1 / 35

THERMOCHEMISTRY

THERMOCHEMISTRY. HESS’ LAW, AND HEAT VS. TEMPERATURE. HESS’ LAW. The change in energy of a process or reaction is a state function, meaning that regardless of the path to reach your goal, the energy to get there is constant.

Download Presentation

THERMOCHEMISTRY

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. THERMOCHEMISTRY HESS’ LAW, AND HEAT VS. TEMPERATURE

  2. HESS’ LAW • The change in energy of a process or reaction is a state function, meaning that regardless of the path to reach your goal, the energy to get there is constant. • For instance if you want to vaporize a solid, you have two pathways. • You can melt it into a liquid and then vaporize it into a gas. • Or you can sublime the solid directly into a gas. • Either pathway gets the desired results and either pathway requires the same amount of heat energy, this is Hess’s Law.

  3. The idea that we can calculate Hsublimation by combining the Hfus with the Hvap is an illustration of Hess’ Law.

  4. HESS’ LAW • Hess’ Law is a law of physical chemistry that states the enthalpy change of a reaction is the same regardless of what pathway is taken to achieve products. • Only the start and end states matter to the reaction not the individual steps in between • This allows the H for a rxn to be calculated even when it cannot be measured directly • This process will feel a little like combining half reactions like we did earlier this semester.

  5. Only the start and end states matter to the reaction not the individual steps in between • For instance let’s look at this synthesis: • N2 + 2H2O  N2H4 + O2DH = +622.2kJ • 2H2 + O2 2H2ODH= -571.6kJ N2 + 2H2 N2H4 Hrxn: ? • We can calculate Hrxn by using a combination of the following 2 rxns: N2 + 2H2 N2H4 DHrxn = 50.6kJ/mol

  6. What if the rxns we are trying to combine don’t combine naturally as presented? • Then we can manipulate the eqnsto make them combine naturally. 2 N2(g) + 5 O2(g) 2 N2O5(g) DHf = ? • We are given a series of related rxns, with enthalpy data, that we will attempt to combine to calculate the Hf above: 2NO(g) + O2(g) 2NO2(g) DH°rxn= -114kJ/mol 4NO2(g) + O2(g) 2N2O5(g) DH°rxn= -110kJ/mol N2(g) + O2(g) 2NO(g) DH°rxn= +181kJ/mol

  7. We need to remember that the amount of energy of a reaction is related to both direction (endo/exo or +/-) and moles (coefficients of a rxn equation). • Because of these connections to our enthalpy, any changes that we make to the reaction equation must be reflected in our given H values. • There are two rules to remember during our manipulations: • If we reverse the rxn, the sign of the DH°rxn is reversed. For example, if: If: 2H2(g)+ O2(g) 2H2O (g) DH°rxn= -482kJ/mol Then: 2H2O (g)2H2(g)+ O2(g)DH°rxn= +482kJ/mol

  8. If we need to multiply our coefficients in a reaction by a value to increase or decrease the amount of products then our enthalpy value must be multiplied by the same factor. For example if we double the following rxn: If: 2H2(g)+ O2(g) 2H2O (g) DH°rxn= -482 kJ/mol Then: 4H2(g)+2O2(g)4H2O(g) H°rxn= -964 kJ/mol • So let’s use these rules to combine the previous reactions to determine the enthalpy of formation of N2O5: 2 N2(g) + 5 O2(g) 2 N2O5(g) DHrxn = ?

  9. 2 N2(g) + 5 O2(g) 2 N2O5(g) DHrxn = ? Goal: • First we want to target reactants or products in our given eqns that already match both in coefficient and in side of eqn with our final reaction eqn. • Since the are identical already, we don’t want to change anything about them. If we were to change something, than they would no longer match. 2NO(g) + O2(g) 2NO2(g) DH°rxn= -114kJ/mol 4NO2(g) + O2(g) 2N2O5(g) DH°rxn= -110kJ/mol N2(g) + O2(g) 2NO(g) DH°rxn= +181kJ/mol

