Thermodynamics
Thermodynamics
Thermodynamics
Thermodynamics is a branch of physical sciences that treats various phenomena of energy and the
related properties of matter, especially of the laws of transformation of heat into other forms of energy and
vice versa.
9 5
F= C+32 C = (F − 32)
5 9
R = F + 460 K = C + 273
TEMPERATURE INTERVAL – is the difference between two temperature readings from the same scale,
and the change in temperature through which the body is heated.
∆TK = ∆TC 5 4
∆𝑇𝐶 = ∆𝑇𝐹 1°Re = ℃
9 5
∆TR = ∆TF
9 1°RE = 20°L
∆TF = ∆T
5 C
Note: 1C° = 9/5 F° and degree is to be written after the scale to indicate that it is temperature change.
Gage Pressure – is the pressure measured from the lvel of atmospheric pressure by most pressure
recording instrument like pressure gage and open-ended manometer.
Note: Pgage = negative (-) when the pressure is vacuum. The pressure in perfect vacuum is -101.325 Kpa
System – is the term given to the collection of matter under consideration enclosed within a boundary.
Surrounding – is the region outside the boundary or the space and matter external to a system.
Closed System – is a system in which there is no transfer of matter across the boundary.
Open System – is a system in which there is a flow of matter across the boundary.
Isolated System – is a system in which neither mass nor energy cross the boundaries and it is not
influenced by the surroundings.
Nonflow process – is a process that takes place in a closed system. Example: Compressor
Steady flow process – is a process that takes place in an open system in which the quantity of matter
within the system is constant. Example: Turbine
Where: P = pressure
V = volume
Mass (m1) entering the system is equal to the sum of the stored mass (Δm) and the mass (m 2) that
leaves the systems.
m1 = m2 + ∆m
∆m = m1 − m2
m1 = m2
A1 V1 ρ1 = A2 V2 ρ2
where:
A = cross-sectional area
V = velocity
ρ = density
❖ HEAT and ENTROPY:
Heat – is a form of energy associated with the kinetic random motion of large number of molecules.
Sensible Heat – is the heat needed to change the temperature of the body without changing its
phase.
Q s = mC∆T
Where: Qs = sensible heat
m = mass
ΔT = change in temperature
C = specific heat
Latent Heat – is the heat needed by the body to change its phase without changing its temperature.
Internal Energy – is the energy stored within the body. It is the sum of the kinetic energies of all its
constituent particles plus the sum of all the potential energies of interaction among
these particles.
H = U + PV
Where: H = enthalpy
U = internal energy
P = absolute pressure
V = volume
Energy cannot be created nor be destroyed, it can only be transformed from form to another.
Where:
PE = potential energy
KE = kinetic energy
H = U + PV
H = enthalpy
PV = mRT ̅T
PV = nR
J ft − lb L − atm
̅ = 8.314
R = 1545 = 0.821
mol. K mol. °R mol. K
✓ Finding the value of the gas constant given the universal gas constant:
̅
R 8.314J⁄mol−K
Examples R(O2 ) = =
MW(O2 ) 32kg⁄mol
R(O2 ) = 0.268 J⁄kg − K
̅
R 1545 ft − lbf ⁄mol − °R
R(O2 ) = =
MW(O2 ) 32 lbm ⁄mol
ft − lbf
R(O2 ) = 48.28
lbm − °R
ft − lbf kJ
R air = 53.34 = 0.287
lbm °R kg − K
Cp − Cv = R Cp
=k
Cv
R kR
Cv = Cp =
k−1 k−1
Where: Cp = specific heat at constant pressure
Cv = specific heat at constant volume
K = specific ratio
R = gas constant
Heat cannot be transferred from cold body to a hot body without an input of work. It similarly states
that heat cannot be converted 100% into work. The bottom line is that an engine must operate
between a hot and cold reservoir. Also indicated, is that energy cannot naturally move from realm of
lower potential to a realm of higher potential.
❖ BOYLE’S LAW
In a confined gas, if the absolute temperature is held constant, the volume is inversely proportional to
the absolute pressure.
P1 V1 = P2 V2
❖ CHARLE’S LAW
In a confined gas, if the absolute pressure is held constant, the volume is directly proportional to ht
absolute temperature.
V1 V
= T2
T1 2
in a confined gas, if the volume is held constant, the absolute pressure is directly proportional to the
absolute temperature.
P1 P
= T2
T1 2
P = P1 + P2 + P3 + ⋯ + Pn
Where:
P = total pressure of the mixture
P1, P2, P3, …, Pn = partial pressure of gases
Partial pressure – is the pressure exerted by each gas.
