Fluid Mechanics
Notes
Differences between solids and fluids:
The
differences between the behaviours of solids and fluids under an applied force
are as follows:
i.
For a solid, the strain is a function of the applied stress,
providing that the elastic limit is not exceeded. For a fluid, the rate of
strain is proportional to the applied stress.
ii.
The strain in a solid is independent of the time over which the
force is applied and, if the elastic limit is not exceeded, the deformation
disappears when the force is removed. A fluid continues to flow as long as the
force is applied and will not recover its original form when the force is
removed.
Differences between liquids and gases:
Although
liquids and gases both share the common characteristics of fluids, they have
many distinctive characteristics of their own. A liquid is difficult to
compress and, for many purposes, may be regarded as incompressible. A given
mass of liquid occupies a fixed volume, irrespective of the size or shape of
its container, and a free surface is formed if the volume of the container is
greater than that of the liquid.
A gas is
comparatively easy to compress. Changes of volume with pressure are large,
cannot normally be neglected and are related to changes of temperature. A given
mass of gas has no fixed volume and will expand continuously unless restrained
by a containing vessel. It will completely fill any vessel in which it is
placed and, therefore, does not form a free surface.
Newtonian fluids:
Fluids which
obey the Newton's law of viscosity are called as Newtonian fluids. Newton's law
of viscosity is given by
t = mdv/dy
where t = shear stress
m = viscosity of fluid
dv/dy =
shear rate, rate of strain or velocity gradient
All gases
and most liquids which have simpler molecular formula and low molecular weight
such as water, benzene, ethyl alcohol, CCl4, hexane and most
solutions of simple molecules are Newtonian fluids.
Non-Newtonian fluids:
Fluids which
do not obey the Newton's law of viscosity are called as non-Newtonian fluids.
Generally
non-Newtonian fluids are complex mixtures: slurries, pastes, gels, polymer
solutions etc.,

Various
non-Newtonian Behaviors:
Time-Independent behaviors:
Properties
are independent of time under shear.
Bingham-plastic: Resist a small
shear stress but flow easily under larger shear stresses. e.g. tooth-paste,
jellies, and some slurries.
Pseudo-plastic: Most non-Newtonian
fluids fall into this group. Viscosity decreases with increasing velocity
gradient. e.g. polymer solutions, blood. Pseudoplastic fluids are also called
as Shear thinning fluids. At low shear rates(du/dy) the shear thinning fluid is
more viscous than the Newtonian fluid, and at high shear rates it is less
viscous.
Dilatant
fluids:
Viscosity increases with increasing velocity gradient. They are uncommon, but
suspensions of starch and sand behave in this way. Dilatant fluids are also
called as shear thickening fluids.
Time dependent behaviors:

Those which
are dependent upon duration of shear.
Thixotropic
fluids:
for which the dynamic viscosity decreases with the time for which shearing
forces are applied. e.g. thixotropic jelly paints.
Rheopectic
fluids:
Dynamic viscosity increases with the time for which shearing forces are
applied. e.g. gypsum suspension in water.
Visco-elastic fluids: Some fluids have elastic properties,
which allow them to spring back when a shear force is released. e.g. egg white.
Physical properties:
Viscosity
The
viscosity (m) of a fluid measures
its resistance to flow under an applied shear stress. Representative units for
viscosity are kg/(m.sec), g/(cm.sec) (also known as poise designated by P). The
centipoise (cP), one hundredth of a poise, is also a convenient unit, since the
viscosity of water at room temperature is approximately 1 centipoise.
The kinematic
viscosity (n) is the ratio of the viscosity to the density:
n = m/r,
and will be
found to be important in cases in which significant viscous and gravitational
forces exist.
Viscosity of liquids:
Viscosity of
liquids in general, decreases with increasing temperature.
The
viscosities (m) of liquids generally
vary approximately with absolute temperature T according to:
ln m = a - b ln T
Viscosity of gases:
Viscosity of gases increases with increase
in temperature.
The
viscosity (m) of many gases is
approximated by the formula:
m = mo(T/To)n
in which T is
the absolute temperature, mo is the viscosity at an absolute reference temperature To,
and n is an empirical exponent that best fits the experimental data.
