

early as 3000 BC.

Page 33: I Introduction 2014

However, the first quantitative scientific laws in

the field of fluid mechanics were not developed

until 250 BC when the Greek scientist,

mathematician, and inventor Archimedes

discovered and recorded the principles of

hydrostatics and flotation.

Page 34: I Introduction 2014

The fundamental principles of hydrodynamics

were not set forth until the 17th and 18th centuries

with the greatest contributions made by Isaac

Newton, Daniel Bernoulli, and Leonhard Euler.

Refer to Table 1.9, pp. 28-29, in the textbook

for a chronological listing of some major

contributors to the science of fluid mechanics, an

excerpt is shown on the following two slides:

Page 35: I Introduction 2014

Table 1.9,pp. 28-29

Page 36: I Introduction 2014

Table 1.9(Continued)

Page 37: I Introduction 2014

D. Units and DimensionsBoth SI and British Gravitational (BG), also called U.S. Customary (USC), units are used:

Physical UnitsQuantity Dimension SI USCForce F N lbMass M kg slugLength L m ftTime T sec sec

Page 38: I Introduction 2014

A consistent set of physical units involves

either: (1) defining the units of F-L-T as the

basic units, then deriving the unit of M from

Newton’s Second Law of Motion (F = ma), or

(2) defining the units of M-L-T, and deriving

the unit of F from Newton’s Second Law.

Page 39: I Introduction 2014

Using SI units, M-L-T units are defined, and the

unit of F is derived:

2

2

secmkg 1 N 1

)m/sec kg)(1 (1 N 1

ma F

1 N is derived as the force required to accelerate a1 kg mass at 1 m/sec2

SI Force Dimensions:

22 or -MLT

TLM

Page 40: I Introduction 2014

Using USC units, F-L-T units are usually

defined, and the unit of M is derived:

ftseclb 1 slug 1

ft/sec 1lb 1 slug 1

aF m

2

2

1 slug is derived as the mass accelerated at 1 ft/sec2 by a force of 1 lb

USC Mass Dimensions:

122

or -LFTLTF

Page 41: I Introduction 2014

Reconsider the derived unit of force in the SI

system of units,

Multiply both sides of this equation by 1 sec2,

2secmkg 1 N 1

mkg 1 secN 1 2

Page 42: I Introduction 2014

Divide both sides of the equation by 1 m and

rearrange,

msecN 1 kg 1

2

These are the same physical dimensions derived for slugs, the unit of mass in the USC system of units:

122

or -LFTLTF

Page 43: I Introduction 2014

A comprehensive listing of dimensions for

common physical quantities encountered in

science and engineering is shown in Table 1.1

Dimensions Associated with Common

Physical Quantities, p. 5 in the textbook:

Page 44: I Introduction 2014
Page 45: I Introduction 2014

Table 1.1 (Continued)

Page 46: I Introduction 2014

Table 1.1 (Continued)

Page 47: I Introduction 2014

Homework No. 1 Dimensional consistency of

mathematical expressions describing fluid

phenomena.

Page 48: I Introduction 2014

E. Fluid Properties

Properties vary from fluid-to-fluid. Properties for

a given fluid frequently vary with temperature.

Refer to Tables 1.5 and 1.6, inside the front

cover of the textbook, as shown on the

following two slides:

Page 49: I Introduction 2014
Page 50: I Introduction 2014
Page 51: I Introduction 2014

Measures of Mass and Weight

(1) Specific Weight, ,

weight per unit volume

SI Units - N/m3

USC Units - lb/ft3

3LF

Page 52: I Introduction 2014

(2) Density, ,

mass per unit volume

SI Units - kg/m3

USC Units - slug/ft3

3LM

Page 53: I Introduction 2014

(3) Relationship Between and ,

Weight and mass are related by Newton’s Second Law,

F = ma

Weight, w, is the gravitational force exerted on a body of mass, m, by the earth and thus,

w = mg

where, g = gravitational acceleration

Page 54: I Introduction 2014

Divide both sides of the previous equation by

the volume, , of the body of weight w and

mass m yields,

By definition,

gVm

Vw

Vmρ and

Vwγ

V

Page 55: I Introduction 2014

Substituting,

Standard gravitational acceleration at mean sea

level (MSL) is,

g = 9.81 m/sec2

g = 32.2 ft/sec2

ρ gγ [Equation (1.6), p. 12]

Page 56: I Introduction 2014

(4) Specific Gravity, S,

S ratio of the density of a fluid to

the density of water at 4° C

S is dimensionless (one of many dimensionless

ratios encountered in fluid mechanics) and,

thus, the numerical value of S does not depend

on the system of units.

