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Lecture 314/10/06
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Thermodynamics: study of energy and transformations Energy Kinetic energy Potential Energy
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Units 1 calorie (cal) 1 calorie (cal) = 4.184 Joule (J) Calorie (Cal)
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1 st Law of Thermodynamics Law of conservation of energy Energy in the universe is conserved System vs. surroundings vs. universe Internal energy
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Specific heat capacity (C) Quantity of energy to increase the temperature of 1 gram of a substance by 1 degree C (liquid water)= 4.184 J/g·K C (ice)= 2.06 J/g·K C (steam)= 1.84 J/g·K C (aluminum)= 0.902 J/g·K Molar heat capacity Quantity of energy that must be transferred to increase the temperature of 1 mole of a substance by 1 °C
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Specific heat capacity (C) q = Cm∆T
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Heat transfer q gained + q lost = 0 q gained = - q lost 55.0 g of iron at 99.8°C is plunged into 225 g of water at 21°C. What is the final temperature? C (iron) = 0.451 J/g-K
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Example 59.8 J are required to change the temperature of 25.0 g of ethylene glycol by 1 K. What is the specific heat capacity of ethylene glycol?
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Does drinking ice water cause you to lose weight? Does drinking ice cold coke?
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Changes in state Temperature stays the same during changes of state Gas/Vapor Liquid Solid ENERGY q = mass x constant q = moles x constant
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Change of state constant??? Depends on two things: Identity of substance Which states are changing
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Solid/Liquid Heat of fusion Solid Liquid Endothermic ice Water (333 J/g or 6 KJ/mol) Heat of crystallization Liquid Solid Exothermic Water ice (- 333 J/g or - 6 KJ/mol)
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Liquid/Gas Heat of vaporization Liquid Gas Endothermic water water vapor (40.7 KJ/mol) Heat of condensation Gas Liquid Exothermic vapor Water (- 40.7 KJ/mol)
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Solid/Gas Heat of sublimation Solid Gas Endothermic Heat of deposition Gas Solid Exothermic
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What is the minimum amount of ice at 0 °C that must be added to a 340 mL of water to cool it from 20.5°C to 0°C? q water + q ice = 0 C water m water ∆T water + m ice ∆H fus = 0 (4.184 J/K-g)(340 g)(0°C - 20.5°C) + (333 J/g)m ice = 0 m ice = 87.6 g
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A rainstorm deposits 2.5 x 10 10 kg of rain. Calculate the quantity of thermal energy in joules transferred when this much rain forms. (∆H vap = - 44 KJ/mol) Exothermic or endothermic? q = 2.5 x 10 10 Kg x (10 3 g/kg) x (1 mol/18 g) x -44 KJ/mol q = -6.1 x 10 13 KJ Exothermic
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1 st Law of Thermodynamics revisited ∆E = q + w Change in Energy content heat work
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work (w) = - F x d w = - (P x A) x d w = - P∆V if ∆V = 0, then no work
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State function property of a system whose value depends on the final and initial states, but not the path driving to Mt Washington route taken vs. altitude change ∆E is a state function q and w are not
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Change in Enthalpy (∆H or q p ) equals the heat gained or lost at constant pressure ∆E = q p + w ∆E = ∆H + (-P∆V) ∆H = ∆E + P∆V
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∆E vs. ∆H Reactions that don’t involve gases 2KOH (aq) + H 2 SO 4 (aw) K 2 SO 4 (aq) + 2H 2 O (l) ∆V ≈ 0, so ∆E ≈ ∆H Reactions in which the moles of gas does not change N 2 (g) + O 2 (g) 2NO (g) ∆V = 0, so ∆E = ∆H Reactions in which the moles of gas does change 2H 2 (g) + O 2 (g) 2H 2 O (g) ∆V > 0, but often P∆V << ∆H, thus ∆E ≈ ∆H
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Enthalpy is an extensive property Magnitude is proportional to amount of reactants consumed H 2 (g) + ½ O 2 (g) H 2 O (g) ∆H = -241.8 KJ 2H 2 (g) + O 2 (g) 2H 2 O (g) ∆H = -483.6 KJ Enthalpy change for a reaction is equal in magnitude (but opposite in sign) for a reverse reaction H 2 (g) + ½ O 2 (g) H 2 O (g) ∆H = -241.8 KJ H 2 O (g) H 2 (g) + ½ O 2 (g) ∆H = 241.8 KJ Enthalpy change for a reaction depends on the state of reactants and products H 2 O (l) H 2 O (g) ∆H = 88 KJ
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Constant pressure calorimetry (cofee cup calorimetry) heat lost = heat gained Measure change in temperature of water 10 g of Cu at 188 °C is added to 150 mL of water in a cofee cup calorimeter and the temperature of water changes from 25 °C to 26 °C. Determine the specific heat capacity of copper.
