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publications > paper > characterization of suspended particles in Everglades wetlands

Characterization of suspended particles in Everglades wetlands

Gregory B. Noe1 and Judson W. Harvey
U.S. Geological Survey, 430 National Center, Reston, Virginia 20192

James E. Saiers
School of Forestry and Environmental Studies, Yale University, 205 Prospect Street, New Haven, Connecticut 06511-2189

1 Corresponding author (gnoe@usgs.gov; tel: 703-648-5826; fax: 703-648-5484).

©2007, by the American Society of Limnology and Oceanography, Inc. Posted here with permission; Limnol. Oceanogr., 52(3), 2007, 1166-1178.

A PDF version of this entire publication is available for download (3.5 MB) from the Water Resources of the United States website. You will need the free Adobe Acrobat Reader in order to view this file.

Abstract

We report the concentration, phosphorus (P) and nitrogen (N) content, and size and chemical fractionation of fine suspended particles (0.2-100 µm) and colloids (3 kilodalton [kDa]-0.1 µm) in the surface water of Everglades wetlands along regional and P-enrichment gradients. Total suspended sediment concentrations ranged from 0.7 to 2.7 mg L-1. Total particulate P concentrations increased from 0.05 µmol L-1 to 0.31 µmol L-1 along the P-enrichment gradient. Particles contained from 20% to 43% of total P but <12% of total N in surface water. Dissolved (<0.2 µm) organic N contained about 90% of total N, with the 3-100-kDa colloidal size class containing the most N of any size class. The 0.45-2.7-µm size fraction held the most particulate P at all sites, whereas particulate N was most abundant in the 2.7-10-µm size class at most sites. Standard chemical fractionation of particles identified acid-hydrolyzable P as the most abundant species of particulate P, with little reactive or refractory organic P. Sequential chemical extraction revealed that about 65% of total particulate P was microbial, while about 25% was associated with humic and fulvic organic matter. The size and chemical fractionation information suggested that P-rich particles mostly consisted of suspended bacteria. Suspended particles in Everglades wetlands were small in size and had low concentrations, yet they stored a large proportion of surface-water P in intermediately reactive forms, but they held little N.

false-color satellite image of the Everglades and south Florida showing the locations of the sampling sites and individual photos of each sampling site
Figure 1. False-color satellite image of the Everglades and south Florida showing the locations of the sampling sites and individual photos of each sampling site. Generalized flow direction is shown as an arrow on the satellite image. [larger version]


Related information:

SOFIA Project: Effect of Water Flow on Transport of Solutes, Suspended Particles, and Particle-Associated Nutrients in the Everglades Ridge and Slough Landscape



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