IE 211
INTRODUCTION TO ENGINEERING THERMODYNAMICS
Chapter1Introduction and Basic Concepts
INDUSTRIAL REVOLUTION
A period in 18th and early 19th
centuries
Major changes in agriculture, mining,
manufacturing, and transportation
The First Industrial Revolution, which
began in the 18th century, merged into the
Second Industrial Revolution around 1850,
when technological and economic
progress
Emerged in United Kingdom, then
spread throughout Europe, North
America and eventually the world
It started with the mechanisation of the textile industries, the development of iron-
making techniques
Trade expansion was enabled by the introduction of canals, improved roads and railways.
The introduction of steam power resulted in enourmous increase in production capacity.
THERMODYNAMICS deals with energy and can be defined as the science of energy. It gives the relation between energy, heat and work.
Therme (heat) dynamis (power)
Stems from the Greek words
Thermodynamics emerged as a science during the construction of the first successful atmospheric steam engines in England (1697-1712)
Thermodynamics term was firstly used in a publication of Lord Kelvin in 1849. The first thermodynamic
textbook was written in 1859 by William Rankine
German physicist, created the science of thermodynamics. The first law of thermodynamics:
(conservation of energy)
He developed the idea of absolute zero and independently recognized its first and second laws of thermodynamics. With James Prescott Joule, Kelvin discovered that gases cool when allowed to expand, the Joule-Thomson effect.
Rudolph Clausius
(William Thomson )Lord Kelvin
The first and second law of thermodynamics emerged simultaneously in 1850s, primarily out of the work of William Rankine, Rudolph Clausius and Lord Kelvin
Proposed another thermodynamic temperature scale which also assigned 0 to thermodynamic absolute zero, but used the degree Fahrenheit as its base unit.
William Rankine
The first law of thermodynamics: (conservation of energy)
‘’Energy can be changed from one form to another, but it cannot be created or destroyed. ‘’
The total amount of energy and matter in the Universe remains constant, merely changing from one form to another.
i.e. Falling of a rockConversion of potential energy to kinetic energy
i.e. Human body
The second law of thermodynamics: (energy has quality as well as quantity)
‘’Heat always flows from a warm body to a cooler one, never the other way.‘’
i.e. Cooling of a cup of coffee
- Actual processes occur in the direction of decreasing quality of energy
THERMODYNAMICS
Classical Thermodynamics Statistical ThermodynamicsAnalyses the macroscopic properties of the system using classical laws of thermodynamics
Analyzes thermodynamic properties by relating them to molecular-level models of microscopic behaviour
Application Areas
Household Appliances-Heating and air conditioning system-Refrigerator-Water heater-The shower
In the design of -Automotive engines-Rockets-Jet engines-Power Plants -Solar collectors
DIMENSIONS AND UNITSPhysical quantity is characterized by dimensions. The magnitudes of the dimensions are specified by units.
1) Fundamentals dimensions; mass(m), length(L), time(t), temperature(T)2) Secondary (drived) dimensions; velocity(v), energy(E), volume ( )
Two sets of units
English SystemUnited States Customary System (USCS)
Metric, SI, International system
Based on decimal relationship between units
.......10-3(milli,m), 10-2(centi, c), 10-1 (deci,d), 101 (deka, da).....
Example:
Dimension:Length; Unit: METER(m) ....mm, cm, m, ..,km....
Dimension:Mass; Unit: GRAM(g) ....mg, cg, g,..., kg
SOME SI and ENGLISH UNITS
SI unit English unit
Kilogram (kg)Meter (m)Second(s)Newton(N)= 1 kg.m/s2
Joules(J) = N.m...
Dimension
MassLengthTimeForceEnergy...
Pound-mass (lbm)Foot(ft)Second(s)1 lbf=32.174 lbm.ft/s2
British thermal unit(Btu)...
1) MASS and WEIGHTMass is an intrinsic property of matterWeight is a force that results from the action of gravity on matter (It’s magnitude is determined from Newton’s second law)
W = m.g (N)
g decreases with altitude, so that a body weighs less on top of a mountain On the surface of moon, an astronaut weighs about one-sixth of what he or she normally weighs on earth
2) DENSITY
= m/V ; (kg/m3 or lbm/ft3)
= f(P,T)
For most gases P 1/T For liquids and solids variation of density with pressure is negligableEffect of temperature;
water= 998 kg/m3 20oC at 1 atm
water = 975 kg/m3 75oC at 1 atm
Specific gravity: density of a substance relative to density of a well-known substance, e.g. water
S.G. = / water(at 4 oC)
Specific weight: The weight of a unit volume of a substance
s = .g
3) TEMPERATURE
We can measure temperature;
by our sensations; freezing cold, warm, hot, red-hot
Mercury in glass thermometer (based on the expansion of
mercury with temperature)
Many physical properties of materials including the phase (solid, liquid, gaseous or
plasma), density, solubility, vapor pressure, and electrical conductivity depend on the
temperature.
