Thermochemistry Thermochemistry is concerned with the heat changes

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Thermochemistry

Thermochemistry

Thermochemistry is concerned with the heat changes that occur during chemical reactions. Can deal

Thermochemistry is concerned with the heat changes that occur during chemical reactions. Can deal with gaining or losing heat

Energy The capacity for doing work or supplying heat. - Energy is only detected

Energy The capacity for doing work or supplying heat. - Energy is only detected because of its effects Energy stored within the structural units of chemical substances is called Chemical Potential Energy (Gasoline)

Heat (q) Energy that transfers from one object to another because of a temperature

Heat (q) Energy that transfers from one object to another because of a temperature difference between them Heat is not detectable, only changes caused by heat Heat always flows from a warmer object to a cooler object

Universe The system and its surroundings make up the universe System – part of

Universe The system and its surroundings make up the universe System – part of the universe you focus on Surroundings – everything else in the universe

Endothermic A process that absorbs heat from the surroundings Heat flowing into a system

Endothermic A process that absorbs heat from the surroundings Heat flowing into a system from its surroundings is defined as positive q heat

syste m

syste m

Exothermic A process that releases heat to its surroundings Heat flowing out of the

Exothermic A process that releases heat to its surroundings Heat flowing out of the system to its surroundings is defined as negative q heat

system

system

Calorie vs. Joule Calorie – the quantity of heat needed to raise the temperature

Calorie vs. Joule Calorie – the quantity of heat needed to raise the temperature of 1 g of water 1 o. C 1 Calorie = 1 kilocalorie = 1000 calories Joule – the quantity of heat needed to raise the temperature of 1 g of water 0. 2390 o. C 1 J = 0. 2390 cal 4. 184 J = 1 cal

Heat Capacity The amount of heat needed to increase the temperature of an object

Heat Capacity The amount of heat needed to increase the temperature of an object exactly 1 o. C The greater the mass of the object, the greater its heat capacity. Which has more heat capacity, a drop of water, or an entire pool?

Specific Heat The amount of heat it takes to raise the temperature of 1

Specific Heat The amount of heat it takes to raise the temperature of 1 g of the substance 1 o. C The higher the specific heat, the longer it takes to heat up. C= q m x ΔT = heat mass (g) x change in temp

Calorimetry The accurate and precise measurement of heat change for chemical and physical processes.

Calorimetry The accurate and precise measurement of heat change for chemical and physical processes. The heat released by the system is equal to the heat absorbed by its surroundings

Calorimeters

Calorimeters

Enthalpy (H) For systems at constant pressure, the heat content is the same as

Enthalpy (H) For systems at constant pressure, the heat content is the same as a property called enthalpy of the system If a reaction occurs at constant pressure, enthalpy can be used interchangeably with heat. q = ΔH ΔH = m x C x ΔT

Thermochemical Equation An equation that includes the heat of change Ca. O(s) + H

Thermochemical Equation An equation that includes the heat of change Ca. O(s) + H 2 O(l) Ca(OH)2(s) + 65. 2 k. J

Heat of Reaction The heat change for the equation exactly as written. Heats of

Heat of Reaction The heat change for the equation exactly as written. Heats of reaction at constant pressure (1 atm @ 25 o C) reported as ΔH

Cont. Exothermic Endothermic Ca. O(s) + H 2 O(l) Na 2 CO 3(s) +

Cont. Exothermic Endothermic Ca. O(s) + H 2 O(l) Na 2 CO 3(s) + H 2 O(g) + CO 2(g) ΔH = -65. 2 k. J Ca(OH)2(s) ΔH + 129 k. J 2 Na. HCO 3(s)

Exothermic Ca. Cl 2(s) H 2 O(l) Ca 2+(aq) + 2 Cl-(aq) ΔHsoln =

Exothermic Ca. Cl 2(s) H 2 O(l) Ca 2+(aq) + 2 Cl-(aq) ΔHsoln = -82. 8 k. J/mol

Endothermic NH 4 NO 3(s) H 2 O(l) NH 4+(aq) + NO 3 -(aq)