  10. 2 N2(g) + 5 O2(g) 2 N2O5(g) DHrxn = ? Goal: • Next we want to target reactants or products in our final rxneqn that are unique to only one of the given rxneqns • We see that in our target eqn we need to end up with 2 mols of N2 gas in the reactants • Our third given eqn has 1 mol of N2 gas in the reactants • If we doubled that rxn it would match… 2NO(g) + O2(g) 2NO2(g) DH°rxn= -114kJ/mol 4NO2(g) + O2(g) 2N2O5(g) DH°rxn= -110kJ/mol N2(g) + O2(g) 2NO(g) DH°rxn= +181kJ/mol 2N2(g) + 2O2(g) 4NO(g) DH°rxn= +362kJ/mol

  11. 2 N2(g) + 5 O2(g) 2 N2O5(g) DHrxn = ? Goal: • Now we want to decide how to make use of the first rxn eqn. • If we multiply it by two, we would be able to cancel out the NO2in 1st first eqn and the NO2 in the 2nd eqn. • That manipulation (since we have changed something in each eqn) should set us up to combine the eqns to receive our target eqn. 4NO(g) + 2O2(g) 4NO2(g) DH°rxn= -228kJ/mol 2NO(g) + O2(g) 2NO2(g) DH°rxn= -114kJ/mol 4NO2(g) + O2(g) 2N2O5(g) DH°rxn= -110kJ/mol 2N2(g) + 2O2(g) 4NO(g) DH°rxn= +362kJ/mol

  12. 2 N2(g) + 5 O2(g) 2 N2O5(g) DHrxn = ? Goal: • Now we should be able to combine the three into one and end up with the one above 4NO(g) + 2O2(g) 4NO2(g) DH°rxn= -228kJ/mol 4NO2(g) + O2(g) 2N2O5(g) DH°rxn= -110kJ/mol 2N2(g) + 2O2(g) 4NO(g) DH°rxn= +362kJ/mol 2N2(g) + 2O2(g) + O2(g) + 2O2(g)  2N2O5(g) 2N2(g) + 5O2(g)  2N2O5(g) DHrxn1 + DHrxn2 + DHrxn3 = DHrxn (-228 kJ/mol)+(-110 kJ/mol)+(362kJ/mol)= 24kJ

  13. 2 2 • Example 2: Given the following information: C2H6C2H4 + H2 137kJ/mol 2H2O2H2+O2 484kJ/mol 2H2O+2CO2C2H4+3O2 1323kJ/mol Find the value of H° for the reaction: 2C2H6 + 7O2 4CO2 + 6H2O

  14. Example 2: Rearranging and multiplying: 2 C2H6  2 C2H4 + 2 H2 274kJ/mol 2H2O2H2+O2 484kJ/mol 2C2H4+6O24H2O+4CO2-2646kJ/mol Find the value of H° for the reaction: 2C2H6 + 7O2 4CO2 + 6H2O

  15. Example 2: Rearranging and multiplying: 2 C2H6  2 C2H4 + 2 H2 274kJ/mol 2H2 + O22H2O- 484kJ/mol 2C2H4+6O24H2O+4CO2- 2646kJ/mol Find the value of H° for the reaction: 2C2H6 + 7O2 4CO2 + 6H2O (274kJ)+(-484kJ)+(-2646kJ) = DHrxn -2856 kJ = DHrxn

  16. Classwork Before pipelines were built to deliver natural gas, individual towns and cities contained plants that produced a fuel known as town gas by passing steam over red-hot charcoal. C(s) + H2O(g)  CO(g) + H2(g) Calculate H for this reaction from the following information.. C(s) + ½O2(g) CO(g)H = -110.53 kJ CO(g) + ½O2(g) CO2(g)H = -282.98 kJ C(s) + O2(g)CO2 (g)H = -393.51 kJ H2(s) + ½O2(g)H2O(g)H = -241.82 kJ

  17. PHASE CHANGES & HEAT • Energy is required to change the phase of a substance • The amount of heat necessary to melt 1 mole of substance • Heat of fusion (Hfus) • It takes 6.00 kJ of energy to melt 18 grams of ice into liquid water. • The amount of heat necessary to boil 1 mole of substance • Heat of vaporization (Hvap) • It takes 40.6 kJ of energy to boil away 18 grams of water.