The viscosity of an ideal gas is independent
of pressure, but the viscosities of real gases and liquids usually increase
with pressure.
Viscosity of
liquids are generally two orders of magnitude greater than gases at atmospheric
pressure. Fow example, at 25oC, mwater = 1 centipoise and mair = 1 x 10-2centipoise.
Compressibility and the Bulk modulus:
All materials,
whether solids, liquids or gases, are compressible, i.e. the volume V of a
given mass will be reduced to V - dV when a force is exerted uniformly all over
its surface. If the force per unit area of surface increases from p to p + dp, the relationship
between change of pressure and change of volume depends on the bulk modulus of
the material.
Bulk modulus
(K) = (change in pressure) / (volumetric strain)
Volumetric
strain is the change in volume divided by the original volume. Therefore,
(change in
volume) / (original volume) = (change in pressure) / (bulk modulus)
i.e., -dV/V = dp/K
Negative
sign for dV indicates the
volume decreases as pressure increases.
In the
limit, as dp tends to 0,
K = -V dp/dV
à 1
Considering
unit mass of substance, V = 1/r à 2
Differentiating,
Vdr + rdV = 0
dV = - (V/r)dr à3
putting the
value of dV from equn.3 to equn.1,
K = - V dp /
(-(V/r)dr)
i.e. K = rdp/dr
The concept
of the bulk modulus is mainly applied to liquids, since for gases the compressibility
is so great that the value of K is not a constant.
The
relationship between pressure and mass density is more conveniently found from
the characteristic equation of gas.
For liquids,
the changes in pressure occurring in many fluid mechanics problems are not
sufficiently great to cause appreciable changes in density. It is therefore
usual to ignore such changes and consider liquids as incompressible.
Gases may
also be treated as incompressible if the pressure changes are very small, but
usually compressibility cannot be ignored. In general, compressibility becomes
important when the velocity of the fluid exceeds about one-fifth of the
velocity of a pressure wave (velocity of sound) in the fluid.
Typical
values of Bulk Modulus:
K = 2.05 x
109 N/m2 for water
K = 1.62 x
109 N/m2 for oil.
Surface
Tension
A molecule I in the
interior of a liquid is under attractive forces in all directions and the
vector sum of these forces is zero. But a molecule S at the surface of a liquid
is acted by a net inward cohesive force that is perpendicular to the surface.
Hence it requires work to move molecules to the surface against this opposing
force, and surface molecules have more energy than interior ones.
The surface
tension (s sigma) of a liquid
is the work that must be done to bring enough molecules from inside the liquid
to the surface to form one new unit area of that surface (J/m2 =
N/m). Historically surface tensions have been reported in handbooks in dynes
per centimeter (1 dyn/cm = 0.001 N/m).
Surface
tension is the tendency of the surface of a liquid to behave like a stretched
elastic membrane. There is a natural tendency for liquids to minimize their
surface area. For this reason, drops of liquid tend to take a spherical shape
in order to minimize surface area. For such a small droplet, surface tension
will cause an increase of internal pressure p in order to balance the surface
force.
We will find the
amount D (Dp = p - poutside)
by which the pressure inside a liquid droplet of radius r, exceeds the pressure
of the surrounding vapor/air by making force balances on a hemispherical drop.
Observe that the internal pressure p is trying to blow apart the two
hemispheres, whereas the surface tension s is trying to pull them together. Therefore,
Dp pr2 = 2prs
i.e. Dp = 2s/r
Similar force
balances can be made for cylindrical liquid jet.
Dp 2r= 2s
i.e. Dp = s/r
Similar treatment can
be made for a soap bubble which is having two free surfaces. Dp pr2 = 2 x 2prs
i.e. Dp = 4s/r
Surface
tension generally appears only in situations involving either free surfaces
(liquid/gas or liquid/solid boundaries) or interfaces (liquid/liquid
boundaries); in the latter case, it is usually called the interfacial
tension.
Representative
values for the surface tensions of liquids at 20oC, in contact
either with air or their vapor (there is usually little difference between the
two), are given in Table.
|
Liquid |
Surface Tension |
|
Benzene |
23.70 |
|
Benzene |
28.85 |
|
Ethanol |
22.75 |
|
Glycerol |
63.40 |
|
Mercury |
435.50 |
|
Methanol |
22.61 |
|
n-Octane |
21.78 |
|
Water |
72.75 |
Capillarity:
Rise or fall
of a liquid in a capillary tube is caused by surface tension and depends on the
relative magnitude of cohesion of the liquid and the adhesion of the liquid to
the walls of the containing vessel.
