BIOGEOCHEMICAL TRANSFORMATIONS OF FE AND MN IN OXIC GROUNDWATER AND WELL WATER ENVIRONMENTS

Citation
L. Tuhela et al., BIOGEOCHEMICAL TRANSFORMATIONS OF FE AND MN IN OXIC GROUNDWATER AND WELL WATER ENVIRONMENTS, Journal of environmental science and health. Part A: Environmental science and engineering, 32(2), 1997, pp. 407-426
Citations number
65
Categorie Soggetti
Environmental Sciences","Engineering, Environmental
ISSN journal
10934529
Volume
32
Issue
2
Year of publication
1997
Pages
407 - 426
Database
ISI
SICI code
1093-4529(1997)32:2<407:BTOFAM>2.0.ZU;2-M
Abstract
This review presents an overview of the oxidation and precipitation of dissolved Fe(II) and Mn(II) in groundwater when exposed to surface co nditions. In water wells, these transformations may eventually result in biofouling problems and deterioration of water quality. Fe(II)-oxid ation products include poorly-ordered Fe(II)-oxides such as ferrihydri te which may be converted via solution to Fe(II)-oxyhydroxides (e.g., goethite) with time. Among Mn-oxides, a typical oxidation product is b irnessite which is structurally analogous to poorly-ordered ferrihydri te. Bacteria implicated in Fe- or Mn-oxidation in neutral-pH environme nts include Gallionella, Sphaerotilus, Leptothrix, Metallogenium, Pedo microbium spp., and magnetotactic bacteria. Very little information is available on the genera Crenothrix, Clonothrix, Toxothrix, and Sidero capsa, This review focuses on the stalked and sheathed bacteria Gallio nella, Leptothrix, and Sphaerotilus.