1/13
Looks like no tags are added yet.
Distinguish between intensive and extensive properties. Distinguish between open, isolated and closed systems.
Thermodynamic vocabulary
System: the portion of the universe under study. Surroundings: everything else. Together they make the universe.
The boundary (real or imaginary) determines what can cross between system and surroundings.
Intensive vs. extensive properties
Extensive property: depends on the amount of matter (extent) present. If you double the sample, the value doubles.
Examples: mass (m), volume (V), moles (n), energy (E), enthalpy (H), entropy (S), Gibbs energy (G), heat capacity (C), length, weight.
Intensive property: independent of the amount present. Mnemonic: INTensive = INDependent.
Examples: temperature (T), pressure (P), density (ρ=m/V), voltage (V = J/C), color, hardness, luster, odor, melting/boiling/freezing point, conductivity, malleability, ductility, specific heat (cs), molar heat capacity (cmolar).
Shortcut rule: the ratio of two extensive properties is intensive. ρ=m/V, cs=C/m, and cmolar=C/n all follow this rule. Doubling the sample doubles both numerator and denominator, so the ratio is unchanged.
Molecular meaning:
Temperature measures average kinetic energy per particle, so it does not scale with N.
Total energy sums over all particles, so it scales with N.
Common pitfalls:
Weight vs. mass: both are extensive (weight depends on amount and gravity).
Concentration is intensive, but amount of solute is extensive. This matters for heterogeneous equilibria later: the “concentration” of a pure solid is constant regardless of how much solid is present.
Thermodynamic functions of the form ΔH, ΔE and ΔG for a reaction are extensive: doubling the balanced equation doubles ΔH. This is why 2C2H2+5O2 gives twice the ΔH of C2H2+25O2.
Classifying systems by what crosses the boundary
System | Matter exchange | Energy exchange (heat/work) | Example |
|---|---|---|---|
Open | Yes | Yes | Living plant, gasoline burning in a car engine, open beaker of boiling water |
Closed | No | Yes | Coolant in a refrigerator coil, mercury in a thermometer, sealed flask in a water bath |
Isolated | No | No | Ideal thermos of coffee, the universe |
Pitfall: “closed” does not mean fully sealed from energy. It is closed to matter only. The fully sealed case is isolated.
The bomb calorimeter is treated as isolated: the sample burns inside a rigid sealed steel bomb (constant V, no matter exchange), and the insulated water jacket is assumed to prevent heat leaving. Strictly, heat flows from the bomb to the water inside the calorimeter, which is why we measure it.
Related process labels (a constraint on a process, not on the system type):
Isothermal: ΔT=0
Isobaric: ΔP=0
Isochoric: ΔV=0
Adiabatic: q=0
Worked classification (from your slide exercise)
Coffee in a very-high-quality thermos → isolated (no matter or energy exchange, ideal case).
Coolant in refrigerator coil → closed (sealed fluid, but it absorbs and releases heat and is worked on by the compressor).
Benzene burned in bomb calorimeter → isolated (sealed, insulated).
Gasoline burning in an automobile engine → open (fuel and air in, exhaust out, heat and work out).
Mercury in thermometer → closed (mercury cannot escape, but it exchanges heat).
A living plant → open (takes in CO₂, H₂O, light; releases O₂, water vapor).
Applying E=23RT to isothermal changes.
Where the equation comes from
For 1 mole of an ideal monatomic gas (He, Ne, Ar, Kr), the only energy is translational kinetic energy. There are 3 translational degrees of freedom (x,y,z), each carrying 21kT per atom (21RT per mole). This is the equipartition theorem.
E=3×21RT=23RT (J/mol), where R=8.314 J K−1mol−1 and T is in kelvin.
Key assumptions (the ideal gas model):
Particles have no intermolecular attractions or repulsions, so there is no potential energy contribution.
Particles are point masses, so there is no rotation or vibration (true for monatomic gases at ordinary temperatures).
Electronic excitation is negligible.
Consequence: E depends only on temperature
ΔE=23RΔT (per mole), or ΔE=23nRΔT for n moles. The 23 and R are constants, so they factor out of the Δ.
Isothermal process: ΔT=0, therefore ΔE=0.
Molecular picture: if the average kinetic energy per particle does not change and there are no interparticle forces, the total energy cannot change. Compression or expansion changes how much space the particles have, not how fast they move.
Since E is a state function, ΔE=0 for any path between two states at the same T, whether sudden or gradual, one step or many.