Liquids rise
in tubes if they wet (adhesion > cohesion) and fall in tubes that do not wet
(cohesion > adhesion).
Wetting and contact angle
Fluids wet
some solids and do not others.
The figure
shows some of the possible wetting behaviors of a drop of liquid placed on a
horizontal, solid surface (the remainder of the surface is covered with air, so
two fluids are present).
Fig.(a)
represents the case of a liquid which wets a solid surface well, e.g. water on
a very clean copper. The angle q shown is the angle between the edge of the liquid surface and
the solid surface, measured inside the liquid. This angle is called the contact
angle and is a measure of the quality of wetting. For perfectly wetting, in
which the liquid spreads as a thin film over the surface of the solid, q is zero.
Fig.(c)
represents the case of no wetting. If there were exactly zero wetting, q would be 180o.
However, the gravity force on the drop flattens the drop, so that 180o
angle is never observed. This might represent water on teflon or mercury on
clean glass.
We normally
say that a liquid wets a surface if q is less than 90o and does not
wet if q is more than 90o.
Values of q less than 20o
are considered strong wetting, and values of q greater than 140o are strong
nonwetting.
Capillarity is important (in fluid measurments) when
using tubes smaller than about 10 mm in diameter.

Capillary rise (or
depression) in a tube can be calculated by making force balances. The forces
acting are force due to surface tension and gravity.
The force due to surface tesnion,
Fs = pdscos(q), where q is the wetting angle or contact angle. If tube (made of glass)
is clean q is zero for water
and about 140o for Mercury.
This is opposed by the gravity force on the column of fluid, which is equal to the
height of the liquid which is above (or below) the free surface and which
equals
Fg = (p/4)d2hgr,
where r is the density of
liquid.
Equating
these forces and solving for Capillary rise (or depression), we find
h = 4scos(q)/(rgd)
Air is introduced through a nozzle into a tank of water to
form a stream of bubbles. If the bubbles are intended to have a diameter of 2
mm, calculate how much the pressure of the air at the tip of the nozzle must
exceed that of the surrounding water. Assume that the value of surface tension
between air and water as 72.7 x 10-3 N/m.
Data:
Surface
tension (s) = 72.7 x 10-3
N/m
Radius of
bubble (r) = 1
Formula:
Dp = 2s/r
Calculations:
Dp = 2 x 72.7 x 10-3
/ 1 = 145.4 N/m2
That is, the
pressure of the air at the tip of nozzle must exceed the pressure of
surrounding water by 145.4 N/m2
A soap bubble 50 mm in diameter contains a pressure (in
excess of atmospheric) of 2 bar. Find the surface tension in the soap film.
Data:
Radius of
soap bubble (r) = 25 mm = 0.025 m
Dp = 2 Bar = 2 x 105
N/m2
Formula:
Pressure
inside a soap bubble and surface tension (s) are related by,
Dp = 4s/r
Calculations:
s = Dpr/4 = 2 x 105
x 0.025/4 = 1250 N/m
Water has a surface tension of 0.4 N/m. In a 3 mm diameter
vertical tube if the liquid rises 6 mm above the liquid outside the tube,
calculate the contact angle.
Data:
Surface
tension (s) = 0.4 N/m
Dia of tube
(d) = 3 mm = 0.003 m
Capillary
rise (h) = 6 mm = 0.006 m
Formula:
Capillary
rise due to surface tension is given by
h = 4scos(q)/(rgd), where q is the contact
angle.
Calculations:
cos(q) = hrgd/(4s) = 0.006 x 1000 x
9.812 x 0.003 / (4 x 0.4) = 0.11
Therfore,
contact angle q = 83.7o
Fluid statics:
Pascal's law for pressure at a point:
The basic
property of a static fluid is pressure. Pressure is familiar as a surface force
exerted by a fluid against the walls of its container. Pressure also exists at
every point within a volume of fluid. For a static fluid, as shown by the
following analysis, pressure turns to be independent direction.

