Download presentation
Presentation is loading. Please wait.
Published byMervin Bell Modified over 6 years ago
1
THERMODYNAMICS. Elements of Physical Chemistry. By P. Atkins
Concerned with the study of transformation of energy: Heat work
2
CONSERVATION OF ENERGY – states that:
Energy can neither be created nor destroyed in chemical reactions. It can only be converted from one form to the other. UNIVERSE System – part of world have special interest in… Surroundings – where we make our observations
3
↔ matter ↔ energy ↔ energy not matter matter × Energy ×
Example: ↔ matter ↔ energy ↔ energy not matter matter × Energy × → → Open system Closed system Isolated system
4
If system is themally isolated called Adiabatic system eg: water in vacuum flask.
5
HCl(aq) + NaOH(aq) → NaCl(aq) + H2O(l) - heat given off.
WORK and HEAT Work – transfer of energy to change height of the weight in surrounding eg: work to run a piston by a gas. Heat – transfer of energy is a result of temperature difference between system and surrounding eg: HCl(aq) + NaOH(aq) → NaCl(aq) + H2O(l) - heat given off. If heat released to surroundings – exothermic. If heat absorbed by surroundings – endothermic.
6
Example: Gasoline, 2, 2, 4 trimethylpentane
CH3C(CH3)2CH2CH(CH3)CH3 + 25/2 O2 → 8CO2(g) +H2O(l) 5401 kJ of heat is released (exothermic) Where does heat come from? From internal energy, U of gasoline. Can represent chemical reaction: Uinitial = Ufinal + energy that leaves system (exothermic) Or Ui = Uf – energy that enters system (endothermic)
7
Hence, FIRST LAW of THERMODYNAMICS (applied to a closed system)
The change in internal energy of a closed system is the energy that enters or leaves the system through boundaries as heat or work. i.e. ∆U = q +w ∆U = Uf – Ui q – heat applied to system W – work done on system When energy leaves the system, ∆U = -ve i.e. decrease internal energy When energy enter the system, ∆U = +ve i.e. added to internal energy
8
Different types of energies:
Kinetic energy = ½ mv2 (chemical reaction) kinetic energy (KE) k T (thermal energy) where k = Boltzmann constant Potential energy (PE) = mgh – energy stored in bonds Now, U = KE + PE
9
w = force × distance moved in direction of force
3. Work (W) w = force × distance moved in direction of force i.e. w = mg × h = kg × m s-2 × m = kg m2 s-2 (m) (g) (h) 1 kg m2 s-2 = 1 Joule - Consider work – work against an opposing force, eg: external pressure, pex. Consider a piston
10
Piston
11
w = distance × opposing force w = h × (pex × A) = pex × hA
Work done on system = pex × ∆V ∆V – change in volume (Vf – Vi) Work done by system = -pex × ∆V Since U is decreased
12
Example: C3H8(g) + 5 O2(g) → 3CO2(g) + 4H2O(l) at 298 K 1 atm (1 atm = Pa), kJ = q What is the work done by the system? For an ideal gas; pV = nRT (p = pex) n – no. of moles R – gas constant T = temperature V – volume p = pressure
13
V= nRT/p or Vi = niRT/pex
6 moles of gas: Vi = (6 × × 298)/ = m3 3 moles of gas: Vf = (3 × × 298)/ = m3 work done = -pex × (Vf – Vi) = ( – ) = J
14
NB: work done = - pex (nfRT/pex – niRT/pex)
= (nf – ni) RT Work done = -∆ngasRT i.e. work done = - (3 – 6) × × 298 = J Can also calculate ∆U ∆U = q +w q = kJ w = J = 7.43 kJ ∆U = = kJ
15
NB: qp ∆U why? Only equal if no work is done i.e. ∆V = 0
i.e. qv = ∆U
16
Example: energy diagram
17
Since work done by system = pex∆V
System at equilibrium when pex = pint (mechanical equilibrium) Change either pressure to get reversible work i.e. pex > pint or pint > pex at constant temperature by an infinitesimal change in either parameter
18
For an infinitesimal change in volume, dV Work done on system = pdV
For ideal gas, pV = nRT p = nRT/ V work = p dV = nRT dV/ V = nRT ln (Vf/Vi) because dx/x = ln x Work done by system= -nRT ln(Vf/Vi)
19
Enthalpy, H Most reactions take place in an open vessel at constant pressure, pex. Volume can change during the reaction i.e. V 0 (expansion work). Definition: H = qp i.e. heat supplied to the system at constant pressure.
20
Properties of enthalpy
Enthalpy is the sum of internal energy and the product of pV of that substance. i.e H = U + pV (p = pex) Some properties of H
21
Hf – Hi = Uf – Ui +p(Vf – Vi)
Hi = Ui + pVi Hf = Uf + pVf Hf – Hi = Uf – Ui +p(Vf – Vi) or H = U + p V
22
Since work done = - pex V
H = (- pex V + q) +p V (pex= p) H = ( -p V + q) + p V = q H = qp
23
suppose p and V are not constant?