Pitfalls and edge cases
ΔE=0 for an isothermal process is exact only for ideal gases. For real gases, liquids and solids, E also depends on volume (through intermolecular forces).
Phase changes are isothermal but ΔE=0. Melting or boiling absorbs heat at constant T because that energy goes into potential energy (breaking intermolecular attractions), not kinetic energy.
ΔE=0 does not mean q=0 or w=0. Both can be nonzero, but they must cancel (see Card 4).
For polyatomic ideal gases, E is larger (25RT or 3RT, see Card 12), but it still depends only on T, so isothermal ΔE=0 still holds.
Worked example
Q: How much does the internal energy change when 2.00 mol of He is heated from 300 K to 400 K? What if the same gas is compressed isothermally at 300 K?
Heating: ΔE=23nRΔT=23(2.00 mol)(8.314 J K−1mol−1)(100 K)
Units: mol × J K⁻¹ mol⁻¹ × K = J
ΔE=2494 J≈ +2.49 kJ
Isothermal compression: ΔT=0⇒ ΔE=0
First law of thermodynamics (in words and in equation form).
Statement in words
Energy cannot be created or destroyed; it can only be converted from one form to another or transferred. The energy of the universe is constant.
For a closed system, the change in internal energy equals the heat added to it plus the work done on it.
Equation
ΔE=q+w
ΔE = change in internal energy of the system (J), the total of all kinetic and potential energy of the particles. It is a state function.
q = heat transferred across the boundary (J), driven by a temperature difference. It is a path function.
w = work done on or by the system (J). It is a path function.
Sign convention (system’s point of view): + means energy enters the system, − means energy leaves (see Card 4).
Conceptual background
Heat is not a substance (the old “caloric” theory is wrong). It is a mechanism of energy transfer driven by a temperature gradient, flowing hot → cold until thermal equilibrium.
Joule’s experiment (1840s): a falling weight turned a paddle wheel in water, and the water warmed without contact with any hotter body. This showed mechanical work converts to heat. 1 cal = 4.184 J (mechanical equivalent of heat).
Analogy to other “potential” differences:
Electrical current flows with a difference in electrical potential.
Heat flows with a difference in temperature.
Chemical reactions proceed with a difference in chemical potential (ΔG).
Why E is a state function but q and w are not
State function: depends only on the current state (P, V, T, n), not on how it was reached. Examples: E,H,S,G,P,V,T.
Path function: depends on the route. Only the sum q+w is path-independent.
Analogy: the elevation difference between two towns is fixed, but the distance walked depends on the road.
Pitfalls
Writing Δq or Δw: these are not changes in state functions, so write q and w.
Using the opposite sign convention. Some textbooks define w as work done by the system, giving ΔE=q−w. Your course uses ΔE=q+w.
The first law says nothing about direction or spontaneity. That requires the second law.
Worked example
*Q: A system’s internal energy increases by 80 J while 50 J of work is done on it. What is q?*
ΔE=q+w⇒80 J=q+50 J
q=80−50= +30 J
The positive sign means 30 J of heat flowed into the system.
Application of the first law to isothermal conditions and sign convention for heat and work.
Sign convention (system’s perspective)
q>0: heat flows into the system (endothermic).
q<0: heat flows out of the system (exothermic).
w>0: work done on the system (e.g., compression, ΔV<0).
w<0: work done by the system on the surroundings (e.g., expansion, ΔV>0).
Mnemonic: think of a bank account. Whatever enters the system is +.
Isothermal ideal-gas process
For an ideal gas, E=23RT (monatomic), so ΔE=23RΔT.
Isothermal: ΔT=0⇒ΔE=0.
First law: ΔE=q+w⇒0=q+w.
Therefore q=−w.
Interpretation in words
Heat absorbed by the system equals work done by the system on the surroundings. (And vice versa for compression.)
Expansion (w<0): the gas does work and would cool, but heat flows in from the surroundings (q>0) to keep T constant.
Compression (w>0): work is put in, and the same amount of energy leaves as heat (q<0) so T stays constant.
Molecular picture: during expansion, molecules colliding with a receding piston lose kinetic energy. The thermal reservoir resupplies it.
Pitfalls
q=−w holds only when ΔE=0 (isothermal ideal gas). In general, ΔE=0.
Isothermal does not mean no heat flow. Isothermal means constant T. No heat flow is adiabatic.
q and w depend on the path (reversible vs. irreversible) even though q=−w always holds on each path.
