2011
DOI: 10.1016/j.watres.2010.09.020
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Release of organic P forms from lake sediments

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Cited by 102 publications
(39 citation statements)
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“…Because of a relatively small water depth and a large water surface area, shallow lakes are particularly susceptible to eutrophication-induced algal bloom and water quality degradation [8][9][10]. For a shallow lake, the wind-induced shear stress on the lake surface can be efficiently transferred downward through the shallow water column to the lakebed, resuspending bed sediments from which nutrients can be released into the ambient water [11][12][13][14][15][16]. The threshold shear stress, beyond which the resuspension of bed sediments will incept, depends on the physiochemical characteristics (e.g., texture, age and compaction) of the sediments [17,18].…”
Section: Introductionmentioning
confidence: 99%
“…Because of a relatively small water depth and a large water surface area, shallow lakes are particularly susceptible to eutrophication-induced algal bloom and water quality degradation [8][9][10]. For a shallow lake, the wind-induced shear stress on the lake surface can be efficiently transferred downward through the shallow water column to the lakebed, resuspending bed sediments from which nutrients can be released into the ambient water [11][12][13][14][15][16]. The threshold shear stress, beyond which the resuspension of bed sediments will incept, depends on the physiochemical characteristics (e.g., texture, age and compaction) of the sediments [17,18].…”
Section: Introductionmentioning
confidence: 99%
“…Although this reduction was half what could be achieved, it could be much worse with a low Fe/P ratio -even below 10% [34][35]. The low DO level (Table 2) could be another factor that affects the low reduction in laboratory studies [34][35][36]. The efficiency measured during the field experiment was found to be similar (49%) to the lab results for 5% FeCl 3 (Table 3), despite the use of a higher FeCl 3 concentration.…”
Section: Discussionmentioning
confidence: 57%
“…Many studies have indicated that oxygen is the vital factor controlling P release in the sediment, which means the P generally has a higher release rate under anoxic conditions, via its effect on Fe (III) and Mn (IV) (Ahlgren et al 2011;Kraal et al 2013). There are also many researches indicated the dissolved oxygen (DO) is the vital environment factor for P release and burial (Ingall et al 1993;Sulu-Gambari et al 2015).…”
Section: Conceptual Model Of P Biogeochemical Cyclementioning
confidence: 99%