❖ AVOGADRO’S LAW
At equal volume, at the same temperature and pressure conditions, the gases contain the same
number of molecules.
m1 M R1 M
= M1 or = M1
m2 2 R2 2
Where:
m1 & m2 are masses
M1 & M2 are Molecular weights
R1 & R2 are gas constants
∆H = mCp ∆T
Where:
❖ THERMODYNAMIC PROCESSES
PROCESSES
Whenever a system undergoes any change, it is said to have described a process.
CYCLIC PROCESS
Cyclic Process – a process which gives the same states/conditions after the system undergoes a
series of processes.
QUASI-STATIC PROCESS
Quasi-static Process – is one in which system departs from equilibrium state only infinitesimally at
every instant.
P1 P2
=
T1 T2
b. PV and TS Diagram
c. Nonflow Work
2
Wn = ∫1 PdV where: dV = 0 @ V = C
Wn = 0
∆𝑈 = 𝑚𝐶𝑣 ∆𝑇
f. Change in Enthalpy
∆𝐻 = 𝑚𝐶𝑝 ∆𝑇
g. Heat Transferred
𝑄 = ∆𝑈 + 𝑊𝑛
𝑊𝑛 = 0 @ 𝑉 = 𝐶
𝑄 = ∆𝑈
h. Change in Entropy
𝑑𝑄
𝑓𝑟𝑜𝑚: 𝑑𝑆 =
𝑇
𝑇2
∆𝑆 = 𝑚𝐶𝑣 ln ( )
𝑇1
2. Isobaric Process
a. PV an T relation (P = C)
𝑉1 𝑉
= 𝑇2 (Charles’ Law)
𝑇1 2
b. PV and TS Diagram
c. Nonflow Work
2
Wn = ∫ Pdv
1
Wn = P(V2 − V1 )
Wn = ∫ VdP where ∶ dP = 0 @ P = C
1
Ws = 0
∆U = mCv ∆T
f. Change in Enthalpy
∆H = mCp ∆T
g. Heat Transferred
Q = ∆U + Wn
Q = ∆U + ∆PV
Q = ∆H
h. Change in Entropy
dQ
from ∶ dS =
dT
T2
∆S = mCp ln ( )
T1
3. Isothermal Process
Isothermal Process is an internally reversible constant temperature process of a working
substance.
a. PV and T relation ( T = C )
P1 V1 = P2 V2 (Boyle′ s Law)
b. PV and TS Diagram
c. Nonflow Work
2
Wn = ∫ PdV
1
C
Where: P =
v
V2 V2
Wn = P1 V1 ln ( ) = mRT ln ( )
V1 V1
∆𝑈 = 0
f. Change in Enthalpy
∆𝐻 = 0
g. Heat Transferred
𝑄 = ∆𝑈 + 𝑊𝑛
∆𝑆 = 𝑊𝑛 (𝑓𝑜𝑟 ∆𝑈 = 0)
h. Change in Entropy
𝑑𝑄
𝑓𝑟𝑜𝑚 ∶ 𝑑𝑆 =
𝑇
𝑉2
∆𝑆 = 𝑚𝑅 ln ( )
𝑉1
4. Isentropic Process
Isentropic Process is an internally reversible constant entropy process of a working substance. It
is also known as a reversible adiabatic process.
Adiabatic Process is a reversible process in which there is no flow of heat between a system and
its surroundings ( Q = 0 ).
T1 V2 k−1
=( ) ⇒ temperature − volume
T2 V1
k−1
T1 P1 k
=( ) ⇒ temperature − pressure
T2 P2
b. PV and TS Diagram
c. Nonflow Work
2
C
Wn = ∫ Pdv where: P =
Vk
1
P2 V2 − P1 V1 mR(T2 − T1 )
Wn = =
1−k 1−k
k(P2 V2 − P1 V1 ) kmR(T2 − T1 )
Ws = =
1−k 1−k
Ws = kWn
∆𝐻 = 𝑚𝐶𝑣 ∆𝑇 = −𝑊𝑛
f. Change in Enthalpy
∆𝐻 = 𝑚𝐶𝑝 ∆𝑇
𝑄=0
𝑄 = ∆𝑈 + 𝑊𝑛
∆𝑈 = −𝑊𝑛
h. Change in Entropy
∆𝑆 = 0
5. Polytropic Process
Polytropic Process is an internally reversible process during which PVn = C, where; n is constant.