Worked example (from your slides): bicycle pump
*Q: Air is compressed in a pump of inner diameter 3.0 cm, depressed 20. cm against 2.00 atm. Find w and its sign.*
w=−PextΔV, and ΔV=−(πr2⋅ℓ) (volume decreases).
r=1.5 cm, so V=π(1.5)2(20.) cm3=141 cm3=0.141 L (using 1 L=1000 cm3).
w=−(2.00 atm)(−0.141 L)= +0.28 atm·L
In joules: 0.283 atm⋅L×101.3 J/(atm⋅L)≈ +28.7 J
Positive: work is done on the air.
Derivation of work for irreversible and reversible expansions.
Step 1: general expression for pressure-volume work
Work = force × distance. For a gas pushing a piston of area A against an external force Fext through a displacement dz:
dw=−Fextdz (minus sign: the system expands against a force, so it loses energy).
Pressure = force/area, so Fext=PextA:
dw=−PextAdz
Area × distance = volume: dV=Adz
dw=−PextdV
Integrate:
w=−∫ViVfPextdV (i)
Note: the work depends on Pext, the pressure the surroundings exert. This is not necessarily the pressure of the gas.
Step 2: irreversible (sudden) expansion at constant Pext
Pext is constant, so it comes out of the integral:
wirr=−Pext(Vf−Vi)=−PextΔV
Variables: Pext (Pa, atm or bar), ΔV (m³ or L).
Units: Pa·m³ = J. With atm and L, 1 L·atm = 101.325 J (equivalently 8.314/0.08206=101.3).
This is “irreversible” because the system is not in equilibrium during the process (gas pressure > Pext throughout expansion).
Step 3: reversible (gradual) isothermal expansion of an ideal gas
Reversible means infinitely slow change in which the system is always in equilibrium with its surroundings: Pext=Psys at every instant.
Substitute into (i) and use PV=nRT, so P=nRT/V:
w=−∫ViVfVnRTdV
n, R and T are constant (isothermal), so pull them out:
w=−nRT∫ViVfV1dV
Use ∫x1dx=lnx:
w=−nRT[lnV]ViVf=−nRT(lnVf−lnVi)
Use lnA−lnB=ln(A/B):
wrev=−nRTlnViVf
Since PiVi=PfVf for an isothermal ideal gas, this can also be written wrev=−nRTlnPfPi.
Corresponding heat
For an isothermal ideal gas, q=−w, so qrev=nRTlnViVf and qirr=+PextΔV. Heat is also path-dependent.
Dividing by T gives ΔS=qrev/T=nRln(Vf/Vi), the macroscopic entropy definition, which is a state function.
Assumptions and pitfalls
The reversible formula requires an ideal gas and constant T.
Reversibility is a theoretical limit. No real expansion is truly reversible, but it defines the maximum work.
Sign check: expansion has Vf>Vi, so ln(Vf/Vi)>0 and w<0. Compression gives w>0.
Do not use w=−PΔV with the gas pressure unless the process is irreversible.
Worked example (from your slides)
*Q: 1.00 mol ideal gas at 298 K expands isothermally from 1.00 m³ to 11.0 m³. Find w for (a) one-step irreversible expansion against the final pressure and (b) reversible expansion.*
nRT=(1.00)(8.314)(298)=2478 J
(a) Final pressure Pf=nRT/Vf=2478/11.0=225 Pa (1 Pa = 1 J/m³)
wirr=−PextΔV=−(225 J/m3)(10.0 m3)= −2.25 × 10³ J
(b) wrev=−(2478 J)ln(11.0/1.00)=−(2478)(2.398)= −5.94 × 10³ J (your slide: −5941 J)
The reversible path extracts more than twice the work.
⚠ Slide correction: the 5-step expansion total on your slide reads −4325 J with steps “−1625, −982…”. Recomputing each step (2 m3×P) gives −1652, −991, −708, −551, −450 J, totaling ≈ −4352 J. The slide has transposed digits. The trend (more steps → closer to −5941 J) is unaffected.
Work done under reversible conditions is greater than when done irreversibly.
Statement
For a given initial and final state, the maximum work that a system can do on its surroundings is obtained when the process is carried out reversibly.
Expansion: ∣wrev∣>∣wirr∣ (the reversible path gives the most negative w).
Compression: the reversible path requires the least work input (wrev is the smallest positive value).
Your slide’s shorthand “wrev>wirr” refers to the magnitude of work done by the system.
Why: the physical argument
Work of expansion = −∫PextdV. Magnitude = area under the Pext vs. V curve.
During expansion, Pext≤Psys (otherwise the gas wouldn’t expand).