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Bomb calorimetry Mainly for combustion experiments ∆V = 0 q rxn + q bomb + q water = 0 Often combine q bomb + q water into 1 calorimeter term with q cal = C cal ∆T combustion chamber
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Bomb calorimeter math K & T: q rxn + q bomb + q water = 0 q rxn + C bomb ∆T + C water m water ∆T = 0 In the lab: q rxn + q calorimeter = 0 q calorimeter = q bomb + q water q rxn + C calorimeter ∆T = 0 empirically determined same value On the exam
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Bond enthalpies
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Enthalpies of formation
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Hess’ Law
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Example A hot plate is used to heat two 50-mL beakers at the same constant rate. One beaker contains 20.0 grams of graphite (C=0.79 J/g-K) and one contains 10 grams of ethanol (2.46 J/g-K). Which has a higher temperature after 3 minutes of heating?
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Standard heat of reaction (∆H° rxn ) Same standard conditions as before: 1 atm for gas 1 M for aqueous solutions 298 K For pure substance – usually the most stable form of the substance at those conditions
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Standard heat of formation (∆H° f ) Enthalpy change for the formation of a substance from its elements at standard state Na(s) + ½ Cl 2 (g) NaCl (s) ∆H° f = -411.1 kJ Three points An element in its standard state has a ∆H° f = 0 ∆H° f = 0 for Na(s), but ∆H° f = 107.8 KJ/mol for Na(g) Most compounds have a negative ∆H° f formation reaction is not necessarily the one done in lab
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Using ∆H° f to get ∆H° rxn 2 ways to look at the problem Calculate ∆H° rxn for: C 3 H 8 (g) + 5 O 2 3 CO 2 (g) + 4 H 2 O (l) Given: 3 C(s) + 4 H 2 (g) C 3 H 8 (g) ∆H° f = -103.85 KJ/mol C(s) + O 2 (g) CO 2 (g) ∆H° f = -393.5 KJ/mol O 2 (g) + 2 H 2 (g) 2H 2 O (l) ∆H° f = -285.8 KJ/mol
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Using Hess’s Law and ∆H° f to get ∆H° rxn 1 st way: Hess’s Law C 3 H 8 (g) + 5 O 2 3 CO 2 (g) + 4 H 2 O (l) ∆H° rxn = ∆H 1 + ∆H 2 + ∆H 3 Reverse 1 st equation: C 3 H 8 (g) 3 C(s) + 4 H 2 (g) ∆H 1 = - ∆H° f = 103.85 KJ Multiply 2 nd equation by 3: 3C(s) + 3O 2 (g) 3CO 2 (g) ∆H 2 = 3x∆H° f = -1180.5 KJ Multiply 3 rd equation by 2: 2O 2 (g) + 4 H 2 (g) 4H 2 O (l) ∆H 2 = 2x∆H° f = -571.6 KJ ∆H° rxn = (103.85 KJ) + (-1180.5 KJ) + (-571.6 KJ) ∆H° rxn = -1648.25 KJ
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Using ∆H° f to get ∆H° rxn 2 nd way C 3 H 8 (g) + 5 O 2 3 CO 2 (g) + 4 H 2 O (l) ∆H° rxn = Σn ∆H° f (products) - Σn ∆H° f (reactants) ∆H° rxn = [3x(-393.5 KJ/mol) + 2x(-285.8 KJ/mol)] – [(-103.85 KJ/mol) + 0] ∆H° rxn = [-1752.1 KJ] – [-103.85 KJ] ∆H° rxn = -1648.25 KJ
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Spontaneity Some thought that ∆H could predict spontaneity Exothermic – spontaneous Endothermic – non-spontaneous Sounds great BUT some things spontaneous at ∆H > 0 Melting Dissolution Expansion of a gas into a vacuum Heat transfer Clearly enthalpy not the whole story
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Entropy (Measurement of disorder) Related to number of microstates S = klnW ∆S universe = ∆S system + ∆S surroundings 2 nd Law of Thermodynamics Entropy of the universe increases with spontaneous reactions Reversible reactions ∆S universe = ∆S system + ∆S surroundings = 0 Can be restored to the original state by exactly reversing the change Each step is at equilibrium Irreversible reaction ∆S universe = ∆S system + ∆S surroundings > 0 Original state can not be restored by reversing path spontaneous
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3 rd Law of thermodynamics S = O at O K S° - entropy gained by converting it from a perfect crystal at 0 K to standard state conditions ∆S° = ΣS°(products) - ΣS°(reactants)
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