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Chapter 14 Heat, Work, Energy, Enthalpy

Chapter 14 Heat, Work, Energy, Enthalpy. 1 The Nature of Energy 2 Enthalpy 3 Thermodynamics of Ideal Gases 4 Calorimetry 5 Hess's Law 6 Standard Enthalpies of Formation 7 Present Sources of Energy (skip) 8 New Energy Sources (skip). James Prescott Joule (1818-1889). Highlights

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Chapter 14 Heat, Work, Energy, Enthalpy

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  1. Chapter 14Heat, Work, Energy, Enthalpy 1 The Nature of Energy 2 Enthalpy 3 Thermodynamics of Ideal Gases 4 Calorimetry 5 Hess's Law 6 Standard Enthalpies of Formation 7 Present Sources of Energy (skip) 8 New Energy Sources (skip)

  2. James Prescott Joule(1818-1889) Highlights • English physicist and !!brewer!! • Studied the nature of heat, and discovered its relationship to mechanical work • Challenged the "caloric theory”l that heat cannot be created nor destroyed. • Led to the theory of conservation of energy, which led to the development of the first law of thermodynamics • Worked with Lord Kelvin to develop the absolute scale of temperature • Pupil of John Dalton (Atomic Theory) • Joule effect: found the relationship between the flow of current through a resistance and the heat dissipated, now called Joule's law Moments in a Life (Death) • Gravestone is inscribed with the number “772.55” the amount of work, in ft lb, he determined experimentally to be required to raise the temperature of 1 lb of water by 1° Fahrenheit. “772.55”

  3. Thermite Reaction Reactants → Products 2 Al (s) + Fe2O3 (s) → Al2O3 (s) + 2Fe (s)

  4. Energy • Definition of Energy: Capacity to do work. • The study of energy and its interconversions is called Thermodynamics. • 1St Law of Thermodynamics: Conservation of energy. • Energy can be converted from one form to another but cannot be created of destroyed. • The energy of the universe is constant. • The energy of a closed system is constant. • Heat and work are interconvertable

  5. Forms of Energy • Chemical Energy • Potential energy (e.g., ΔEpotential= mgΔh) • Kinetic energy (e.g., ΔEKinetic=Δ(1/2mv2) • Electrical Energy • Nuclear Energy • Energy transfer • Through heat • Through work

  6. Energy • Energy is a state property, which means it depends on the initial and final state, not the path between them. ΔE = Efinal – Einitial ΔE = Eproducts – Ereactants

  7. What is a “State Property”?

  8. Thermodynamics: Systems and Surroundings A thermodynamic system is the part of the universe that is under consideration. A boundary separates the system from the rest of the universe, which is called the surroundings. A system can be anything that you wish it to be, for example a piston, and engine, a brick, a solution in a test tube, a cell, an electrical circuit, a planet, etc.

  9. Heat (q) and Work (w) ΔE = q + w • q = Heat absorbed by the system • If q > 0 , heat is absorbed • If q < 0 , heat is given off • w = Work done on the system • Increase the energy of a system by heating it (q>0) or by doing work on it (w>0). Work • w = Force x distance = (Pressure x area) x distance = pressure x ΔV = PΔV Work is Pressure-Volume work (P-V)

  10. Exothermic reactions release energy to surroundings (by heating the surroundings) CH4 (g) + 2O2 (g) → CO2 (g) +2 H2O (g) + heat In an exothermic process, the energy stored in chemical bonds/molecular interactions is converted to thermal energy (random kinetic energy).

  11. Endothermic reactions absorb energy N2 (g)+ O2 (g) + Energy (heat)→ 2 NO (g) An endothermic reaction consumes heat and stores energy in the chemical bonds/molecular interactions of the products.

  12. Work w = F x Δh P=F/A P x A x Δh ΔV = A Δh W=P ΔV

  13. Force exerted by heating = P1A • Where P1 is the pressure inside the vessel • Where A is the Area of the piston • Pext = P1 if balanced • w = F x d = F x Δh = P x A x Δh • ΔV = A Δh • w = −PextΔV • Units are atm·L or L atm • Where 1 L atm = 101.3 Joules

  14. Expansion (w<0) • The system does work on the surroundings. • Compression (w>0) • The surroundings do work on the system.