Page 57: I Introduction 2014

Viscosity

Contrary to the case of solid bodies, specific

weight and density are insufficient to uniquely

characterize the dynamic behavior of fluids

when acted upon by external forces. For

example, two fluids with similar density, such

as certain oils and water, can behave quite

differently when flowing.

Page 58: I Introduction 2014

There is need for an additional physical

property to describe the “fluidity” of gases and

liquids. This property is called viscosity.

Viscosity is the fluid property that offers

resistance to shear stresses.

Page 59: I Introduction 2014

Film Clip Textbook film, Segment V1.3: Viscous Fluids.

Page 60: I Introduction 2014

Isaac Newton made pioneering experimental

observations of fluids upon which shear forces

were applied. He discovered that the resulting

velocity gradient created within the fluid was

directly proportional to the applied shear stress.

Page 61: I Introduction 2014

His discovery is called Newton’s Law of

Viscosity, and for one-dimensional flow in the

x-direction it is written as,

where,

dydu

[Equation (1.9), p. 15]

Page 62: I Introduction 2014

= shear stress applied to the fluid [F/L2]

u = velocity in the x-direction [L/T]

y = distance along the y-axis [L]

(i.e., distance above the x-axis)

= velocity gradient perpendicular to the

direction of flow

= viscosity

dydu

LTL

22 or

FTL

LTF

Page 63: I Introduction 2014

is given the name viscosity but is also called

the absolute viscosity or dynamic viscosity.

Typical units are,

SI Units — (no special name)

USC Units — (no special name)

c-g-s — (named Poise, P)

2msecN

2ftseclb

2cmsecdyne

Page 64: I Introduction 2014

Consider an experiment where a fluid film of

thickness “b” is located between a moving top

plate having velocity U in the +x-direction, and

a parallel but fixed bottom plate as shown in

Figure 1.5, p. 15 in the textbook, slightly

modified on the following slide:

Page 65: I Introduction 2014

Figure 1.5, p. 15 –Modified

bU

dydu

x

1

Page 66: I Introduction 2014

The constant velocity of the top plate, U, is

induced by applying a constant horizontal force,

P, to the plate. For a plate having planar area A,

the shear stress (i.e., force per unit area)

applied to the fluid by the top plate is simply:

2

LF

AP

Page 67: I Introduction 2014

The fluid between the plates deforms continuously

under the action of the shear stress, . The fluid

motion may be conceptualized as many thin

horizontal layers sliding one over another at

differing rates yielding a velocity gradient ,

which is also the rate of angular deformation of

the fluid as illustrated in Figure 1.5. Hence, is

sometimes called the rate of shearing strain.

dydu

dydu

Page 68: I Introduction 2014

Experimental observations reveal that fluids

“stick” to solid boundaries due to molecular

adhesion forces. Thus, fluid particles in direct

contact with moving solid boundaries move with

the same velocity as the solid surface, and fluid

particles contacting stationary solid boundaries

have zero velocity. This is called the no-slip

condition for flowing fluids.

Page 69: I Introduction 2014

Film Clip Textbook film, Segment V1.4: No-Slip Condition.

Page 70: I Introduction 2014

Experimental observations for the geometry of the current experiment reveal that the fluid velocity u increases linearly when proceeding upward in the +y-direction, hence is constant, i.e.,

The no-slip condition establishes the boundary conditions: (i) u = 0, y = 0 at the bottom plate, and (ii) u = U, y = b at the top plate. Thus,

bU

dydu

bU

dydu

00

dydu

yu

dydu

Page 71: I Introduction 2014

Viscosity is also a constant, i.e., a characteristic

physical property of the specific fluid used in the

experiment. Therefore, according to Newton’s Law

of Viscosity, , the shear stress must

remain constant throughout the fluid, ,

being transmitted from one sliding fluid layer to

the next.

