39
-LOI
O)
20
40
60
mmm|
%
Ill
m I
a. Laaffe~
-I0
%1
20
",
40
6O
86
"
80
o 2 4 6 8 lOO
i
" -I0)
,
...-- 01
9
9
E 20
m ~
40
9
~: 60
"
r-,,
80
-I0
0
20
40
60
80
0
2
4
6
8 10 0
1
-10
0
20
40
60
mm a
2
3
4 -2
-I0
0 9
20
40
60
80 L--_..~ 9 :
0
2
b. Kochendorf
-i0,
9
01
9
i
9
201
i N
9
401
:
i
!
80i
2
3
4 -2
c. Wieblingen
0
2
I II
.'..,
80
t
80
,
0
2
4
6
8 lO 0
1
2
-IC
2C
4c
8C
Ca2+(mM)
4 -2
0
2
4
Saturation Index (SI)
M g 2+ ( m M )
o calcite' m dolomite 9 m n g ~ i t e
Fig. 4.13. Dissolved Ca :+, Mg '§ and SI of their minerals in the porewater of the Neckar River
-LOI
O)
20
40
60
mmm|
%
Ill
m I
a. Laaffe~
-I0
%1
20
",
40
6O
86
"
80
o 2 4 6 8 lOO
i
" -I0)
,
...-- 01
9
9
E 20
m ~
40
9
~: 60
"
r-,,
80
-I0
0
20
40
60
80
0
2
4
6
8 10 0
1
-10
0
20
40
60
mm a
2
3
4 -2
-I0
0 9
20
40
60
80 L--_..~ 9 :
0
2
b. Kochendorf
-i0,
9
01
9
i
9
201
i N
9
401
:
i
!
80i
2
3
4 -2
c. Wieblingen
0
2
I II
.'..,
80
t
80
,
0
2
4
6
8 lO 0
1
2
-IC
2C
4c
8C
Ca2+(mM)
4 -2
0
2
4
Saturation Index (SI)
M g 2+ ( m M )
o calcite' m dolomite 9 m n g ~ i t e
Fig. 4.13. Dissolved Ca :+, Mg '§ and SI of their minerals in the porewater of the Neckar River