𝑇1 𝑉2 𝑛−1
=( ) ⇒ 𝑡𝑒𝑚𝑝𝑒𝑟𝑎𝑡𝑢𝑟𝑒 − 𝑣𝑜𝑙𝑢𝑚𝑒
𝑇2 𝑉1
𝑛−1
𝑇1 𝑃1 𝑛
=( ) ⇒ 𝑡𝑒𝑚𝑝𝑒𝑟𝑎𝑡𝑢𝑟𝑒 − 𝑝𝑟𝑒𝑠𝑠𝑢𝑟𝑒
𝑇2 𝑃2
b. PV and TS Diagram
c. Nonflow Work
2
C
Wn = ∫ Pdv where: P =
Vn
1
P2 V2 − P1 V1 mR(T2 − T1 )
Wn = =
1−n 1−n
k(P2 V2 − P1 V1 ) kmR(T2 − T1 )
Ws = =
1−n 1−n
Ws = nWn
∆U = mCv ∆T
f. Change in Enthalpy
∆H = mCp ∆T
g. Heat Transferred
Q = mCn ∆T
k−n
Where; Cn = Cv ( )
1−n
h. Change in Entropy
dQ
from: dS =
T
T2
∆S = mCn ln ( )
T1
𝐏𝐕 𝐧 = 𝐂
If:
n = 0; Isobaric Process
n = 1; Isothermal Process
n = k; Isentropic Process
n = −∞ to +∞; Polytropic Process
n = ∞; Isometric Process
𝑚 = 𝑚1 + 𝑚2 + 𝑚3 + ⋯ + 𝑚𝑛
𝑣 = 𝑣1 + 𝑣2 + 𝑣3 + ⋯ + 𝑣4
𝑃 = 𝑃1 + 𝑃2 + 𝑃3 + ⋯ + 𝑃𝑛
Saturation Temperature is the temperature at which liquid start to boil and vapour start to condense.
Example, water boils @ 200°C at a pressure of 1.55 MPa
Subcooled Liquid is a liquid whose temperature is lower than the saturation temperature
corresponding to the given pressure.
Example, Liquid water @ 50°C and 97.78 kPa is Subcooled liquid since 50°C is less than 99°C (t sat
@ 97.78 kPa).
Compressed Liquid is a liquid whose pressure is higher than the saturation pressure corresponding
to the given temperature.
Example, Liquid water @ 105 kPa and 90°C is a compressed since 105 kPa is greater than
70.14kPa (Psat @ 90°C).
Saturated Liquid is a liquid at the saturation temperature or pressure whose temperature is equal to
the boiling point corresponding to the given pressure. It has no vapour content.
Example, Liquid water @ 50°C and 12.35 kPa is a saturated liquid since the given temperature,
50°C is equal to 50°C (tsat @ 12.35 kPa).
Vapor is the term given to a gaseous phase that is in contact with the liquid phase.
Example, steam
Saturated Vapor is a vapor whose temperature and pressure. It has no liquid or moisture content.
Example, Steam at 300°C and 8.58 MPa
Superheated Vapor is a vapor whose temperature is higher than the saturation temperature
corresponding to the given pressure.
Example, Steam @ 350°C and 11.8 MPa is a superheated vapor since 350°C is greater than
324°C (tsat @ 11.88 Mpa)
Degrees Superheat is the difference between the actual superheated temperature and the saturation
temperature.
Example, find the degrees superheated of steam at 350°C and 8.58 MPa.
Solution:
Degrees Subcooled is the difference between the saturation temperature and the actual Subcooled
temperature.
Example, Find the degrees Subcooled of liquid water @ 50°C and 19.94 MPa.
Solution:
Example, Steam @ 15 MPa and 310°C is a wet vapor since 310°C is less than 342.24°C (tsat @ 15
MPa).
Quality of Wet Vapor is the fraction or percentage by weight that is saturated vapor. It is the ratio of
the mass of saturated vapor to the total mass of the mixture.
mg
x= mt
Where: x = quality of wet vapor
mg = mass of vapor
mt = mass of the mixture (wet vapor)
Percentage moisture is the fraction or percentage by weight that is saturated liquid. It is the ratio of
the mass of saturated liquid to the total mass of the mixture.
m
y = mf
t
Critical Point is a point that represents the pressure and temperature at which liquid and vapor can
coexist in equilibrium.