bU

dydu

Page 72: I Introduction 2014

Most fluids adhere to Newton’s Law of Viscosity

—shear stress varying as a linear function of

velocity gradient and having viscosity, μ, as the

constant of proportionality. These fluids are

termed Newtonian fluids. Fluids that do not

adhere to the law are classed as non-Newtonian

fluids. Figure 1.7, p. 16 in the textbook

graphically compares Newtonian and several

common classes of non-Newtonian fluids:

Page 73: I Introduction 2014

Figure 1.7, p. 16 –Modified

μ1

Page 74: I Introduction 2014

Film Clip Textbook film, Segment V1.6: Non-Newtonian Behavior – Shear-Thickening

Page 75: I Introduction 2014

It is sometimes convenient in fluid mechanics to

use the kinematic viscosity, , which is defined

as the viscosity divided by the density of the

fluid:

M

TLFLMLTF3

2

Page 76: I Introduction 2014

From Newton’s Second Law of Motion, force has

equivalent dimensions of which yields the

common dimensions for kinematic viscosity, ,

that is:

TL2

2TLM

TL

MTLTLM

MTLF 22

Page 77: I Introduction 2014

Common units for kinematic viscosity are,

SI Units - m2/sec (no special name)

USC Units - ft2/sec (no special name)

c-g-s - cm2/sec (named Stoke, St)

Page 78: I Introduction 2014

Viscosity does not vary significantly with pressure and, as such, is assumed solely a function of temperature. Figure 1.8, p. 17 in the textbook is reproduced on the following slide, showing that:

(i) Liquids – viscosity decreases dramatically with increasing temperature

(ii) Gases – viscosity increases slightly with increasing temperature

(iii) Viscosities for common liquids are several orders of magnitude higher than those of gases.

Page 79: I Introduction 2014

Figure 1.8,p. 17

Dyn

amic

Vis

cosi

ty, μ

(N·s

/m2 )

Temperature, C

Page 80: I Introduction 2014

Homework No. 2 Newton’s Law of Viscosity.

Page 81: I Introduction 2014

Vapor Pressure

Vapor pressure, pv , is defined as,

pv the absolute pressure at which a

liquid will boil at a given temperature

Vapor pressure increases as the temperature of the liquid increases, refer to Handout — I.E. Properties of Common Fluids. A liquid can be made to boil at low temperature by reducing the pressure.

Page 82: I Introduction 2014

In many common liquid flow situations (e.g., in

some hydraulic machinery such as pumps and

turbines, inside valves, and along the face of

dam spillways) pressures at or below the vapor

pressure of the liquid can occur. Under these

conditions, the liquid flashes to vapor forming

tiny bubbles or gas pockets.

Page 83: I Introduction 2014

As the bubbles are carried along by the flow,

they can enter zones of higher pressure where

the vapor condenses and the bubbles collapse.

As the liquid rushes into the vacuum left by the

collapsed bubble, high transient forces are

generated (like tiny hammer blows).

Page 84: I Introduction 2014

Where the collapsing bubbles are in contact

with solid boundaries these “hammer blows”

can cause pitting and erosion of the solid

surface. The phenomena of vapor pocket

formation and collapse is called cavitation.

Page 85: I Introduction 2014

Cavitation

Page 86: I Introduction 2014

Worker inspecting cavitation damage to spillway

Cavitation – Glen Canyon Dam Spillway near Page, AZ

Page 87: I Introduction 2014

Workers repairing cavitation damage to dam spillway

Cavitation – Dworshak Dam Spillway near Ashaka, Idaho

Page 88: I Introduction 2014

Bulk Modulus of Elasticity

Bulk Modulus of Elasticity, Ev , often simply

called the Bulk Modulus, is a measure of the

elasticity of a liquid.

Let,

= volume of liquid [L3]

p = pressure [F/L2]

V

Page 89: I Introduction 2014

Then,

vEV

dpVd

Rate of change ofvolume with respect to pressure

The minus sign indicates that volume decreases with increasing pressure

Page 90: I Introduction 2014

Rearranging yields,

SI Units - N/m2 (called the Pascal)

USC Units - lb/ft2 which is frequently

converted to lb/in2 or psi

2

LF

VVddpEv

PressureDimensions

[Equation (1.12), p. 20]

Page 91: I Introduction 2014

Since a decrease in volume (i.e., ) for a

given mass, , causes an increase in

density (i.e., d > 0), the previous equation may

also be written:

2

LF

ddpEv

PressureDimensions

[Equation (1.13), p. 20]

0Vd

Vm

Page 92: I Introduction 2014

Values of Ev tend to be very large for common

liquids, e.g., approximately 300,000 psi for

water. For other examples refer to Handout —

I.E. Properties of Common Fluids,

emphasizing that liquids can be assumed

incompressible for the vast majority of applied

fluid mechanics problems.

