Which ions were always soluble in your grid? (Group 1 cations and ammonium; nitrate.)
Which anions were usually insoluble, and with what exceptions? (Carbonate and phosphate are generally insoluble except with group 1 and ammonium.)
What was the general trend for sulfate salts? (Often soluble; notable insoluble exceptions include PbSO₄, BaSO₄, and frequently SrSO₄.)
What halide exceptions did you observe? (Ag⁺ and Pb²⁺ commonly form insoluble halides such as AgCl and PbI₂.)
How do ion charges relate to precipitation likelihood? (Higher charge magnitude increases lattice energy, favoring precipitation.)
In your observations, which rule takes precedence when rules seem to conflict—group 1/ammonium or anion insolubility? (Group 1 and ammonium solubility generally overrides anion insolubility.)
Write the net ionic equation for a magnesium precipitate you observed. (Example: Mg²⁺(aq) + CO₃²⁻(aq) → MgCO₃(s), if that pair precipitated in your data.)
Why are nitrate salts used as cation sources and sodium salts as anion sources? (Both nitrate and sodium/ammonium salts are typically soluble, ensuring the reacting ions are available in solution.)
What is the role of spectator ions in your total ionic equations? (They remain unchanged and are omitted from the net ionic equation.)
How could you reduce uncertainty in borderline cases? (Replicate trials, use clearer backgrounds, allow more settling time, or confirm in a test tube.)