  15. Energy • Energy is the capacity to do work. • Energy is a state property, which means it depends on the initial and final state, not the path between them. ΔE = Efinal – Einitial ΔErxn = Eproducts – Ereactants

  16. Enthalpy • Heat is a means by which energy is transferred. • For processes carried out at constant pressure, the heat absorbed equals a change in Enthalpy, ΔH. qp= ΔH Enthalpy Change (p denotes constant pressure) • Enthalpy is a state property, which means it depends on its initial and final state, not the path between them. ΔH = Hfinal – Hinitial ΔHrxn = Hproducts – Hreactants

  17. Enthalpy • ΔE=q+w = ΔH + w (at constant P) • If a chemical reaction occurs in solution with no PV work (no change in V), then w=0 and ΔE = ΔH. • ΔH for a reaction may be either positive (absorbs heat from surroundings) or negative (disperses heat to the surroundings). • For a gas phase reaction, where ΔV is allowed, then ΔE ≠ΔH.

  18. GAS Condensation Sublimation Deposition Evaporation Melting/Fusion SOLID LIQUID Freezing Phase Changes Phase changes (are not chemical reactions) but involve enthalpy changes Melt ice: H2O(s) → H2O(l) ΔHfusion= + 6 kJ at 0C ΔHfusion is positive means endothermic (add heat) if reversed H2O(l) → H2O(s) ΔHfreeze= – 6 kJ ΔHfreeze= –ΔHfusion ΔHvaporization = – ΔHcondensation ΔHsublimation = – ΔHdeposition

  19. Thermodynamics of Ideal Gases(volume changes) (KE)avg is the average translational energy of 1 mole of a perfect gas. The energy (“heat”) required to change the translational energy of 1 mole of an ideal gas by ΔT is

  20. Heat Capacity (C) • How much heat is required to raise the temp of one mole of something by 1 degree? C is a proportionality constant linking T and q. CΔT=q If no work is allowed (ΔV = 0) CvΔT=q If work is allowed (ΔP=0) CpΔT=q Cp>Cv

  21. Heating an Ideal Gas Molar Heat Capacity (C) of a substance is defined as the heat (q) required to raise the temperature of 1 mole of a substance by 1K. • Molar Heat Capacity: Cv = 3/2 R (constant volume) (for a perfect monatomic gas) • Molar Heat Capacity: Cp = 5/2 R (constant pressure) (for a perfect monatomic gas) • polyatomic molecules have larger Cv‘s & Cp’s due to vibrational and rotational degrees of freedom.

  22. Thermodynamic Properties of an Ideal Gas ΔE = q + w = ΔH + w (const P) ΔH = ΔE + (PΔV) = qp ΔH = ΔE + PΔV = ΔE + nRΔT = qp

  23. Example Consider 2.00 mol of a monoatomic ideal gas that is take from state A (PA = 2.00 atm, VA = 10.0 L) to state B (PB = 1.00 atm, VB = 30.0 L) Calculateq, w, ΔE, and ΔH Know: PV=nRT, and Cp, Cv, for monatomic gas. Conversion: L-atm to Joules = 1 L atm = 101.3 Joules

  24. Two pathways from A to BI) Step 1. A to C (constant P) Step 2. C to B (constant V)II) Step 3. A to D (constant P) Step 4. D to B (constant V) State A V=10 L P=2 atm State B V=30 L P=1 atm

  25. State A State B Vi = 10L Vf = 30L Pi = 2 atm Pf = 1atm Calculate q, w, ΔE, ΔH q q1, q4: Steps 1 and 4 are constant pressure, use Cp q2, q3: Steps 2 and 3 are constant volume, use Cv

  26. State A State B Vi = 10L Vf = 30L Pi = 2 atm Pf = 1atm Calculate q, w, ΔE, ΔH w q2, q3: Step 1 and 4 are constant volume, w2=w3=0 w1= -2(20) = -40 l-atm w2 = 0 (ΔV = 0) w3 = 0 (ΔV = 0) w4= -1(20) = -20 l-atm

