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Phosphate Chemistry in Lake Sediments
Author(s) -
Syers J. K.,
Harris R. F.,
Armstrong D. E.
Publication year - 1973
Publication title -
journal of environmental quality
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.888
H-Index - 171
eISSN - 1537-2537
pISSN - 0047-2425
DOI - 10.2134/jeq1973.00472425000200010001x
Subject(s) - sediment , eutrophication , environmental chemistry , sink (geography) , phosphate , sorption , water column , calcareous , desorption , environmental science , chemistry , geology , geochemistry , nutrient , oceanography , geomorphology , adsorption , paleontology , cartography , organic chemistry , geography
The amounts and forms of inorganic and organic phosphate (P) in lake sediments are discussed in relation to sediment composition and properties. The ability of noncalcareous and calcareous sediments to sorb and desorb added P in the laboratory and in the lake environment is interpreted in terms of the amounts and reactivities of sediment components involved in the sorption of P; emphasis is placed on the role of an Fe‐rich gel complex. Factors controlling the chemical mobility and biological availability of sediment inorganic and organic P are considered. Whether sediments act as a P source or sink is determined by sediment composition and limnological conditions. The factors involved in the interchange of P between the sediment interstitial water and the overlying water column are reviewed. The role of P in lake eutrophication is discussed briefly.