Chalk−1

Chemistry · General chemistry II · Worked example

Enthalpy of solution of NaCl from a cycle

One consistent set of data gives a lattice energy of −787 kJ⁢/⁢mol for NaCl and a hydration enthalpy of −784 kJ⁢/⁢mol for one Na+ ion and one Cl− ion together. Build the energy cycle and find Δ⁢H⁢(soln).

NaCl⁢(s)→Na+(aq)+Cl−(aq)

Break the lattice

The lattice energy describes forming the solid from gaseous ions. Going from the solid to gaseous ions is the reverse, so its sign flips and it costs +787 kJ⁢/⁢mol.

NaCl⁢(s)→Na+(g)+Cl−(g)ΔHsolute=+787 kJ/mol
NaCl⁢(s)→Na+(g)+Cl−(g)ΔHsolute=+787 kJ/mol

Hydrate the ions

Each gaseous ion releases energy as water surrounds it. NaCl gives one of each, and the data give the pair together, −784 kJ⁢/⁢mol, because measurements fix the sum. A table that lists each ion on its own has to split that sum by a convention, so its values belong with its own lattice energy.

ΔHhydration=−784 kJ/mol

Close the cycle

Add the two paths. Hess’s law allows it, because the climb and the drop together lead from the solid to the dissolved ions. The lattice cost and the hydration payback almost cancel.

ΔHsoln=+787+(−784)=+3 kJ/mol
ΔHsoln=+787+(−784)=+3 kJ/mol

Judge the result

+3 kJ⁢/⁢mol is the difference of two numbers near 785, so a few kJ⁢/⁢mol either way in a table would change it. The measured value is +3.88 kJ⁢/⁢mol, slightly endothermic, with almost no temperature change. The salt still dissolves because entropy increases.

Result

Δ⁢H⁢(soln)≈+3 kJ⁢/⁢mol from this data (measured +3.88 kJ⁢/⁢mol). Dissolving NaCl is nearly thermoneutral, slightly endothermic.

Your turn

1. One like the example

For CaCl2, use a lattice energy of −2258 kJ⁢/⁢mol and hydration enthalpies of −1616 kJ⁢/⁢mol for Ca2+ and −364 kJ⁢/⁢mol for Cl−. Find Δ⁢H⁢(soln), and say whether the solution warms or cools.

Show the answer and explanation

−86 kJ⁢/⁢mol, so it warms.

Δ⁢H⁢(solute) =+2258 kJ⁢/⁢mol. Hydration counts two chloride ions, −1616+2⁢(−364) =−2344 kJ⁢/⁢mol. The sum is 2258+(−2344) =−86 kJ⁢/⁢mol. Dissolving releases heat, which is why CaCl2 is used in hot packs and to melt ice.

−1616kJ/mol+2⁢(−364kJ/mol)=−2344kJ/mol2258kJ/mol+(−2344kJ/mol)=−86kJ/mol
−1616kJ/mol+2⁢(−364kJ/mol)=−2344kJ/mol2258kJ/mol+(−2344kJ/mol)=−86kJ/mol

2. A variation

For KBr, a table gives Δ⁢H⁢(soln)=+19.9 kJ⁢/⁢mol and a lattice energy of −671 kJ⁢/⁢mol. What is the combined hydration enthalpy of K+ and Br−?

Show the answer and explanation

−651 kJ⁢/⁢mol.

This time the hydration term is the unknown. Solve the cycle for it before putting in numbers, Δ⁢H⁢(hydration) =Δ⁢H⁢(soln)+Δ⁢H⁢(lattice). Then 19.9+(−671) =−651 kJ⁢/⁢mol. It is slightly smaller in size than the lattice cost, which is why KBr cools the water a little.

ΔHsoln=−ΔHlattice+ΔHhydrationΔHhydration=ΔHsoln+ΔHlatticeΔHsoln=19.9kJ/molΔHlattice=−671kJ/molΔHhydration=19.9kJ/mol+(−671kJ/mol)=−651kJ/mol
ΔHsoln=−ΔHlattice+ΔHhydrationΔHhydration=ΔHsoln+ΔHlatticeΔHsoln=19.9kJ/molΔHlattice=−671kJ/molΔHhydration=19.9kJ/mol+(−671kJ/mol)=−651kJ/mol

3. Somewhere new

5.00 g of CaCl2 (Δ⁢H⁢(soln)=−86 kJ⁢/⁢mol, from the first item) dissolves in 100.0 g of water. About how much does the temperature rise? Take c=4.184 J⁢/⁢(g⋅°⁢C) for the solution and assume no heat is lost.

Show the answer and explanation

About 8.8 °⁢C.

5.00 g÷110.98 g/⁢mol =0.04505 mol. The dissolving releases 0.04505×86=3.874 kJ, which is 3874 J and good to two figures. The 105.0 g of solution absorbs it, so Δ⁢T=3874÷(105.0×4.184) =8.8 °⁢C.

5.00gCaCl2×1molCaCl2110.98gCaCl2=0.04505molCaCl2(0.04505mol)⁢(86kJ/mol)=3.874kJ3874J(105.0g)⁢(4.184Jg−1∘C−1)=8.8∘C
5.00gCaCl2×1molCaCl2110.98gCaCl2=0.04505molCaCl2(0.04505mol)⁢(86kJ/mol)=3.874kJ3874J(105.0g)⁢(4.184Jg−1∘C−1)=8.8∘C

Keep exploring

Open the CaCl2 cycle of the first practice item in Energy diagrams and watch Δ⁢H⁢(soln) come out at −86 kJ⁢/⁢mol. Then set the chloride count to 1 and see how far one missing ion moves it.

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Study the 7 key terms Build the CaCl2 cycle in Energy diagrams Try the three-step model Check the cycle in a Chemistry box Open worked example on a board Chemistry formulas: energy and thermodynamics

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