1. 𝑣 = 𝑣𝑓 + 𝑥𝑣𝑓𝑔
2. 𝑢 = 𝑢𝑓 + 𝑥𝑢𝑓𝑔
3. ℎ = ℎ𝑓 + 𝑥ℎ𝑓𝑔
4. 𝑠 = 𝑠𝑓 + 𝑥𝑠𝑓𝑔
Note: 𝑥 = 1 − 𝑦
5. 𝑣𝑓𝑔 = 𝑣𝑔 − 𝑣𝑓
6. 𝑢𝑓𝑔 = 𝑢𝑔 − 𝑢𝑓
7. ℎ𝑓𝑔 = ℎ𝑔 − ℎ𝑓
8. 𝑠𝑓𝑔 = 𝑠𝑔 − 𝑠𝑓
Where:
v = specific volume
u = specific internal energy
h = specific enthalpy
s = specific entropy
x = quality
f = fluid
g = vapor
fg = mixture change by evaporation
y = % moisture
Note: The properties of liquid and vapor at a given temperature and pressure can be found in Steam table
and Mollier chart.
❖ PROCESS INVOLVING PURE SUBSTANCE
Vapors (steam) and Ideal gases have similarity in their processes but ideal gas equations are not
generally applicable to vapors.
b. Nonflow Work
2
Wn = ∫ PdV
1
Where: dV = 0 @ V
Wn = 0
Ws = ∫ VdP = V(P1 − P2 )
1
Ws = Q − ∆KE − ∆PE − ∆H
∆U = m(u2 − u1 )
e. Change in Enthalpy
∆H = m(h2 − h1 )
f. Heat Transferred
Q = ∆U
Q = m(u2 − u1 )
g. Change in Entropy
∆S = m(s2 − s1 )
2. Isobaric Process
Isobaric process is a constant pressure process of a pure substance.
a. PV and TS Diagram
b. Nonflow Work
2
Ws = − ∫ VdP
1
Ws = 0 where: dP = 0 ( P = C )
∆U = m(u2 − u1 )
e. Change in Enthalpy
∆H = m(h2 − h1 )
f. Heat Transferred
Q = u2 − u1 + Wn
Q = h2 − h1
g. Change in Entropy
∆S = m(s2 − s1 )
3. Isothermal Process
Isothermal process is an internally reversible constant temperature process of a pure substance.
a. PV and TS Diagram
b. Nonflow Work
Wn = Q − ∆U
Ws = Q − ∆KE − ∆PE − ∆H
∆U = m(u2 − u1 )
e. Change in Enthalpy
∆H = m(h2 − h1 )
f. Heat Transferred
Q = T∆S = T(S2 − S1 )
g. Change in Entropy
∆S = m(s2 − s1 )
a. PV and TS Diagram
b. Nonflow Work
Wn = Q − ∆U where ; Q = 0 (adiabatic)
Wn = −∆U
c. Steady Flow Work
Ws = −∆KE − ∆PE − ∆H
∆U = m(u2 − u1 )
e. Change in Enthalpy
∆H = m(h2 − h1 )
f. Heat Transferred
Q=0
g. Change in Entropy
∆S = 0
h2 = h1 = hf1 + x1 hfg1
h2 = hg + Cp ∆T (Approx. )
Ws = 0
c. Change in Internal Energy
∆U = m(u2 − u1 )
d. Change in Enthalpy
∆H = 0
e. Heat Transferred
Q=0
f. Change of Entropy
∆S = m(s2 − s1 )
6. Polytropic Process
Polytropic process is reversible process during which PVn = C, where; n is a constant.
a. PV and TS Diagram
b. Nonflow Work
2
P2 V2 − P1 V1
Wn = ∫ PdV =
1−n
1
∆U = m(u2 − u1 )
e. Change in Enthalpy
∆H = m(h2 − h1 )
f. Heat Transferred
𝑄 = ∆𝑈 + 𝑊𝑛
g. Change in Entropy
∆𝑆 = 𝑚(𝑠2 − 𝑠1 )
❖ CARNOT CYCLE
Carnot Cycle – is the most efficient thermodynamic cycle. It consists of two isothermal and two
isentropic processes.
𝑄𝐴 = 𝑇1 (𝑆1 − 𝑆2 )
b. Heat Rejected
𝑄𝑅 = 𝑇2 (𝑆2 − 𝑆3 )
𝑄𝑅 = 𝑇2 (𝑆1 − 𝑆4 )
𝑊𝑛𝑒𝑡 = 𝑄𝐴 − 𝑄𝑅
𝑊𝑛𝑒𝑡 = (𝑇1 − 𝑇2 )(𝑆1 − 𝑆4 )
d. Cycle Efficiency
𝑊𝑛𝑒𝑡 𝑄𝑅
𝑒= = 1−
𝑄𝐴 𝑄𝐴
𝑇1 − 𝑇2 𝑇2
𝑒= =1−
𝑇1 𝑇1
e. Heat-temperature relations
𝑄𝑅 𝑇2
=
𝑄𝐴 𝑇1
Note: Carnot Cycle Efficiency can be increased by increasing T 1 and lowering T2.