H = U + ( pV) expands to: H = U + pi V + Vi P + (P) (V) i.e. H under all conditions. When p = 0 get back H = U + pi V U + p V When V = 0: H = U + Vi p
24
Enthalpy is a state function.
25
NB: work and heat depend on the path taken and are written as lower case w and q. Hence, w and q are path functions. The state functions are written with upper case. eg: U, H, T and p (IUPAC convention).
26
Standard States By IUPAC conventions as the pure form of the substance at 1 bar pressure (1 bar = 100,000 Pa). What about temperature? By convention define temperature as 298 K but could be at any temperature.
27
Example: C3H8(g) + 5 O2(g) → 3CO2(g) + 4H2O(l)
at 1 bar pressure, qp = kJmol-1. Since substances are in the pure form then can write H = kJ mol-1 at 298 K represents the standard state.
28
H2(g) → H(g) + H(g), H diss = +436kJmol-1
H2O(l) → H2O(g), H vap = kJmol-1 Calculate U for the following reaction: CH4(l) + 2 O2(g) → CO2(g) + 2H2O(l), H = kJmol-1
29
H = U + (pV) = U + pi V + Vi p + p V NB: p = 1 bar, i.e. p = 0 H = U + pi V Since -pi V = - nRT, U = H - nRT
30
calculation U = – ((1 – 2)(8.314) 298)/ 1000 = – (-1)(8.314)(0.298) = kJ mol-1
31
STANDARD ENTHALPY OF FORMATION, Hf
Defined as standard enthalpy of reaction when substance is formed from its elements in their reference state. Reference state is the most stable form of element at 1 bar atmosphere at a given temperature eg. At 298 K Carbon = Cgraphite Hydrogen = H2(g) Mercury = Hg(l) Oxygen = O2(g) Nitrogen = N2(g)
32
NB: Hf of element = 0 in reference state
Can apply these to thermochemical calculations eg. Can compare thermodynamic stability of substances in their standard state. From tables of Hf can calculate H f rxn for any reaction.
33
Eg. C3H8 (g) + 5O2(g) → 3CO2(g) + 4H2O(l)
Calculate Hrxn given that: Hf of C3H8(g) = kJ mol-1 Hf of O2(g) = 0 (reference state) Hf of CO2(g) = kJ mol-1 Hf of H2O(l) = kJ mol-1 Hrxn = n H (products)- n H(reactants)
34
Hf(products) = 3 (- 393.5) + 4 (- 285.8)
= = kJ mol-1 Hf(reactants) = 0 = kJ mol-1 Hrxn = – ( ) = kJ mol = kJ mol-1
35
Answer same as before. Eq. is valid.
Suppose: solid → gas (sublimation) Process is: solid → liquid → gas Hsub = Hmelt + Hvap Ie. H ( indirect route) = . H ( direct route)
36
Hess’ Law - the standard enthalpy of a reaction is the sum of the standard enthalpies of the reaction into which the overall reaction may be divided. Eg. C (g) + ½ O2(g) → CO (g) , Hcomb =? at 298K
37
From thermochemical data:
C (g) +O2 (g) → CO 2(g) Hcomb = kJmol-1…………………………….(1) CO (g) +1/2 O2 (g) →CO 2(g), Hcomb = kJ mol-1…………………… (2) Subtract 2 from 1 to give: C (g) + O2 (g) – CO (g) – 1/2 O2 (g) → CO2 (g) – CO2 (g) C (g) + ½ O 2 (g) → CO (g) , Hcomb= – (-283.0) = kJ mol-1
38
Bond Energies eg. C-H bond enthalpy in CH4 CH4 (g) → C (g) + 4 H (g) , at 298K. Need: Hf of CH 4 (g) =- 75 kJ mol-1 Hf of H (g) = 218 kJ mol-1 Hf of C (g) = 713 kJ mol-1
39
Hdiss = nHf (products) - nHf ( reactants)
= ( 4x 218) – (- 75) = 1660 kJ mol-1 Since have 4 bonds : C-H = 1660/4 = 415 kJ mol-1
40
Variation of H with temperature
Suppose do reaction at 400 K, need to know Hf at 298 K for comparison with literature value. How? As temp.î HmÎ ie. Hm T Hm = Cp,m T where Cp,m is the molar heat capacity at constant pressure.
41
Cp,m = Hm/ T = J mol-1/ K = J K-1 mol-1
HT2 = HT1 + Cp ( T2 - T1) Kirchoff’s equation. and Cp = n Cp(products)- nCp(reactants) For a wide temperature range: Cp ∫ dT between T1 and T2. Hence : qp = Cp( T2- T1) or H = Cp T and.
