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Advection, dispersion, and filtration of fine particles within emergent vegetation of the Florida Everglades
Author(s) -
Huang Yong H.,
Saiers James E.,
Harvey Judson W.,
Noe Gregory B.,
Mylon Steven
Publication year - 2008
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2007wr006290
Subject(s) - advection , wetland , hydrology (agriculture) , environmental science , ridge , particulates , particle (ecology) , dispersion (optics) , vegetation (pathology) , surface water , filtration (mathematics) , soil science , atmospheric sciences , geology , ecology , environmental engineering , oceanography , geotechnical engineering , physics , medicine , statistics , mathematics , pathology , optics , thermodynamics , paleontology , biology
The movement of particulate matter within wetland surface waters affects nutrient cycling, contaminant mobility, and the evolution of the wetland landscape. Despite the importance of particle transport in influencing wetland form and function, there are few data sets that illuminate, in a quantitative way, the transport behavior of particulate matter within surface waters containing emergent vegetation. We report observations from experiments on the transport of 1 μ m latex microspheres at a wetland field site located in Water Conservation Area 3A of the Florida Everglades. The experiments involved line source injections of particles inside two 4.8‐m‐long surface water flumes constructed within a transition zone between an Eleocharis slough and Cladium jamaicense ridge and within a Cladium jamaicense ridge. We compared the measurements of particle transport to calculations of two‐dimensional advection‐dispersion model that accounted for a linear increase in water velocities with elevation above the ground surface. The results of this analysis revealed that particle spreading by longitudinal and vertical dispersion was substantially greater in the ridge than within the transition zone and that particle capture by aquatic vegetation lowered surface water particle concentrations and, at least for the timescale of our experiments, could be represented as an irreversible, first‐order kinetics process. We found generally good agreement between our field‐based estimates of particle dispersion and water velocity and estimates determined from published theory, suggesting that the advective‐dispersive transport of particulate matter within complex wetland environments can be approximated on the basis of measurable properties of the flow and aquatic vegetation.