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Work-Heat-Internal energy and First law
Typology: Lecture notes
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p
V
(p 1 , V 1 )
(p 2 , V 2 )
reversible
irrevesible
δW = F~ · d~x → W 12 =
1
~F · d~x
dz =
∂z
∂x
y
dx +
∂z
∂y
x
dy ⇒
1
dz =
C
∂z
∂x
y
dx +
∂z
∂y
x
dy
∂z
∂x
y
∂z
∂y
x
∂y
x
∂x
y
Isothermal : Wif =
f
Vi
p dV = nRT
f
Vi
dV
= nRT ln
Vf
Vi
Isobaric : Wif =
f
Vi
p dV = p
f
Vi
dV = p (Vf − Vi )
Isochoric : Wif =
Vf
Vi
p dV = 0
π
π
⇒ p = kD = k
π
and k = p 1
π
2
1
p dV = k
π
V 2
V 1
1 / 3 dV
= k
π
4 / 3
2
V 1
3 k
π
4 / 3 2
4 / 3 1
3 k
π
4 / 3 1
p 1
π
π
4 / 3 1
3 2
D^3 1
= π p 1
= 3. 436 kJ.
1
p dV =
2
V 1
patm +
k
2
dV
patmV +
k
2
2
2
V 1
= patm (V 2 − V 1 ) +
k
2
= patm (V 2 − V 1 ) ︸ ︷︷ ︸
work done on atmosphere
k
work done on spring
= 0 .125 kJ
◦
◦
δW = J
δQ
p
V
A
B
C
2
1
Cycle I :
1
δQA +
2
δQB =
1
δWA +
2
δWB
Cycle II :
2
1
δQA +
1
2
δQC =
2
1
δWA +
1
2
δWC
isochoric : CV =
δQ
dT
V
isobaric : CP =
δQ
dT
p
dU =
V
dT +
T
dV
δQ = dU + δW =
V
dT +
T
dV
δQ
dT
V
V
dV =
p
dT +
∂p
T
dp
δQ = CV dT +
T
p
dT +
∂p
T
dp
δQ
dT
p
T
p
T
p
nR
p
⇒ CP = CV + nR
H = U + pV
p=const −−−−−→ dH = dU + pdV = δQ − δW + pdV = δQ
δQ
dT
P
p
U = U(T , V ) → dU =
V
dT +
T
dV ⇒
T
U = U(T , p) → dU =
p
dT +
∂p
T
dp ⇒
∂p
T
dT =
V
dU +
U
dV =
U
dV = μJ dV
f
Vi
μJ dV