Uploaded by ASUKA WATANABE

Thermodynamics Cheat Sheet

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Thermodynamics
Zeroth Law:
• Thermal equilibrium is transitive
First Law:
• Energy is conserved, its form can
be converted
Second Law:
• Energies can flow, equilibrate
Third Law:
• “Driving Force” for equilibration
uniquely defined
• Boltzmann’s Relation: S = k ln p
Where: k = 1.3806 x 1023 J/K
Systems of Units
Newton’s Second Law: 𝐹 =
gc = 1
%+ ⋅(#
CGS: 𝑔( = 1 -./0
⋅ 12
SI: 𝑔( = 1
3%+ ⋅#
4 ⋅ 12
156%⋅78
English: 𝑔( = 1 59
:
⋅ 12
#$
%&
gc ¹ 1
% ⋅(#
CGS: 𝑔( = 980.66 %+ ⋅ 12
Weight: 𝐹
=
#%P
%&
:
3% ⋅#
SI: 𝑔( = 9.8066 3% +⋅ 12
:
59 ⋅78
English: 𝑔( = 32.174 59 +⋅ 12
At the earth’s sea level, the local
acc. due to the gravity (𝑔Q ) is:
980.66 cm/ s2
:
9.8066 m/s2
Poundal
𝑙𝑏# ⋅ 𝑓𝑑
𝑔( = 1
π‘π‘œπ‘’π‘›π‘‘π‘Žπ‘™ ⋅ 𝑠 O
32.174 ft/s2
Conversion
Temperature
1 slug = 32.174 lbm
Celsius à Fahrenheit
1 kgm = 2.205 lbm
t(°C) = S [t(°F) – 32]
1 ft = 0.3048 m = 30.48 cm
Celsius à Kelvin
1 N = 100,000 dynes
t(K) = t(°C) + 273
1 lbf = 32.174 poundal = 4.4484 N
Fahrenheit à Rankine
1 kgf = 9.8066 N
t(R) = t(°F) + 460
1 lbm = 453.592 gm
R
Density
ρ=
#
T
Mass density of water at sea level at
standard
condition
(Standard
temperature of 39.2°F or 4°C and
standard pressure of 1 atm)
62.4 lbm / ft3
Specific Volume
𝑣=
T
#
V
=W
1000 kgm / m3
1 kgm / L
Mass density of air at sea level at standard
conditions (Standard temperature of 70°F
or 21.11°C and standard pressure of 1 atm)
Conversion for Volume
0.075 lbm / ft3
1 gal = 3.78 L
1.2 kgm / m3
1 ft3 = 7.48 gal
1 m3 = 1000 L
Specific Weight
𝛾=
𝐹%
π‘šπ‘”Q πœŒπ‘”Q
𝑔Q
=
=
=
𝑉
𝑔( 𝑉
𝑔(
𝑔( 𝜐
Specific weight of water at sea level at
standard conditions (Standard
temperature of 39.2°F or 4°C and
standard pressure of 1 atm)
62.4 lbf / ft3
1000 kgf / m3
9.8066 kN / m3
0.98066 dyne / cm3
Specific weight of water at sea level at
standard conditions (Standard
temperature of 70°F or 21.11°C and
standard pressure of 1 atm)
0.075 lbm / ft3
1.2 kgm / m3
11.768 N / m3
Specific gravity of liquids
𝑠. 𝑔 =
𝜌
𝜌]
Specific gravity of gases
𝑠. 𝑔 =
𝜌
𝜌$
Specific gravities of common liquids
Water – 1.0
Mercury – 13.6
Oil – 0.8
Seawater – 1.03
Measuring pressure
Standard atmospheric pressure at sea level
Atmospheric Pressure (Barometer)
1 atm
𝑃$8#
πœŒπ‘”Q β„Ž$8#
=
𝑔(
Gage Pressure (Manometer)
πœŒπ‘”Q β„Ž%
𝑃% =
𝑔(
101.325 πΎπ‘ƒπ‘Ž$
760 mmHg
33.9 ft 𝐻O 𝑂
14.696 𝑝𝑠𝑖$
1.0332 kgf / cm2
29.92 in Hg
Vacuum
πœŒπ‘”Q β„Ž%
𝑃% = −
𝑔(
760 torrs
1.01325 bars
Internal Energy
Terms
