Explain why dissolution is a balance of competing effects
Combine lattice, hydration and entropy terms without claiming a universal dissolution sign.
Learning outcome: Combine lattice, hydration and entropy terms without claiming a universal dissolution sign.
Starting recap
Breaking solute interactions costs energy; new solute-solvent interactions release energy.
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A hypothetical salt has lattice cost 650 and hydration release 650 kJ/mol, with assigned positive entropy.
Open the experimentPredict
Must an endothermic dissolution be unfavorable?
Experiment
Compare equal cost/release with cost 700 and release 650, then reverse those values. Explain why a large computed ideal solubility is not automatically physically plausible.
Balance dissolution contributions
Worked teaching model · synthetic values · Hypothetical 1:1 salt, ideal activities and pure solid present; ΔS° dissolution assigned +50 J/(mol K), T=298.15 K. ΔH° is lattice cost minus hydration release. This two-term model does not predict real salts or make entropy universally positive.
Reset keeps your prediction, captures and practice history.
| Quantity | Value | Unit |
|---|---|---|
| Lattice cost | 650 | kJ/mol |
| Hydration contribution | -650 | kJ/mol |
| ΔH° dissolution | 0 | kJ/mol |
| ΔG° dissolution | -14.9075 | kJ/mol |
| log10 Ksp | 2.611681 | decade |
Products favored relative to the assigned standard state.
Small differences between large contributions control the result. Actual dissolution also depends on Q versus Ksp and inventory. Ideal 1:1 solubility s satisfies Ksp=(s/c°)² only with pure water, no common ion, and ideal activities; extremely large predicted s invalidates dilute-solution assumptions.
Predict before changing a control. Save two contrasting captures and explain what is held fixed. Displayed digits are calculation precision, not experimental uncertainty.
Products favored relative to the assigned standard state.
Small differences between large contributions control the result. Actual dissolution also depends on Q versus Ksp and inventory. Ideal 1:1 solubility s satisfies Ksp=(s/c°)² only with pure water, no common ion, and ideal activities; extremely large predicted s invalidates dilute-solution assumptions.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
Understand
Apply
Public practice checks a specific claim. It does not establish independent mastery.
Show your calculation or representation, explain the changed case, and separate the stated model from measured evidence. Combine lattice, hydration and entropy terms without claiming a universal dissolution sign.
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