The reversible process sets Pext as large as possible at every step, equal to Psys. Any irreversible path has Pext lower somewhere, so it traces less area.
Graphical picture (your slides): with 1 step, the rectangle is small. As steps increase (5 → 40 → ∞), the rectangles approach the curve and the area approaches the maximum.
Numerical illustration (1 mol, 298 K, 1 → 11 m³)
Path | Work done by gas |
|---|---|
1 sudden step | ≈ 2250 J |
5 steps | ≈ 4350 J |
40 steps | ≈ 5672 J |
Infinite steps (reversible) | 5941 J (maximum) |
Connection to entropy and the second law
ΔS is a state function, equal to qrev/T for any path.
Because ∣q∣=∣w∣ at constant T and ∣wirr∣<∣wrev∣, we get ∣qirr∣<∣qrev∣, so:
ΔS>Tqirr for an irreversible process.
Interpretation: the “missing” work is dissipated as increased disorder in the universe, which is why ΔSuniv>0 for irreversible processes.
Pitfalls
A reversible process is not one that merely “can go backward.” It is one that proceeds through a continuous sequence of equilibrium states, infinitely slowly.
Phase changes at the transition temperature (melting ice at 0 °C, 1 atm) are naturally reversible equilibrium processes. Gas expansions are not.
ΔE, ΔH and ΔS are the same for both paths. Only q and w differ.
Worked example
*Q: 1.00 mol ideal gas at 298 K expands from 1.00 L to 10.0 L. Compare ∣w∣ for a single step against Pext = final pressure vs. reversible.*
nRT=2478 J
Pf=nRT/Vf=2478 J/(10.0 L)=247.8 J/L
∣wirr∣=PfΔV=(247.8 J/L)(9.00 L)=2230 J
∣wrev∣=nRTln(10.0)=(2478)(2.303)=5706 J
Ratio ≈ 2.6: the reversible path does about 2.6× more work.
Calculate the work done by a gas due to expansion (not necessarily isothermal). Calculate the change in internal energy due to heat and work.
Choosing the right work formula
Constant external pressure (irreversible): w=−PextΔV
Reversible isothermal ideal gas: w=−nRTln(Vf/Vi)
Free expansion into vacuum (Pext=0): w=0
Reaction producing or consuming gas at constant P and T: using PΔV=ΔngasRT:
w=−ΔngasRT
Δngas = (moles gas products) − (moles gas reactants). Solids and liquids contribute negligible volume.
Calculating ΔE
ΔE=q+w, with each term in joules.
Heat from an electric heater: q=Ppower×t, where 1 W = 1 J/s.
Unit management (the most common source of error)
1 L⋅atm=101.325 J; also R=8.314 J K−1mol−1=0.08206 L atm K−1mol−1.
Convert kJ ↔ J before adding. Temperatures in K for RT terms. 1 mL=10−3 L.
Sign check: expansion → w negative; compression → w positive.
Worked example 1: heater and expansion (your slide)
*Q: A 100. W heater runs for 10.0 min heating a gas that expands from 2.00 L to 10.0 L against a constant 0.975 atm. Find ΔE.*
q=(100. J/s)(10.0×60 s)=6.00×104 J=+60.0 kJ
ΔV=10.0−2.00=8.00 L
w=−PextΔV=−(0.975 atm)(8.00 L)(101.33 J/L⋅atm)=−790 J=−0.790 kJ
ΔE=q+w=60.0−0.790= +59.2 kJ
Worked example 2: simple expansion
*Q: A gas expands by 500. mL against 1.20 atm. Find w in J.*
w=−(1.20 atm)(0.500 L)=−0.600 L⋅atm
−0.600 L⋅atm×101.3 J/(L⋅atm)= −60.8 J
Worked example 3: work from a chemical reaction
*Q: Ni(s) + 4 CO(g) → Ni(CO)₄(g) for 1.00 mol Ni at 75 °C. Find w.*
Δngas=1−4=−3 mol (solid Ni is ignored)
T=75+273=348 K
w=−ΔngasRT=−(−3.00 mol)(8.31 J K−1mol−1)(348 K)= +8.68 × 10³ J
Positive: the gas volume shrinks, so surroundings do work on the system.
Calorimetry. Use the heat capacity of a substance to calculate the heat required to raise its temperature by a given amount.
Core concept
Calorimetry measures heat flow by monitoring a temperature change in a known mass of a known substance (often water).