Ice (freezing) point: A mixture of ice and liquid water that is in equilibrium
with air saturated with vapor at 1 atm. pressure is said to be at the ice point.
Steam (boiling) point: Mixture of liquid water and water vapor (with no air) in
equilibrium at 1 atm. pressure is said to be at the steam point.
Phase Changes;
Celcius(oC), Fahrenheit(oF), Kelvin(K), Rankine(R)
In most of the world the Celsius scale is used for most temperature measuring
purposes.
TEMPERATURE SCALES:
SI Units English System
oC (Celcius scale)
0 oC
100 oC
oF (Fahrenheit scale)
32 oF
212 oF
Ice point.............
Steam point.....
These are often referred to as two-point scales since temperature values are
assigned at two different points
Conversion: 9/5T(oC) + 32 = T(oF)
Temperature scale that is independent of the properties of any substance is
called thermodynamic temperature scale.
Kelvin(K) scale (lowest temperature on this scale is 0 K)
SI Units English System
K (Kelvin scale) R (Rankine scale)
Conversion:
T(R) = 1.8T(K)
T(K) = T(oC) + 273.15
T(R) = T(oF) + 459.67
T(oF) = 9/5T(oC) + 32
SI system English system
Temp. Difference:
T(oC) = T(K)
T(oF) = T(R)
IDEAL GAS TEMPERATURE SCALE:
The temperatures on this scale are measured using a constant-volume gas
thermometer, which is basically a rigid vessel filled with a gas, usually hydrogen or
helium, at low pressure.
This thermometer is based on the principle that at low pressures, the temperature
of a gas is proportional to its pressure at constant volume.
T = a + bP
Ideal gas temperature scale can be
developed by measuring the pressure of gas
at ice and steam points
ABSOLUTE GAS TEMPERATURE SCALE:
Constant ‘’a’’ is assumed to be zero.
T = bP
4) PRESSURE
A normal force exerted by a fluid per unit area (related to gas or liquid). In solids
it is normal stress.
It has the unit of newtons per square meter (N/m2), which is called
a pascal (Pa)
Other pressure units: bar, standard atmosphere, kilogram-force per square
centimeter
How a person can walk on fresh snow without sinking by wearing large
snowshoes? And how a person cuts with little effort when using a sharp
knife?
SI Units English System
Pa (N/m2), atm, bar, kgf/cm2 , mmHg psi(lbf/in2), Psia, lbf/ft2, in Hg
Conversion between SI units:
1 bar = 105 Pa = 0.1 MPa1 atm = 760 mmHg = 101.325 kPa = 1.01325 bars1 kgf/cm2 = 9.807 N/cm2 = 9.807x104 Pa = 0.9807 bar = 0.9679 atm
ABSOLUTE PRESSURE: The actual pressure at a given position. It is measured
relative to absolute vacuum(absolute zero pressure)
GAGE PRESSURE: The difference between the absolute pressure and the
local atmospheric pressure.Example:The gage used to measure the air pressure in an automobile tire relative to atmospheric pressure
VACUUM PRESSURE: Pressure below atmospheric pressure
Pgage = Pabs - PatmPvac = Patm - Pabs
In thermodynamic calculations absolute pressure is used.
VARIATION of PRESSURE WITH DEPTH
Pressure in a fluid increases with depth because more fluid rests on deeper
layers.
P2 = Patm + gh
A consequence of the pressure in a fluid remaining constant in horizontal
directions is that ‘’ the pressure applied to a confined fluid increases the pressure
throughout the same amount’’ This is called PASCAL’S LAW
Force applied by a fluid is proportional to the surface area
This enables us to lift a car easily by one arm, e.g. Hydraulic lifts
Two hydraulic cylinders of different areas
could be connected, and the larger could
be used to exert a proportionally greater
force than that applied to the smaller.
P1 = P2 at the same levels, then;
F1/A1 =F2/A2 F2/F1 = A2/A1
THE MANOMETER
A manometer consists of a glass or plastic U-tube containing mercury,
water, alcohol or oil and it is used measure the gas pressures
P2 = Patm + gh
P2 = Patm + 1gh1 + 2gh2 + 2gh2
A manometer containing multiple immiscible fluids:
THE BAROMETER
Atmospheric pressure is measured by barometer (Italian Evangeliste Torricelli,
1608-1647)
Atmospheric pressure can be measured by inverting a mercury filled tube into
a mercury container that is open to the atmosphere.
PB = Patm, Pc 0
Pc + gh = PB = Patm
Patm = gh
Pressure units
760 mmHg = 1 atm
1 mmHg = 1 Torr
1 atm = 101.325 kPa
At sea level !!!
