The formation of [32P]pyrophosphate from acetyl phosphate and [32P]orthophosphate was studied under conditions in which phosphate-metal salts or acetyl phosphate-metal salts precipitate. In the absence of precipitates in purely aqueous media, the initial rate constant of transphosphorylation (kobs) was extremely small and the formation of pyrophosphate was detected only in the presence of calcium. In various combinations, conditions such as high pH, high concentrations of reactants, and the presence of dimethyl sulfoxide caused three types of precipitates to form. In completely aqueous solution with an excess of orthophosphate, the crystals formed at high pH contained 3 mol of calcium for 2 mol of phosphate and they were poorly effective at promoting phosphorolysis. In the presence of dimethyl sulfoxide, the ratio of calcium to phosphate in the sediment was 1:1 and phosphorolysis proceeded at a high rate. In either solvent, an excess of acetyl phosphate caused precipitation of a complex containing 1 mol of acetyl phosphate to 1 mol of calcium. In aqueous media the rate constant of phosphorolysis increased with increasing precipitation of the acetyl phosphate-calcium complex. With destabilization of the anions by dimethyl sulfoxide the increase in kobs for a given amount of acetyl phosphate-calcium precipitated was 200-fold higher. Magnesium did not form precipitates and was ineffective in promoting transphosphorylation in completely aqueous media, either in the presence of excess phosphate or in the presence of excess acetyl phosphate. However, when precipitation of phosphate-magnesium or acetyl phosphate-magnesium was promoted by addition of dimethyl sulfoxide, phosphorolysis was observed with rate constants as high as those found in the presence of calcium. These results indicate that phosphorolysis of acetyl phosphate occurs at higher rates on the surface of solid structures, through highly specific interactions involving acetyl phosphate, orthophosphate, and divalent cations.