14
F. J. Millero
Ji0i~' ~CI- : 0' ' ~
Br' : ~ r::, (] 'r:;:;:]
_ 10'~ ____ ~ ____ ~ ____ - L _ _ _ _ ~ _ _ _ _ ~ _ _ _ _ _ _ L -_ _ _ _ i -____ ~ ____ ~
5 Ir-----,------.------r-----,------.------r-----,------.-----.
x
5
HCO;
I
'&
O~:ts:n __ A
A
~~-A __
~ - --6.-'....l....- -- -- -/:). -- -~
~
'0
Xl j
~
-s
10
L
o
•
•
-1 0 l
- 20 I- 30 I••
\
\
I
I
\
\
\
\
\
I
T
501_L
I
I
-
-
\- -- -- ~ -- -- --. -- -- -.------• •
••
-40 LI ----~------~----~----~--____ ~ _ _ _ _ ~ _ _ _ _ ~ _ _ _ _ _ _ ~ _ _ _ _ ~
20
40
60
80
100
(/(%0)
Fig. 1.11. The changes in the anions during the evaporation of Mexican lagoon waters
(Millero 2000a). The results as a function of temperature for the differences in the
measured densities and compressibilities and the calculated values shown in Table 1.3
agree to within 2 ppm and 0.006 ppm, respectively, in density and compressibility. The
measurements as a function of depth are compared to the calculated values in Fig. 1.14.
The increases in the density in the deep waters are due to the addition of nutrients