By
considering the equilibrium of a small fluid element in the form of a
triangular prism ABCDEF surrounding a point in the fluid, a relationship can be
established between the pressures Px in the x direction, Py
in the y direction, and Ps normal to any plane inclined at any angle q to the horizontal at
this point.
Px
is acting at right angle to ABEF, and Py at right angle to CDEF, similarly Ps
at right angle to ABCD.
Since there
can be no shearing forces for a fluid at rest, and there will be no
accelerating forces, the sum of the forces in any direction must therefore, be
zero. The forces acting are due to the pressures on the surrounding and the
gravity force.
Force due to
Px = Px x Area ABEF = Pxdydz
Horizontal
component of force due to Ps = - (Ps x Area ABCD) sin(q) = - Psdsdz dy/ds = -Psdydz
As Py
has no component in the x direction, the element will be in equilibrium, if
Pxdydz + (-Psdydz) = 0
i.e. Px
= Ps
Similarly in
the y direction, force due to Py = Pydxdz
Component of
force due to Ps = - (Ps x Area ABCD) cos(q) = - Psdsdz dx/ds = - Psdxdz
Force due to
weight of element = - mg = - rVg = - r (dxdydz/2) g
Since dx, dy, and dz are very small
quantities, dxdydz is negligible in
comparison with other two vertical force terms, and the equation reduces to,
Py
= Ps
Therefore, Px
= Py = Ps
i.e. pressure
at a point is same in all directions. This is Pascal's
law.
This applies to fluid at rest.
Fine powdery
solids resemble fluids in many respects but differs considerably in others. For
one thing, a static mass of particulate solids, can support shear stresses of
considerable magnitude and the pressure is not the same in all directions.
Variation of pressure with elevation:
Consider a
hypothetical differential cylindrical element of fluid of cross sectional area
A and height (z2 - z1).
Upward force
due to pressure P1 on the element = P1A
Downward
force due to pressure P2 on the element = P2A
Force due to
weight of the element = mg = rA(z2 - z1)g
Equating the
upward and downward forces,
P1A
= P2A + rA(z2 - z1)g
P2 -
P1 = - rg(z2 - z1)
Thus in any fluid
under gravitational acceleration, pressure decreases, with increasing height z
in the upward direction.
Equality of pressure at the same level in a static fluid:

Equating the
horizontal forces, P1A = P2A (i.e. some of the horizontal
forces must be zero)
Equality of pressure at the same level in a continuous body
of fluid:
Pressures at the same
level will be equal in a continuous body of fluid, even though there is no
direct horizontal path between P and Q provided that P and Q are in the same
continuous body of fluid.
We know
that, PR = PS
PR
= PP + rgh à 1
PS
= PQ + rgh à 2
From equn.1
and 2, PP = PQ
General equation for the variation of pressure due to
gravity from point to point in a static fluid:
Resolving the forces
along the axis PQ,
pA - (p + dp)A - rgAds cos(q) = 0
dp = - rgds cos(q)
or in
differential form,
dp/ds = - rgcos(q)
In the
vertical z direction, q = 0.
Therefore,
dp/dz = -rg
This
equation predicts a pressure decrease in the vertically upwards direction at a
rate proportional to the local density.
Absolute Pressure, Gage Pressure, and Vacuum
In a region
such as outer space, which is virtually void of gases, the pressure is
essentially zero. Such a condition can be approached very nearly in a
laboratory when a vacuum pump is used to evacuate a bottle. The pressure in a
vacuum is called absolute zero, and all pressures refernced with respect
to this zero pressure are termed absolute pressures.
Many
pressure-measuring devices measure not absolute pressure but only difference in
pressure. For example, a Bourdon-tube gage indicates only the difference between
the pressure in the fluid to which it is tapped and the pressure in the
atmosphere. In this case, then, the reference pressure is actually the
atmospheric pressure. This type of pressure reading is called gage pressure.
For example, if a pressure of 50 kPa is measured with a gage referenced to the
atmosphere and the atmospheric pressure is 100 kPa, then the pressure can be
expressed as either
p = 50 kPa gage or p = 150 kPa absolute.
