The beakers were cautiously heated over a free flame to drive off any remaining ammonium salts or organic matter. The soluble material was dissolved in distilled water and filtered into weighed 100-ml. tail-form beakers. A few milliliters of concentrated hydrochloric acid were added and the solutions evaporated to dryness. The residues were cautiously heated to dnve off any moisture, cooled, and weighed. The results obtained (total weight of sodium chloride plus potassium chloride) are tabulated in Table II.
DISCUSSIONPerhaps the most attractive feature of the J. Lawrence Smith method of silicate decomposition is the simultaneous removal of most of the nonalkali basic constituents. The hydrofluoricperchloric acid decomposition, as used above, accomplishes the same purpose. The perchlorates of magnesium, iron, and aluminum all form oxides upon thermal decomposition, thus rendering them insoluble. The sodium, potassium, and calcium salts, however, form soluble chlorides which can readily be dissolved away from the insoluble oxides. Inasmuch as the special equipment required for the hydrofluoric-perchloric acid decomposition is a platinum dish, and the operation of grinding an already weighed sample may be avoided, this method has certain advantages over the J. Lawrence Smith method.