I ' 58 QUANTITATIVE AGRICULTURAL AXALYMH I Heat about 25 gm of high-grade sodium bicarbonate in an elect ric oven j [ to 300° for three to five hours. A platinum dish is bc'.st for this purpoHf*. I < Cool the product in a desiccator and preserve in a tightly .stoppered hot lie. ! ], ' On a counterpoised glass weigh exactly 5.300 gm of the pure sodium car- ' ' bonate. Brush this into a dry funnel which rente in the nerk of a 5(X)-n; I \ volumetric flask. Jar most of the salt into the iia.sk and rin.se down the J | , remainder with distilled water. Remove the* funnel, gently agitate until ' the carbonate is dissolved, then dilute to the murk and rt.ix well. * Titration. — Fill two burettes with the respective solutions. Before ; \ • proceeding with the titrations, practice reading t he color changes a,s follows: 1 f , Place 100 cc of distilled water in a beaker and add a drop of methyl orange ! and 0.5 cc of carbonate solution. Drop in acid until'! he last drop changes ! ' the tint from yellow to pink. Now, drop in carbonate solution until tin? 'l yellow color reappears. Repeat the process until the color change can be 4 » observed when but one drop of cither solution is added. It will aid in thcs J next process if this solution is preserved and another prepared, the two I showing the two colors of methyl orange. These are set asid<* for comparison. "t Measure out exactly 25 cc of the sodium carbonate .solution into a ; beaker or Erlenmeyer flask, placed on a white, surface. Add a drop of I ' methyl orange and then carefully run in add solution from the other burette I f until one drop changes the color from yellow to pink. Record t he volume of ' I acid required to do this. In case the end point, has been overstepped, t I add 5 cc more of the carbonate solution to that already in the fla*k and [ I ; < continue the titration. Finally record the volumes of both carhoimte and I acid. I f I Since the carbonate solution was exactly fifth-normal, 1 «'<• is equivalent to ! < 0.007294 gm of hydrochloric acid. The concentration fin grains of H( 1 per cubic centimeter) of the titrated solution IK then " '"'' ••*» where \'f and Va are the volumes of carbonate and «cid, rcHpectively, t ,t ,., , .., . . . t . . * . to each other, and that of the original sample IH ' , r » where *S* * S \r a is the volume of sample used for the dilution. Gmwn />*r ruhir crnltmHcr may be converted into per cent by waif/hi by dividing by tin* specific gravity of the sample, measured at 20°. The nvnrutlUy of the* titrated ncid solu- tion is obtained, if desired, as in the case of «ilver nit rate Miiliif ion : ^ • 'r ...•< normality, Fa being the volume of acid equivalent to 25 re of t In- lift h-nor »i«I carbonate. For the original sample, normality - 1CX^ f^,2r>N . Volumetric, by Titration with Potassium Hydroxide. In the number of determmation.H of hydrochloric arid to !M* umd small, no advantage is gained by Urn UHCJ of standnnl | hydroxide. This m bccaunc th<» most sttfisfacfory nwtliod for Rtandardimtion of this nolution is by fitrafion apiinsf. an ari«I o n