Whenever
atmospheric pressure is used as a reference, the possibility exists that the
pressure thus measured can be either positive or negative. Negative gage
pressure are also termed as vacuum pressures. Hence, if a gage tapped
into a tank indicates a vacuum pressure of 31 kPa, this can also be stated as
70 kPa absolute, or -31 kPa gage, assuming that the atmospheric pressure is 101
kPa absolute.
Pressure Measurement
Fluid Pressure
In a
stationary fluid the pressure is exerted equally in all directions and is
referred to as the static pressure. In a moving fluid, the static
pressure is exerted on any plane parallel to the direction of motion. The fluid
pressure exerted on a plane right angles to the direction of flow is greater
than the static pressure because the surface has, in addition, to exert
sufficient force to bring the fluid to rest. The additional pressure is
proportional to the kinetic energy of fluid; it cannot be measured
independently of the static pressure.
When the
static pressure in a moving fluid is to be determined, the measuring surface
must be parallel to the direction of flow so that no kinetic energy is
converted into pressure energy at the surface. If the fluid is flowing in a
circular pipe the measuring surface must be perpendicular to the radial
direction at any point. The pressure connection, which is known as a piezometer
tube, should flush with the wall of the pipe so that the flow is not
disturbed: the pressure is then measured near the walls were the velocity is a
minimum and the reading would be subject only to a small error if the surface
were not quite parallel to the direction of flow.
The static
pressure should always be measured at a distance of not less than 50 diameters
from bends or other obstructions, so that the flow lines are almost parallel to
the walls of the tube. If there are likely to be large cross-currents or
eddies, a piezometer ring should be used. This consists of 4 pressure
tappings equally spaced at 90o intervals round the circumference of
the tube; they are joined by a circular tube which is connected to the pressure
measuring device. By this means, false readings due to irregular flow or
avoided. If the pressure on one side of the tube is relatively high, the
pressure on the opposite side is generally correspondingly low; with the
piezometer ring a mean value is obtained.
Barometers 
A barometer
is a device for measuring atmospheric pressure. A simple barometer consists of
a tube more than 30 inch (760 mm) long inserted in an open container of mercury
with a closed and evacuated end at the top and open tube end at the bottom and
with mercury extending from the container up into the tube. Strictly, the space
above the liquid cannot be a true vaccum. It contains mercury vapor at its
saturated vapor pressure, but this is extremely small at room temperatures
(e.g. 0.173 Pa at 20oC).
The
atmospheric pressure is calculated from the relation Patm = ρgh
where ρ is the density of fluid in the barometer.
Piezometer
For
measuring pressure inside a vessel or pipe in which liquid is there, a tube may
be attached to the walls of the container (or pipe) in which the liquid resides
so liquid can rise in the tube. By determining the height to which liquid rises
and using the relation P1 = ρgh, gauge pressure of the liquid
can be determined. Such a device is known as piezometer. To avoid
capillary effects, a piezometer's tube should be about 1/2 inch or greater.
It is important that
the opening of the device to be tangential to any fluid motion, otherwise an
erroneous reading will result.
Manometers:
Manometers
A somewhat
more complicated device for measuring fluid pressure consists of a bent tube
containing one or more liquid of different specific gravities. Such a device is
known as manometer.
In using a
manometer, generally a known pressure (which may be atmospheric) is applied to
one end of the manometer tube and the unknown pressure to be determined is
applied to the other end.
In some
cases, however, the difference between pressure at ends of the manometer tube
is desired rather than the actual pressure at the either end. A manometer to
determine this differential pressure is known as differential pressure
manometer.
Manometers - Various forms
1. Simple U - tube
Manometer
2. Inverted U - tube
Manometer
3. U - tube with one leg
enlarged
4. Two fluid U - tube
Manometer
5. Inclined U - tube
Manometer
Simple U - tube Manometer
Equating the pressure
at the level XX'(pressure at the same level in a continuous body of fluid is
equal),
For the left
hand side:
Px
= P1 + rg(a+h)
For the
right hand side:
Px'
= P2 + rga + rmgh
Since Px
= Px'
P1
+ rg(a+h) = P2 + rga + rmgh
P1
- P2 = rmgh - rgh
i.e. P1
- P2 = (rm - r)gh.
