2007
DOI: 10.1016/j.desal.2006.05.058
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Preservation of water quality in accumulation Lake Rovni: the estimate of the emission of phosphorus from inundation area

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Cited by 11 publications
(18 citation statements)
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“…Exchangeable Al was determined by the titration method after Sokolov ( Jakovljevic et al 1985). Speciation of phosphorus was done using sequential extraction procedure: a modified Chang and Jackson method (Manojlovic et al 2007): step I -water soluble P (NH 4 Cl mol/L); step II -Al bound P (NH 4 F 0.5 mol/L); step III -Fe bound P (NaOH 0.1 mol/L); step IV -reducible P (Na dithionite, Na citrate 0.3 mol/L); step V -occluded P (NaOH 0.1 mol/L) and step VI -Ca bound P (H 2 SO 4 0.25 mol/L).…”
mentioning
confidence: 99%
“…Exchangeable Al was determined by the titration method after Sokolov ( Jakovljevic et al 1985). Speciation of phosphorus was done using sequential extraction procedure: a modified Chang and Jackson method (Manojlovic et al 2007): step I -water soluble P (NH 4 Cl mol/L); step II -Al bound P (NH 4 F 0.5 mol/L); step III -Fe bound P (NaOH 0.1 mol/L); step IV -reducible P (Na dithionite, Na citrate 0.3 mol/L); step V -occluded P (NaOH 0.1 mol/L) and step VI -Ca bound P (H 2 SO 4 0.25 mol/L).…”
mentioning
confidence: 99%
“…In acid mineral soils, such as Podzols, P is mostly retained by A l a n d F e o x i d e s b y the ligand exchange mechanism where the OH -or H 2 O groups of sesquioxides surfaces were are displaced by dihydrogenphosphate anions (Simard et al, 1995). In certain soils, this bound is not strictly confined to Al but can bound bind to Si, as well (Manojlovic, et al 2007). However, in the studied Stagnosol, the strong correlation of Al-P with Al extracted in the step 2 (Al II) could be attributed to carbonates and alumosilicates (r=0.998**).…”
Section: Fraction Of Soil P Extracted By 05m Nh 4 F Solution (Al Boumentioning
confidence: 99%
“…Fraction of soil P isolated by such a strong reagent may have a high content in soil and mainly is greater than that bound to Al (Manojlovic et al, 2007, Mustapha et al, 2007, ranging between few hundred mg per kilogram. From the chemistry viewpoint, such bounded P is characteristic for the slow-flowing processes involving formation of covalent Fe-P or Al-P bonds on Fe and Al oxide surfaces (Willett et al 1988) which can be an additional source of available P (Beck & Sanchez, 1994).…”
Section: Fraction Of Soil P Extracted By M Naoh Solution (Fe Bound P)mentioning
confidence: 99%
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