Page 93: I Introduction 2014

However, there are a few engineering

applications involving extremely large pressure

changes where it becomes necessary to consider

the compressibility of liquids:

Page 94: I Introduction 2014

• Water hammer – rapid valve closure can

cause large pressure transients that

generate loud “bangs”, shaking, and even

rupture of piping.

• Pumping of groundwater from deep

confined aquifers.

Page 95: I Introduction 2014

Valve Closure Water Hammer

Water Hammer Damage

Water Hammer Shock Alleviation

Page 96: I Introduction 2014

Wells in Confined Aquifers

Page 97: I Introduction 2014

Surface Tension

At interfaces between liquids and gases,

between two immiscible liquids, and between

liquids and solids unbalanced cohesive forces

develop that cause the liquid surface to appear

and behave as if it were a “skin” or “membrane”

stretched over the fluid mass.

Page 98: I Introduction 2014

Consider a liquid-gas interface, e.g., the

interface between water in a drinking glass and

the surrounding air. Molecules within the

interior of the liquid mass experience balanced

cohesive forces because they are surrounded by

like molecules that are attracted to each other

equally.

Page 99: I Introduction 2014

Conversely, liquid molecules residing at the liquid-

gas interface are subjected to a net force toward the

interior of the liquid mass because the cohesive

forces between liquid molecules are much stronger

than the adhesive forces between the liquid

molecules and the overlying gas. The unbalanced

cohesive forces along the interface create the

appearance of a taut skin over the liquid surface.

Page 100: I Introduction 2014

A tensile force acts in the plane of the surface

“skin,” along any line in the surface, much like

the tensile force in a drum head. The intensity of

the tensile force per unit length is called surface

tension, σ [F/L].

Page 101: I Introduction 2014

Surface tension is a characteristic property of a given liquid, as illustrated in Handout — I.E. Properties of Common Fluids for various liquids in contact with air (e.g., 0.466 N/m for mercury compared to 0.022 N/m for gasoline). However, surface tension also depends on the other substance—liquid, gas, or solid—forming the interface with the liquid. Furthermore, surface tension varies with temperature, tending to decrease with increasing temperature.

Page 102: I Introduction 2014

Surface tension forces are usually negligible compared to inertial and viscous shear forces in flowing fluids. However, there are a number of interesting and/or important phenomena involving surface tension:

• Steel needles, razor blades, and water walking insects can float on water under the right conditions, because the tensile force in the taut skin balances their weight.

• Liquids can form tight, compact droplets when placed on smooth solid surfaces.

Page 103: I Introduction 2014

Film Clip Textbook film, Segment V1.9:

Floating Razor Blade.

Water Strider Insect Mercury Droplets

Page 104: I Introduction 2014

• Formation of liquid droplets and gas bubbles, e.g., break up of liquid jets into discrete droplets through fuel injectors and atomizing spray nozzles, and diffusing compressed air into aeration tanks.

• Formation of a meniscus and the associated capillary rise (wetting liquids) or fall (non-wetting liquids) in small diameter tubes; involves liquid-gas-solid interfaces

Page 105: I Introduction 2014

Atomizing Spray Nozzles Fuel Injectors

Ceramic Disk, Fine BubbleAir Diffuser

Page 106: I Introduction 2014

Figure 1.10, p. 25Effect of capillary action in small tubes. (a) Rise of column for a liquid that wets the tube, e.g., water in a glass tube. (b) Free-body diagram for calculating column height. (c) Depression of column for a non-wetting liquid, e.g., mercury in a glass tube.

Page 107: I Introduction 2014

• Formation of a capillary fringe above ground

water aquifers, where the tiny interstitial

spaces between soil grains (soil porosity)

create natural “capillary tubes.”

Refer to Handout I.E. Surface Tension –

Examples Problems.

Page 108: I Introduction 2014

Homework No. 3 Surface tension.


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