How to use (3 steps)
- Pick a mode: Ksp → solubility, solubility → Ksp, Q vs Ksp (precipitation test), or simple fractional precipitation.
- Enter the salt, stoichiometric coefficients, Ksp or solubility, and concentrations or volumes as needed.
- Compute to see solubility, Ksp, Q vs Ksp, and interval summaries. Copy the URL to share the exact setup.
Default examples use classic salts such as AgCl and CaF2 so that you can see results immediately and compare with textbook values.
Results
Mode: Ksp → solubility
In the Q vs Ksp mode we use Q = [cation]_mix^{ν_cation}[anion]_mix^{ν_anion} and compare it to Ksp. The summary below also shows log10 Q and pQ.
How it's calculated
- Steps will appear here after calculation.
Using the Ksp and precipitation modes
Use Ksp to solubility when you want the molar solubility of one salt in pure water. Use Q vs Ksp when you already know the mixed ion concentrations and need to decide whether a precipitate forms.
Suggested workflow
- Choose the mode that matches your question before editing concentrations.
- Enter stoichiometric coefficients exactly as written for the dissolving salt so the exponent pattern in Ksp is correct.
- After computing, read both the summary and the step log to confirm which quantity the page solved for.
What the fractional-precipitation view assumes
The shared-anion view compares two salts against the same free anion concentration. It is useful for classroom selectivity problems, but it does not model activity coefficients, ionic-strength corrections, or complex side equilibria.
Common mistakes to avoid
- Entering a concentration after mixing into the solubility mode, which expects Ksp and stoichiometry instead.
- Forgetting that Q and Ksp use powers from the dissolution stoichiometry, not just a simple product of concentrations.
- Comparing salts with different stoichiometries in the shared-anion range without checking whether the interpretation still matches your lesson.
See also
FAQ
Does this tool account for activities and ionic strength?
For simplicity, it treats activities as equal to molar concentrations and does not include activity coefficients or ionic-strength corrections. It is meant for teaching-level Ksp and precipitation exercises, not for precise analytical calculations.
Which salts and stoichiometries can I use?
The core formulas accept general ν_cation and ν_anion coefficients (for example 1:2 salts such as CaF₂), as long as you provide the correct stoichiometric coefficients and Ksp values. For fractional precipitation, the built-in explanation assumes simple 1:1 salts with a shared anion.
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