An ICE (Initial, Change, Equilibrium) table is a systematic way to track the concentrations of species in an equilibrium reaction.
For the ionization of hydrazoic acid, the table helps understand the changes each component undergoes as the reaction progresses towards equilibrium.
Here's how it is set up:
- Initial: Start with the initial concentrations of \( \mathrm{HN}_3 \), \( \mathrm{H}^+ \), and \( \mathrm{N}_3^- \). Initially, \([\mathrm{H}^+]\) and \([\mathrm{N}_3^-]\) are zero because no reaction has occurred yet.
- Change: As the reaction progresses, \( \mathrm{HN}_3 \) decreases by \( x \), while \( \mathrm{H}^+ \) and \( \mathrm{N}_3^- \) increase by \( x \).
- Equilibrium: By the time equilibrium is established, the concentrations are \([\mathrm{HN}_3]+x\), \([\mathrm{H}^+]-x\), and \([\mathrm{N}_3^-]-x\).
Using the ICE table, you can substitute these values into the equilibrium expression for \( K_a \), and solve for \( x \). This approach simplifies the computation of percent ionization and helps verify assumptions in weak acid equilibrium calculations.