Thermodynamic Processes

Calculation Session 6:
Exercise 6
Kaleigh Soucy (‘23)
Donovan Cho (‘25)
Vivian Liu (‘26)
Professor Molenium
@ STP
Professor Molenium
@ 0.5 atm
Fun Fact:
You can purchase a
Professor Molenium
keychain from the
American Chemical
Society website.
Problem Breakdown!
 
Initial
 
Final
 
T
i 
= 298 K
 
P
i 
= 10 atm
 
T
f 
= 253.2 K
 
P
f 
= 2 atm
 
P
ext 
= 2 atm
Given
 
i
 
f
 
Δ
U?
 Δ
H? 
Δ
S?
 
Are 
Δ
U, 
Δ
H, and 
Δ
S 
path
functions
 or 
state functions
?
 
State Functions!
 
Path Independent
 
Does the path matter?
 
Reversible for 
Δ
S
Path Options
Lecture T4
 
Not always reversible!
Δ
U?
 
1: Isotherm
 
2: IsoV
 
2: IsoP
 
OR
 
0
 
Initial
 
Final
 
Δ
U?
1: IsoT
2: IsoV
 
Δ
H?
 
1: Isotherm
 
2: IsoV
 
2: IsoP
 
OR
 
Initial
 
Final
 
0
 
Δ
H?
1: Isotherm
2: IsoP
 
Initial
 
Final
Δ
S?
 
1: Isotherm
 
Final
 
Initial
Δ
S?
 
Δ
S
total 
= 
Δ
S
14
 
+ 
Δ
S
43 
= 
9.99 J/mol
 
1: Isotherm
 
2: IsoP
 
Initial
 
Final
 
Key Takeaways!
 
Δ
U, 
Δ
H, 
Δ
S are state functions!
There are no wrong paths – only inefficient
ones
Understand reversible vs. irreversible
processes
Δ
U = 
Δ
H = 0 for isothermal processes
(ideal gas)
Δ
H = q at constant pressure
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The concepts of internal energy, enthalpy, and entropy through a breakdown of a thermodynamic problem involving different paths and states. Gain insights into reversible and irreversible processes, state functions, and path independence. Discover the calculations and relationships between temperature, pressure, volume, and work in various thermodynamic scenarios.

  • Thermodynamics
  • Processes
  • Internal Energy
  • Enthalpy
  • Entropy

Uploaded on Mar 06, 2025 | 0 Views


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  1. Calculation Session 6: Exercise 6 Kaleigh Soucy ( 23) Donovan Cho ( 25) Vivian Liu ( 26) Professor Molenium @ STP Professor Molenium @ 0.5 atm

  2. Fun Fact: You can purchase a Professor Molenium keychain from the American Chemical Society website.

  3. Problem Breakdown! Initial Ti = 298 K Pi = 10 atm Final Tf = 253.2 K Pf = 2 atm Pext = 2 atm

  4. Given i U? H? S? f Are U, H, and S path functions or state functions? State Functions! Path Independent Does the path matter? Reversible for S

  5. Path Options Lecture T4 Isobaric, P = 0 Not always reversible! state 1 state 4 P1 Isothermal, = 0 1 = ( ) P nRT for an ideal gas: V Adiabatic (q = 0) Isochoric V = 0 state 2 P2 state 3 0 0 V1 V2

  6. U? Initial 1: Isotherm Path 1: Isothermal Isothermal paths are convenient! ? = ???? ?1 2 = 0 Path 2: Isochoric Makes sense for Cv ? = ???? ?2 3 = 3 0 Final 2: IsoP OR 2: IsoV 2??(?3 ?2)

  7. U? 1: IsoT 2: IsoV ?2 3 = 3 2??(?3 ?2) ?2 3 = 3 Utotal = ?1 2+ ?2 3 = 0 559 J = -559 J 2(1.0 mol)(8.314 J/mol K)(253.2 298 K) = -559 J

  8. H? Initial 1: Isotherm Path 1: Isothermal Isothermal paths are convenient! ? = ???? ?1 4 = 0 Path 2: Isobaric Makes sense for Cp ? = ???? ?4 3 = 5 Final 0 2: IsoP OR 2: IsoV 2??(?3 ?4)

  9. H? Initial 1: Isotherm ?4 3 = 5 2??(?3 ?2) Final 2: IsoP ?4 3 = 5 Htotal = ?1 4+ ?4 3 = 0 931 J = -931 J 2(1.0 mol)(8.314 J/mol K)(253.2 298 K) = -931 J ? = ? + ?? also works!

  10. S? Initial 1: Isotherm 1: dS = ???? ? Final U =q + w = 0 q = -w = PdV P = ??? ?? ??? ? dS = S14 = -(1.0 mol)(8.314 J/mol K) ln(2 ??? = 13.38 J/mol 10 ???) ?? ??) = -nR ln( ?? ??) S = nR ln(

  11. S? Initial 1: Isotherm 2: At constant pressure, H = q S = ?? ??) = 5 S43 = 5 ???? ? Final 2: IsoP ?? ??) S = Cp ln( 2 nR ln( 2(1.0 mol)(8.314 J/mol K) ln(253.2 ? 298 ?) = -3.39 J/mol Stotal = S14+ S43 = 9.99 J/mol

  12. Key Takeaways! U, H, S are state functions! There are no wrong paths only inefficient ones Understand reversible vs. irreversible processes U = H = 0 for isothermal processes (ideal gas) H = q at constant pressure For an ideal monatomic gas: Cv = 3 Cp = 5 2nR 2nR

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