Endothermic NH 4 NO 3(s) H 2 O(l) NH 4+(aq) + NO 3 -(aq) ΔHsoln = 25. 7 k. J/mol

Heat of Combustion The heat of reaction for the complete burning of one mole

Heat of Combustion The heat of reaction for the complete burning of one mole of a substance. CH 4(g) + 2 O 2(g) CO 2(g) + 2 H 2 O(l) + 890 k. J OR CH 4(g) + 2 O 2(g) CO 2(g) + 2 H 2 O(l) ΔH = - 890 k. J

Molar Heat of Fusion (ΔHfus) The heat absorbed by one mol of a substance

Molar Heat of Fusion (ΔHfus) The heat absorbed by one mol of a substance in melting from a solid to a liquid at a constant temperature. H 2 O(s) H 2 O(l) ΔHfus = 6. 01 k. J/mol

Molar Heat of Solidification (ΔHsolid) The heat lost when one mole of a liquid

Molar Heat of Solidification (ΔHsolid) The heat lost when one mole of a liquid solidifies at a constant temperature H 2 O(l) H 2 O(s) ΔHsolid = -6. 01 k. J/mol

Molar Heat of Vaporization (ΔHvap) The amount of heat necessary to vaporize one mole

Molar Heat of Vaporization (ΔHvap) The amount of heat necessary to vaporize one mole of a given liquid H 2 O(l) H 2 O(g) ΔHvap = 40. 7 k. J/mol

Molar Heat of Condensation (ΔHcond) The amount of heat released when 1 mol of

Molar Heat of Condensation (ΔHcond) The amount of heat released when 1 mol of vapor condenses H 2 O(g) H 2 O(l) ΔHcond = -40. 7 k. J/mol

Molar Heat of Solution (ΔHsoln) The heat change caused by dissolution of one mole

Molar Heat of Solution (ΔHsoln) The heat change caused by dissolution of one mole of substance Na. OH(s) H 2 O(l) Na+(aq) + OH-(aq) ΔHsoln = -445. 1 k. J/mol

Hess’s Law Indirect method to measure heat reaction If you add two or more

Hess’s Law Indirect method to measure heat reaction If you add two or more thermochemical equations to give a final equation, then you can also add the heats of reaction to give the final heat of reaction

Cont. Diamond to Graphite a. C(s, graphite) + O 2(g) CO 2(g) ΔH= -393.

Cont. Diamond to Graphite a. C(s, graphite) + O 2(g) CO 2(g) ΔH= -393. 5 k. J b. C(s, diamond) + O 2(g) CO 2(g) ΔH= -395. 4 k. J Write equation a in reverse to cancel out unwanted information c. CO 2(g) C(s, graphite) + O 2(g) ΔH= 393. 5 k. J

Cont. Now, add equation b and c b. C(s, diamond) + O 2(g) c.

Cont. Now, add equation b and c b. C(s, diamond) + O 2(g) c. CO 2(g) C(s, graphite) + O 2(g) ΔH= -395. 4 k. J ΔH= 393. 5 k. J

Cont. • Now, add equation b and c b. C(s, diamond) + O 2(g)

Cont. • Now, add equation b and c b. C(s, diamond) + O 2(g) c. CO 2(g) C(s, graphite) + O 2(g) C (s, diamond) C (s, graphite) ΔH= -395. 4 k. J ΔH= 393. 5 k. J ΔH= -1. 9 k. J

Standard Heat of Formation (ΔHfo) The change in enthalpy that accompanies the formation of

Standard Heat of Formation (ΔHfo) The change in enthalpy that accompanies the formation of one mole of a compound from its elements with all substances in their standard states at 25 o. C ΔHo = ΔHfo (products) – ΔHfo (reactants)