2001
DOI: 10.1007/s102010170018
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Geochemical processes of iron and manganese in a seasonally stratified lake affected by coal-mining drainage in China

Abstract: Lake water, pore water, and sediments were sampled in a seasonally stratified lake affected by coalmining drainage. Contrasting geochemical processes of iron and manganese in summer were investigated by studying the seasonal distributions of iron and manganese species in the water column, pore water, and sediments. The results show that iron buildup in the water during summer was mainly from the gradual dissolution of particulate matter due to the pH decrease, whereas manganese oxide reduction and manganese-bo… Show more

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Cited by 6 publications
(4 citation statements)
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“…In terms of spatial and temporal variations in metals concentrations, a number of studies confirmed that the process of thermal stratification has a strong influence on their dynamics (Hudson & Morel 1993;Wu et al 2001;Vasconcelos et al 2002). Namely, redox sensitive elements such as Fe, Mn and Cu exhibit seasonal changes resulting from changes in oxidizing and reducing conditions in lakes and reservoirs that stratify in summer.…”
Section: Dynamics Of the Limnological Characteristicsmentioning
confidence: 89%
“…In terms of spatial and temporal variations in metals concentrations, a number of studies confirmed that the process of thermal stratification has a strong influence on their dynamics (Hudson & Morel 1993;Wu et al 2001;Vasconcelos et al 2002). Namely, redox sensitive elements such as Fe, Mn and Cu exhibit seasonal changes resulting from changes in oxidizing and reducing conditions in lakes and reservoirs that stratify in summer.…”
Section: Dynamics Of the Limnological Characteristicsmentioning
confidence: 89%
“…However, no surficial peaks were observed in the Fe and Mn profiles of Soledad core and it is therefore, very likely that hypoxic-reduced conditions prevail in the Soledad Lagoon sampling site. The lower Mn concentrations found at the surficial layers of the core in contrast to the highest concentrations of Fe, could be explained on the basis of preferential reduction of manganese oxides to iron oxides (Wu et al 2001), since Fe oxides reduction requires stronger reduction conditions (below +100 mV) than Mn oxides, which begin to reduce at values slightly below 250-300 mV (Presley and Trefry 1980). Another interesting feature to note is the decreasing trend of CaCO 3 concentrations observed in the upper layers of the Soledad core.…”
Section: Sediment Characterizationmentioning
confidence: 98%
“…Another interesting feature to note is the decreasing trend of CaCO 3 concentrations observed in the upper layers of the Soledad core. As Mn species in the sediments might include Mn-bound carbonates in the particulate matter, and they can be dissolved due to a decrease in pH, promoted by the gradual decay of organic matter in the sediments (as explained below), the Mn loss from the sediments might not only be a result of Mn oxides reduction, but also due to CaCO 3 dissolution (Wu et al 2001). …”
Section: Sediment Characterizationmentioning
confidence: 98%
“…In the sediment-water interface, under certain biogeochemical conditions, through a variety of microbial and physico-chemical processes (e.g., pH changes, microbial activities, sediment redox condition), the possibility of heavy metals in the sediment recycled back into the overlying water may be enhanced remarkably (Clark et al, 1998;Guo et al, 1997;Wu et al, 2001). Hence, the heavy metal polluted aquatic sediments may be seen as "time bombs" for future pollution of the overall ecosystem including overlying water quality.…”
Section: Introductionmentioning
confidence: 99%