  27. State A State B Vi = 10L Vf = 30L Pi = 2 atm Pf = 1atm Calculate q, w, ΔE, ΔH ΔE Use ΔE1 = q1+w1 ΔE2 = q2+w2 ΔE3 = q3+w3 ΔE4 = q4+w4 ΔEAB Use ΔEAB = ΔE1 + ΔE2 or ΔEAB = ΔE3 + ΔE4

  28. Heat Capacity • Heat Capacity, Cp, is the amount of heat required to raise the temperature of a substance by one degree at constant pressure. • Cp is always a positive number • q and ΔT can be both negative or positive • If q is negative, then heat is evolved or given off and the temperature decreases • If q is positive, then heat is absorbed and the temperature increases

  29. Heat Capacity (continued) • Cp units are energy per temp. change • Cpunits are Joule/oK or JK-1 • Molar heat capacity • Units are J/K/mole or JK-1mol-1

  30. Specific Heat Capacity • The word Specific before the name of a physical quantity very often means divided by the mass • Specific Heat Capacity is the amount of heat required to raise the temperature of one gram of material by one degree Kelvin (at constant pressure)

  31. Standard State Enthalpies • Designated using a superscript ° (pronounced naught) • Is written as ΔH° • OFB text appendix D lists standard enthalpies of formation of one mole of a variety of chemical species at 1 atm and 25°C. • Standard State conditions • All concentrations are 1M or 1 mol/L • All partial pressures are 1 atm

  32. Standard Enthalpies of Formation ΔH°rx is the sum of products minus the sum of the reactants For a general reaction a A + b B → c C + d D

  33. Enthalpy of Reaction: ΔHrxn CO (g) + ½ O2 (g) → CO2 (g)

  34. CO (g) + ½ O2 (g) → CO2 (g) ΔH°rxn= – 283kJ/mol An exothermic reaction If stoichiometric coefficients are doubled (x2), then double ΔH° 2CO (g) + 1 O2 (g) → 2 CO2 (g) ΔH°rxn= (2)(-283kJ/mol) If the reaction direction is reversed CO2 (g) → CO (g) + ½ O2 (g) Change the sign of ΔH°rxn

  35. How much heat heat at constant pressure is needed to decompose 9.74g of HBr (g) (mwt =80.9 g/mol) into its elements? H2 + Br2→ 2HBr (g) ΔH°rxn = -72.8 kJmol-1 Strategy: • Decomposition is actually the reverse reaction • ΔH to decompose 2 moles of HBr is +72.8kJ/mol

  36. Hess’s Law • Sometimes its difficult or even impossible to conduct some experiments in the lab. • Because Enthalpy (H) is a State Property, it doesn’t matter what path is taken as long as the initial reactants lead to the final product. • Hess’s Law is about adding or subtracting equations and enthalpies. • Hess’s Law:If two or more chemical equations are added to give a new equation, then adding the enthalpies of the reactions that they represent gives the enthalpy of the new reaction.

  37. Principle of Hess's law N2 (g) + O2 (g) → 2 NO ΔH2 = +180 kJ 2 NO (g) + O2 (g) → 2 NO2ΔH3 = –112 kJ N2 (g) + 2 O2 (g) → 2 NO2ΔH1 = +68kJ

  38. Suppose hydrazine and oxygen react to give dinitrogen pentaoxide and water vapor: 2 N2H4(l) + 7 O2(g)→ 2 N2O5(s) + 4 H2O (g) Calculate the ΔH of this reaction, given that the reaction: N2 (g) + 5/2 O2(g) →N2O5(s) has a ΔH of -43 kJ.

  39. 2 N2H4 (l) + 7 O2 (g) → 2 N2O5 (s) + 4 H2O (g) ΔHr° = 2 x ΔHf°N2O5(s) + 4 x ΔHf°H2O (g) – 2 x ΔHf° N2H4(l)– 7 x ΔHf°O2(g) What values to use? ΔHf°N2O5 (s) given ΔH° = ─ 43 kJmol-1 ΔHf°H2O (g) look up in App. 4 ΔHf° N2H4 (l) look up in App. 4 ΔHf°O2 (g) look up in App. 4 = ΔHr° =

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