Heat capacity (C): the heat needed to raise the whole sample’s temperature by 1 K (or 1 °C). Units: J/K (extensive).
q=CΔT
Specific heat capacity (cs): heat per gram per kelvin. Units: J g⁻¹ K⁻¹ (intensive).
q=mcsΔT
Molar heat capacity (cmolar): heat per mole per kelvin. Units: J mol⁻¹ K⁻¹ (intensive).
q=ncmolarΔT
ΔT=Tfinal−Tinitial. A temperature difference in °C equals that in K, so no conversion is needed for ΔT.
Molecular meaning
Substances with many ways to store energy (rotation, vibration, hydrogen bonds) have large heat capacities. Water has a high cs (4.184 J g⁻¹ °C⁻¹) due to extensive hydrogen bonding, which absorbs energy.
Calorimetry principle (isolated system)
Energy conservation: heat lost by the hot object = heat gained by the cold object.
−qhot=+qcold, or equivalently ∑q=0.
Assumptions: no heat exchange with the surroundings or the container (or the container’s heat capacity is included explicitly), and no phase changes.
Coffee-cup calorimeter: include the calorimeter heat capacity: qtotal=CcalΔT+mcsΔT.
Pitfalls
Using T in the wrong units in RT but not here. For ΔT alone, °C and K are interchangeable.
Sign errors: the metal’s ΔT is negative (cooling), so qmetal<0.
⚠ Your slide has a typo in its first example, writing 4.148 instead of 4.184 for water’s cs. The final answer (0.434) uses the correct value.
Worked example 1: heat required
*Q: How much energy is needed to raise an 8.50 × 10² g aluminum block from 22.8 °C to 94.6 °C? (cs = 0.900 J g⁻¹ °C⁻¹)*
ΔT=94.6−22.8=71.8 °C
q=(8.50×102 g)(0.900 J g−1°C−1)(71.8 °C)
Units: g × J g⁻¹ °C⁻¹ × °C = J
q=5.49×104 J= 54.9 kJ (3 sig. figs.)
Worked example 2: final temperature
*Q: 840 J is absorbed by 10.0 g of water at 25.0 °C. Find Tf.*
ΔT=q/(mcs)=840/(10.0×4.18)=20.1 °C
Tf=25.0+20.1= 45.1 °C
Calculate energy changes from calorimetry data. Difference between cmolar and cspecific. How C is related to c. Relation between CP and CV.
Three related quantities
Symbol | Name | Units | Extensive? |
|---|---|---|---|
C | Heat capacity | J K⁻¹ | Extensive |
cs | Specific heat capacity | J g⁻¹ K⁻¹ | Intensive |
cmolar | Molar heat capacity | J mol⁻¹ K⁻¹ | Intensive |
Relationships: C=mcs=ncmolar
Conversion between the intensive forms: cmolar=cs×M (molar mass, g/mol).
Rule: lowercase c = intensive; uppercase C = extensive.
CV vs. CP
CV (constant volume): CV=ΔTΔE, since ΔE=qV=CVΔT.
CP (constant pressure): CP=ΔTΔH, since ΔH=qP=CPΔT.
Derivation of the ideal-gas relation:
H=E+PV and PV=nRT gives H=E+nRT.
ΔH=ΔE+nRΔT
Divide by ΔT: ΔTΔH=ΔTΔE+nR
CP=CV+nR (extensive form) and cP=cV+R (per mole).
Why CP>CV: at constant P, part of the heat supplied goes into expansion work against the surroundings (PΔV=nRΔT), so more heat is needed for the same ΔT. At constant V, all heat raises internal energy.
This relation is exact for ideal gases. For solids and liquids CP≈CV because they barely expand.
Energy changes from calorimetry data
Identify what absorbs heat (water, solution, calorimeter hardware).
Compute q=CΔT or mcsΔT for each, and add them.
Apply energy conservation: qrxn=−(qwater+qcal).
Divide by moles for kJ/mol.
Worked example (from your slides): unknown metal
*Q: 18.0 g metal at 100 °C is placed in 50.2 g water at 22.0 °C. Final T = 24.8 °C. Find cs of the metal.*
−qmetal=+qwater
−[18.0 g cmetal(24.8−100)]=+[50.2 g(4.184)(24.8−22.0)]
cmetal(18.0)(75.2)=(50.2)(4.184)(2.8)
cmetal=1354588= 0.434 J g⁻¹ °C⁻¹
From internal energy to enthalpy. Why do we need enthalpy? Relation to calorimetry.
The problem with ΔE
First law at constant pressure for expansion work only: ΔE=q−PΔV.
