1956 年 10 巻 2 号 p. 71-76
(1) The chlorine content and the percentage volume after concentrating have been calculated from the specific gravity of the water at various degree of concentration by the following formulas.
For the 1st part
S1=0.997968+0.012794.Cl1...(1)
For the 2nd part
S2=1.002943+0.011830.Cl2...(2)
For the 3rd part
S3=1.011613+0.010865.Cl3...(3)
For the 1st part
C1=172.21/(78.16041.S1-78.00159)...(4)
For the 2nd part
C2=172.21/(84.53013.S2-84.77891)...(5)
For the 3rd part
C3=172.21/(92.03611.Sa-93.10493)...(6)
where Sn=Ihe specific gravity of water
Cla=The chlorine content in grams per 100cc of water
Cl=100 Clo/Cln=The percentage volume after concentrating
Clo=The chlorine content of sea water=1.7221g/100cc in table 2.
Estimation has been made within the limits of concentration from the sea water to the water concentrated up to saturation with NaCl. Tabulation is as table 1 and 2.
(2) dC/dS has been calculated from the above formulas (4),(5) and (6), and tabulated in table 3 (Fig. 1). From these results the relation between the specific gravity and the percentage volume after concentrating may be observed.
(3) The point at which sea water becomes saturate with NaCl by concentrating has been estimated as follows S=1.2159, Cl=18.804.