Elsevier

Chemical Geology

Volume 44, Issue 4, June 1984, Pages 359-383
Chemical Geology

Research paper
Oxidation products of Mn(II) in lake waters

https://doi.org/10.1016/0009-2541(84)90149-9Get rights and content

Abstract

Oxygenation of Mn(II)-rich water samples taken from two English lakes (Esthwaite Water, Cumbria, and Rostherne Mere, Cheshire) during the summer months caused the precipitation of Mn-oxide, the process being catalysed by particulate matter. The Mnoxide formed resembles vernadite (δ-MnO2) with regard to: (1) Mn oxidation state (> 3.6 in all but one case); and (2) its fine morphology (crumpled thin sheets) as determined by electron microscopy. The precipitates are, however, rather amorphous to X-rays, giving only very weak reflections which cannot be assigned unequivocally. Electron probe microanalysis shows the presence of a number of other elements in the Mn-containing phase. The most abundant is Ca (Ca/Mn weight ratio ⋍ 0.1), others are Mg, Si, P, S, Cl, K, Ba and Fe. The precipitates contain much organic matter (20–30 wt.%) but little appears to be associated directly with the Mn phase. Only small amounts (∼ 1 wt.%) of humic substances are present. Some but not all of the specimens examined had the gross morphology of Metallogenium, a Mn-depositing bacterium.

Naturally occurring Mn-oxides present in Esthwaite Water during the summer resemble, the products of oxygenation in their fine morphology and contents of other elements. Mn-oxides present during the winter are somewhat different morphologically. In one summer sample of particulate matter from Esthwaite Water no Mn-oxide could be found by electron microscopic examination, but Mn was found concentrated in bacteria. This observation, the rapid rates of oxidation and the high Mn oxidation states, suggest that bacteria might play a rôle in catalysing the oxidation of Mn(II).

References (54)

  • E. Tipping

    Adsorption by goethite (α-FeOOH) of humic substances from three different lakes

    Chem. Geol.

    (1981)
  • E. Tipping

    The adsorption of aquatic humic substances by iron oxides

    Geochim. Cosmochim. Acta

    (1981)
  • E. Tipping et al.

    The effects of adsorbed humic substances on the surface charge of goethite (α-FeOOH) in freshwaters

    Geochim. Cosmochim. Acta

    (1982)
  • E. Tipping et al.

    The adsorption of aquatic humic substances by two oxides of manganese

    Geochim. Cosmochim. Acta

    (1983)
  • E. Tipping et al.

    Iron oxide from a seasonally anoxic lake

    Geochim. Cosmochim. Acta

    (1981)
  • O. Bricker

    Some stability relations in the system Mn“O2“H2O at 25° and one atmosphere total pressure

    Am. Mineral.

    (1965)
  • S.M. Bromfield

    The properties of a biologically formed manganese oxide, its availability to oats and its solution by root washings

    Plant Soil

    (1958)
  • E. Callender et al.

    Freshwater ferromanganese deposits

  • T.R. Carrick et al.

    Concentrations of major ions in lakes and tarns of the English Lake District (1953–1978)

    Freshwater Biol. Assoc., Occas. Publ.

    (1982)
  • S.D. Chapnick et al.

    Microbially mediated manganese oxidation in a freshwater lake

    Limnol. Oceanogr.

    (1982)
  • F.V. Chukhrov et al.

    Manganese minerals in clays: a review

    Clays Clay Miner.

    (1980)
  • W. Davison

    Sampling and handling procedures for the polarographic measurement of oxygen in hypolimnetic waters

    Freshwater Biol.

    (1977)
  • W. Davison

    The polarographic measurement of O2, Fe2+, Mn2+ and S2− in hypolimnetic water

    Limnol. Oceanogr.

    (1977)
  • W. Davison

    Supply of iron and manganese to an anoxic lake basin

    Nature (London)

    (1981)
  • W. Davison

    Transport of iron and manganese in relation to the shapes of their concentration—depth profiles

    Hydrobiologia

    (1982)
  • W. Davison et al.

    A study of the cycling of manganese and other elements in a seasonally anoxic lake, Rostherne Mere, U.K.

    Water Res.

    (1984)
  • W. Davison et al.

    Seasonal transformations and movements of iron in a productive English lake with deep-water anoxia

    Schweiz. Z. Hydrol.

    (1981)
  • Cited by (63)

    • Oxygen

      2023, Wetzel's Limnology: Lake and River Ecosystems, Fourth Edition
    • Coupled redox cycling of Fe and Mn in the environment: The complex interplay of solution species with Fe- and Mn-(oxyhydr)oxide crystallization and transformation

      2022, Earth-Science Reviews
      Citation Excerpt :

      The extensive deposit of MnOx covers 10–30% of the deep Pacific floor (Crerar and Barnes, 1974; Barrón and Torrent, 2013). Although the concentration of MnOx in the natural environment is one or two orders of magnitude lower than that of FeOx, they exert considerable geochemical influences as efficient scavengers of many elements and strong oxidants (Tipping et al., 1984; Usui and Someya, 1997; Müller et al., 2002; Hochella et al., 2005b; Johnson et al., 2015). Mn generally occurs in three different oxidation states (i.e., +2, +3, +4) in the environment, giving rise to a variety of multivalent phases (more than 30) (Post, 1999; Yang et al., 2021).

    • Texture, mineralogy and geochemistry of late Quaternary sediments of the Mahi River basin, western India: Implications to climate and tectonics

      2021, Applied Geochemistry
      Citation Excerpt :

      However, converted to less mobile manganese oxides on the soil-water system's increased pH or oxidation level (Lindsay, 1972). Further, despite its large surface area and surface chemistry (negative surface charge at near-neutral pH), MnO is less suitable for phosphorous sorption than for Fe oxides (Kawashima et al., 1986; Tipping et al., 1984; Yao and Millero, 1996) and to a more significant extent supported by the FeOt and P2O5 concentration variation (not shown in Fig. 4). The positive correlation between MgO and CaO considered an established phenomenon (Daly, 1909; Van Moort, 1973; Veizer, 1978).

    • Effectiveness of hypolimnetic oxygenation for preventing accumulation of Fe and Mn in a drinking water reservoir

      2016, Water Research
      Citation Excerpt :

      However, under similar conditions the half-time for soluble Mn can be > 1 year (Morgan, 1967). Soluble Mn oxidation occurs much faster in oxic lake water than observed under abiotic conditions, with several studies observing soluble Mn oxidation half-times between 1 and 30 days at pH between 6.5 and 8.4 (Chapnick et al., 1982; Diem and Stumm, 1984; Kawashima et al., 1988; Tipping et al., 1984). Chapnick et al. (1982) and Diem and Stumm (1984) identified Mn-oxidizing organisms in the reservoir water and showed that when these organisms were removed by filtration, Mn oxidation was negligible within the duration of their incubation experiments (10–30 days).

    View all citing articles on Scopus
    View full text