CHAPTER 1 • Sea Water as an Electrolyte
6
5
4
.,
~
~
3
+"
' "
~
2
o ~r-=~-L ____ - L ____ ~ ____ ~ ____ ~L-_ ___ L -____ ~ ____ ~ ____ ~ ____ - L ____ ~
0.75 I
~
0.60
~ 0.45
~
~
~
- 0.30
0.15
0.00 o
2
4
6
(/(%0)
8
10
11
6
5
4
~
3;§
~
«
2
o
Fig. 1.S. The concentration of cations in the baltic estuary as a function of chlorinity (Millero 1996)
where gR is the grams of river salts. The values of gi for conservative elements can be
obtained from the measured values in the estuary (gE):
(gE - gsw) 19.374
g. =
!
19.374 - Cl(%o)
(1.11)
6
5
4
.,
~
~
3
+"
' "
~
2
o ~r-=~-L ____ - L ____ ~ ____ ~ ____ ~L-_ ___ L -____ ~ ____ ~ ____ ~ ____ - L ____ ~
0.75 I
~
0.60
~ 0.45
~
~
~
- 0.30
0.15
0.00 o
2
4
6
(/(%0)
8
10
11
6
5
4
~
3;§
~
«
2
o
Fig. 1.S. The concentration of cations in the baltic estuary as a function of chlorinity (Millero 1996)
where gR is the grams of river salts. The values of gi for conservative elements can be
obtained from the measured values in the estuary (gE):
(gE - gsw) 19.374
g. =
!
19.374 - Cl(%o)
(1.11)
