An Introduction to Environmental Chemistry

(Rick Simeone) #1
eqn. 5.15
followed by the oxidation of ferrous iron (Fe(II)) to ferric iron (Fe(III)):

eqn. 5.16

Oxidation happens very slowly at the low pH values found in acid mine waters.
However, below pH 3.5 iron oxidation is catalysed (see Box 4.4) by the iron
bacterium Thiobacillus thiooxidans. At pH 3.5–4.5 oxidation is catalysed by
Metallogenium. Ferric iron may react further with pyrite:

41 Fe^2 O22l 048 H O Fe OH 3 H

Fe II Fe III

()aq g s aq
+
++() () ()()+ +()

()() ()()

158 Chapter Five


25

50

10

25

New York

Atlantic
Ocean

Gulf of
Mexico

Miami

10

50

Chicago

(b)^25

km

0 300

N

25

Fig. 5.7Cont.
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