If volume is constant (ΔV=0), ΔE=qV, so heat measures ΔE directly (bomb calorimeter).
But most laboratory and biological chemistry occurs at constant pressure (open beakers, 1 atm). Constant volume is experimentally difficult to maintain.
At constant P, the heat flow qP equals ΔE plus the expansion work term, so qP=ΔE. We need a state function whose change equals qP.
Definition of enthalpy
H=E+PV (state function, extensive, J). Since E, P and V are state functions, so is H.
At constant P: ΔH=ΔE+PΔV.
Substitute ΔE=q−PΔV: ΔH=q−PΔV+PΔV
ΔH=qP
Meaning: ΔH is the heat absorbed or released at constant pressure. ΔH<0 is exothermic; ΔH>0 is endothermic.
PV term physically: the energy needed to “make room” for the system by pushing back the atmosphere.
Relating ΔH and ΔE for reactions
For ideal gases, PΔV=ΔngasRT:
ΔH=ΔE+ΔngasRT
If Δngas=0 (or only solids/liquids), ΔH≈ΔE.
Relation to calorimetry
Constant volume (bomb): qV=ncVΔT=mcs,VΔT=ΔE
Constant pressure (coffee cup): qP=ncPΔT=mcs,PΔT=ΔH
Absolute vs. relative values
Absolute E and H can’t be measured, only differences. We choose a reference: ΔHf∘=0 for elements in their standard state (298 K, 1 atm). For hydrogen the standard state is H₂(g), not H(g).
Pitfall: ΔH=qP is valid only at constant pressure with only expansion work.
Worked example
*Q: For ½H₂(g) + ½I₂(s) → HI(g), ΔH=+39.7 kJ at 298 K. Find ΔE.*
Δngas=1−21=+21 mol (I₂(s) not counted)
ΔH=ΔE+ΔngasRT⇒ΔE=ΔH−ΔngasRT
ΔngasRT=(0.5)(8.314)(298)=1239 J=1.24 kJ
ΔE=39.7−1.24= 38.5 kJ
Distinguish between the internal energy and the enthalpy of a process and describe how each is measured.
Comparison
Internal energy ΔE | Enthalpy ΔH | |
|---|---|---|
Definition | Total kinetic + potential energy change of the system | ΔH=ΔE+Δ(PV) |
Equals heat at… | Constant volume: ΔE=qV | Constant pressure: ΔH=qP |
Instrument | Bomb calorimeter (rigid sealed steel vessel) | Coffee-cup (constant-pressure) calorimeter |
Heat capacity used | CV | CP |
State function? | Yes | Yes |
Includes expansion work? | No (wPV=0 at constant V) | Accounts for it automatically |
Measuring ΔE: bomb calorimeter
The sample burns in a sealed rigid “bomb” (constant V) surrounded by water in an insulated container. An ignition wire triggers the reaction.
qrxn=−(qwater+qbomb)=−(mwcw+Ccal)ΔT, and ΔE=qV=qrxn.
Measuring ΔH: constant-pressure calorimeter
A reaction occurs in solution in an insulated cup with a loosely fitting lid (open to atmosphere at ~1 atm).
qrxn=−(msolncs+Ccal)ΔT, and ΔH=qP=qrxn.
ΔH per mole = qrxn/nlimiting reagent.
Pitfalls
Sign: if the temperature of the solution rises, the reaction is exothermic, so ΔH is negative.
Limiting reagent: divide by moles of the limiting reactant, not by moles of “solution.”
⚠ Slide correction: your KOH(s) + HCl(aq) calorimetry example computes q=6762 J correctly but (1) divides by 0.08 mol labeled “moles of solution” (it is the limiting reagent HCl: 0.800 L × 0.100 M), and (2) reports +84.5 kJ/mol, but since T rose, the correct answer is ΔH = −84.5 kJ/mol.
