Research paperOxidation products of Mn(II) in lake waters
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Cited by (63)
Oxygen
2023, Wetzel's Limnology: Lake and River Ecosystems, Fourth EditionCoupled 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 ReviewsCitation 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 GeochemistryCitation 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 ResearchCitation 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).