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Solubility and pH

General Chemistry • Solubility and Complex Ion Equilibria

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Solubility and pH — Hydroxide Salts

Analyze sparingly soluble hydroxides of the form M(OH)n(s) ⇌ Mn+(aq) + n OH(aq). This calculator can check precipitation at a chosen pH or pOH, or compute the threshold pH at which precipitation just begins. Pure water at 25 °C is assumed, so Kw = 1.0 × 10−14.

Recognized keys: mode, n, M, Ksp, M0, pKind, pVal, precision.

Hydroxide salt

Hydroxide stoichiometry n

Core inputs

Mode 1 — Check precipitation at a given pH or pOH

pH specification
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Frequently Asked Questions

How does pH affect the solubility of metal hydroxides?

Metal hydroxides dissolve to produce OH-, so changing [OH-] changes the ion product and the position of equilibrium. Higher pH (higher [OH-]) generally favors precipitation and lowers solubility.

What is Qsp and how is it used to predict precipitation?

Qsp is the ion product computed from current ion concentrations, using the same form as Ksp. If Qsp is greater than Ksp, the solution is supersaturated and precipitation is favored; if Qsp is less than Ksp, no precipitation is expected.

What is the threshold pH for precipitation?

The threshold pH is the pH at which precipitation just begins, meaning Qsp is approximately equal to Ksp. The calculator finds the critical [OH-] from Ksp and [M^n+]0, then converts it to pOH and pH at 25 C.

Why does the calculator assume pH + pOH = 14.00?

At 25 C, Kw is taken as 1.0 x 10^-14, so pKw = 14.00 and pH + pOH = 14.00 follows directly. If temperature changes, Kw can change and the relationship may differ.

Does this tool account for buffers or complex-ion formation?

No, pH is treated as an input value and the model focuses only on the hydroxide solubility equilibrium using concentrations. Effects such as buffering capacity, complex ions, or activity coefficients are not included.