Worked example 1: constant-pressure (coffee cup)
*Q: 0.0300 mol NaOH(s) is added to 1000 mL of 0.0300 M HNO₃ at 23.000 °C. Tf = 23.639 °C. Ccal = 451 J/°C; cs = 4.18 J g⁻¹ °C⁻¹; density = 1.00 g/mL. Find ΔH per mole.*
ΔT=0.639 °C
qcal=(451)(0.639)=288 J
qsoln=(1000 g)(4.18)(0.639)=2671 J
qtotal gained=2959 J, so qrxn=−2959 J
ΔH=−2959 J/0.0300 mol=−98,600 J/mol= −98.6 kJ/mol
Worked example 2: constant-volume (bomb)
*Q: 5.000 g methanol (32.04 g/mol) burns in a bomb with 4000 g water (T: 24.000 → 29.765 °C); Ccal = 2657 J/°C. Find ΔE per mole.*
ΔT=5.765 °C
qcal=2657(5.765)=15,318 J; qwater=4000(4.184)(5.765)=96,486 J
Total heat released by reaction = 111.8 kJ per 5.000 g
Per mole: 111.8×(32.04/5.000)=716 kJ/mol
Exothermic: ΔE=−716 kJ/mol
Contributions to internal energy in the case of monoatomic, polyatomic (linear), polyatomic (non-linear) species.
Foundation: equipartition
Each quadratic degree of freedom contributes 21kT per molecule, i.e., 21RT per mole.
k=1.381×10−23 J K−1 (Boltzmann’s constant); NAk=R.
Ideal gas assumption: no intermolecular potential energy, so E is purely the sum of molecular motions.
Types of motion
Translation: 3 degrees of freedom for any gas particle (movement along x, y, z).
Rotation: present for molecules, not atoms (point masses have negligible moment of inertia).
Vibration: only significantly excited at high temperatures, ignored at room temperature (the energy spacing is large compared to kT; quantum mechanically the mode is “frozen out”).
Results
Species | Translational | Rotational | Total E (per mol) | CV | CP=CV+R |
|---|---|---|---|---|---|
Monoatomic (He, Ar) | 3 × ½RT | 0 | 23RT | 23R | 25R |
Linear polyatomic (H₂, N₂, CO₂) | 3 × ½RT | 2 × ½RT | 25RT | 25R | 27R |
Non-linear polyatomic (H₂O, NH₃, CH₄) | 3 × ½RT | 3 × ½RT | 3RT (= 26RT) | 3R | 4R |
Why linear molecules have only 2 rotations
A linear molecule can tumble about two axes perpendicular to the molecular axis. Rotation about the bond axis involves essentially no change in the positions of the atomic nuclei (point-like masses on the axis), so its moment of inertia is negligibly small.
Quantized rotational energy ∝1/I, so the first excited level of this mode is enormously high, so it is never populated at accessible temperatures. Your slide expresses this as requiring energies so large that the molecule would dissociate first.
Non-linear molecules have atoms off any single axis, so all 3 rotational axes have appreciable moments of inertia.
Pitfalls
These values hold at moderate temperatures. At high T, vibrations contribute (each vibrational mode adds kT: ½ kinetic + ½ potential), so measured CV rises above these values.
The CP=CV+R shortcut applies to 1 mole of ideal gas.
In liquids and solids, intermolecular potential energy matters, so these formulas do not apply.
Worked example
*Q: Estimate the molar internal energy of N₂(g) and CO₂(g) at 298 K, and ΔE for heating 1.00 mol of H₂O vapor by 50.0 K (ideal, no vibration).*
N₂ and CO₂ are both linear: E=25RT=2.5(8.314)(298)=6194 J/mol≈ 6.19 kJ/mol
H₂O is non-linear: CV=3R=24.94 J K−1mol−1
ΔE=nCVΔT=(1.00)(24.94)(50.0)= 1247 J ≈ 1.25 kJ
Use standard enthalpies of formation to calculate the standard enthalpy of a reaction.
Definitions
Standard enthalpy of formation (ΔHf∘): the enthalpy change when 1 mole of a compound forms from its elements in their standard states at 1 bar/1 atm (and usually 298 K). Units: kJ/mol.
Elements in their standard states have ΔHf∘=0: O₂(g), H₂(g), N₂(g), C(graphite), Fe(s), Hg(l), Br₂(l). Not H(g), O(g) or C(diamond).
Formation of a compound is written with a coefficient of 1 on the product, e.g. C(s) + 2H₂(g) → CH₄(g).
Formula
ΔHrxn∘=∑npΔHf∘(products)−∑nrΔHf∘(reactants)
np,nr = stoichiometric coefficients (mol) from the balanced equation.
Explicitly, for aA+bB→cC+dD:
ΔHrxn∘=cΔHf∘(C)+dΔHf∘(D)−[aΔHf∘(A)+bΔHf∘(B)]
Why it works
H is a state function. Imagine decomposing all reactants into elements (enthalpy change =−ΔHf∘ of reactants) and then forming all products from elements (+ΔHf∘ of products). The elements cancel, and the net change equals the formula above (a special case of Hess’s law).