The maximum value of P1 - P2 is limited by the height of the
manometer. To measure larger pressure differences we can choose a manometer
with heigher density, and to measure smaller pressure differences with accuracy
we can choose a manometer fluid which is having a density closer to the fluid
density.
Inverted U - tube Manometer
Inverted U-tube
manometer is used for measuring pressure differences in liquids. The space
above the liquid in the manometer is filled with air which can be admitted or
expelled through the tap on the top, in order to adjust the level of the liquid
in the manometer.
Equating the
pressure at the level XX'(pressure at the same level in a continuous body of
static fluid is equal),
For the left
hand side:
Px
= P1 - rg(h+a)
For the
right hand side:
Px'
= P2 - (rga + rmgh)
Since Px
= Px'
P1
- rg(h+a) = P2
- (rga + rmgh)
P1
- P2 = (r - rm)gh
If the
manometric fluid is choosen in such a way that rm << r then,
P1
- P2 = rgh.
For inverted
U - tube manometer the manometric fluid is usually air.
U - tube with one leg enlarged
Industrially,
the simple U - tube manometer has the disadvantage that the movement of the
liquid in both the limbs must be read. By making the diameter of one leg large
as compared with the other, it is possible to make the movement the large leg
very small, so that it is only necessary to read the movement of the liquid in
the narrow leg.
In figure,
OO' represents the level of liquid surface when the pressure
difference P1 - P2 is zero. Then when pressure is
applied, the level in the right hand limb will rise a distance h vertically.
Volume of
liquid transferred from left-hand leg to right-hand leg
= h(p/4)d2
where d is
the diameter of smaller diameter leg. If D is the diameter of larger diameter
leg, then, fall in level of left-hand leg
= Volume transferred/Area
of left-hand leg
= (h(p/4)d2) / ((p/4)D2)
= h(d/D)2
For the
left-hand leg, pressure at X , i.e. Px = P1 + rg(h+a) + rg h(d/D)2
For the
right-hand leg, pressure at X', i.e. Px' = P2 + rga + rg(h + h(d/D)2)
For the
equality of pressure at XX',
P1
+ rg(h+a) + rg h(d/D)2
= P2 + rga + rmg(h + h(d/D)2)
P1
- P2 = rmg(h + h(d/D)2) - rgh - rg h(d/D)2
If
D>>d then, the term h(d/D)2 will be negligible( i.e
approximately about zero)
Then P1
- P2 = (rm - r)gh.
Where h is the
manometer liquid rise in the right-hand leg.
If the fluid
density is negligible compared with the manometric fluid density ( eg. the case
for air as the fluid and water as manometric fluid ), then P1 - P2
= rm gh.
Two fluid U-tube Manometer
Small differences in
pressure in gases are often measured with a manometer of the form
Inclined U-tube manometer
Limititation
Manometers
The
manometer in its various forms is an extremely useful type of pressure
measuring instrument, but suffers from a number of limitations.
Pressure Gauges
Bourdon
Gauge:

The pressure
to be measured is applied to a curved tube, oval in cross section. Pressure
applied to the tube tends to cause the tube to straighten out, and the
deflection of the end of the tube is communicated through a system of levers to
a recording needle. This gauge is widely used for steam and compressed gases.
The pressure indicated is the difference between that communicated by the
system to the external (ambient) pressure, and is usually referred to as the
gauge pressure.
Buoyancy
Upthrust on
body = weight of fluid displaced by the body
This is known as Archimedes principle.
If the body is immersed so that part of its
volume V1 is immersed in a fluid of density r1 and the rest of its volume V2 in another immiscible
fluid of mass density r2,
Upthrust on upper part, R1 = r1gV1
acting through G1, the centroid of V1,
Upthrust on lower part,R2 = r2gV2
acting through G2, the centroid of V2,
Total upthrust = r1gV1 + r2gV2.
The positions of G1 and G2 are not necessarily on the same vertical line, and
the centre of buoyancy of the whole body is, therefore, not bound to pass
through the centroid of the whole body.
Systems of Units:
The official
international system of units (System International d'Units). Strong efforts
are underway for its universal adoption as the exclusive system for all
engineering and science, but older systems, particularly the cgs and fps
engineering gravitational systems are still in use and probably will be around
for some time. The chemical engineer finds many physiochemical data given in
cgs units; that many calculations are most conveniently made in fps units; and
that SI units are increasingly encountered in science and engineering. Thus it becomes
necessary to be expert in the use of all three systems.
