COPRECIPITATION ACCUMULATION DISTRIBUTION OF MANGANESE AND IRON, AND ELECTROCHEMICAL CHARACTERISTICS OF MN IN CALCAREOUS SEAWATER

Citation
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
Citations number
74
Categorie Soggetti
Chemistry Analytical
ISSN journal
09370633
Volume
352
Issue
3-4
Year of publication
1995
Pages
341 - 353
Database
ISI
SICI code
0937-0633(1995)352:3-4<341:CADOMA>2.0.ZU;2-8
Abstract
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.