DocumentCode :
497046
Title :
Study on the Phosphorus Immobility of the Re-suspended Sediments
Author :
Li Dapeng ; Huang Yong
Author_Institution :
Dept. of Environ. Sci. & Eng., Suzhou Univ. of Sci. & Technol., Suzhou, China
Volume :
1
fYear :
2009
fDate :
4-5 July 2009
Firstpage :
97
Lastpage :
100
Abstract :
The variation of EPC0s of the re-suspended sediments is studied and the relationship between the distribution of phosphorus forms and EPC0s of sediments is investigated. Results of this study show that sediment re-suspension could promote phosphorus migration from overlying water to the sediments. The EPC0 of the re-suspended sediments reduced evidently from 0.069 mgldrL-1 (the initial state) to 0.034 mgldrL-1, whereas the values of the sediments without re-suspension increased slightly from 0.069 mgldrL-1 (the initial state) to 0.071 mgldrL-1 (the control experiment) and 0.073 mgldrL-1 (aerating to water), respectively. The EPC0s of the sediments had remarkable positive correlation with the concentrations of various phosphorus forms (BD-P+Al-P+NaOH-nrP) in those sediments except for the re-suspended sediments. It was suggested that the characteristics of BD-P, Al-P and NaOH-nrP formed under sediment re-suspension was different evidently from the initial state.
Keywords :
environmental factors; phosphorus; sediments; water quality; P; equilibrium phosphate concentration; phosphorus distribution; phosphorus immobility; phosphorus migration; resuspended sediment EPC0 variation; resuspended sediments; Chemicals; Containers; Data mining; Electronics packaging; Irrigation; Laboratories; Sampling methods; Sediments; Soil measurements; Water storage; equilibrium phosphate concentration (EPC0); immobility; sediment re-suspension;
fLanguage :
English
Publisher :
ieee
Conference_Titel :
Environmental Science and Information Application Technology, 2009. ESIAT 2009. International Conference on
Conference_Location :
Wuhan
Print_ISBN :
978-0-7695-3682-8
Type :
conf
DOI :
10.1109/ESIAT.2009.304
Filename :
5200073
Link To Document :
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