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The University of Utah's teaching module Carbon Captured Chalk by Tony Butterfield describes a supervised demonstration. Its Materials and Methods uses a balance, weighing boats, spatula, separate centrifuge tubes, a volume-measuring vessel and filter paper. Sodium carbonate and calcium chloride are dissolved separately in water before mixing. The reported readout is an initially opaque mixture followed by a milky dispersion of fine solid particles; filtration retains the chalk-like product, which is then dried. The module also proposes observing drops together on a slide using an optical microscope.^[ref]

The handout does not report blank trials. Useful additional controls would retain each starting chemical solution separately, mix each with water, and pass water alone through the same filter. A new solid only in the combined sample would support a mixing-dependent chemical reaction; these are proposed comparisons, not reported results. Residue from a filter blank would instead flag contamination.

Cloudiness plus a retained solid supports phase separation; appearance alone cannot establish composition, a particular crystal polymorph, quantitative yield or the solubility product. Fine solid particles may pass through a filter, and retained liquid can leave dissolved salts on drying. Identifying calcium carbonate needs additional chemical or structural evidence. The teaching source supplies no measured ion products, instrument-calibrated cloudiness series or equilibration test. Its concentrated demonstration therefore illustrates precipitation without validating the toy model's conditional constant or proving complete removal of dissolved calcium.

The ion product evaluates the same dissolved-ion thermodynamic activity product as the solubility product, but at the current composition rather than necessarily at chemical equilibrium. For AB, $Q_{\mathrm{sp}}=a_{\mathrm{A}}{a}_{\mathrm{B}}$; its concentration counterpart is $Q_c=c_{\mathrm{A}}{c}_{\mathrm{B}}$. Compare $Q_c$ with $K_{\mathrm{sp},c}$ only under compatible activity coefficient assumptions.^[ref]

For other stoichiometries, use the dissolution coefficients as powers: ${\mathrm{AB}}_2(s)\rightleftharpoons {\mathrm{A}}^{2+}(aq)+2{\mathrm{B}}^{-}(aq)$ gives $Q_{\mathrm{sp}}=a_{\mathrm{A}}{a}_{\mathrm{B}}^2$. A solubility product is not itself the molar concentration dissolved; even in the ideal AB model in pure water, that concentration is $\sqrt{K_{\mathrm{sp},c}}$.

A net ionic equation retains the chemical species changed by a chemical reaction and cancels spectator ions present unchanged on both sides. Dissolved strong electrolytes are represented by their separated ions, while a solid product retains its chemical formula. Cancellation preserves both elemental inventories and electric charge conservation.^[ref]

For the calcium carbonate example, the complete ionic account isCanceling the sodium cations and chloride anions yields the net ionic equation above. Neither cancellation nor the conventional sodium chloride formula implies that the remaining dissolved ions have become paired molecules.

For this schematic, let $\xi$ be the amount of substance of AB formed. With no competing chemical reactions or losses,Adding each dissolved inventory to its contribution in the solid recovers its initial total. Each dissolved pair has net electric charge zero, so transferring a pair into neutral AB also preserves electric charge conservation. This is a short stoichiometry argument; choosing the actual $\xi$ additionally needs chemical equilibrium or chemical kinetics information.

The solubility product is the equilibrium constant for dissolution of a specified solid into its dissolved ions. For a pure bulk AB solid at the chosen temperature, pressure and standard states,The pure bulk solid's thermodynamic activity is one in this convention. Coexisting solid and chemical solution at chemical equilibrium give this equality. If all available solid dissolves, the final chemical solution may instead be undersaturated; do not impose equality merely because a salt was initially added.^[ref]

Using the thermodynamic activity definition $a_i={\gamma }_i{c}_i/c^{\circ }$, with activity coefficients ${\gamma }_i$ and reference molar concentration $c^{\circ }$, gives the independent conversionThus $K_{\mathrm{sp}}$ is dimensionless, while the conditional concentration form $K_{\mathrm{sp},c}$ has units ${\mathrm{M}}^2$ for this one-to-one model. Treating $K_{\mathrm{sp},c}$ as constant requires a justified fixed or approximately fixed activity coefficient product. Changing ionic strength can change that product even at fixed temperature; changing temperature can change the equilibrium constant itself. Specify the solid thermodynamic phase too: different crystal polymorphs need not have the same solubility product.

A supersaturated solution has an ion product above the relevant solubility product. It can persist through metastability: nucleation must first create a sufficiently large new solid region. Added surfaces, impurities and mixing history can affect that barrier. Therefore a clear sample during a finite observation does not prove undersaturation, and visible cloudiness does not measure the ion product.