SI system:
Primary
quantities:
|
Quantity |
Unit |
|
Mass in
Kilogram |
kg |
|
Length in
Meter |
m |
|
Time in
Second |
s or as
sec |
|
Temperature
in Kelvin |
K |
|
Mole |
gmol or
simply as mol |
Derived
quantities:
|
Quantity |
Unit |
|
Force in
Newton (1 N = 1 kg.m/s2) |
N |
|
Pressure
in Pascal (1 Pa = 1 N/m2) |
N/m2
|
|
Work,
energy in Joule ( 1 J = 1 N.m) |
J |
|
Power in
Watt (1 W = 1 J/s) |
W |
cgs Units:
The older centimeter-gram-second
(cgs) system has the following units for derived quantities:
|
Quantity |
Unit |
|
Force in
dyne (1 dyn = 1 g.cm/s2) |
dyn |
|
Work,
energy in erg ( 1 erg = 1 dyn.cm = 1 x 10-7 J ) |
erg |
|
Heat
Energy in calorie ( 1 cal = 4.184 J) |
cal |
fps Units:
The
foot-bound-second (fps) system has long been used in commerce and engineering
in English-speaking countries.
|
Quantity |
Unit |
|
Mass in
pound ( 1 lb = 0.454 kg) |
lb |
|
Length in
foot (1 ft = 0.3048 m) |
ft |
|
Temperature
in Rankine |
oR |
|
Force in
lbf ( 1 lbf = 32.2 lb.ft/s2) |
lbf |
Conversion factors:
Mass:
1 lb = 0.454
kg
Length:
1 inch =
2.54 cm = 0.0254 m
1 ft = 12
inch = 0.3048 m
Energy:
1 BTU = 1055
J
1 cal =
4.184 J
Force:
1 kgf
= 9.812 N
1 lbf
= 4.448 N
1 dyn = 1
g.cm/s2
Power:
1 HP = 736 W
Pressure:
1 Pa = 1 N/m2
1 psi = 1 lbf/inch2
1 atm =
1.01325 x 105 N/m2 = 14.7 psi
1 Bar = 105
N/m2
Viscosity:
1 poise = 1
g/(cm.s)
1 cP =
(1/100) poise = 0.001 kg/(m.s)
Kinematic
viscosity:
1 Stoke = 1
St = 1 cm2/s
Volume:
1 ft3
= 7.481 U.S. gal
1 U.S. gal =
3.785 litre
Temperature:
ToF
= 32 + 1.8oC
ToR
= 1.8K
Gas
Constant:
R = 8314 J /
(kmol.K)
Dimensions:
Dimensions of the primary quantities:
|
Fundamental dimension |
Symbol |
|
Length |
L |
|
Mass |
M |
|
Time |
t |
|
Temperature |
T |
Dimensions of derived quantities, can be expressed in terms of the
fundamental dimensions.
|
Quantity |
Representative symbol |
Dimensions |
|
Angular
velocity |
w |
t-1 |
|
Area |
A |
L2 |
|
Density |
r |
M/L3 |
|
Force |
F |
ML/t2 |
|
Kinematic
viscosity |
n |
L2/t |
|
Linear
velocity |
v |
L/t |
|
Linear
acceleration |
a |
L/t2 |
|
Mass flow
rate |
m. |
M/t |
|
Power |
P |
ML2/t3 |
|
Pressure |
p |
M/Lt2 |
|
Sonic
velocity |
c |
L/t |
|
Shear
stress |
t |
M/Lt2 |
|
Surface
tension |
s |
M/t2 |
|
Viscosity |
m |
M/Lt |
|
Volume |
V |
L3 |
Similitude and model studies:
Similitude
Whenever it
is necessary to perform tests on a model to obtain information that cannot be obtained
by analytical means alone, the rules of similitude must be applied. Similitude
is the theory and art of predicting prototype performance from model
observations.
Model Study: Present engineering practice makes use of
model tests more frequently than most people realize. For example, whenever a
new airplane is designed, tests are made not only on the general scale model
but also on various components of the plane. Numerous tests are made on
individual wing sections as well as on the engine pods and tail sections.