Bond picture: breaking bonds is endothermic (ΔH>0), forming bonds is exothermic (ΔH<0). Products − reactants = final − initial.
Pitfalls
Multiply each ΔHf∘ by its coefficient.
Phase matters: ΔHf∘[H₂O(l)] = −285.8 vs. ΔHf∘[H₂O(g)] = −241.8 kJ/mol. The difference is the enthalpy of vaporization (≈44 kJ/mol).
Order: products minus reactants (not the reverse).
Units: “kJ/mol” in this context means kJ per mole of reaction as written.
Extensive: doubling the equation doubles ΔHrxn∘.
⚠ Slide corrections (acetylene examples): C₂H₂ is acetylene (ethylene is C₂H₄). The accepted ΔHf∘[C₂H₂(g)] is +226.7 kJ/mol (consistent with your own Hess’s-law question, 226.7), not +277. With H₂O(g) at −241.8, the correct combustion enthalpy is 2(−393.5)+(−241.8)−226.7=−1255.5 kJ/mol.
Worked example (from your slides)
*Q: Calculate ΔH∘ for CH₄(g) + 2O₂(g) → CO₂(g) + 2H₂O(l). Given ΔHf∘: CH₄ = −74.8, CO₂ = −393.5, H₂O(l) = −285.8 kJ/mol.*
Products: (1)(−393.5)+(2)(−285.8)=−393.5−571.6=−965.1 kJ
Reactants: (1)(−74.8)+(2)(0)=−74.8 kJ (O₂ is an element)
ΔHrxn∘=−965.1−(−74.8)= −890.3 kJ/mol (exothermic)
Calculate an overall reaction enthalpy from the enthalpies of the reactions in a reaction sequence by using Hess’s law.
Hess’s law
The enthalpy change for a reaction is the same whether it occurs in one step or through a series of steps; the overall ΔH is the sum of the ΔH values of the individual steps.
Basis: H is a state function, so ΔH depends only on initial and final states: ΔHRP=ΔHRI+ΔHIP (reactants → intermediates → products).
Utility: lets us find ΔH for reactions that are hard to measure directly (e.g., C → CH₄, diamond → graphite) from combustion or other easily measured reactions.
Three manipulation rules
Reverse a reaction → change the sign of ΔH.
Multiply a reaction by a factor k → multiply ΔH by k (ΔH is extensive).
Add equations → add their ΔH values. Species that appear on both sides cancel.
Problem-solving strategy
Write the target equation clearly.
Locate each target reactant/product in exactly one given equation, and orient and scale that equation to match.
Add the modified equations. Check that all intermediates cancel and the result equals the target.
Sum the modified ΔH values. Keep track of signs and units (kJ).
Pitfalls
Forgetting to flip the sign when reversing.
Forgetting to multiply ΔH when scaling coefficients.
Mismatched phases (H₂O(l) vs. H₂O(g)).
The same ΔG logic also follows Hess’s law, which is why coupled biochemical reactions (e.g., ATP hydrolysis driving glucose phosphorylation) simply add their ΔG values.
Worked example 1 (from your slides): ΔH_f of propane
Target: 3C(gr) + 4H₂(g) → C₃H₈(g)
Given:
(a) C₃H₈ + 5O₂ → 3CO₂ + 4H₂O(l) ΔH=−2220 kJ
(b) C(gr) + O₂ → CO₂ ΔH=−394 kJ
(c) H₂ + ½O₂ → H₂O(l) ΔH=−286 kJ
Reverse (a) (propane must be a product): 3CO₂ + 4H₂O → C₃H₈ + 5O₂ ΔH=+2220 kJ
Multiply (b) by 3 (need 3 C): 3C + 3O₂ → 3CO₂ ΔH=3(−394)=−1182 kJ
Multiply (c) by 4 (need 4 H₂): 4H₂ + 2O₂ → 4H₂O ΔH=4(−286)=−1144 kJ
Add: CO₂, H₂O and O₂ cancel (5 O₂ produced on the right; 3 + 2 = 5 O₂ consumed on the left).
ΔH=+2220−1182−1144= −106 kJ
Worked example 2: diamond → graphite (from your slides)
C(diamond) + O₂ → CO₂ −395.4 kJ (as given)
2CO₂ → 2CO + O₂ +566.0 kJ (as given)
2CO → C(graphite) + CO₂ −172.5 kJ (as given)
Adding: C(diamond) → C(graphite), ΔH=−395.4+566.0−172.5= −1.9 kJ
Slightly exothermic, so graphite is the more stable form.