  18. boils condenses melts freezes

  19. There are 5 distinct sections we can divide the curve into • Ice • Water & ice • Water only • Water & steam • Steam only • We can calculate the amount of energy involved in each stage • There are two types of calculations • Temperature changes use H=mCT • Phase changes use (#mols)Hfus or (#mols)Hvap

  20. SOLID ICE • Let’s say we have 18.0g of ice at –10°C, & we begin heating it on a hot plate with sustained continuous heat. • Heat energy absorbs into the ice increas-ing the vibrational or kinetic energy of the ice molecules • The temp will increase & will continue to increase until just before the ice has enough energy to change from solid to liquid • We can calc the energy absorbed by the ice to this point • Use the eqn DH=mCDT (cice=2.09J/g°C)

  21. = ice 376.2J H D DHice=mCiceDT DHice =(18g)(2.09J/g°C)(0°C-(-10°C)) DHice=376.2J 0° -10°

  22. WATER & ICE (MELTING) • Any additional heat absorbed by the ice goes into partially breaking the connections between the ice molecules. • There is no change in the kinetic energy of the molecules (curve flattens out) • No change in temp • All of the energy goes into breaking the connections • As long there is solid ice present, the temp cannot increase. • The solid & liquid are in equilibrium if they are both present

  23. The H required to change from the solid to the liquid phase is called the heat of fusion & depends on the amnt of the substance (DHfus of H2O=6000J/mol or 6kJ/mol) 1 mol H2O 6000J = D H 18g H2O 1 mol H2O = ice 376.2J H melting D 6000J • Using the formula: DHmelting =(mol) DHfus 18g H2O = 6000J 0° -10°

  24. ALL WATER • Now all of the particles are free to flow, • The heat energy gained now goes into the vibrational energy of the molecules. • The temp of the water increases • The rate of temp increase now depends on the heat capacity of liquid water • Cwater=4.180J/g°C • The temp continues to increase until it just reaches boiling stage (for water = 100ºC) • again, Hwater=mCwaterT

  25. = = D H = ice water 376.2J H melting D H D DHwater=(18g)(4.18J/g°C)(100°C-0°C) DHwater= 7524J 100° 0° 7524J 6000J -10°

  26. STEAM & WATER (VAPORIZING) • Any additional heat absorbed by the water goes into completely breaking the connections between the water molecules. • Again the heat does not increase the KE of the molecules so the temp does not change, • the energy is used to vaporize the water • If there are still connections to break or there is liquid present, the temp cannot increase. • The energy required to change from the liquid to the vapor phase is called the heat of vaporization; using Hboiling=(mol)Hvap • Hvap of H2O=40,790J/mol

  27. 40,790J 1 mol H2O 1mol H2O 18g H2O 7524J = = D H = ice water 376.2J H melting 40,790J D H D = boiling H D 18g H2O 100° Hboiling=(mol)HVAP 0° 6000J -10°

  28. STEAM ONLY (VAPOR PHASE) • Again the heat energy goes into the vibrational energy of the molecule. • Rate of temp increase depends on CH2O vapor=1.84J/g°C • The temp can increase indefinitely, or until the substance decomposes (plasma) • We’ll stop at 125°C.

  29. 7524J = = 828J D H = ice water 376.2J H melting 40,790J D H = D steam = H D boiling H D 125° DHSTEAM=(m)(CWATER VAPOR)(T) DH=(18g)(1.84J/g°C)(125°-100°) 100° 0° 6000J -10°

  30. To figure out how much energy we need would need all together to heat up the water this much, we just need to add up the energy of each step. DHtotal= (376J + 6000J +7524J + 40,790J + 829J) DHtotal =55,500J • Notice, the majority of the energy is needed for the vaporization step. • The connections between molecules of H2O must be broken completely to vaporize

  31. Classwork We have a collection of steam at 173°C that occupies a volume of 30.65 L and a pressure of 2.53 atm. How much energy would it need to lose to end up as a block of ice at 0.00°C?

More Related