Models of
automobiles and high-speed trains are also tested in wind tunnels to predict
the drag and flow patterns for the prototype. Information derived from these
model studies often indicates potential problems that can be corrected before
prototype is built, thereby saving considerable time and expense in development
of the prototype.
Marine
engineers make extensive tests on model shop hulls to predict the drag of the
ships.
Geometric similarity refers to linear
dimensions. Two vessels of different sizes are geometrically similar if the
ratios of the corresponding dimensions on the two scales are the same. If
photographs of two vessels are completely super-impossible, they are
geometrically similar.
Kinematic similarity refers to motion
and requires geometric similarity and the same ratio of velocities for the
corresponding positions in the vessels.
Dynamic similarity concerns forces and
requires all force ratios for corresponding positions to be equal in
kinematically similar vessels.
The requirement for similitude of flow between model and
prototype is that the significant dimensionless parameters must be equal for
model and prototype
Dimensional Analysis:
Many important
engineering problems cannot be solved completely by theoretical or mathematical
methods. Problems of this type are especially common in fluid-flow, heat-flow,
and diffusional operations. One method of attacking a problem for which no
mathematical equation can be derived is that of empirical experimentations. For
example, the pressure loss from friction in a long, round, straight, smooth
pipe depends on all these variables: the length and diameter of the pipe, the
flow rate of the liquid, and the density and viscosity of the liquid. If any
one of these variables is changed, the pressure drop also changes. The
empirical method of obtaining an equation relating these factors to pressure
drop requires that the effect of each separate variable be determined in turn
by systematically varying that variable while keep all others constant. The
procedure is laborious, and is difficult to organize or correlate the results
so obtained into a useful relationship for calculations.
There exists
a method intermediate between formal mathematical development and a completely
empirical study. It is based on the fact that if a theoretical equation does
exist among the variables affecting a physical process, that equation must be
dimensionally homogeneous. Because of this requirement it is possible to group
many factors into a smaller number of dimensionless groups of variables. The
groups themselves rather than the separate factors appear in the final
equation.
Dimensional
analysis does not yield a numerical equation, and experiment is required to
complete the solution of the problem. The result of a dimensional analysis is
valuable in pointing a way to correlations of experimental data suitable for
engineering use.
Dimensional
analysis drastically simplifies the task of fitting experimental data to design
equations where a completely mathematical treatment is not possible; it is also
useful in checking the consistency of the units in equations, in converting
units, and in the scale-up of data obtained in physical models to predict the
performance of full-scale model. The method is based on the concept of
dimension and the use of dimensional formulas.
Important Dimensionless Numbers in Fluid Mechanics:
|
Dimensionless Number |
Symbol |
Formula |
Numerator |
Denominator |
Importance |
|
Reynolds number |
NRe |
Dvr/m |
Inertial
force |
Viscous
force |
Fluid flow
involving viscous and inertial forces |
|
Froude number |
NFr |
u2/gD |
Inertial
force |
Gravitational
force |
Fluid flow
with free surface |
|
Weber number |
NWe |
u2rD/s |
Inertial
force |
Surface
force |
Fluid flow
with interfacial forces |
|
Mach number |
NMa |
u/c |
Local
velocity |
Sonic
velocity |
Gas flow
at high velocity |
|
Drag coefficient |
CD |
FD/(ru2/2) |
Total drag
force |
Inertial
force |
Flow around
solid bodies |
|
Friction factor |
f |
tw/(ru2/2) |
Shear
force |
Inertial
force |
Flow
though closed conduits |
|
Pressure coefficient |
CP |
Dp/(ru2/2) |
Pressure
force |
Inertial
force |
Flow
though closed conduits. Pressure drop estimation |
(a) Newton's range of
operation
(b) Intermediate range of operation
Part B (5 x 12 = 60 Marks)
Or
Or
Or
(i) Porosity of static bed
and porosity of fluidized bed
(ii) Minimum pressure drop and bed pressure drop in fluidized process.
(c) Differentiate between the
following in a fluidized bed reactor. (4)
(i) Working velocity
(ii) Actual velocity
Or
Or
Mathematics for
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EngineeringOCTechnology
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Last Updated: 03/10/03
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