5) HEAT (Q)
Heat is defined as an energy transfer to a body in any other way than due
to work performed on the body
SI Units :Joules(J)
Energy transfer by heat can occur between objects by radiation, conduction
and convection
A red-hot iron rod from which heat transfer to the
surrounding environment will be primaily through
radiation.
HEAT TRANSFER
6) WORK (W)
Form of energy; force times distance, (N.m) or joules(J)
In metric system: The amount of energy needed to raise the temperature of 1 g of water at 14.5 oC by 1 oC is defined as 1 calorie (cal)
1 cal = 4.1868 J
In English system: Energy unit is the Btu (British thermal unit) : energy required to raise the temperature of 1 lbm of water at 68 oF by 1 oF
1 Btu = 1.0551 kJ
Definition of work
SYSTEMS AND CONTROL VOLUMES
The mass or region outside the system
The real or imaginary surface that seperates system from its surroundings (has zero thickness)
Quantity of matter or region in space chosen for study
SYSTEMS
Closed Systems (Control mass) Open Systems (Control volume)
Consists of fixed amount of mass No mass can cross its boundaryEnergy (heat&work) can cross the boundary Volume does not have to be fixed
Special Case: isolated system
Rigid walls. No mass and energy (heat&work) transfer!
Encloses a device that involves mass flow such as a compressor, turbine or nozzleBoth mass and energy(heat&work) can cross the boundary A control volume may also involve a moving boundary
Control surface
Adiabatic system: A kind of closed system
No mass transfer Energy can cross the boundary only in the form of work
Water heater
Car radiator
Air compressor
Examples of Open Systems (Control Volumes)
Wind Turbine
Gas Turbine
PROPERTIES OF A SYSTEM
Any characteristics of a system is called property
e.g. Pressure, temperature, volume, mass, viscosity, thermal conductivity, thermal expansion coefficient
1) Intensive Properties: Independent of the mass of a systemTemperature (T); (oC, K, oF, oR)Pressure (P); (Pa or Psi)Chemical potential ( i); (kJ/mole, Btu/mole)
2) Extensive Properties: Depend on the size or extent of the systemMass(m); (kg or lbm)volume ( ); (m3 or ft3)Momentum EnergyEnthalpyEntropy
Extensive properties per unit mass are called specific properties
e.g. Specific volume; = /m; (m3/kg or ft3/lbm)Specific total energy, e = E/m; (kJ/kg)
STATE AND EQUILIBRIUM The stationary condition of the system at which properties are defined is called state of system.
Equilibrium implies a state of balance.A system in equilibrium experiences no changes when it is isolated from its surroundings
• Thermal equilibrium (temp. is same)• Mechanical equilibrium (pressure is same)• Phase equilibirum (mass of each phase reaches an equilibrium level)• Chemical equilibrium (chemical composition does not change with time)
Expansion of gas
THE STATE POSTULATE
When sufficient number of properties are specified the rest of the properties assume certain values automatically.
The number of properties required to fix the state of a system is given by the system postulate
The state of a simple compressible system (absence of electrical, magnetic, gravitational, motion and surface tension effects) ;
Specified by two independent, intensive properties (temperature and specific volume)
PROCESSES AND CYCLES Process: changes that occur when a system changes its state from one
equilibrium state to another
(Series of states that system passes during a process)
Cycle: a system is said to have undergone a
cycle if it returns to its initial state at the end of
process
Property A
Property B
State 1
State 2
Quasistatic or quasi-equilibrium process: System is close to equilibrium
Example: Very slow compression of a gas
Gas molecules will have sufficient time to redistribute and there
will not be a molecule pile up in front of the piston
PROCESSES
Isothermal Process Isobaric Process Isochoric (or isometric) Process
Temperature remains
constant
Constant pressureConstant specific volume
STEADY-STATE
A system in a steady state has numerous properties that are unchanging in time
In steady-state processes fluid flows through a control volume steadilyExample: Turbines, pumps, boilers, refrigeration systems
During steady-state flow fluid properties can change from point to point within
the control volume, but at any fixed point they remain the same during the entire
process
Therefore, volume ( ), mass(m) and total energy (E) remain constant
TEMPERATURE AND ZEROTH LAW OF THERMODYNAMICS
When two materials at different temperatures contact each other heat is
transferred from the body at higher temperature to one lower temperature until
both bodies attain the same temperatures (thermal equilibrium)
Zeroth Law of Thermodynamics: If two bodies are in thermal equilibrium with
a third body, they are also in thermal equilibrium with each other
Third body may be replaced by a thermometer (object#1)
Note: they are not in contact
Assignments:
Examples 1-6, 1-7, 1-8, 1-9