42
qv = Cv ( T2 – T1) or Cv T = U ie. Cp = H / T ; Cv =U /T For small changes: Cp = dH / dT ; Cv = du / dT For an ideal gas: H = U + p V For I mol: dH/dT = dU/dT + R Cp = Cv + R Cp / Cv = γ ( Greek gamma)
43
Work done along isothermal paths
Reversible and Irreversible paths ie T =0 ( isothermal) pV = nRT= constant Boyle’s Law : piVi =pf Vf Can be shown on plot:
44
pV diagram Pivi pV= nRT = constant Pfvf
45
Work done = -( nRT)∫ dV/V
= - nRT ln (Vf/Vi) Equation is valid only if : piVi=pfVf and therefore: Vf/Vi = pi/pf and Work done = -( nRT) ln (pi/pf) and follows the path shown.
46
pV diagram An irreversible path can be followed: Look at pV diagram again.
47
An Ideal or Perfect Gas NB For an ideal gas, u = 0
Because: U KE + PE k T + PE (stored in bonds) Ideal gas has no interaction between molecules (no bonds broken or formed)
48
Therefore u = 0 at T = 0 Also H = 0 since (pV) = 0 ie no work done This applies only for an ideal gas and NOT a chemical reaction.
49
Calculation eg. A system consisting of 1mole of perfect gas at 2 atm and 298 K is made to expand isothermally by suddenly reducing the pressure to 1 atm. Calculate the work done and the heat that flows in or out of the system.
50
w = -pex V = pex(Vf -Vi) Vi = nRT/pi = 1 x x (298)/202650 = x 10-2 m3 Vf = 1 x x 298/ = x 10-2 m3 therefore, w = -pex (Vf- Vi) = ( ) x 10-2 = J U = q + w; for a perfect gas U = 0 therefore q = -w and q = -(-1239) = J
51
Work done along adiabatic path
ie q = 0 , no heat enters or leaves the system. Since U = q + w and q =0 U = w When a gas expands adiabatically, it cools. Can show that: pVγ = constant, where ( Cp/Cv =γ ) and: piViγ = pfVfγ and since: -p dV = Cv dT
52
Work done for adiabatic path = Cv (Tf- Ti)
For n mol of gas: w = n Cv (Tf –Ti) Since piViγ = pfVf γ piViγ/Ti = pfVf γ/ Tf Tf = Ti(Vi/Vf)γ-1 w =n Cv{ ( Ti( Vi/ Vf)γ-1 – Ti} An adiabatic pathway is much steeper than pV = constant pathway.
53
Summary piVi = pfVf for both reversible and irreversible Isothermal processes. For ideal gas: For T =0, U = 0, and H=0 For reversible adiabatic ideal gas processes: q=0 , pVγ = constant and Work done = n Cv{ ( Ti( Vi/ Vf)γ-1 – Ti} piViγ = pfVfγ for both reversible and irreversible adiabatic ideal gas.
54
2nd Law of Thermodynamics
Introduce entropy, S (state function) to explain spontaneous change ie have a natural tendency to occur- the apparent driving force of spontaneous change is the tendency of energy and matter to become disordered. That is, S increases on disordering. 2nd law – the entropy of the universe tends to increase.
55
Entropy S = qrev /T ( J K-1) at equilibrium
Sisolated system > 0 spontaneous change Sisolated system < 0 non-spontaneous change Sisolated system = 0 equilibrium
56
Properties of S If a perfect gas expands isothermally from
Vi to Vf then since U = q + w = 0 q = -w ie qrev = -wrev and wrev = - nRT ln ( Vf/Vi) At eqlb., S =qrev/T = - qrev/T = nRln (Vf/Vi) ie S = n R ln (Vf/Vi) Implies that S ≠ 0 ( strange!) Must consider the surroundings.
57
Surroundings Stotal = Ssystem + Ssurroundings
At constant temperature surroundings give heat to the system to maintain temperature. surroundings is equal in magnitude to heat gained or loss but of opposite sign to make S = 0 as required at eqlb.
