A. Boughriet et al., COPRECIPITATION ACCUMULATION DISTRIBUTION OF MANGANESE AND IRON, AND ELECTROCHEMICAL CHARACTERISTICS OF MN IN CALCAREOUS SEAWATER, Fresenius' journal of analytical chemistry, 352(3-4), 1995, pp. 341-353
A study of manganese and iron associated with particulate matter in se
awaters derived from the English Channel (and North Sea). Sequential e
xtraction procedures have been used to identify geochemical processes
that govern Mn and Fe coprecipitation/accumulation/distribution in dif
ferent particulate phases (carbonate; FeMn(hydr)oxides; organic matter
and residual phase). The oxidation states of Mn and Fe, some mechanis
ms of bonding and the magnetic characteristics of particles have been
investigated by Mossbauer spectroscopy, electron spin resonance(ESR) s
pectroscopy, and mass susceptibility balance. The effect of pH and red
ox potential on stability of different dissolved and particulate Mn sp
ecies was also examined. In the these calcareous seawaters, manganese
(II) is predominantly bound to the carbonate phase (calcite) in the fo
rm of MnxCa1-xCO3. However the persistent occurrence of Mn in oxidatio
n states > 2 in these particles has suggested the existence of mangane
se(III) in the polymeric FeOOH structures as an ''intermediate'' entit
y during Mn(II) oxidation in the sea. The activity coefficient of the
entity ''MnOOH'' in FeOOH has been evaluated and p epsilon-pH diagrams
of Mn have been proposed under marine conditions.