To investigate how temperature affects the solubility of calcium hydroxide (Ca(OH)₂) and to determine its thermodynamic properties (ΔH°, ΔS°, and ΔG°) by measuring the solubility product (Ksp) at different temperatures through acid-base titration.
Prepare saturated Ca(OH)₂ solutions at low, room, and high temperatures.
Perform titrations using standardized HCl to determine OH⁻ concentration.
Calculate Ksp at each temperature from ion concentrations.
Use Ksp values to determine ΔG°, and create a ΔG° vs. T plot.
Use LINEST in Excel to derive ΔH° and ΔS° from the plot.
Understand the relationship between solubility, temperature, and thermodynamics.
Apply Le Chatelier’s principle to predict solubility changes.
Analyze dissolution using ΔG = ΔH - TΔS and ΔG = -RTlnK.
Interpret the signs and magnitudes of ΔH° and ΔS° in relation to solubility trends.
Ca(OH)₂ Dissolution Reaction:
Ca(OH)₂ (s) ⇌ Ca²⁺ (aq) + 2 OH⁻ (aq)
The solubility of Ca(OH)₂ varies with temperature.
Solubility Product (Ksp):
Ksp=[Ca2+][OH−]2K_{sp} = [Ca^{2+}][OH^-]^2Ksp=[Ca2+][OH−]2
Thermodynamics Connection:
ΔG° = –RT ln K
ΔG° = ΔH° – TΔS°
A plot of ΔG° vs. T yields a line with slope = –ΔS° and y-intercept = ΔH°.
Predicting Behavior:
If dissolution is exothermic, increasing temperature decreases solubility.
If endothermic, increasing temperature increases solubility.
Dissolution increases disorder (ΔS° > 0).
Preparation of Saturated Solutions:
Dissolve ~0.5 g of Ca(OH)₂ in 50 mL DI water at three temperatures: ice bath (~5–10°C), room temp, and boiling (~100°C).
Stir each solution for 5–10 min to allow saturation.
Filtration:
Filter 40–50 mL of each solution using pre-wetted filter paper (with saturated solution, not water).
Keep filtered low-temp solution in ice bath to prevent solubility changes.
Titration:
Titrate 10 mL of each filtered solution with <1 M standardized HCl using bromothymol blue.
End point: green (neutral). Indicator turns yellow (acid) beyond equivalence.
Perform 2–3 titrations per solution to ensure accuracy.
Calculate [OH⁻] from the volume of HCl used and its concentration.
Calculate [Ca²⁺] using the 1:2 molar ratio from the dissolution equation.
Determine Ksp using Ksp=[Ca2+][OH−]2K_{sp} = [Ca^{2+}][OH^-]^2Ksp=[Ca2+][OH−]2.
Calculate ΔG° for each temperature:
ΔG∘=−RTlnKsp\Delta G^\circ = -RT \ln K_{sp}ΔG∘=−RTlnKsp
Graphical Analysis:
Plot ΔG° (y-axis) vs. Temperature in K (x-axis).
Use LINEST in Excel to determine slope (–ΔS°) and intercept (ΔH°).
Calculate ΔG° and Ksp at 25°C using derived values.
Compare to Theoretical Values:
Use thermodynamic tables (e.g., Tro Table 18.2) to find literature values of ΔH°, ΔS°, and Ksp.
Calculate % error for your results.
Discussion Points:
Did ΔH° and ΔS° match expected signs and values?
Explain how solubility changes with temperature and why titrating cold solutions must occur in an ice bath.
Assess the spontaneity of dissolution at different temperatures using ΔG°.