The ICE table is a useful tool for organizing and calculating the concentrations of species at initial, change, and equilibrium stages in chemical reactions. It stands for Initial, Change, and Equilibrium - the three stages that describe the quantitative progression of a reaction over time.
To set up an ICE table for an acid like monochloroacetic acid, you list the species involved in its dissociation, typically the undissociated acid, the hydrogen ion, and the conjugate base.
Here's how each step works:
- **Initial (I):** Record the starting concentrations before any reaction occurs.
- **Change (C):** Determine the change in concentration, usually represented by \( x \), as the system moves towards equilibrium.
- **Equilibrium (E):** Represent the final concentrations after the reaction has reached equilibrium, often a function of the initial concentrations and \( x \).
This structured approach makes it easier to form an equation based on the dissociation reaction, utilizing the \( K_a \) to relate these concentrations. By solving this equation, you determine \( x \), which then allows you to calculate properties such as pH, reflecting the solution's acidity.