1) By minute micro-analysis, average content of Pb in the sea-water is found to be about 2γ/L.
2) By using ThB as radioactive indicator, the precipitation ratio of Ph salts in this analysis was determined in order to obtain accuracy of analysis value, and the salt effect on the sea-water was examined.
3) Deducing from the fact that Ph does not exist in brine, it was found that, alike Au and Ra, at the salt manufacturing process Ph is transferred into the deposited solid substance, and not into brine.
4) Under various presumption, a new method of determining the age of the ocean by the quantity of U and Pb (206) in the sea-water was proposed.
In conclusion, the writers express their hearty thanks to the Department of Education for bestowing the fund for the scientific research for a part of this research.
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