U = f (m, T)
1 BTU: amount of heat needed to raise the
temperature of 1 lbm of water at 68°F by
1°F
𝑒=
π‘ˆ
π‘š
Conversion
1 BTU = 1.055 kJ = 778 ft-lbf
1 kCal = 4.187 kJ = 428.1 kg-m
1 calorie: amount of heat needed to raise
the temperature of 1g of water at 14.5°C
by 1°C
Thermodynamic Property
Intensive Property: independent of the
mass of the substance
Extensive Property: dependent on the
mass of the substance
Law of Conservation of Mass
E = mc2
Where c = speed of light in a vacuum
= 2.9979 x 108 m/s
Volume flow rate (𝑉̇)
𝑉̇ = A𝜐
Mass flow rate (π‘šΜ‡)
π‘šΜ‡ =
Ṫ
g
= 𝜌𝐴𝜐
Where: A = cross sectional area of the stream
𝜐 = average speed
Forms of Energy
Potential Energy (PE) à f (m, z)
Δ𝑃𝐸 =
π‘šΜ‡ V = π‘šΜ‡O
𝐴V 𝜐V 𝜌V = 𝐴O 𝜐O 𝜌O
π‘šπ‘”Q
(𝑧O − 𝑧V )
𝑔(
Kinetic Energy (KE) à f(m, 𝜐)
Law of Conservation of Energy
Δ𝐾𝐸 =
V#
O %&
(𝜐OO − 𝜐VO )
Internal Energy (U) à f(m, T)
βˆ†π‘ˆ = π‘šπ‘p (𝑇O − 𝑇V )
Flow work/ energy (Wf) à f (P, V)
βˆ†π‘Š7 = (𝑃O 𝑉O − 𝑃V 𝑉V )
Where: 𝑐p = specific heat at constant volume
Enthalpy (H)
H = U + Wf
βˆ†π» = π‘šπ‘s βˆ†π‘‡
Heat (Q)
Q = ∫ 𝑇𝑑𝑆
(for any ideal gas or vapor as working substance)
Q = mcβˆ†T
(for any ideal gas as working substance)
Where: c = specific heat of gas (depending upon
the process involved during the change of state)
βˆ†T = change in absolute temperature
𝑄̇ is constant during a process:
Q = π‘„Μ‡βˆ†t
Where: βˆ†t = process time interval
= t2 – t1
𝑄̇ is not constant during a process:
82
𝑄 = w 𝑄̇𝑑𝑑
8x
Mechanical Work (W)
W = 𝐹𝑑
Mechanical Power (π‘ŠΜ‡ )
y zP = 8 = 8 = F𝜐
Non-flow work (Wn)
Thermodynamic properties vs. energy
transfer mechanisms
Example of point function: change in volume
O
w 𝑑𝑉 = 𝑉O − 𝑉V = βˆ†π‘‰
O
Wn = ∫V 𝑝𝑑𝑉
V
Example of path function: work
π›Ώπ‘Š = π‘ŠV|O ≠ βˆ†π‘Š
Steady Flow Energy Equation
Ein = Eout
PE1 + KE1 + U1 + P1V1 + Q = PE2 + KE2 + U2 + P2V2 + Ws
Notes:
Heat(Q)
• (+) if heat is added to the system
by the surroundings
• (–) if heat is rejected by the
system to the surroundings
Steady flow work (WS)
• (+) if work is done by the system
o Turbine
• (–) if work is done to the system
o Compressor
o Pump
Non-Flow Energy Equation
Q = βˆ†π‘ˆ + π‘Š/
Notes:
Heat(Q)
• (+) if heat is added to the system
by the surroundings
• (–) if heat is rejected by the system
to the surrounding
Non flow work (Wn)
• (+) if work is done by the system
• (–) if work is done to the system
Power Conversion
1 hp equals
33000 ft-lbf /min
550 ft-lbf /sec
42.4 BTU/min
2544 BTU/hr
0.746 kW
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