ICE stands for
Initial,
Change, and
Equilibrium, and the method involves setting up a table to systematically calculate the equilibrium concentrations of all species in a reaction. It's a visual tool that helps clarify the step-by-step changes occurring in a reaction mixture.
Using an ICE table starts with noting the initial concentrations of reactants and products prior to any reaction occurring. Then, you denote the changes in concentrations as the reaction proceeds towards equilibrium, typically represented by variables like 'x'. Finally, you calculate the equilibrium concentrations.
For our problem where lead chloride dissolves in water:
- Initial concentrations of Pb²⁺ and Cl⁻ are known from the Pb(NO₃)₂ and KCl solutions provided.
- The change in concentrations is expressed in terms of 'x', corresponding to the number of moles of PbCl₂ that dissolve.
- Equilibrium concentrations involve the initial concentrations adjusted by these changes (subtracting 'x' for Pb²⁺ and '2x' for Cl⁻ due to the stoichiometry).
The ICE table provides a simple yet powerful way to visualize and solve for equilibrium conditions, especially when dealing with solubility equilibria as illustrated in our exercise.