58
Rem: dq = Cv dT and dS = dqrev / T dS = Cv dT/ T and S = Cv ∫ dT /T between Ti and Tf S = Cv ln ( Tf/ Ti ) When Tf/ Ti > 1 , S is +ve eg. L → G , S is +ve S → L , S is +ve and since qp = H Smelt = Hmelt / Tmelt and Svap = Hvap / Tvap
59
Third Law of Thermodynamics
eg. Standard molar entropy, SmThe entropy of a perfectly crystalline substance is zero at T = 0 Sm/ J K-1 at 298 K ice water NB. Increasing disorder water vapour 189 For Chemical Reactions: Srxn = n S (products) - n S ( reactants) eg. 2H2 (g) O2( g) → 2H2O( l ), H = kJ mol-1
60
Calculation Ie surroundings take up + 572kJ mol-1 of heat Srxn = 2S(H2Ol) - (2 S (H2g ) + S (O2g) ) = JK-1 mol-1 ( strange!! for a spontaneous reaction; for this S is + ve. ). Why? Must consider S of the surroundings also. S total = S system + S surroundings S surroundings = + 572kJ mol-1/ 298K = x 103JK-1 mol-1 S total =( JK-1mol-1) x 103 = 1.59 x 103 JK-1 mol-1 Hence for a spontaneous change, S > 0
61
Free Energy, G Is a state function. Energy to do useful work.
Properties Since Stotal = Ssystem + Ssurroundings Stotal = S - H/T at const. T&p Multiply by -T and rearrange to give: -TStotal = - T S + H and since G = - T Stotal ie. G = H - T S Hence for a spontaneous change: since S is + ve, G = -ve.
62
Free energy ie. S > 0, G < 0 for spontaneous change ;
at equilibrium, G = 0. Can show that : (dG)T,p = dwrev ( maximum work) G = w (maximum)
63
Properties of G G = H - T S dG = dH – TdS – SdT H = U + pV
dH = dU + pdV + Vdp Hence: dG = dU + pdV + Vdp – TdS – SdT dG = - dw + dq + pdV + Vdp – TdS – SdT dG = Vdp - SdT
64
For chemical Reactions:
G = n G (products) - n G (reactants) and Grxn = Hrxn - T Srxn
65
Relation between Grxn and position of equilibrium
Consider the reaction: A = B Grxn = GB - GA If GA> GB , Grxn is – ve ( spontaneous rxn) At equilibrium, Grxn = 0. ie. Not all A is converted into B; stops at equilibrium point.
66
Equilibrium diagram
67
For non-spontaneous rxn. GB > GA, G is + ve
68
Gas phase reactions Consider the reaction in the gas phase:
N2(g) + 3H2(g)→ 2NH3(g) Q =( pNH3 / p)2 /( ( pN2/ p) (pH2/ p)3 ) where : Q = rxn quotient ; p = partial pressure and p = standard pressure = 1 bar Q is dimensionless because units of partial pressure cancelled by p . At equilibrium: Qeqlb = K = (( pNH3 / p)2 / ( pN2/ p) (pH2/ p)3 )eqlb
69
Activity ( effective concentration)
Define: aJ = pJ / p where a = activity or effective concentration. For a perfect gas: aJ = pJ / p For pure liquids and solids , aJ = 1 For solutions at low concentration: aJ = J mol dm-3 K = a2NH3 / aN2 a3H2 Generally for a reaction: aA + bB → cC + dD K = Qeqlb = ( acC adD / aaA abB ) eqlb = Equilibrium constant
70
Relation of G with K Can show that: Grxn = Grxn + RT ln K
At eqlb., Grxn = 0 Grxn = - RT ln K Hence can find K for any reaction from thermodynamic data.
71
Can also show that: ln K = - G / RT K = e - G / RT eg H2 (g) + I2 (s) = 2HI (g) , Hf HI = kJ mol-1 at 298K; Hf H2 =0 ; Hf I 29(s)= 0
72
calculation Grxn = 2 x 1.7 = + 3.40 kJ mol-1
ln K = x 103 J mol-1 / J K-1 mol-1 x 298K = ie. K = e – = 0.25 ie. p2 HI / pH2 p = ( rem. p = 1 bar; p 2 / p = p ) p2 HI = pH2 x 0.25 bar
73
Example: relation between Kp and K
Consider the reaction: N2 (g) + 3H2 (g) = 2NH3 (g) Kp =( pNH3 / p)2 / ( pN2/ p )( pH2 / p)3 and K = [( pNH3 / p)2 / ( pN2/ p )( pH2 / p)3] eqlb Kp = K (p)2 in this case. ( Rem: (p)2 / (p)4 = p -2
74
For K >> 1 ie products predominate at eqlb. ~ 103
K<< 1 ie reactants predominate at eqlb. ~ 10-3 K ~ 1 ie products and reactants in similar amounts.
75
Effect of temperature on K
Since Grxn = - RT ln K = Hrxn - TSrxn ln K = - Grxn / RT = - Hrxn/RT + Srxn/R ln K1 = - Grxn / RT1 = - Hrxn/RT1 + Srxn/R ln K2 = - Grxn / RT2 = - Hrxn/ RT2 + Srxn/ R ln K1 – ln K2 = - Hrxn / R ( 1/ T1 - 1/ T2 ) 0r ln ( K1/ K2) = - Hrxn / R ( 1/ T1 - 1/ T2 ) van’t Hoff equation
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.