Geology Reference
In-Depth Information
M
31
(aq)
,M(OH)
21
(aq)
,M(OH)
2
1
(aq)
,M(OH)
3
0
(aq)
,andM(OH)
4
(aq)
are
the hydrolysis products for many M
III
cations (see Section 3.2.3.2).
M
31
(aq)
is generally found at low pH and only at extremely high pH is
M(OH)
4
formed. The dependence of Cr
III
hydrolysis reactions on pH is
illustrated in Example 3.8.
Example 3.8: Determination of Cr
III
speciation in an aqueous solution at
pH 1, 6, and 11. Use
{
Cr
III
T
} ¼
10
6
mol L
1
and log*b
1
¼
4.00,
log*b
2
¼
9.62, log*b
3
¼
16.75, and log*b
4
¼
27.77. Assume that no
Cr(OH)
3
is precipitated, i.e. homogeneous solution, and that inorganic
and organic ligands are absent.
Cr
3
þ
þ
H
2
O
Ð
CrOH
2
þ
þ
H
þ
b
1
Cr
3
þ
þ
2H
2
O
Ð
Cr
ð
OH
Þ
2
þ
2H
þ
b
2
Cr
3
þ
þ
3H
2
O
Ð
Cr
ð
OH
Þ
3
þ
3H
þ
b
3
Cr
3
þ
þ
4H
2
O
Ð
Cr
ð
OH
Þ
4
þ
4H
þ
b
4
f
Cr
II
T
g¼f
Cr
3
þ
gþf
CrOH
2
þ
gþf
Cr
ð
OH
Þ
2
gþf
Cr
ð
OH
Þ
3
g
þf
Cr
ð
OH
Þ
4
g¼
10
6
mol L
1
¼f
Cr
3
þ
gð
1
þ
b
1
=f
H
þ
gþ
b
2
=f
H
þ
g
2
þ
b
3
=f
H
þ
g
3
þ
b
4
=f
H
þ
g
4
Þ
This equation can be solved for {Cr
31
} at various pH values by using
the equilibrium constants for each of the four equilibria above,
e.g. at pH 2, {Cr
31
}
¼
9.90
10
7
mol L
1
.
The concentrations of all other species can be calculated using {Cr
31
}
at each selected pH value,
e.g. at pH 2, {CrOH
21
}
¼
(*b
1
/{H
1
}) {Cr
31
}
¼
0.01
9.90
10
7
¼
9.90
10
9
mol L
1
.
Plotting
log{}against pH illustrates that the dominant species of
Cr
III
are Cr
31
, Cr(OH)
2
1
, and Cr(OH)
4
at pH 1, 6, and 11,
respectively. Alternatively, the same information may be presented
in a plot of mole fraction, w, against pH. The mole fractions can be
obtained by dividing species activity by the total activity of Cr
III
, e.g.
w
Cr31
¼
{Cr
31
}/{Cr
III
T
}.