(Supplement to part 3). On the manganese content of evaporating salt.
The Mn contents of various home product salt were determined colorimetrically by the periodate method after being collected by coprecipitation with ferric hydroxide.
Analysis showed that the Mn content of 12 samples is far little than that of the solar salt (8.3 p.p.m. on the average as reported already), and lies from 0.5 to 1.67p.p.m.(0.80p.p.m. on the avevage).
The manganese is distributed rather in the insoluble matter than the water soluble part.
(part 4). Colorimetric determination of iron in common salt with O-Phenanthroline.
Colorimetric determination of iron with O-Phenanthroline were made on the analysis of common salt, and the following results were obtained.
(1) This method is superior to the thiocyanate method as the color is stable and the procedure is simple.
(2) Iron in common salt can be determined directly as little as few microgram.
(3) Iron content and the tendency of distribution between the water soluble and the insoluble part of common salts was similar to the results already reported in this journal.
(part 5) On the lead content of common salt.
The lead contents of various solar and evaporating salt were determined colorimetrically by the dithizone method.
It was found that the Pb content of solar salt variedl from 0.4 to 7.1p.p.m.(2.3p.p.m. on the average of 17 samples), and lead is distributed mostly in the water soluble part.
The Pb content of evaporating salt manufactured in Japan is far little and is varied from 0.1 to 1.7p.p.m.(0.47p.p.m. on the average of 14 samples) and lead is distributed similarly both in soluble and insoluble matter.
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