W. Huanxin et al., DISTRIBUTION AND SOURCES OF PHOSPHORUS IN TIDAL RIVER SEDIMENTS IN THE WASHINGTON, DC, AREA, Environmental geology, 30(3-4), 1997, pp. 224-230
Citations number
31
Categorie Soggetti
Water Resources","Environmental Sciences","Geosciences, Interdisciplinary
Sediments in the rivers and basins around Washington, DC, have high co
ncentrations of phosphorus, which, based on geographic distributions i
s largely derived from urban runoff and municipal sewage. Dissolved-pa
rticulate phosphate exchange reactions adn biological uptake of dissol
ved phosphorus from the water column may be an added source of phospho
rus to the sediments. Concentrations of total sedimentary phosphorus r
anged form 24 to 56 mu m P/g-dw, and were highest in areas near combin
ed sewer outfalls. As a part of this study, sedimentary phosphorus was
fractionated into Fe-P, Ca-P, Al-P, and organic phases using a select
ive-sequential leaching procedure. The distribution of the phases in a
ll sediments analyzed follow the order, Fe-P > Ca-P > Al-P. Spatial va
riations in the amounts of phosphorus in the different phases is relat
ed to the sources of phosphorus to the area. The proportions of occlud
ed Al-P and organic P are 10-20% of the total P, respectively. This su
ggests that phosphorus from natural sources is small compared to anthr
opogenic inputs in this area. The high leachable Fe-P and Ca-P in thes
e sediments might contribute a substantial amount of P to the water co
lumn under conditions of remobilization.